NEW ZEALAND OFFICIAL YEARBOOK 1969

GEOGRAPHICAL POSITION—The islands of New Zealand have been shaped from the projecting crests of earth folds which rise as broad ridges from the floor of the South Pacific Ocean, 1,000 miles east of the continent of Australia. There are three main islands—North, South, and Stewart separated only by relatively narrow straits—with adjacent islets and a small group called Chatham Islands, 530 statute miles to the east of Lyttelton. Dating from 1842 the administrative boundaries of New Zealand, exclusive of island territories, extend from 33 degrees to 53 degrees south latitude and from 162 degrees east longitude to 173 degrees west longitude. Inhabited outlying minor islands are Raoul Island in the Kermadec Group, 620 statute miles north-east of the Bay of Islands, and Campbell Island, 370 statute miles south of Stewart Island.

New Zealand is also responsible for the administration of two island groups in the southwest Pacific—Niue Island and the Tokelau Islands. These are incorporated within the boundaries of New Zealand. Niue Island is 1,540 statute miles north-east of Auckland, while the Tokelau Islands are 704 statute miles further north. The territorial area reaches to within 8 degrees of the Equator.

The Ross Dependency, some 1,500 statute miles to the south, has been under New Zealand's jurisdiction since 1923 and comprises the sector of the Antarctic continent between 160 degrees east and 150 degrees west longitude, together with the islands lying between those degrees of longitude and south of latitude 60 degrees south.

The administrative area of New Zealand can be classified as follows. In this Yearbook, in general, New Zealand refers to the group of islands shown in (a) only.

Western Samoa became an independent territory from 1 January 1962. The 16 Cook Islands achieved a status of self-government in free association with New Zealand on 4 August 1965; more detail is given in Section 38 of this Yearbook.

GEOGRAPHICAL FEATURES: Coastline—Since the combined length of the North and South Islands extends just over a thousand miles, and since the width of neither Island exceeds 280 miles at its broadest point, New Zealand possesses a very lengthy coastline in proportion to its area. With the exception of the low-lying North Auckland Peninsula, the New Zealand land mass lies along a south-westerly and north-easterly axis, parallel to the direction of its mountain chains.

By reason of the latter fact the coastline is, on the whole, not greatly indented; and, as a consequence, New Zealand is not well endowed with natural harbours. In the North Island, Auckland and Wellington are two safe natural harbours of which the fullest commercial use is made and the use of Tauranga harbour is expanding. On the east coast of the North Auckland Peninsula several deep and sheltered harbours exist, but production from the hinterland is limited. In the South Island the Marlborough Sounds and the West Coast Sounds form perfect land-locked harbours, but owing to their situations and to the rugged nature of the terrain they have—with the exception of Queen Charlotte Sound—little or no commercial utility. Where vital localities have not been endowed with ideal harbours it has been necessary to improve existing facilities by dredging and by breakwater construction, etc. In this manner efficient ports, capable of accommodating overseas vessels, have been formed in Lyttelton, Otago, and Bluff Harbours. On the west coast of both Islands the strong ocean drifts and high seas cause shoaling at river mouths and harbour entrances, while on the east coast of the South Island similar circumstances prevail, due to the large quantities of shingle brought down by the rivers being spread along this coast by ocean currents. The mountainous nature of the country makes the haulage of goods to and from the better equipped natural harbours both costly and difficult, and the construction and maintenance of further ports at various points along the coasts of both Islands has been necessary, either by dredging river mouths or by harbour-construction work.

Mountains—The mountainous nature of New Zealand is one of its most striking physical characteristics, less than one-quarter of the land surface lying below the 650 ft contour. In the North Island the higher mountains occupy approximately one-tenth of the surface; but, with the exception of the four volcanic peaks of Egmont (8,260 ft), Ruapehu (9,175 ft), Ngauruhoe (7,515 ft), and Tongariro (6,458 ft), they do not exceed an altitude of 6,000 ft. Of these four volcanoes only the first named can be classed as dormant. Ruapehu and Ngauruhoe have been particularly active from time to time. Other volcanoes include Mount Tarawera and White Island, each of which has, upon one occasion within historical times, erupted with disastrous consequences. Closely connected with the volcanic system are the multitudinous hot springs and geysers.

The mountain system of the North Island runs generally in a south-west direction, parallel to the coast, from East Cape to Turakirae Head, and includes the following ranges from the north: Raukumara, Huiarau, Ruahine, Tararua, and Rimutaka. This chain is flanked on the west between the Huiarau and Ruahine by the Ahimanawa, Kaweka, and Kaimanawa Ranges, while west of the Kaimanawa is the National Park volcanic group comprising Mounts Ruapehu, Ngauruhoe, and Tongariro. The Hauhangaroa and Rangitoto Ranges run in a northerly direction from the National Park group. In the east the Moehau Range parallels the length of the Coromandel Peninsula. Mount Egmont forms the only area above 4,000 ft on the west coast of this Island.

The South Island is much more mountainous than the North, but shows fewer manifestations of recent volcanic activity. Along almost the entire length of the Island runs the massive chain known as the Southern Alps, which attains its greatest height in Mount Cook (12,349 ft), while no fewer than 16 peaks exceed 10,000 ft. West and north-west of the main portion of the Southern Alps are the Victoria, Brunner, and Lyell Ranges and the Tasman Mountains, the Victoria Range being flanked by the Paparoa Range. To the north run the St. Arnaud and Richmond Ranges, while to the north-cast are the Spenser Mountains and the Kaikoura and Seaward Kaikoura Ranges, the two latter ranges running parallel to the east coast. The south portion of the Southern Alps breaks up into a miscellany of ranges dominating the mountainous Fiord and north-western Southland regions.

As might be expected, the higher mountains of the South Island have exerted a greater influence on the economic development of the country than those of the North Island. For many years the Southern Alps were an effective barrier to communication by land between the east and west coasts, while their climatic effects on the Canterbury plains and Otago plateaus determined the types of cultivation undertaken. Moreover, the existence of much elevated open country led to the development of pastoral holdings on a large scale. While the mountains in the North Island are not as high nor as extensive as those of the South Island, in the early days they effectively isolated various portions of the coastal plains and valleys. Their effect on climatic conditions, however, is considerably less, the rainfall being more evenly distributed. Owing to this more even distribution of the rainfall, and to the existence of considerable areas of lower relief, the foothills of the mountain systems were heavily wooded, and so proved a hindrance to agrarian development.

There are at least 223 named peaks of 7,500 ft or more in altitude. Below is a list of the peaks restricted to the four largest volcanic cones in the North Island and to mountains of a minimum height of 9,000 ft in the South Island.

Glaciers—In keeping with the dimensions of the mountain system, New Zealand possesses, in the South Island, a glacial system of some magnitude. Of the glaciers the largest is the Tasman, which, with others of comparable size, rises in the more elevated area surrounding Mount Cook. Flowing down the eastern slope of the range, the Tasman Glacier has a length of 18 miles and a width of 11/4 miles. In common with other glaciers on the eastern slope, of which the more important are the Murchison (11 miles), the Mueller (8 miles), the Godley(8 miles), and the Hooker (71/4 miles), its rate of flow is slow, while its terminal face is at an altitude of somewhat over 2,000 ft. On the western slope of the range, owing to the greater snow precipitation, the glaciers are more numerous and descend to lower levels, while the steeper slope gives them a more rapid rate of flow. The two largest of these are the Fox and the Franz Josef, with lengths of 93/4 miles and 81/2 miles respectively, and terminal faces at altitudes of 670 ft and 690 ft.

As will be realised, these glaciers are an important tourist attraction, and as such have definite economic significance. Moreover, those glaciers on the eastern slopes which feed rivers utilised for irrigation and hydro-electric purposes are valuable in that they help to ensure a steady volume of water throughout the year.

Rivers—Of the numerous New Zealand rivers few are of sufficient length or volume to be navigable. Moreover, owing to the high relief of the country, they are mostly swift-flowing, while, as mentioned previously, nearly all are obstructed at their mouths by bars. For the purpose of internal communication, therefore, they are of little economic utility, and only in two or three isolated instances have they been thus consistently used. With improved roading conditions, however, their traffic has become negligible even in these cases.

As sources of hydro-electric power New Zealand rivers are of considerable importance, since their rapid rate of flow and dependable volume of ice-free water make them eminently suitable for this purpose. At the present time the Waikato and the Mangahao in the North Island and the Waitaki, Cobb, Clutha, and Waipori in the South are used for major hydro-electric schemes. The characteristics just mentioned are also important for purposes of irrigation, but, owing to the country's reliable rainfall, there are few areas other than in Canterbury and Otago where the rivers are so utilised.

Following is a list of the more important rivers. For purposes of uniformity, the length of a river is taken to be the distance from the mouth to the farthest point in the system, whether this should happen to bear the same name or that of an affluent, and is inclusive of the estimated course of a river flowing into and emerging from any lake in the system.

Cook Strait is defined as follows: northern limit is a line between northern points of Stephens Island and Kapiti Island: southern limit is a line between Cape Palliser and Cape Campbell.

The discovery in 1861 that the beds of numerous rivers in the South Island contained extensive deposits of alluvial gold was of considerable importance in the economic development of the country. Not only did it lead to an increase in population and in wealth, but, through the following of the numerous streams to their sources, it also led to the rapid exploration of large tracts of remote country. The exploitation of these deposits has been carried on with varying degrees of success up to the present time by both manual and mechanical means, but the amount of gold now extracted is comparatively small.

A further factor in connection with the rivers is that, owing to the very successful acclimatisation of freshwater fish, notably trout, many of them now provide exceptionally fine fishing.

Lakes—In considering New Zealand's numerous lakes a distinction can be made, especially from the scenic viewpoint, between the lakes of the two Islands. Surrounded by extremely rugged country the larger lakes of the South Island are distinguished by the grandeur of their alpine settings, while those of the North Island, situated on a volcanic plateau, are of interest by reason of the neighbouring thermal activity. Owing to the excellence of their fishing, the North Island lakes possess an added tourist attraction. In both Islands the larger lakes are situated at high altitudes, and their consequent remoteness renders them unsuitable as a means of communication. In their functions as reservoirs the lakes of both Islands are of vital importance for the maintenance of the streams draining them and as a means of flood prevention. More especially is this the case where hydro-electric schemes are involved, Lakes Waikaremoana and Taupo in the North Island, and Lakes Coleridge, Pukaki, Tekapo, Wanaka, Hawea, and Wakatipu in the South Island, being of particular significance in this respect. A series of narrow man-made lakes have been produced in connection with hydro-electric development along some of the rivers. Early in 1965 Lake Benmore, New Zealand's largest artificial lake, was created. This lies on the Waitaki River in North Otago and is the first in a series of lakes to be created along this river in connection with the production of hydro electricity. The lake covers 301 square miles in area and consists of two arms, the main arm being 181/2 miles in length and the Ahuriri Arm 1111/2 miles in length.

Some particulars of the more important lakes are given in the following table.

GEOLOGY—The islands of New Zealand are part of the unstable circum-Pacific Mobile Belt; this is a region where volcanoes are active and where the earth's crust has long been buckling and breaking at a geologically rapid rate. The interplay, in the past, of earth movements and erosion has made the sedimentary rocks that cover almost three-quarters of New Zealand. Land areas that the earth movements have raised have been attacked by erosion, and the sand, mud, shingle, and other debris thus formed has been carried away to the sea, where it has accumulated in great thicknesses to form rocks such as sandstone, mudstone, greywacke, and conglomerate; the shells and other skeletons of sea creatures have accumulated to form thick layers of limestone. Many of the sedimentary rocks are in distinct layers called strata; earth movements have later raised them above the sea to form land, and the strata are in many places tilted and folded by pressure. Seas have advanced and retreated over New Zealand many times, and these sedimentary rocks represent almost every geological period since the Cambrian (see Time Scale); their age is revealed by the shells, foraminifera, and other fossils that they contain.

As well as sedimentary rocks, and volcanic rocks of various ages, New Zealand incorporates in its complex structure schist, gneiss, marble and other metamorphic rocks, and granite, diorite, gabbro, serpentine, and other intrusive igneous rocks. Most of these metamorphic and intrusive rocks are hundreds of millions of years old—they were formed at depth in the earth's crust early in New Zealand's history, in the “roots” of ancient mountain ranges, long ago destroyed, and are visible at the land surface today only because erosion has removed thousands of feet thickness of other rocks that once covered them. The metamorphic rocks developed when huge, elongated sea basins (geosynclines) were formed, in which tens of thousands of feet thickness of sediments accumulated; when these geosynclines were slowly compressed during major mountain-building episodes the deeper sediments were subjected to great pressure and shearing stress, which caused new minerals and structures to develop, changing the sediments into metamorphic rocks. The granites and other intrusive rocks are coarsely crystalline, and are usually considered to have been intruded into the outer crust in molten state during mountain building; some, however, may be the products of intense metamorphism of sediments.

GEOLOGICAL TIME SCALE

Geological History—Evidence of the earliest-known events in New Zealand's history is given by ancient rocks in Nelson, Westland, and Fiordland that were formed in the early Paleozoic era, perhaps as long as 600 million years ago (some in Westland may be older). They include thick, geosynclinal sedimentary rocks; this suggests that a large land mass existed at that time to yield the great volume of sediments, but little has been deduced about its shape or position.

The history of the later part of the Paleozoic era, and the Mesozoic era, is rather better understood; for a vast span of time from the Carboniferous period—probably until the early Cretaceous period—an extensive geosyncline occupied the New Zealand region. At first, during much of late Paleozoic time, huge quantities of submarine lava and volcanic tuff were included in the materials that accumulated in the geosyncline, but in the later Permian and Mesozoic times the sediments were mainly sand and mud, derived probably from some land west of present New Zealand; they were compacted into hard greywacke (a type of sandstone) and argillite (hard, dark mudstone).

In the early Cretaceous period one of the main mountain-building episodes in New Zealand's history took place: although geosynclinal sedimentation continued through the Cretaceous period in eastern New Zealand, the geosyncline elsewhere was compressed, and the sediments were intensely crumpled and broken and raised above the sea, probably forming a large, mountainous landmass. Some of the geosynclinal deposits, now exposed over much of Otago, alpine Westland, and parts of Marlborough Sounds, were metamorphosed into schist and gneiss by the tremendous deforming pressures to which the geosyncline was subjected.

The time that has elapsed since the intense folding of the strata in the New Zealand Geosyncline in the mid-Cretaceous period may be considered as the later geological history of this country; it embraces roughly 100 million years.

During the early part of this late history, erosion slowly wore down the mountains that had risen, producing a land of low relief. Over these worn-down stumps of the Mesozoic mountains the sea gradually advanced, beginning its transgression earlier in some areas than in others: in the early Cretaceous period it began to submerge land in the region of present North Auckland and the eastern margins of the North and South Islands, and thick deposits of mudstone and sandstone accumulated in some parts of these areas. At the close of the Mesozoic era, and in the very early Tertiary, land became so reduced in size and relief that little sediment was formed, and only comparatively thin deposits of fine bentonitic and sulphurous muds, and fine, white, foraminiferal limestone accumulated. In some areas New Zealand's main coal deposits accumulated, in swamps on the surface of the old land; these became buried by marine deposits as the sea continued its transgression in the Eocene period.

By the Oligocene period, most of the land was submerged, and in shallow waters free of land sediments thick deposits of shell and foraminiferal limestone accumulated. (Scattered, remnant patches of this Oligocene limestone furnish most of New Zealand's cement and agricultural lime.)

After the Oligocene submergence earth movements became more vigorous; many ridges rose from the sea as islands, and sank or were worn down again; sea basins formed and rapidly filled with sediments. New Zealand's late Tertiary environment has been described as follows: “The pattern of folds, welts and troughs that developed was on a finer scale than in the Mesozoic . . . the land moved up and down as a series of narrow, short, interfingering or branching folds. . . we can think of Tertiary New Zealand as an archipelago. . a kind of writhing of part of the mobile Pacific margins seems to have gone on . . .^*“ The thick deposits of soft, grey mudstone and sandstone that now make up large areas of the North Island, and some parts of South Island, are the deposits that accumulated rapidly in the many sea basins, large and small, that developed in the later Tertiary.

Very late in the Cenozoic era—in the Pliocene and Pleistocene periods—one of the greatest episodes of mountain building in New Zealand's history took place. Earth movements became intense, and slowly pushed up the Southern Alps and other main mountain chains, and determined the general shape and size of the present islands of New Zealand. Much of the movement during this mountain building period (the Kaikoura Orogeny) took the form of displacement of blocks of the earth's crust along fractures called faults. The total movements of the earth blocks adjacent to major faults amounted to thousands of feet; it must have been achieved very slowly, probably by innumerable small movements, each of a few inches or feet. The blocks adjacent to “transcurrent” faults moved not only vertically but also laterally along the faults. The New Zealand landscape today in some regions shows well preserved tilted fault blocks bounded by fault-scarps—steep faces hundreds or even thousands of feet high. Fault movements continue to the present day, and have accompanied several major earthquakes of the past century. Many minor but revealing landscape features such as scarplets, fault ponds, and shutter ridges show where movement has been occurring in recent centuries.

*“New Zealand Biogeography” by Charles A. Fleming. Tuatara Vol. 10, No. 2, June 1962, pp. 53—108.

Erosion during this time has eaten into the major landscape forms that the earth movements have built, carving the detailed landscape pattern of peaks, ridges, valleys, and gorges, and has built up alluvial plains, shingle fans, and other constructional forms; at the coast, waves have driven back the headlands, and built beaches, spits, and bars. The Pleistocene period was the time of the Ice Age, and in the high mountains of the South Island glaciers carved deep valleys and carried huge loads of rock, dumping them as moraines. The late Pleistocene glaciers carved the fiords of Fiordland and the basins occupied by most South Island lakes; there were small glaciers also on Ruapehu, where remnants survive, and on Mount Egmont and the Tararua Range.

Volcanic activity of the past few million years has played an important part in making the rocks and shaping the landscape of parts of the central and northern North Island; Banks Peninsula, a twin volcanic dome in Canterbury, achieved much of its growth then, too. The largest volcanic outpourings of late geological times in New Zealand have been in the region between Tongariro National Park and the Bay of Plenty Coast: andesite lava, scoria, and ash were erupted in the Pleistocene period and later to build the huge volcanoes, Ruapehu, Tongariro, and Ngauruhoe; more than 2,000 cubic miles of molten rhyolitic magma was erupted in the form of ignimbrite, pumice, and rhyolite lava, building up the Volcanic Plateau.

The Geological Survey, Department of Scientific and Industrial Research, has built up this body of geological knowledge.

Geological Maps—The geological maps show the present distribution of major rock groups in New Zealand, brought about by the events and processes that have been summarised in previous paragraphs. (These maps were originally prepared for the New Zealand Encyclopaedia.)

Older Rocks—Much of the late Cretaceous and Tertiary sedimentary rock that once must have covered a large part of the South Island has been worn off by erosion since the Kaikoura Orogeny, and the “undermass” of old rocks has been exposed.

The oldest of these rocks lie to the west: Fiordland is made up mainly of metamorphic diorite, granite, and coarse schist, gneiss, and marble, with Ordovician graptolite-bearing slates in its south-west extremity; greywackes and argillites of possibly pre-Cambrian age occur in Westland and south-west Nelson, and further north in Nelson there are large areas of complexly folded Cambrian and Ordovician sedimentary and metamorphic rocks. Large granitic masses, hundreds of square miles in area, occur in Westland, Nelson, and Stewart Island.

These ancient rocks terminate with an abrupt boundary (which shows clearly even on this small-scale map) extending from Milford Sound along the western margin of the Southern Alps. This boundary is the Alpine Fault, a great fracture that divides the South Island into two areas of dissimilar geological structure: to the west of it, and in Fiordland, are the granites and other ancient rocks just described; to the east, the undermass rocks are predominantly the sedimentary and marine volcanic rocks of the New Zealand Geosyncline, and their metamorphosed forms, of later Paleozoic and Mesozoic age. From Marlborough, through Canterbury to North Otago, the map shows an almost continuous expanse of these rocks; here they are mainly sparsely fossiliferous greywackes and argillite strata of Triassic and Jurassic age. On the western flanks of the Southern Alps, and in Otago, these sedimentary rocks merge gradually with schist and gneiss. Those of the Southern Alps show on the map as a very narrow belt, cut off by the Alpine Fault, but the southern schists form a belt some 60 miles wide extending for about 150 miles across Otago. To the south, also, this schist mass merges gradually with sedimentary rocks of the New Zealand Geosyncline, here of Permian age: these strata, mainly tuffs and tuffaceous greywackes forming a belt that stretches across Southland the northern limb of a major downfold or syncline; Triassic and Jurassic strata occupy its core, making up much hill country of Southland. The southern limb rocks include much marine volcanic rock, and in the core of the syncline in western Southland a belt of dunite and serpentine is intruded and is well exposed in the Olivine and Red Hill ranges.

A sequence of rocks very like that of Southland is found also in eastern Nelson; here, fossiliferous Triassic rocks and Permian sedimentary and volcanic rocks closely resembling those of Southland are found, and a belt of dunite and serpentine (the Nelson “mineral belt”) intrudes them. It has been suggested that the Nelson and Southland rocks, which terminate abruptly at the Alpine Fault and its continuation as the Wairau Fault, were originally joined, and have been displaced some 300 miles by lateral movement at the fault.

Younger Rocks—On the eastern side of the South Island, upper Cretaceous and Tertiary strata survive only as small patches, the remnants of a once fairly complete cover of younger rocks. Thick geosynclinal Cretaceous strata are found in the Clarence and Awatere Valleys of Marlborough, but elsewhere in the eastern South Island the upper Cretaceous and lower Tertiary strata are thin. They include foraminiferal limestone, greensands, sandstones, and other shell deposits formed during slow transgression by the sea. Oligocene limestone remnants mark the period of maximum transgression.

On the western side of the South Island the younger rocks are more widespread, and include some thick sequences that were formed in rapidly sinking basins. The oldest are the coal measures, mainly Eocene in age. They are overlain in some areas by thick lower Tertiary marine strata. In Southland, thick Tertiary strata occupy the Waiau Syncline, between Lake Te Anau and Foveaux Strait.

The map shows some large areas of Pleistocene to Recent terrestrial deposits in the South Island. The largest forms the Canterbury Plains, and consists of old shingle deposits of unknown thickness washed from the Southern Alps during the Pleistocene glaciation. Others occupy the Moutere depression of Nelson, and form Southland Plains, and intermontane basins, such as the McKenzie Plains, in the main mountain chains. Thick Pleistocene moraines form the main surface rocks of South Westland.

Banks Peninsula is the only large mass of young volcanic rocks in the South Island; there are smaller areas at Timaru,oamaru, and in the Dunedin district.

Older Rocks—Unlike the South Island, the North Island has no large expanses of granite or of metamorphic rocks: the undermass rocks are almost wholly complexly folded and faulted greywackes and argillites of the New Zealand Geosyncline, predominantly Mesozoic in age.

The largest expanse of these hard rocks forms the main mountain backbone of the North Island, extending from Cook Strait to the East Cape area. Smaller areas of them are exposed between north Taranaki and Auckland; they include the richly fossiliferous strata of the Kawhia Syncline, a major downfold of the undermass rocks.

In North Auckland, deeply weathered undermass rocks, in part of Permian age, form low hill country in the east, particularly between Whangaroa and Whangarei harbours.

Younger Rocks—Over most of the North Island the older rocks are hidden by Cretaceous, Tertiary and Quaternary sedimentary rocks and by young volcanic rocks. In some areas the younger sedimentary rocks are thin and patchy; in others they are many thousands of feet thick over hundreds of square miles. The bulk of them are poorly consolidated sandstones, and grey mudstones to which the colloquial name “papa rock” is often applied.

The main areas with thick sequences of these young strata are the Taranaki - Wanganui - Rangitikei district, and the region east of the main ranges, including most of the Gisborne, Hawke's Bay, and Wairarapa districts. In both areas intensive oil prospecting of recent years has greatly added to knowledge of the structure.

In the Taranaki - Wanganui - Rangitikei district the strata dip gently south, so that increasingly young rocks are exposed in this direction, the lower Tertiary being seen only in the north. However, recent oil bores drilled to depths of about 13,000 ft at Kapuni in Taranaki, passed through a full sequence of strata from Pleistocene through all Tertiary stages, finally reaching Eocene coal measures.

In the eastern North Island the structure of the younger rocks is much more complex than in the western area. Upper Cretaceous strata are followed by Tertiary in many sedimentary basins large and small, with many unconformities. The southern part of the region is broken by many transcurrent faults, and hard lower Cretaceous greywacke piercement bodies project from the younger rocks.

Younger rocks of South Auckland do not form such large basins as those just described. The oldest of these strata are the Eocene coal measures of the Waikato region. Upper Cretaceous strata, mainly mudstones, are the most widespread of the younger rocks of North Auckland.

Young volcanic rocks are widespread in the North Island. The largest area of them is the Central Volcanic District: north of the three great andesite volcanoes, Ruapehu, Ngauruhoe, and Tongariro, lies the “volcanic plateau”, an expanse of some 10,000 square miles made up of several thousand cubic miles of ignimbrite, rhyolite lava, and pumice. This is one of the largest and youngest accumulations of acid volcanic rocks in the world. Most of it has been erupted in late Pliocene and Pleistocene times. The belt of most recent activity in the Central Volcanic District is known as the Taupo Volcanic Zone; it contains all this country's active volcanoes, many inactive ones, and all the geysers and boiling springs.

Mount Egmont is a huge, conical, andesite volcano, with the remnants of two other volcanic cones nearby; all are of Pleistocene age. In the Waikato there are eroded Pleistocene cones of approximately basic andesite composition; the largest is Pirongia, some 3,000 ft high. Auckland city and the area immediately to the south has been the scene of many eruptions of basalt lava and scoria in late Pleistocene and Holocene times; many small scoria cones are seen at Auckland city. Late Tertiary and Quaternary basaltic eruptions in North Auckland have built lava plateaus and many young scoria cones.

A Descriptive Atlas of New Zealand contains geological maps of New Zealand and summaries of New Zealand's geology and landscape development. New Zealand Geological Survey Bulletin 66, The Geological Map of New Zealand, 1:2,000,000, is a lengthier summary with a more detailed geological map and cross sections.

G.C.S.

EARTHQUAKES: Geophysical Background—Earthquakes are geographically associated with active volcanoes and with major earth movements such as mountain building; these three types of disturbance are confined, for the most part, to certain limited regions of the world. Such disturbed regions, of which New Zealand is one, are evidently the site of some kind of development affecting the outer shell of the Earth. Little is yet known about the internal processes that give rise to these geophysical disturbances, nor are the relations connecting them understood in any detail.

Formerly earthquakes were believed to be caused by volcanic activity, but it is now recognised that volcanic earthquakes are restricted to small shocks in the immediate vicinity of the volcanism. In New Zealand, tremors of this kind are experienced in the zone of active volcanism that extends from Mount Ruapehu to White Island.

In some places geological faulting at the surface gives visible evidence that a major earth movement has occurred. Occasionally movement on a fault has been observed to occur simultaneously with an earthquake in the same vicinity. New Zealand provided one of the earliest examples of this to become generally known, when movement took place on the Wairarapa Fault at the time of the great Wellington earthquake of 1855. Such events as this have led to the idea that earthquakes in general are caused by fault movements, but it has proved difficult to find convincing evidence in support of this theory. It is noteworthy that there seems to be little earthquake activity along much of the Alpine Fault, which has been traced for 300 miles from Milford Sound to Lake Rotoiti and is classed by geologists as one of the largest and most active faults in the world. The nature of the connection between earthquakes and faulting is still somewhat obscure.

The great majority of the world's earthquakes occur at depths of less than 40 miles, and in many earthquake zones there are no shocks at any greater depth. A moderate number of New Zealand earthquakes are classed as intermediate in depth, i.e., originating at between 40 miles and 190 miles deep. The two deepest New Zealand earthquakes recorded so far occurred four and a half minutes apart on 23 March 1960, with a common focus 370 miles deep under north Taranaki; this is about 80 miles shallower than the deepest earthquake known.

It is difficult to compare the degree of earthquake activity in New Zealand with that in other regions because of the many differences that arise in earthquake type and mode of occurrence. New Zealand and California are often regarded as roughly similar, with an activity very much less than, for example, Japan or Chile.

Regional Distribution—There are two separate regions of earthquake activity in New Zealand. The larger, northern region may be roughly defined as lying between latitude 361/2°S and 431/2°S. It thus includes the northern half of the South Island, and all the North Island apart from the North Auckland peninsula; but the area from Kaipara Harbour to the lower Waikato River should be excluded. The southern active region lies to the west of longitude 1691/2°E, and incorporates Southland, western Otago, and southern Westland. Earthquakes have only occasionally been located in the parts of New Zealand lying outside these two regions.

Within the active regions the occurrence of shallow earthquakes is widely scattered. There has been a tendency, however, for the larger shallow earthquakes to lie towards the Pacific side of the northern active region and towards the Tasman side of the southern active region. Earthquakes with deeper foci are mostly confined to a narrow belt in the northern region, extending from the Bay of Plenty south-westwards to Tasman Bay.

The historical record is too brief to support a quantitative assessment of the frequency with which one might expect earthquakes to be felt at a given intensity in various parts of New Zealand. Considering the distances to which major earthquakes can be effective, in relation to the size of New Zealand, it would be imprudent to regard any part of the country as permanently exempt from the possibility of earthquake damage.

Outside the active regions there are many areas, however, where no damaging intensity has actually been experienced in historical times. Moreover, since the major shallow earthquakes on record have been rather widely distributed within the active regions, there appears to be no particular area of markedly intense seismicity.

The Hawke's Bay earthquake of 3 February 1931 resulted directly or indirectly in 255 deaths. The total of deaths that have been recorded as due to other earthquakes since 1848 is 32, of which three resulted from the Inangahua earthquake of 1968.

Seismological Observatory—Earthquake recorders are operated continuously at the following stations by the Seismological Observatory, Wellington: Apia and Afiamalu (Western Samoa); Suva (Fiji); Rarotonga (Cook Islands); Raoul Island (Kermadecs); Cape Reinga, Onerahi, Auckland, East Cape, Karapiro, Wairakei, Gisborne, Tuai, Tarata, Chateau, Castlepoint, Mangahao, and Wellington (North Island); Cobb, Kaimata, Gebbies Pass, Mount John, Milford Sound, Roxburgh, Monowai, and Waipapa Point (South Island); Chatham Islands; Campbell Island; and Scott Base (Antarctica). The Naval Research Laboratory, Auckland, operates a station on Great Barrier Island, the records from which are analysed at the Seismological Observatory. The installations at the following stations include instruments for recording distant earthquakes: Afiamalu, Rarotonga, Wellington, Roxburgh, Scott Base. At the Pacific and Antarctic stations preliminary readings are made locally and notified by radiogram. The analysis of records from all stations is carried out at the Observatory in Wellington.

The Observatory publishes regular reports of all significant earthquakes occurring in the New Zealand region; in a normal year there are about 400 such earthquakes, and about 100 of these are reported felt. The analysis involves using observations from stations in other countries as well as those from the local network, and the Observatory likewise contributes data to the international seismological agencies about distant earthquakes as well as large local ones. Details of tremors felt in New Zealand are supplied to the public and the press. In the study of felt earthquakes the instrumental results are augmented by “felt reports”; these are supplied by a large number of voluntary observers throughout New Zealand in response to a standard questionnaire issued by the Observatory.

Earthquake data are used by the Observatory for studying the fundamental characteristics of the Earth's crust in New Zealand, Antarctica, and the neighbouring oceanic regions, and also for contributing to geophysical knowledge of the Earth's deep interior.

Earthquakes in 1968—There was more activity in the New Zealand region in 1968 than for some years. Besides the major Inangahua earthquake and its aftershocks, a large shallow earthquake occurred to the south of the Fiordland coast, and both Christchurch and Wellington experienced moderately-sized earthquakes centred close to these cities.

The Inangahua earthquake originated in rough hill country about 10 miles to the north of Inangahua, in Westland, at 5.24 a.m. on 24 May 1968. It had a magnitude of 7.0 (Richter Scale) and was the largest New Zealand earthquake since that off the Fiordland coast in May 1960, which also had a magnitude of 7.

The earthquake resulted in three deaths and injuries to 14 people. There were major landslides in the gorge of the Buller River, with extensive slumping and fissuring in the epicentral area. At Inangahua houses were destroyed, bridges were damaged and railway lines were distorted, indicating an intensity of X on the Modified-Mercalli Scale. Other centres badly affected were Reefton, Westport, and Greymouth, where intensities ranged from MM VI on better ground to perhaps MM X on poorly consolidated sand and alluvium. At these places, many chimneys were destroyed, and some damage was done to buildings. The earthquake was felt over the entire country, with the exception of northeasterly parts of the North Island, and south-eastern Otago.

At Inangahua, an existing fault scarp was rejuvenated with maximum movement of about 15 in., and 6 miles to the south, near Rotokohu, other displacements have been interpreted as traces of bedding faults in the underlying sediment.

The main Inangahua earthquake was followed by numerous after-shocks, mostly in an elliptical area about 25 to 15 miles, extending to the south-south-east from the main shock. The largest aftershock took place at 8.58 a.m. on 25 May, and had a magnitude of 5.9.

Several other earthquakes of note occurred during the year besides those of the Inangahua sequence. The largest of these had a magnitude of 6.4 and originated about 20 miles to the south of Puysegur Point on 25 September. It was felt extensively in Southland and Otago, and caused minor damage at Otautau. Another shock in the Fiordland region, of magnitude 5.9, occurred on 2 April.

Several shocks of lesser magnitude attracted attention by occurring close to centres of population, where they caused minor damage. One of these, of magnitude 5, originated within a few miles of Christchurch on 24 January. Its effects were strongest in Christchurch, and extended over much of North Canterbury. An earthquake of magnitude 51/4 occurred near Turangi on 30 January, and caused some minor damage to buildings there. On 1 November a shock of magnitude 51/2, which was centred about 20 miles to the south-east of Wellington, caused extensive minor damage and, with the possible exception of the Seddon earthquake of April 1966, was felt more strongly than any other shock in this city since the Wairarapa earthquakes of 1942.

There was no exceptional deep earthquake activity during 1968, but shocks that occurred at depths of about 140 miles beneath the centre of the North Island on 5 May (magnitude 5.9) and 2 November (magnitude 6.3) were felt in Wanganui, Hawke's Bay, and as far south as Wellington.

Large earthquakes in the region surrounding New Zealand include one of magnitude 61/2, which occurred about 100 miles to the north-east of East Cape on 10 March, and two that originated near the Kermadec Islands, about 600 miles north of New Zealand. These shocks occurred on 25 July (magnitude 73/4) and 27 September (magnitude 71/4) and were felt on Raoul Island.

WEATHER INFORMATION—The collection of weather information and the provision of weather forecasts and climatic data for diverse interests in aviation, shipping, agriculture, Government Departments, and the general public are functions of the New Zealand Meteorological Service. By arrangement with the administrations concerned the Service performs similar functions for British territories in the Pacific.

Weather reports for use in forecasting are made at about 140 places within New Zealand and 40 in Pacific islands and collected by telegraph and radio, along with measurements of winds at upper levels made at nine radio wind stations and of temperatures made at eight radiosonde stations. Daily observations are made for climatological purposes at about 230 places in New Zealand and 80 in the islands. Rainfall measurements are made at a total of about 1,500 places within New Zealand and 260 outside the country.

Detailed climatological statistics are published annually by the New Zealand Meteorological Service in the Meteorological Observations and in the Fiji Annual Meteorological Summary. Current statistics appear monthly in the New Zealand Gazette and in the Fiji Gazette.

CLIMATE—Situated between 34°S and 47°S the main islands lie within the broad belt of strong westerly winds which encircles the hemisphere south of about latitude 35°S. Just to the north is the high-pressure ridge of the subtropics from which barometric pressure decreases southwards over New Zealand to the deep low-pressure trough located near latitude 60°S.

In the Australasian region there is no semipermanent anticyclone, as exists in subtropical latitudes in the Indian and eastern Pacific Oceans. Instead, a continual eastward migration of anticyclones takes place, roughly at weekly intervals. Most of the centres pass over or to the north of the North Island. The low-pressure troughs which separate successive anticyclones are associated with deep depressions centred far to the south. A period of disturbed weather accompanies the trough with a change to cold southerly or south-westerly winds as it advances north-eastwards over New Zealand. Conditions improve again with the approach of the next anticyclone from the west. While this simple progression dominates the day-to-day weather, the situation frequently becomes much more complex. The troughs are unstable systems where depressions commonly form, some of which develop into vigorous storms that travel south-eastwards across New Zealand.

The anticyclones themselves continually vary in size, intensity, and rate of movement. Their tracks are furthest north in the spring, on the average, and reach their southern limit in late summer or early autumn when most of the centres cross central New Zealand. At this time of the year, too, northern and eastern districts of the North Island occasionally come under the influence of deep cyclones of tropical origin.

The other main factors which influence the climate of New Zealand are, first, its position in the midst of a vast ocean, and second, the shape and topography of the country itself.

Australia, the nearest continent, is 1,000 miles to the west; Antarctica is 1,400 miles to the south. Hot air masses from the interior of Australia in summer, or freezing air masses from the Antarctic, which occasionally reach New Zealand, retain little of their original character after their long ocean passage. Thus, there is an absence of extreme variations of temperature. On the other hand, since abundant supplies of moisture are supplied by evaporation from the oceans, and depressions are frequent and vigorous, the average precipitation is high.

The chain of high mountains, which extends from south-west to north-east through the length of the country, rises as a formidable barrier in the path of the prevailing westerly winds. The effect is to produce much sharper climatic contrasts from west to east than in the north-south direction. In some inland areas of the South Island just east of the mountains the climate is distinctly continental in character, despite the fact that no part of New Zealand is more than 80 miles from the sea.

Winds—Winds from a westerly quarter prevail in all seasons, with a general tendency to increase in strength from north to south. However, considerable local modifications to the general air flow occur during its passage across the mountainous terrain. Approaching the main ranges the flow from the west turns towards the north-east and on descending on the eastern side swings towards the south-east. This results in an increased number of south-westerlies in Westland and a predominance of north-westerlies in inland districts of Otago and Canterbury, where strong gales from this quarter occur at times in the late spring and summer. Daytime sea breezes usually extend from the coast inland for 20 miles or more during periods of settled weather in summer. On the Canterbury coast the wind comes most frequently from the north-east, partly because there is a persistent sea breeze from this quarter, but south of Dunedin south-westerlies predominate. Cook Strait, the only substantial gap in the main mountain chain, acts as a natural funnel for the air flow and is a particularly windy locality afflicted by gales from the south-east as well as the north-west. This “funnel” effect is also in evidence about Foveaux Strait. North of Taranaki the general air flow is more from the south-west, and there is a noticeable reduction in windiness in the summer.

An indication of the variation in the frequency of strong winds from summer to winter, and in different parts of the country, is given in the next table. These were all obtained by the use of Dines pressure-tube anemometers at well exposed sites.

NOTE—These are all aerodromes, with the exception of Auckland (Mechanics Bay) and Wellington (Kelburn).

Rainfall—The distribution of rainfall is mainly controlled by mountain features, and the highest rainfalls occur where the mountains are exposed to the direct sweep of the westerly and north-westerly winds. The mean annual rainfall (see map) ranges from as little as 13 in. in a small area of Central Otago to over 300 in. in the Southern Alps. The average for the whole country is high, but for the greater part it lies between 25 and 60 in., a range regarded as favourable for plant growth in the temperate zone. The only areas with under 25 in. are found in the South Island, to the east of the main ranges. These include most of Central and North Otago, and South Canterbury. In the North Island, the driest areas are central and southern Hawke's Bay, Wairarapa, and Manawatu where the average rainfall is 30-40 in. a year. Of the remainder, much valuable farm land, chiefly in northern Taranaki and Northland, has upwards of 60 in. Over a sizeable area of both Islands rainfall exceeds 100 in. a year but, with the exception of Westland, this is mountainous and unoccupied, much of it being forest covered.

For a large part of the country the rainfall is spread evenly through the year, although its effectiveness in summer is, of course, much reduced. The greatest contrast is found in the north, where winter has almost twice as much rain as summer. This predominance of winter rainfall diminishes southwards. It is still discernible over the northern part of the South Island but, over the southern half, winter is the season with least rainfall, and a definite summer maximum is found inland due to the effect of convectional showers. The rainfall is also influenced by seasonal variations in the strength of the westerly winds. Spring rainfall is increased in and west of the ranges as the westerlies rise to their maximum about October, while a complementary decrease occurs at the same time in the lee of the ranges.

Areas which are exposed to the west and south-west experience much showery weather, and rain falls on roughly half the days of the year. Over most of the North Island rain can be measured on at least 150 days a year except to the east of the ranges where there are, in places, fewer than 125 rain days. Those areas of the South Island with annual rainfall under 25 in. generally have about 100 rain days a year. In the far south the frequency of rain increases sharply; in Stewart Island and Fiordland rain days exceed 200 a year. Over most of the country between 55 and 65 percent of the rain days also qualify as wet days (0.10 in. or more). The percentage increases to over 70 in Westland, but in the low rainfall area of inland Otago there are only about 40 wet days a year compared with 100 rain days.

On the whole the seasonal rainfall does not vary greatly from year to year, the reliability in spring being particularly advantageous for agricultural purposes. It is least reliable in late summer and autumn when very dry conditions may develop east of the ranges, particularly in Hawke's Bay.

The highest daily rainfall on record is 22 in., which occurred at Milford Sound where the mean annual rainfall is 250 in. Other areas with considerably lower rainfall are also subject to very heavy daily falls; such areas are to be found in northern Hawke's Bay and in northeastern districts of the Auckland Province. By contrast, in the Manawatu district and in Otago and Southland daily falls reaching 3 in. are very rare.

NORMAL MONTHLY AND ANNUAL RAINFALL (INCHES) (1921-50)

Thunderstorms—Thunderstorms are not numerous. Their frequency is greatest in the north and west where thunder is heard on 15 to 20 days a year; east of the ranges (except in Gisborne) the figure is five or less.

Hail—Hail is most frequent in the south-west where it is reported on about 20 days a year, but for the greater part of the country it occurs on about five days a year or less. Most of the hailstones are small, but occasionally large stones cause local damage to glasshouses, and to orchards and market gardens, chiefly in Canterbury and Hawke's Bay.

Temperature—Mean temperatures at sea level decrease steadily southwards from 59°F in the far north to 54° about Cook Strait, then to 49° in the south. With increasing altitude, temperatures drop about 3° per 1,000 ft. January and February, with approximately the same mean temperature, are the warmest months of the year; July is the coldest. Some temperature statistics for selected places are included in the table on climatological averages. Highest temperatures are recorded east of the main ranges, where they rise to the nineties on a few afternoons in most summers, usually in association with a north-westerly Föhn wind. The extremes for New Zealand (measured in a standard thermometer screen) are 101° at Ashburton and —3° at Ophir (Central Otago).

As is to be expected, there is a small annual range of temperature (difference between mean temperature of the warmest and coldest months). In Northland and in western districts of both Islands the annual range is about 15°F. For the remainder of the North Island, and east coast districts of the South Island, it is 17°–19°. Further inland it exceeds 20° in places, reaching a maximum of 25° in Central Otago where there is an approach to a continental type of climate.

Frost—It is well known that local variations in frostiness are considerable, even within quite small areas. On a calm, clear night the cold air in contact with a sloping surface gravitates slowly downhill to collect in valleys and depressions, and it is these “Katabatic” drifts which are mainly responsible for local temperature variations at night. Gently sloping ground with a northerly aspect tends to be least affected by frost. Favourable sites in coastal areas of Northland are free of frost, although further inland light frosts occur frequently in the winter months. At Albert Park, Auckland, the screen minimum thermometer (4 ft above the ground) has registered below 32°F only once in nearly 50 years, yet across the harbour at Whenuapai Aerodrome there are eight screen frosts per annum on the average. Excluding the uninhabited mountainous areas, the most severe winter conditions are experienced in Central Otago and the Mackenzie Plains of inland Canterbury, and on the central plateau of the North Island. Even in these areas night temperatures as low as 10° are rarely recorded. Elsewhere over the North Island the winters are very mild and pastures maintain continuous growth. In both Islands sheep and cattle remain in the open all the year round.

Snow—The majority of New Zealanders rarely see snow except on the mountains. The North Island has a small permanent snow field above about 8,000 ft on the central plateau, but the snow line rarely descends below 2,000 ft even for brief periods in winter. In the South Island snow falls on a few days a year in eastern coastal districts and in some years may lie for a day or two even at sea level. In Westland it does not lie at sea level. The snow line on the Southern Alps is around 7,000 ft in summer, being slightly lower on the western side where the Franz Josef and Fox Glaciers descend through heavy bush to within 1,000 ft of sea level. In inland Canterbury and Otago, where there are considerable areas of grazing lands above 1,000 ft, snowfalls are heavier and more persistent and have caused serious losses of sheep during severe winters in the past. However, only rarely does the winter snow line there remain permanently below 3,000 ft.

Relative Humidity—Humidity is commonly between 70 and 80 percent in coastal areas and about 10 percent lower inland. It varies inversely to the temperature, falling to a minimum in the early afternoon when temperature is highest and frequently lying between 90 and 100percent during clear nights. As the following table shows, the diurnal variation is greater than the difference between summer and winter.

Very low humidities—between 20 and 30 percent or lower—occur at times in the lee of the Southern Alps where the Föhn effect is often very marked. In summer the hot, dry “Canterbury Norwester” is generally a most unpleasant wind. Cool south-westerlies are also at times very dry when they reach eastern districts. In Northland the humid mid-summer conditions are inclined to be rather oppressive though temperatures rarely reach 85°. Dull, humid spells are generally not prolonged anywhere, but their frequency shows a marked increase in the south.

Sunshine—The sunniest areas are to be found near Blenheim, Nelson, and Whakatane, where the average duration of bright sunshine exceeds 2,400 hours per annum. The rest of the Bay of Plenty and Napier are only slightly less sunny. A large portion of the country is favoured with at least 2,000 hours. Even Westland, despite its high rainfall, has 1,800 hours. Southland, where sunshine drops sharply to 1,700 hours per annum, lies on the northern fringe of a broad zone of increasing cloudiness. Four hundred miles further to the south at Campbell Island the sunshine has the extremely low value of 650 hours per annum. A pleasant feature of the New Zealand climate is the high proportion of sunshine during the winter months. To eliminate the effect of varying day-length the summer and winter sunshine at a few selected stations have been expressed as a percentage of the possible sunshine.

As these figures indicate, there is a marked increase in cloudiness in the North Island in winter, but little seasonal change in the South Island, except in Southland.

Climatological Averages—The following table provides a brief summary of the main climatological elements for selected locations.

NOTES: (1) Averages of rain days and wet days 1950-66; sunshine 1935-60; mean temperature 1931-60; other temperature data and days of screen frost, various periods—all exceeding 10 years.

(2) For normal monthly and annual rainfall for these stations, see table under subsection on Rainfall.

Normal Seasonal Temperature Pattern—A feature of the seasonal pattern of temperature for New Zealand is the near symmetry about either the hottest summer months or the coldest winter months. In other words the summer-winter decline is an almost identical reversal of the winter-summer rise. This shows up clearly when temperatures for 100 climatological stations are averaged month by month. The first two months of the calendar year, the summer months of January and February, display the same average temperature, that of 61.3°F. This temperature is the highest average for any month, being approached by only the December average of 59.2°F. Once February is past a decline sets in, the estimated average New Zealand temperature falling by 2.5°F from February to March to give a March average of 58.8°F. Thereafter, successive inter-monthly temperature drops of 4.4°, 5.4°, 4.2°, and 1.2°F finally produce a July average of 43.6°F, which makes this month the coldest of the year. Progressing through and past July the temperature steadily rises, the increments being successively, 1.8°, 3.4°, 3.8°, 3.2°, 3.4°, and 2.1°F, finally returning to the January mark of 61.3°F.

ESTIMATED NORMAL NEW ZEALAND TEMPERATURE (°F)^*

The following diagram illustrates the seasonal temperature pattern.

Brief Review of 1968:Year—Rainfall was above average over the greater part of the country, mainly by about 20 percent. Highest departures of 40–60 percent were recorded in parts of Central Otago and the upper Waitaki basin, around the coast of North Otago and South Canterbury, in the Marlborough high country, and in a considerable area of Northland centred near Dargaville. The only considerable area with rainfall as much as 10–15 percent below average was one extending from just east of Rotorua through Kawerau to Opotiki.

Temperatures were mainly warmer than average by half a degree; highest departures of a degree were recorded around Christchurch. It was cooler than average by half a degree in the upper Waitaki basin, the Southern Lakes district, and western Southland. The mean temperature over the whole country was 0.2°F warmer than the 1931-60 average.

Sunshine was below average by about 100 hours in most northern districts of the North Island, in Wairarapa, in Nelson and Buller, and around Invercargill. A surplus of about the same amount was recorded in Gisborne and northern Hawke's Bay, about Cook Strait, and in Canterbury and Otago, except for Central Otago.

Nineteen sixty-eight was an unusually windy year. Aerodromes where the number of days with wind gusts to 40 m.p.h. or over was the highest in 15-30 years of record included Kaitaia, Gisborne, Napier, Ohakea, Nelson, and Blenheim.

Seasonal Notes—The first 2 months of the year were both dry over the North Island, and this was the driest February there since 1946. Northern districts were especially affected by the lack of rain and they reported a drop in dairy production.

March was exceptionally warm, in many districts the warmest for 60 years. The dry weather persisted over the North Island, except in Northland. Serious flooding was reported in coastal districts from Dunedin to south Canterbury following heavy rain on 8–9 March.

The weather for April was dominated by a storm of tropical origin which passed along the east coast from North Cape to Banks Peninsula. The greatest damage occurred in and around Wellington as it passed just to the east on the morning of 10 April. In the suburban area mean wind speeds of up to 90 m.p.h. were recorded, with gusts to 123 m.p.h. These were the strongest winds yet recorded in any built-up area in New Zealand, and they caused damage to over 200 houses. The inter-island steamer Wahine sank in Wellington Harbour as a result of the storm, with the loss of 51 lives. The storm also caused flooding in Canterbury, Otago, and Southland. Generally, April was very wet and very cloudy.

May was a mild month marked by an unusually high frequency of northwesterly winds. June was a very wet month-too wet for many farmers. It was also unusually cloudy over the North Island.

Persistent cold southwesterlies from about 27 June to 4 July brought snow to much of the South Island and higher levels of the North Island. In the South Island, even at low levels, falls were over a foot deep in many places. However, the effects were most serious at higher altitudes. Heavy frost followed the snow, and even in some areas below 2,000 ft several inches of snow were still lying at the end of July. Stock in some areas were isolated for weeks, and an estimated 60,000 sheep died.

July was marked by an unusually high frequency of winds from an easterly quarter, causing wet conditions in Gisborne and Hawke's Bay. August was a mild month, especially in the South Island.

The spring months of September, October, and November were marked by unusually strong and persistent westerly winds, the worst for 30 years in eastern districts. This was also the coolest spring since 1946. Rainfall was the highest on record in the Alps, with a total of 97.86 in. at Otira. The cool temperatures led to many complaints of slow growth; and the persistent dry weather in Canterbury and Hawke's Bay caused a shortage of feed. The week 22–29 October was a particularly stormy period, with reports of serious damage from Canterbury and North Otago on the 26th and 29th.

December was also cool, but with an unusually high frequency of easterly to northeasterly winds, bringing welcome rain to eastern districts, with generally favourable conditions for growth. On 7 December, during violent thunderstorms in the Taihape district, exceptionally heavy rain over a period of 1–2 hours caused large slips and washouts near Mangaweka, disrupting road and rail traffic for several days.

Summary of Meteorological Observations for 1968—The observations from which the following summary was compiled for the year 1968 were taken at 0900 hours New Zealand standard time, i.e., 2100 hours Greenwhich mean time.

For 1968 the mean sea level pressure values in millibars at 0900 hours New Zealand standard time were: Auckland 1014.0; Kelburn, Wellington 1011.0; Nelson Airport 1011.7; Hokitika 1011.4; Christchurch 1009.9; and Dunedin 1008.8.

EARLY HISTORY: General—When New Zealand was discovered by Europeans in 1642 it was found to be inhabited by a race of Polynesians called Maoris, who had migrated to these islands at least 300 years previously. It is generally accepted that the Maoris came originally from South-East Asia, whence, as proto-Polynesians, they moved eastwards from island to island until they reached the eastern Pacific, where they settled the islands now known collectively as Polynesia. From Polynesia the ancestors of the Maori sailed south-west in ocean-going canoes to reach New Zealand and these voyages were probably spread over several generations, perhaps several centuries. Oral Maori history and genealogy support the view that there was a final wave of migration of considerable magnitude about A.D. 1350. Adapting themselves to a new physical environment, in isolation from the outside world, the Maoris produced forms of social and economic organisation and material culture which were significantly different from their Polynesian prototypes.

Coming from tropical latitudes, the Maoris mainly confined themselves to the warmer North Island, and when discovered by Europeans were in a high state of neolithic civilisation, with marked superiority in the arts of wood carving and military engineering. Their principal social unit was the family group, and from combinations of the numerous groups were formed the subtribes and tribes. They had highly developed social and ritualistic customs, and their system of land tenure and methods of cultivation were communal within the subtribes. Inter-tribal and intra-tribal warfare was common, and as individuals they displayed exceptional courage and intelligence.

The immediate effect of European contacts on the Maoris was the outburst of a series of tribal wars waged with greater ferocity and a vastly greater loss of life than was customary in pre-European tribal engagements. The high mortality could, of course, be credited to the acquisition of a more lethal weapon, the musket. The advantage lay originally with the coastal tribes as a result of their earlier contact with Europeans, the wars continuing until all tribes were equally well armed. These wars were later followed by wars against the colonists, but after 1870 the story has been one of unbroken peace between Maoris and Europeans.

The introduction of European diseases and firearms, and the impact of European civilisation on the traditional way of life and customs of the Maoris, had such an adverse effect that their numbers must have been reduced by over half during the nineteenth century. However, the virility of the race gradually asserted itself, and from the beginning of the twentieth century the Maori population has been rapidly increasing.

The overseas territories of Niue Island and the Tokelau Islands had also long been inhabited by Polynesians from various successive migrations extending over considerable periods prior to their discovery by Europeans.

Discovery by Europeans—On 13 December 1642, Abel Janszoon Tasman, a navigator of the Dutch East India Company, discovered the country to which he gave the name of Staten Land, and which later became known as “Nieuw Zeeland”. Tasman had left Batavia on 14 August 1642, and, after having discovered Tasmania, he steered eastward and sighted the west coast of the South Island, described by him as a high mountainous country. Sailing north, he had the misfortune to come into conflict with the Maoris at Golden Bay, on the north coast of the South Island, so that, though he continued his northward journey until he reached the northern tip of the country, he did not again attempt to land. His exploration was of necessity very cursory, for having explored only part of one coast he had no knowledge of the country's extent or shape.

There is no record of any European visit to New Zealand after Tasman's departure until Captain Cook sighted land on 6 October 1769, at Young Nick's Head, near Gisborne. On his first voyage Cook spent six months exploring the New Zealand coastline, and he completely circumnavigated the North and South Islands. His activities can be best described by saying “he found New Zealand a line on the map, and left it an archipelago”. Not only was Cook's ability shown by his cartographical accuracy, but also in his peaceful dealings with the truculent Maoris. He returned to New Zealand again in 1773, in 1774, and in 1777.

Several other explorers also visited New Zealand during the latter portion of the eighteenth century, amongst whom may be mentioned M. de Surville 1769, M. Marion du Fresne 1772, Captains Vancouver and Broughton 1791, Captain Raven 1792-93, Alejandro Malaspina and Jose de Bustamente y Guerra 1793, and Lieutenant Hanson 1793.

The European discovery of Niue Island was made by Captain Cook in 1774. The first recorded discovery of the Tokelau Islands was made by Quiros in 1606.

European Settlement and Colonisation—So far as is known, the first instance of Europeans being left in New Zealand to their own resources occurred in 1792, when Captain Raven of the Britannia landed a sealing party at Facile Harbour, on the west coast of the South Island, where they remained a little over 12 months before being called for.

In the years that followed, whaling stations sprang up along the coast, and a trade with New South Wales began not only in whale oil and seal skins, but also in flax and timber. In 1814 Samuel Marsden, chaplain to the Governor of New South Wales, obtained permission to send two of his protégés, Kendall and Hall, to the Bay of Islands to consider the desirability of establishing a mission station. Later they returned to Sydney for Marsden, who arrived in New Zealand to preach his first sermon at the Bay of Islands on Christmas Day, 1814. Of the many admirable activities undertaken by the missionaries, their action in having the Maori language “reduced to a rational orthography” deserves special mention.

In 1825 three separate, but abortive, attempts were made to found colonies; however for some years the only settlements were those round the principal whaling stations, although a number of Europeans gradually penetrated inland and resided there permanently, many marrying Maori women.

The first body of immigrants under a definite scheme of colonisation arrived in Port Nicholson in January 1840, there to found the town of Wellington, just one week before Captain William Hobson arrived at the Bay of Islands as Governor to proclaim British sovereignty (see later). These settlers were brought out from England by the New Zealand Company, whose moving spirit was Edward Gibbon Wakefield.

It was hoped that, by producing a proper balance of capitalists and artisans, self-contained communities could be successfully established. However, owing to the unsatisfactory nature of the land purchases, considerable difficulty was experienced in these initial settlements, and friction grew up not only between settlers and the Maoris, but also between the Governor and the settlers. Before his death in 1842 Governor Hobson had transferred his capital from Russell to Auckland, but this transfer was of little assistance to the colonists, who had extended their settlements to Wanganui, New Plymouth, and Nelson.

Following the death of Hobson, the existence of the colony became precarious, for, through lack of funds and weak administration, Maori aggression became a real menace. To cope with the situation, the Colonial Office appointed Captain George Grey as Governor. Being well equipped with troops and funds, as well as being a man of vigour and perception, Grey soon restored order and won the confidence of both the settlers and the Maoris. During Grey's term two further organised settlements were made. In co-operation with the New Zealand Company the Free Church of Scotland sponsored the Dunedin Settlement of 1848, and the Church of England the Canterbury Settlement of 1850. These settlements, owing to their more favoured situations, their satisfactory land-purchase agreements, and their freedom from trouble with the Maoris, achieved a greater measure of success in carrying out the company's avowed aims.

After Grey's departure the question of relationship with the Maoris again came to the fore through the land-purchasing activities of the settlers—a situation aggravated by subsequent lack of consideration for the Maori system of land tenure. Following an incident at Waitara in the Taranaki district, where a dispute arose concerning land titles, war broke out in 1860 and lasted spasmodically till 1870. The recall of Grey did not solve the problem, as Grey, an autocrat, could not work with the elected Ministers, nor did his presence prevent the confiscation of land belonging to the Maoris, whether friendly or hostile. It was under the sympathetic administration of Sir Donald McLean as Minister for Maori Affairs that the dispute finally died down.

These hostilities were confined to the North Island; and, in the meantime, in 1861, large alluvial deposits of gold had been discovered in the South Island—leading to a tremendous influx of population and an alteration of the economic structure of the country.

No organised form of European colonisation has at any time taken place in Niue Island or the Tokelau Islands.

SUBSEQUENT HISTORY AND DEVELOPMENT (1870 ONWARDS)—The discovery of gold, by increasing the wealth of the South Island, allowed it to obtain a lead in commercial and political development which it long maintained. Moreover, with the subsequent agrarian expansion, especially in the development of the large pastoral holdings, the country ceased to be merely self-sufficient agriculturally, but began to develop a substantial export trade, mainly in wool.

These factors, together with freedom from strife with the Maori population, led after 1870 to a quickening in political activities. Under the leadership of Sir Julius Vogel a policy of extensive borrowing for railway and road construction was begun. The provincial system, which really commenced in 1853, had largely outlived its usefulness; in fact, the parochialism of the provincial assemblies had frequently proved obstructive, and in consequence the system was abolished in 1875, local administration being provided for by the Counties Act and the Municipal Corporations Act of 1876.

Of great social significance was the passing in 1877 of the Education Act, making education free, compulsory, and secular, while the laying during that decade of the first cable between Australia and New Zealand was a major advance in communications. At this time party politics began to enter into the parliamentary system, and the slump conditions which prevailed in the eighties (due to a fall in the world price level) intensified the political atmosphere. By the abolition of plural voting in 1889, and the introduction of female suffrage in 1893, the way was opened for a practical expression of political convictions by all adult members of the community.

In 1891 Ballance, as Leader of the Liberal Party, became Premier, to be followed on his death in 1893 by Seddon, and during the next decade the legislative essays of this party evoked world-wide interest. The main aim of the legislation was social justice, and its principal manifestations were in land division, the establishment of the Court of Arbitration, and the introduction of old-age pensions. The policy of land division aimed at closer land settlement, and it was achieved by the compulsory subdivision of large estates, with subsequent loans to small independent farmers wishing to establish themselves. In inaugurating the Court of Arbitration the object was to eliminate strikes by giving labour a recognised bargaining status; and the enactment was in accord with the enlightened code of labour legislation passed at that time.

With the commencement of the refrigerated trade in 1882, the move to closer land settlement progressed rapidly, since the production of frozen meat and dairy produce for export encouraged more intensive farming. There thus arose a new farming class which in 1911, some five years after Seddon's death, was mainly responsible for the overthrow of the Liberal regime.

The policy of the succeeding Reform Party under Massey was one favouring agricultural production. Farming interests were given constant encouragement by a series of enactments of which the extension of rural credit was typical. Three years after the advent of the Reform Party the First World War, 1914-18, broke out, leading to the formation of a Coalition Government and an Imperial commandeer of exports. War activities were marked by heavy casualty lists, in proportion to the population, and by enhanced cordiality in Imperial relations. One noteworthy outcome of the war commandeer was the precedent given for the establishment, after the war, of control boards to regulate the export of pastoral products.

Though the effects of the post-war depression during the period 1921-24 showed themselves in an increase in unemployment and slight wage reduction, no drastic legislation was necessary to stabilise economic conditions. During the following years the price level rose; and from the administrative side, the period was characterised by extensive public works expenditure, with particular attention to hydro-electric schemes and highways.

Owing to the encouragement given to farming, pastoral production constantly expanded, so that New Zealand became one of the world's greatest exporters of pastoral produce. As a consequence, her national income was extremely sensitive to price fluctuations of these products; so that, with the advent of the depression in 1930, her economic position became extremely vulnerable. In order to produce balanced budgets, both public and private, various legislative remedies were attempted. In particular, enactments were provided for unemployment relief, for the suspension, in effect, of compulsory arbitration, for the establishment of a Reserve Bank, for a mortgage moratorium, for raising the exchange rate, and for reduction in interest rates and wages. With the recovery in price levels and consequent general economic revival, amendments were made to several of these Acts, removing the more stringent measures. The election of a Labour Government in 1935 led to a change in administrative policy, the preoccupation being mainly with social problems. Further amendments were made to the depression legislation, certain restrictive measures were removed, and other temporary adjustments made permanent.

The general climate of opinion and gradual maturity of outlook furnish the background in which certain distinctive trends appear in legislation passed since 1936.

The first major influence was a humanitarian attitude reinforced by a progressive economic policy. Evidence of this is implicit in the provision for a basic wage, and later for a minimum wage, employment-promotion legislation, amendments to workers' compensation, industrial conciliation and arbitration, mining, etc., legislation, the system of basic prices for certain primary produce, the creation of farm industry reserves, and the rationalisation of production and marketing by the establishment of boards for certain items of primary produce.

The second major influence on legislation was conditioned by the outbreak of the Second World War, 1939-45. A vast body of legislation was placed on the statute book during the war period dealing with the control of manpower and materials, stabilisation of prices, wages, and rents, conditions of employment and suspension of certain peacetime features of industrial activity, discouragement of some industries and diversion to or encouragement of other industries, provision for rehabilitation, etc.

A third dominant trend was the acceptance of the principle that society should take active steps towards the improvement of the working, living, and social circumstances of its members. Foremost in this category was the Social Security Act and its later extensions providing for monetary benefits such as age, superannuation, family allowances, sickness, and unemployment, and by the provision of a system of medical, pharmaceutical, hospital, maternity, and other related benefits.

Other legislative enactments under this heading include the provision for paid annual holidays, reduction of working hours, extension of workers' compensation insurance, improvement in safety and health and welfare conditions in industry, and extension of educational facilities and opportunities.

A fourth approach to law making resulting from maturity of outlook has been the increased participation by New Zealand in international affairs consequent on its acceptance of responsibility in the wider issues of the present era. Legislation authorising participation in United Nations activities generally and in particular emergencies, such as military service in Korea, Malaya, and elsewhere; the extension of New Zealand representation in overseas countries and with the United Nations; the greater frequency of Commonwealth consultation; extension of aid to less developed countries, e.g., participation in the Colombo Plan, all bear witness to this change in outlook.

Another influence on legislation presents some parallels to that last mentioned, but is more concerned with the domestic sphere. It is exemplified in the increasing interest taken in welfare and social development generally of both the rapidly growing Maori population and the inhabitants of the islands of the Pacific with New Zealand ties.

Contemporaneously with the expansion of the field of legislative interest, the economic and industrial development of the country has proceeded with marked impetus in recent years. Expansion and diversification of manufacturing and servicing industries have provided avenues of employment for the growing labour force. At the same time the basic industries of the country, those concerned with primary production, have increased output, assisted by the rapid application of technological improvements and research findings.

The history of New Zealand's overseas territories has been largely one of wise paternal oversight, particularly in the earlier periods, by the New Zealand Government and by the various missions established in the islands. More recently, successive Governments have in various ways encouraged the inhabitants to take an increasing share in the administration of their communities, thus paving the way for self-government. Much attention has been paid to combating tropical diseases and to health problems generally; such island industries as citrus fruit and banana growing have been fostered and encouraged in various ways, with outlets being found for produce available for export. Financial and other assistance has been provided from New Zealand Government sources for the expansion of educational facilities and opportunities, public works such as roading, conservation of water supplies by reservoir construction, communication facilities, etc. Fuller information is given in Section 38 of this Yearbook.

For detailed information, reference should be made to the many excellent books dealing with the subject of New Zealand history, of which the more recent ones are listed in the Select Bibliography in this Yearbook. A useful reference is the Encyclopaedia of New Zealand, published in 1966.

SOVEREIGNTY—Following representations from Maori chiefs for protection from the prevailing turmoil and lawlessness caused by tribal warfare and the rough element around the whaling stations, the New South Wales Government appointed, in 1832, Mr James Busby as British Resident at Russell. Owing to the failure to supply him with any means of exerting authority, his appointment was largely ineffective. Finally the disorder, and the friction between the two races, became so intolerable that even the missionaries, who were opposed to annexation, made representations for British sovereignty.

On 29 January 1840, Captain William Hobson, RN, arrived at the Bay of Islands, empowered, with the consent of the Maoris, to proclaim the sovereignty of Queen Victoria over the Islands of New Zealand, and to assume the government thereof. Hobson formally read his commissions at Kororareka on 30 January 1840, and on 6 February of the same year a compact called the Treaty of Waitangi was entered into, whereby all rights and powers of sovereignty were ceded to the Queen, all territorial rights being secured to the chiefs and their tribes.

On 21 May 1840 Governor Hobson proclaimed British sovereignty in the case of the North Island by virtue of the Treaty of Waitangi, and in the case of the South Island and Stewart Island by right of discovery. New Zealand remained a dependency of New South Wales until 3 May 1841, when it was created a separate colony by Royal Charter dated 16 November 1840. The capital was at first transferred from Russell to Auckland, but in 1865 it was again transferred, on this occasion to Wellington, where the seat of Government has since remained.

During Governor Grey's term, steps were taken to draft a constitution for the colony. An Act granting representative institutions was passed by the Imperial Parliament on 30 June 1852, and was published in New Zealand by Proclamation on 17 January 1853. Under it, provision was made for the constitution of a General Assembly consisting of a Legislative Council and a House of Representatives. Provision was also made for the division of the country into provinces, each province having an elected Council and Superintendent. (The provincial system was abolished in 1875 and the Legislative Council in 1950.) In the first General Assembly of 27 August 1854 certain members of this body were associated with the permanent members of the executive but they did not hold any portfolios. It was not until 7 May 1856 that responsible government was actually established.

With the gradual development of the country's economy, the acquisition of political and administrative experience, and the increasing desire for self-reliance in political matters, the degree of self-government became more complete. In recognition of this and of a nascent sense of nationality, New Zealand was given the title of Dominion in lieu of Colony, the new title taking effect on 26 September 1907.

Of the constitutional events in recent years the passing by the United Kingdom Parliament of the Statute of Westminster in December 1931 was of major importance. The draft of this statute was submitted for the confirmation of the various Commonwealth Legislatures before its passage through the United Kingdom Parliament. The statute granted complete autonomy to the various self-governing members countries, but it did not automatically apply to Australia or New Zealand. In other words, its operation in the latter self-governing members of the Commonwealth was declared to require specific adoption by the Legislatures of those countries. It was not until 1947 that the New Zealand Government formally adopted the Statute of Westminister.

NEW ZEALAND'S INTERNATIONAL ACTIVITIES—Though in the nineteenth century Sir Julius Vogel and the Right Hon. R. J. Seddon had original views about the policy which Britain and New Zealand should pursue in the Pacific area—views which they announced with vigour—New Zealand did not acquire the right to conduct an independent foreign policy until the end of the First World War when the full nationhood of the “Dominions” was recognised. For some years after this, however, successive New Zealand Governments chose not to exercise this right and (pursuing a passive role in the League of Nations and refraining from establishing diplomatic relations with foreign Governments, or with other members of the Commonwealth apart from Britain) preferred to make known any views on matters of foreign affairs only to the British Government and through the confidential channels of intra-Commonwealth consultation.

Few pressures existed in the 1920s and early 1930s to impel New Zealand towards enunciating an independent foreign policy. The population was mainly British in composition and comparatively few were concerned to distinguish between New Zealand's interests and those of Britain. Nor had they much cause to do so: New Zealand had established a fruitful economic partnership with Britain, upon which country nearly all her material and cultural links were centred; and New Zealand's surest protector against dangers which it was incapable of meeting alone was the Royal Navy. It was, moreover, realised that New Zealand in her own right could make little impact on world affairs, whereas Britain was a great power capable of affecting the pattern of world events. New Zealand “foreign policy” therefore consisted chiefly in seeking to modify British policy in those few cases where New Zealand had a strong interest or a viewpoint rather different from that of Britain.

The emergence of an independent New Zealand foreign policy is usually held to date from 1935. Some Ministers in the new Government were deeply interested in world affairs in general, and the Government's approach was influenced by theory and principle. In particular, they held strong views on the principle of collective security and upon the League of Nations as the embodiment of that principle. In its method of championing the principles of collective security, pressing for the restoration of the authority of the League of Nations and, at a time when the United Kingdom Government was pursuing the policy which came to be known as appeasement, urging positive League action over Abyssinia, Spain, and China, the Government came to depart from the pattern of the previous 16 years: for, in addition to making its views known in confidential communications to the United Kingdom Government, it also stated them with vigour in the international forum of the Council and the Assembly of the League of Nations.

There was, nevertheless, no fundamental departure from the traditional policy of association with Britain. Moreover, the course that would be followed in the event of war was never in doubt. As early as 16 May 1938 a leading member of the Government had said, “If the Old Country is attacked, we are too. we will assist her to the fullest extent possible.” When war broke out the Prime Minister, the Right Hon. M. J. Savage, expressed New Zealand's position in terms that were as true in 1939 as they would have been in 1914:

“Behind the sure shield of Britain we have enjoyed and cherished freedom and self-government. Both with gratitude for the past, and with confidence in the future, we range ourselves without fear behind Britain. Where she goes, we go. Where she stands, we stand.”

But the Second World War changed the pattern of power in the world and made it necessary for New Zealand gradually to revise its foreign policy and its method of implementing that policy. Even though the basic attachment of New Zealanders to Britain was little affected, the fact became manifest that Britain was no longer a power able to determine events on a world scale and that, since New Zealand interests could no longer be protected by British actions alone, it did not suffice to confine New Zealand foreign policy to occasional attempts to persuade the British Government to take note of New Zealand views. Japanese aggression and, later, the rise of Communist China forced New Zealand to face the reality of its geographical location with respect to Asia and the Pacific and to develop an additional relationship with the only other friendly power capable of protecting New Zealand—the United States of America—with the least possible prejudice to its association with the United Kingdom.

During the war years New Zealand was admitted to the councils of the Allies and was expected to advance informed views. The Government honoured its responsibility and, having established in wartime the habit of participating in the making of international decisions, accepted it as natural that New Zealand should continue to participate in the development of a post-war world order and in subsequent international consultations. To this end New Zealand established (in effect from 1943) a professional Department of External Affairs and a career foreign service, and proceeded slowly to establish diplomatic missions in countries where New Zealand's interests merited protection. In particular, New Zealand sought increasingly to make its individual contribution to fostering good relationships with its neighbours in the Pacific and Asia and to increasing the measure of security and welfare in these areas.

To be woven into any post-war policy was the now traditional New Zealand belief in the principle of collective security and international justice, especially as symbolised by the United Nations. This was by no means an easy task in a world where the divisions of the cold war were reflected in competing regional alliances. There had to be a place, too, for belief in the ability of international co-operation to control armaments and to eliminate poverty, disease, and other economic and social causes of international tension.

The threat to New Zealand's security, posed by the entry of Japan into the war at a time when the United Kingdom was fully committed in Europe, brought New Zealand into the closest relations with two of her neighbours on the borders of the Pacific—Australia and the United States. Recognition of the need for a greater measure of collaboration with Australia resulted in the signing in 1944 of the Canberra Pact which provided machinery for continuing consultation between the two Governments. Upon the entry of Japan into the war, both New Zealand and Australia had looked principally to the United States for protection. Relations among the three countries thus entered a new phase. The close association of wartime found expression in peacetime in the Anzus Treaty, in which, for the first time, New Zealand and Australia entered into a treaty of alliance and mutual defence with a foreign country and achieved the aim of both countries to enter into a close relationship with the major Pacific power. The Anzus Treaty, which came into force in April 1952, gives an assurance of United States support in the event of an armed attack from any quarter in the Pacific and so constitutes New Zealand's major safeguard from aggression in the area.

The establishment of SEATO, like the formation of the ANZUS alliance, took place against a background of continuing insecurity and of danger in the Far East. In 1950 New Zealand had participated in collective action by the United Nations in Korea. In 1954, following the Indo-China crisis and the Geneva Accords, a broader collective defence treaty covering South-East Asia and the South West Pacific, known as the Manila Treaty, was signed by New Zealand and Australia, France, Pakistan, the Philippines, Thailand, the United Kingdom, and the United States. The parties agreed that in the event of armed attack on the parties or on a “protocol” State (Laos, Cambodia, and South Vietnam) they would act to meet the common danger. The parties established the South East Asia Treaty Organisation (SEATO) in Bangkok. In furtherance of its obligations under the Manila Treaty, New Zealand sent forces to Thailand for some months in 1962 and to South Vietnam in 1965. In 1955 New Zealand had transferred its war-time commitment from the Middle East to South-East Asia and agreed to contribute forces to a Commonwealth Far East Strategic Reserve. These forces participated in the Malayan Emergency and in the defence of Malaysia and Singapore against Indonesian confrontation. New Zealand, with Australia, became associated with the Anglo-Malayan Defence Agreement concluded in 1957, which subsequently became the Anglo-Malaysian Defence Agreement upon the formation of Malaysia in 1963. More recently New Zealand has participated in defence talks with Britain, Malaysia, Singapore, and Australia in the implication of the British decision to withdraw its forces from South-East Asia by the end of 1971.

These developments reflected a new awareness of the international and strategic implications of New Zealand's position. In 1955 the Minister of External Affairs, the Hon. T. L. Macdonald, discussing New Zealand's foreign policy, said that the only possible threat to New Zealand's security could come from Asia and in particular from the spread of Communist power in South-East Asia. “New Zealand foreign policy grows”, he said, “from the need to reconcile geography and history, economic fact and strategic fact. In practical terms at present this seems that without weakening the many links which bind us to Britain and the whole Atlantic Community we must increase our concern with South-East Asia.”

This concern was already being expressed in social and economic terms as well as in defence. In 1950, New Zealand, along with a group of other Commonwealth countries, had become a member of the Colombo Plan established to assist the countries of South-East Asia to improve their standards of living. To New Zealand, a pioneer in the field of social legislation and a country with a high standard of living fairly evenly shared, the Colombo Plan has a special significance. Contributions, large by New Zealand standards (if small when measured against the potential need), have been made to it. The scope of New Zealand's presence in Asia widened considerably in the years following signature of the Manila Treaty—diplomatic relations were established with a growing number of countries in the area, and increased activity in other fields of co-operation besides that of defence followed the extension of this network of diplomatic posts. By the mid 1960s New Zealand had more complete representation in Asia than in Western Europe. Subsequent accession to regional membership of ECAFE, the Asian Development Bank and ASPAC (the Council for Asian and Pacific Co-operation) is further demonstration of this country's acceptance that it has a role to play in the Asian area.

New Zealand's direct interest in political, social, and economic developments in the South Pacific is reflected not only in its membership of such regional organisations as the South Pacific Commission, but also in a wide and growing range of contacts with island people and an increased sense of involvement in their problems. The evolution of self-government and nationalism in the South Pacific reached a new stage when Western Samoa became the first independent Polynesian state on 1 January 1962. Three years later the Cook Islands achieved internal self-government. New Zealand's own colonial past, its liberal tradition of friendship for emergent peoples, and the fact that large numbers of Polynesian people have settled there, means that the islanders tend to look to New Zealand for leadership and encouragement. In particular, Western Samoa, Tonga, and Fiji already regard New Zealand as an important export market and as a source of administrative and technical assistance. Inevitably, New Zealand is going to be increasingly involved in the South Pacific region.

These regional concerns have implied no weakening of the belief in the pre-eminent value of action organised on a world basis to deal with social and economic, as well as security problems. New Zealand has continued to place special importance upon its membership of the United Nations. It has been an active participant in the work of the General Assembly, has been a member of all Councils of the Organisation, has provided troops to the United Nations Force in Korea, and military observers in Palestine, Kashmir, and Lebanon, and has endeavoured to assist all efforts to attain the political and social objectives outlined in the Charter.

If, since the Second World War, the facts of geography have had an important influence on New Zealand's attitudes towards foreign affairs, history and tradition continue nevertheless to mould its outlook. The historic links with the United Kingdom and with Western Europe and North America remain as close as ever; and the economic links with the United Kingdom, New Zealand's best customer, remain strong. No situation is, however, constant. One of the key problems of external political and economic policy now presented to New Zealand arises out of the movement towards political and economic integration in Europe and the continuing possibility of Britain's membership of the European Economic Community. New Zealand must expand the volume and value of its exports of primary products if the standard of living of its rapidly growing population is to be maintained and improved. In recent years it has become increasingly apparent, however, that the United Kingdom market is capable of only a limited expansion. The development of new markets in Asia and other less developed countries has been slowed by low income levels as well as by consumption patterns in which the type of foodstuff exported by New Zealand has not figured prominently. New Zealand's foreign policy is likely to continue the endeavour to reconcile geography and history, economic fact and strategic fact.

Department of External Affairs—The External Affairs Act 1943 made provision for the appointment of a Minister of External Affairs charged generally with the administration of external and foreign affairs, including relations with other countries, communications with other Governments, representation abroad, and representation of other countries in New Zealand. The Act also authorised the appointment of a Secretary of External Affairs and (superseding the High Commissioner Act of 1908) dealt with the appointment of High Commissioners and of overseas representatives.

The functions of the Department were defined at its inception as follows:

The Act thus established the Ministry of External Affairs as the normal channel of communication with the Governments of other countries. As, however, the new Department was in fact still a part of the Prime Minister's Department, no change in procedure, apart from the use of the changed nomenclature, was necessary.

Dealings with overseas Governments usually involve considerable interdepartmental coordination. Since the Prime Minister's Department has always been regarded primarily as a department of co-ordination, an intimate relationship has existed between the two Departments. The Prime Minister has for three periods found it appropriate to assume the portfolio of External Affairs and the Departments have in any case been run as a unit. The staff is held in common and, though some officers are engaged on work peculiar to one Department, the work of the majority involves both Departments. The Secretary of External Affairs is also Permanent Head of the Prime Minister's Department. For the first 23 years of the existence of the Department of External Affairs, until October 1966, the same person, Mr A. D. McIntosh, held the two posts. His successor, Mr G. R. Laking, also fills both positions. In defence matters the two Departments have been closely associated. During the war, the Permanent Head was also Secretary of the War Cabinet. In that period the responsibility of the Prime Minister's Department for defence co-ordination was extended and developed; in discharging this responsibility the Permanent Head was assisted by the Defence Secretariat of the Prime Minister's Department. The functions of the Secretariat have been taken over by the unified Ministry of Defence which was established by Act of Parliament in November 1964. A close relationship is still maintained between the Ministry of Defence and the Defence Division of the Department of External Affairs, and the head of that Division is chairman of the body which co-ordinates military and civilian intelligence.

In the formulation and application of external affairs policy, close association with other Government Departments is necessary. Participation in the Colombo Plan entails close liaison with the Treasury and with the many Departments which supply experts and training facilities, consular questions with the Department of Labour, and legal questions with the Department of Justice. Moreover, the Department is a clearing house for a wide variety of material provided by overseas posts for other Departments. As well as fulfilling its major function of acting as a channel of communication with other Governments, the Department thus acts as a co-ordinating centre for other Government Departments. The Department and its network of posts overseas also perform numerous services on behalf of Departments which are without overseas representatives of their own.

In the Official Section at the end of the Yearbook the diplomatic and other New Zealand representation overseas is listed.

New Zealand in the Commonwealth—Despite the emphasis in New Zealand's approach to international affairs resulting from the realities of its geographical position, membership of the Commonwealth remains a significant feature of its policy. In the past the Commonwealth tended to be identified with Britain through special and historic ties. As these ties have loosened, with the growing orientation of Britain towards Europe, the Commonwealth has assumed a rather different perspective for New Zealand. Providing as it does for contacts with a wide range of countries, and on a great variety of subjects, it is a ready-made forum for co-operative effort. Thus, although the Commonwealth ideal does not embody the identity of purpose formerly apparent among its members, it nevertheless has an important function, particularly for the smaller and more isolated members such as New Zealand.

Although one of the oldest members, New Zealand, unlike some of its fellow members, did not seek to hasten the process of constitutional transition within the Commonwealth. At the Imperial Conference in 1930 the Prime Minister, the Right Hon. G. W. Forbes; stated that “We have felt that at all times within recent years we have had ample scope for our national aspirations and ample freedom to carry out in their entirety such measures as have seemed to us to be desirable”. There was little interest in the adoption of the relevant provisions of the Statute of Westminster enacted in 1931 to give legal endorsement to the transformation that had taken place in the relationship between Britain and the Dominions. It was not, in fact, until 1947 that the necessary formalities were completed in New Zealand by the passing of the Statute of the Westminster Adoption Act.

Since that time there have been many changes in the Commonwealth association both in constitutional respects and in numbers of members. Whereas at the beginning of the Second World War there were only five members, by the end of 1968 there were 28. The Commonwealth has become an entity embracing several continents and its relationships have taken on a new scope and emphasis. New Zealand, itself a country where two races live side by side, sees in the Commonwealth a special opportunity for multi-racial co-operation and understanding.

New Zealand has as yet exchanged representatives with only the following members of the Commonwealth: Australia, Canada, India, Ceylon^*, Malaysia, Singapore, and Britain.

The importance New Zealand attaches to the Commonwealth association has been given practical expression in its membership of a number of Commonwealth organisations, including the Commonwealth Air Transport Council, the Commonwealth Telecommunications Board, the Commonwealth Agricultural Bureau, the Imperial War Graves Commission, the Commonwealth Institute, the Commonwealth Economic Consultative Council, the Commonwealth Scientific Committee, and the Commonwealth Education Liaison Committee. New Zealand also contributes to the budgets of the Commonwealth Secretariat and the Commonwealth Foundation, which were both established at the Commonwealth Prime Ministers' meeting in 1965.

New Zealand and the South Pacific—The first areas of the world towards which New Zealanders developed a distinct and characteristic attitude was the South Pacific. This is New Zealand's immediate environment, its Polynesian peoples close kin to the New Zealand Maori, its islands nearest and most important in the lines of communication which link New Zealand with America and Europe.

Within a decade of New Zealand's establishment as a British colony Bishop Selwyn had made it the base for Anglican missions in the South Pacific and Sir George Grey as Governor had begun to advocate a policy of expansion in the area. The increasing involvement of other powers and a desire to develop trade led Sir Julius Vogel in the 1870s to take up Grey's idea and to put forward various schemes for political and commercial expansion, which, however, found no favour in London. In the 1880s New Zealand joined the Australian colonies in an effort to preserve “Oceania for the Anglo-Saxons”, and soon after the movement reached its peak in the robust opposition of Richard John Seddon to the bargaining away of Samoa in 1899.

The meagre fruit of half a century's agitation was the annexation in 1901 of the Cook Islands and their inclusion within the boundaries of New Zealand. Thereafter, New Zealand's interest in the South Pacific declined as its trade and its thoughts came to centre more and more on Great Britain. But though declining, the tradition was still strong enough to provide support for the Imperial Federation movement in the first decade of the twentieth century and, more practically, to inspire New Zealand on the outbreak of war in 1914 to occupy Germany's colony of Western Samoa.

At the end of the war Western Samoa, like other former German possessions, was retained by the occupying power under a League of Nations Mandate. New Zealand embarked on its new responsibility with greater enthusiasm than it had shown in the Cook Islands and much effort was devoted to solving the problems of the territory. The rate of change thuscreated, however, proved too rapid for the tradition-loving Samoans. In the late 1920s a series of unfortunate incidents occurred and, for some time afterwards, the pace slackened. The opening up in the late 1930s of air routes across the Pacific led New Zealand, along with other countries, to take an increased interest in some of the more remote islands in the area, but it was the outbreak of the Second World War which forcibly reminded the country of its situation.

The New Zealand High Commissioner in India is also appointed High Commissioner in Ceylon.

Overnight half-forgotten islands became strategic points for the defence of New Zealand and its allies, and New Zealanders again became aware of the need to prevent them from falling into unfriendly hands. Accordingly, New Zealand joined with Australia in seeking ways to guarantee the future security of the area, and there emerged first the Canberra Pact of 1944 and later the 1947 Agreement to establish the South Pacific Commission.

Through the Commission the Governments administering territories in the South Pacific— Britain, the United States, France, Australia, New Zealand, and (until 1962) the Netherlands— have made a concerted effort to promote the economic and social development of the area and its peoples. In the 20 years of its existence the Commission has, within its budgetary limits (it currently spends about NZ$870,000 annually), done much valuable work, particularly in bringing the islanders together and developing a sense of community amongst them. Originally laying much stress on research, the Commission has come to concentrate mainly on providing technical assistance and on pooling experience of handling common problems of development. It maintains close working links with the United Nations Specialised Agencies which are taking, an increasing interest in the region.

But New Zealand has not been content with promoting progress in the economic and social spheres only. At the San Francisco Conference in 1945 it took a leading part in working out the trusteeship system embodied in the United Nations Charter, and subsequently the League of Nations Mandate for Western Samoa was replaced by a trusteeship agreement.

In accordance with the wishes of the Samoan people, a programme of political and constitutional development was launched which continued throughout the 1950s and which culminated in the establishment of the independent State of Western Samoa on 1 January 1962. The transfer of sovereignty did not, however, weaken the close and friendly relationship which had grown up between Western Samoa and New Zealand and this was confirmed in a Treaty of Friendship between the two countries signed in August 1962. In the educational as well as in other fields New Zealand assists Western Samoa.

Whilst Western Samoa was moving towards independence, constitutional development was taking place in New Zealand's other island territories. Following expert surveys a programme of economic and social development for the Cook Islands was formulated in 1955 and legislative assemblies for the Cook Islands and for Niue were set up in 1957. In 1962 the New Zealand Government gave these bodies full responsibility for allocating the large subsidies granted by New Zealand. In the same year possible alternatives concerning constitutional development were submitted to the assemblies. Both chose full internal self-government together with a continued association with New Zealand. Events thereafter moved most rapidly in the Cook Islands. In 1963 a “Shadow” Cabinet was set up and a Leader of Government Business elected. The following year the New Zealand House of Representatives passed the Cook Islands Constitution Act, with provision for the Act itself to come into force after a General Election in the Cook Islands. This election was held on 20 April 1965 and after the New Zealand Parliament had at the request of the Cook Islands Government made certain amendments to the Constitution Act, the new Constitution was brought into force on 4 August 1965 and the Cook Islands became a self-governing nation in free association with New Zealand. The Legislative Assembly, assured of New Zealand's financial assistance, is fully responsible for the internal affairs of the Cook Islands.

Similar progress in the constitutional field has also been made in Niue and the Tokelau Islands, New Zealand's remaining dependent territories. The Executive Committee of the Niue Island Assembly exercises power delegated to it by the Resident Commissioner over a wide range of Government activities. Responsibility for deciding priorities for government works and expenditure has been given by the Administrator to the Tokelau Islands Councils or Fonos which have also fully discussed their future development and have expressed the wish to retain their association with New Zealand. At the request of the Fonos the New Zealand Government has instituted a pilot programme to assist Tokelau Islanders to resettle in New Zealand.

The independence of Western Samoa, self-government in the Cook Islands and the progress of the remaining New Zealand territories are indicative of broader changes in the South Pacific. Economic, social and educational development has made the peoples of the area more self-conscious and desirous of managing their own affairs, and the intensification by the United Nations of interest in still dependent territories is likely to bring the South Pacific into yet greater prominence.

New Zealand in the United Nations—For New Zealand, geographically isolated and with limited direct diplomatic relations, the United Nations is inevitably one of the most important forums available, not only to influence the course of international events, but also to secure the friendship and understanding of the world community. For any country, its international reputation is a valuable asset. If New Zealand is better known and commands more influence in international affairs than some other small States similarly situated, this is, in some measure at least, due to New Zealand's record of active participation in the United Nations.

New Zealand's share of the United Nation's regular budget is 0.36 percent; in 1968 this meant a New Zealand contribution to the organisation of US$408,112.

Collective Security Arrangements—It has been noted earlier that the first significant expression of an independent New Zealand foreign policy occurred in the League of Nations and was directed to supporting the principle of collective security. Support for this principle later and through the United Nations has remained a cornerstone of New Zealand's foreign policy.

The purposes which motivated the policy in 1935 were strongly held beliefs rather than principles developed from any careful assessments by a national foreign service. The beliefs were nevertheless a reflection of widely held concern over world events, a concern which the succeeding years were to reinforce. It was, therefore, perhaps understandable that at San Francisco in 1945 New Zealand should argue so forcibly, if unsuccessfully, to eliminate the veto and to strengthen the collective security provisions of the United Nations Charter.

Despite its physical isolation, New Zealand has felt unable to regard with unconcern the fate of other small countries helpless to defend themselves against a powerful aggressor and thus liable to be picked off one by one.

The United Nations does not, it is true, offer a complete guarantee of New Zealand's or any other small country's security against aggression. Nor has it yet achieved agreement on disarmament. But New Zealand Governments have acted upon the conviction that the United Nations, and it alone, contains the rudiments of a universal collective security system and that it is through the United Nations and not through its abandonment in favour of some alternative, that an effective and comprehensive collective security system may eventually be developed and agreement on disarmament achieved.

Within the United Nations the expression of this policy has taken several forms. New Zealand has sought to remove the causes which might produce the need for recourse to collective security action. Its representatives have urged that the Assembly be used as a place for harmonising relations between nations: they have voiced the need for restraint in the pursuit of national objectives; they have consistently sought and supported responsible action in aid of an effective international organisation; they have reiterated the need for the early adoption of a broad programme of supervised disarmament.

New Zealand was elected to the Security Council, which is charged with the primary responsibility for the maintenance of international peace and security, for the years 1954 and 1955, and for a second term in 1966 when membership of the Council was increased from 10 to 15.

New Zealand has also advocated adequate and timely preparations in case aggression should occur and has supported the fullest possible development of the United Nations' capacity for peacekeeping. When occasion has arisen, New Zealand has been prepared to play its part: troops were supplied to the United Nations Force in Korea, and military observers to the United Nations Observer Groups in Palestine, Kashmir, and Lebanon; a civilian police unit has served in Cyprus; and the Government has indicated to the Secretary-General its intention in principle to designate a stand-by unit which would be available for properly instituted peacekeeping operations of the organisation in the future.

In some respects, however, the United Nations has not lived up to the hopes placed in it. There has never been complete agreement in the United Nations itself on peacekeeping issues, and further practical developments to increase United Nations capability for peacekeeping are not likely to occur, due to the existing power conflicts in the world, or in view of the divergent interests of many of its present members. New Zealand has therefore recognised that the objective of developing the United Nations potential in security and peacekeeping is a long-term one, and that the United Nations in its present form must be buttressed by regional defensive alliances.

Economic and Social Activities—Apart from this substantial and primary concern with international peace and security, other aspects of the work of the United Nations have increased greatly in importance in recent years. Article 55 of the United Nations Charter recognised that peaceful and friendly relations among nations depend largely on conditions of economic and social progress. Advancement in these latter fields absorbs annually more and more of the United Nations' resources, and represents at least one area in which international understanding and co-operation are reaping tangible rewards. The United Nations organ with primary responsibility in this vast field is the Economic and Social Council (or ECOSOC), an elective body of 27 members, which co-ordinates the activities of the wide variety of bodies with interests in these fields, ranging from the functional commissions and committees of the United Nations itself to the independent Specialised Agencies.

The biggest single task now facing ECOSOC is to promote and direct programmes for economic development in underdeveloped countries. New Zealand has always recognised the need for this type of development, and has been concerned to ensure that the international programmes in this field should be effective and realistic. Its interest in social and economic questions is illustrated by its membership of ECOSOC from 1947-49 and 1959-61. New Zealand in 1963 became a full regional member of the Economic Commission for Asia and the Far East (ECAFE), a body of which it had previously been a non-regional member. New Zealand has also served terms of office from time to time on the Status of Women Commission, the Technical Assistance Committee, and on the Statistical, Social, and Fiscal Commissions. It is currently serving on the Commission of Human Rights for a second consecutive term for the period 1969-71.

In undertaking these responsibilities, New Zealand may to some extent be regarded as “taking its turn”. It is, however, keenly aware of the advantages of doing so. It certainly shares with others an interest in ensuring that economic and social conditions are such as to permit ordered political progress. It is concerned to ensure that where political principals are at issue, the beliefs which New Zealanders hold as essential should be recognised and, if possible, accepted by the world community. Sometimes, too, there are strong reasons of self-interest; it is important that New Zealand's interests and its special problems be taken into account in the work of these bodies. Moreover, the international activities of the various agencies are nowadays on such a scale (the United Nations Development Programme, for example, spends almost $200 million a year), that detailed knowledge of their work can provide mutually valuable opportunities for New Zealand to provide goods and expert services for their programmes.

Specialised Agencies—New Zealand is a member of all the Specialised Agencies except the International Development Association, and is also a member of the International Atomic Energy Agency (IAEA), which though not strictly a Specialised Agency, exist under the aegis of the United Nations. New Zealand's contributions to the regular budgets of the agencies, which are based for the most part on a scale of assessments similar to that used in the United Nations itself, range from $2,600 to $17,000 annually. New Zealand has also subscribed capital to the financial agencies.

Convinced of the value of the form of international co-operation that the agencies represent, New Zealand participates actively in their work. In the case of the technical agencies, there are direct benefits to New Zealand in membership. Membership of the Universal Postal Union, for example, is essential to facilitate the efficient international movement of mails to and from this country; and the International Telecommunication Union works to promote the most rational and efficient operation of world-wide telecommunications services. The World Meteorological Organisation is the medium for establishing a world-wide network for the rapid exchange of meteorological information, which is of particular value to remote areas like New Zealand. In other cases, New Zealand benefits by the free interchange of knowledge and experience, and from the endeavours of the agencies to establish world-wide standards of safety, to promote facilitation of international traffic, and to examine restrictive or discriminatory practices in these fields. Minimum standards of working and living conditions for wage-earners are the concern of the International Labour Organisation.

In the case of the “humanitarian” agencies—the Food and Agriculture Organisation (FAO), the World Health Organisation (WHO), and the Educational, Scientific, and Cultural Organisation (UNESCO)—the emphasis tends understandably, to be more on catering for the urgent needs of peoples in underdeveloped countries who lack the necessities basic to human dignity: food, shelter, and education. Here the pooled resources of the richer nations can provide a wealth of expertise and technical and financial assistance to which New Zealand is glad to contribute its measure of support.

In addition to its contributions to the regular budgets of the agencies, New Zealand gives voluntary assistance in the form of further monetary grants, the services of experts to developing countries (for example in physiotherapy, police work, forestry, and education), and donations of equipment or commodities.

Two major fields of this sort of additional assistance are the contributions made to the United Nations Development Programme and to the World Food Programme. New Zealand gave $400,000 to UNDP in 1968; and in addition has sent experts abroad to work in the field on UNDP assignments. The WFP is a programme approved by the United Nations in 1961 and administered jointly by the United Nations and FAO. For the three years, 1965-68, New Zealand made a total grant of US$750,000, part in cash and part in commodities.

New Zealand's accession to the International Bank for Reconstruction and Development, the International Monetary Fund, and the International Finance Corporation not only allows this country to participate in measures designed to increase the stability of international trade and promote the economic development of the underdeveloped areas of the world, but also serves to strengthen New Zealand's own economic position by providing access to more varied sources of capital for capital projects or for balance of payments purposes.

New Zealand has strongly supported any expansion of agency activity which will help the social and economic development of the Pacific Islands for which it is directly responsible. WHO has assisted in the past in the eradication of yaws and tuberculosis; FAO is at present the executive agency for a UNDP project designed to control the rhinoceros beetle which ravages much of the islands' coconut crops; and expert services have supplied assistance in several smaller projects. Within the General Assembly of the United Nations and in specialised forums New Zealand will continue to draw attention to the needs of the South Pacific.

New Zealand has in the past served on the governing bodies of WHO, FAO, and UNESCO, and is currently a member of the Executive Council of the UPU. Although because of its size and limited scale of contributions, New Zealand is not likely to be elected frequently to the boards of at least the larger agencies, it can expect, over the years, to bear its share of administrative responsibility within them. In any case, by participation in the plenary sessions of the assemblies of the agencies, New Zealand is able to play some part in trying to ensure that the agencies do not duplicate activities with one another, that there is rational budgetary growth, and that the rightful spheres of activity of the agencies are not unduly disrupted by the political conflicts that occur in the main United Nations forums.

Conference on Trade and Development—As a result of the United Nations Conference on Trade and Development held in Geneva in 1964, the General Assembly agreed to hold a triennial conference on Trade and Development with the objective of promoting international trade, particularly between countries at different stages of development, with a view to accelerating the economic growth of developing countries. UNCTAD is therefore the United Nations body generally responsible for all matters relating to trade and development. It is open to all United Nations members and other states members of the Specialised Agencies and the International Atomic Energy Agency. The Conference has become a permanent organisation, with a Trade and Development Board which conducts the affairs of the organisation between plenary conferences. New Zealand commenced its second consecutive term on the board in 1968. There are also within the organisation functional committees on commodities, manufactures, financing of trade and shipping. New Zealand held a seat on the Committee on Commodities until the end of 1967 and was re-elected to the Committee on Shipping in 1968 for a further three-year term. UNCTAD held its second session in New Delhi early in 1968.

GATT—New Zealand has been a contracting party to the General Agreement on Tariffs and Trade since its inception in 1947. Although not strictly a specialised agency, the GATT has assumed the characteristics of one, and its activities have extended into all aspects of international trade including, more recently, measures to liberalise non-tariff barriers to agricultural trade and to provide special export opportunities for the goods of the developing countries.

New Zealand and Collective Defence—The defence of New Zealand has been judged by successive governments to call for active support for the concept of collective security. New Zealand alone is unable to defend its considerable but very isolated territory against aggression by any militarily significant power. As a small country with limited resources, New Zealand is in no position to maintain the extensive defence effort needed if all possible contingencies are to be met. It has therefore supported efforts to promote the effective implementation of those provisions of the United Nations Charter that are designed to establish a universal system of collective security and, until this goal is reached, has accepted that its defence efforts should be made in concert with like-minded countries in order to create a broader framework for security than its individual national effort could provide. This in turn involves the obligation to make credible and effective contributions to collective defence arrangements from New Zealand's own armed services.

Since the Second World War, New Zealand has contributed collective security action under the United Nations flag in Korea where two frigates and a special combat unit were sent from New Zealand in support of United Nations forces. From 1955, units from the three services were based in Malaya, where they took part in actions during the emergency. During 1962, New Zealand took part in a SEATO deployment to Thailand. New Zealand forces actively supported Malaysia in its successful resistance to Indonesian Confrontation. In 1964, in accordance with the same principle of support for collective seurity, a New Zealand Army Engineer detachment was sent to South Vietnam. In 1965, this unit was replaced by an artillery battery, which has subsequently been joined by two infantry companies, for service with 1st Australian Task Force.

ANZUS—A basic expression of New Zealand's support for the principles of collective security is provided by the ANZUS Pact. This tripartite security treaty between Australia, New Zealand, and the United States was signed at San Francisco on 1 September 1951 and came into force on 29 April 1952. The Treaty assured New Zealand and Australia of American support in the event of aggression in the Pacific and also provided for periodic discussions of common problems at ministerial level. ANZUS is a defensive arrangement among the three parties. It has been agreed that, in keeping with the close ties between the three countries, the machinery for consultation should be as simple and flexible as possible. The main provision of the ANZUS Pact is that each party recognises “that an armed attack in the Pacific area on any of the Parties would be dangerous to its own peace and safety and declares that it will act to meet the common danger in accordance with its constitutional processes”. In the context of the agreement an armed attack on any of the Parties is deemed to include “an armed attack on a metropolitan territory of any of the Parties or on the island territories under its jurisdiction in the Pacific or on its armed forces, public vessels or aircraft in the Pacific”.

SEATO—The Geneva Agreements for Vietnam, Laos, and Cambodia, which were completed on 21 July 1954, were an achievement of considerable importance and value, but they fell short of a fully guaranteed settlement of the security issues then posed in the area of Indo-China. Eight governments—Australia, Britain, France, New Zealand, Pakistan, the Philippines, Thailand, and the United States—signed the South-East Asia Collective Defence Treaty, also known as the Manila Treaty, on 8 September 1954. The Treaty was ratified by New Zealand on 19 February 1955. Under its terms, each party recognised that aggression by means of armed attack in South-East Asia or the South West Pacific against any of the Parties or against a “protocol state” (Cambodia, Laos, and South Vietnam) would endanger its own peace and safety, and agreed that it would act to meet the common danger in accordance with its constitutional processes. In the event of any other threat, the parties would consult on the measures to be taken for the common defence.

The South-East Asia Treaty Organisation, or SEATO, established under the Treaty is headed by the Council, made up of the Foreign Ministers of the signatory governments, which meet annually in members' capitals. Between meetings a body known as the Council Representatives provides continuity with representatives made up of the heads of member countries' diplomatic missions in Bangkok; New Zealand is thus represented by its Ambassador to Thailand. From time to time various expert committees and study groups are convened to give collective advice to Council Representatives. The Council also agreed in February 1955 that the Military Advisers to the Ministers should meet as a group to advise it on measures for common defence. In 1957, a Military Planning Office was established in Bangkok. From 1958 to 1960, the chief of this office was a New Zealander (the present Chief of Defence Staff). Joint military exercises in which units of the sea, land, and air forces of members countries participate are held regularly. The civil and military Secretariat has its headquarters at Bangkok.

SEATO is essentially a defensive alliance and provides a forum for military planning. New Zealand has long recognised that political stability and economic progress go hand in hand with security. SEATO has special significance because it is the only multilateral defence treaty applying to South-East Asia and the only treaty under which the United States has an obligation towards mainland South-East Asia. It is also the only treaty under which Thailand has any security guarantee. Thus the treaty helps maintain the fabric of collective defence without which the region would become the target of intensified Communist pressure. It provides a backing for the efforts of those countries of the area striving, as the Manila Treaty states, “to uphold the principles of democracy, individual liberty and the rule of law”.

Neither in concept nor in structure is SEATO fitted for a major role in spheres other than defence. Nevertheless, the nature of the challenge in South-East Asia was well recognised by the member nations in making provision in the treaty for joint action in the economic, social, and educational fields. While most of this action is taken outside the framework of SEATO, it has a useful aid programme designed to meet particular needs of the members of the treaty area. Thus SEATO has sponsored wide-ranging research efforts in the field of tropical medicine, agriculture, and engineering. A number of special SEATO professorships, post and under-graduate scholarships, research fellowships, and travelling lectureships have been established. The SEATO Graduate School of Engineering, established in Bangkok in September 1959, has now developed into an independent institution known as the Asian Institute of Technology. A programme to provide for a SEATO agricultural survey of the farming problems of the South-East Asian member governments has recently been initiated; New Zealand has contributed one expert to this programme. The New Zealand Government has also established a fund of $20,000 from which to contribute to SEATO aid programmes.

Commonwealth Arrangements—The Commonwealth defence arrangements known as ANZAM has provided a further basis for co-operation in defence matters, between Britain, Australia, and New Zealand. Unlike SEATO or ANZUS, it is not an organisation established by a formal treaty but has gradually evolved from certain general principles of closer defence co-ordination among the three countries. One of the main functions of the ANZAM machinery has been the preparation of joint plans for the defence of the area as a whole, and the co-ordination of existing plans drawn up by the respective national authorities. The three Governments, however, retain full control over their individual defence policies. ANZAM meetings are usually held in Canberra, making use of the Australian higher defence organisation with the participation of the New Zealand and United Kingdom liaison staffs.

In 1955, New Zealand transferred its wartime commitment from the Middle East to South-East Asia and agreed to contribute with Britain and Australia to a Commonwealth Strategic Reserve to be established in Malaya and Singapore. Upon its accession to independence in 1957, the Federation of Malaya concluded the Anglo-Malayan Defence Agreement, which was subsequently extended to Malaysia on that nation's formation in September 1963 and renamed the Anglo-Malaysian Defence Agreement. Under its provisions, the United Kingdom undertook to assist in the defence of Malaysia and was accorded the right to maintain forces, including a Commonwealth Strategic Reserve as agreed, for the defence of Malaysia and for the fulfilment of Commonwealth and international obligations.

The Agreement has been accepted as applying generally to Singapore upon its accession to independence in August 1965. New Zealand, together with Australia, is associated with the Anglo-Malaysian Defence Agreement by an exchange of letters placing on record the fact that the provision of the Agreement applicable to the Commonwealth Strategic Reserve, in particular the provisions dealing with the status of forces, apply in respect of New Zealand forces in the Reserve. In a statement made when tabling the relevant document in Parliament on 20 September 1963, the Prime Minister noted that “New Zealand has always given cause to believe that she would not stand idly aside in the event of an armed attack on Malaysia” and stated that “in the event of any armed threat against Malaysia the New Zealand Government would promptly consult with the Malaysian and other Governments concerned in the measures to be taken”.

New Zealand's military contribution in the area of Malaysia and Singapore has varied according to the circumstances of the time. In general, however, New Zealand has in recent years maintained in the area one infantry battalion, one RNZN frigate, and one squadron of RNZAF transport. These forces have taken part in the Malayan Emergency and in the defence of Malaysia and Singapore against Indonesian confrontation.

The British Government announced in January 1968 that its forces in South-East Asia would be finally withdrawn by the end of 1971. The New Zealand Government stated that it would continue to seek its security in concert with like-minded nations and to play its part in collective defence. Discussions among the Commonwealth countries concerned have steadily continued.

New Zealand Aid—New Zealand aid for overseas development and relief takes many forms including capital aid projects in Asia and Africa, technical assistance (experts and students), food aid, and loans. It is channelled through a number of programmes: these are multilateral, bilateral, or non-governmental.

New Zealand has for many years played an active role in aid programmes initiated by the United Nations and its specialised agencies. Contributions to voluntary programmes such as UNICEF, UNDF, the World Food Programme, UNRWA and European refugees, amounted to $788,000 for the financial year ended 31 March 1968.

The biggest bilateral aid programmes undertaken by New Zealand are those to the islands of the South West Pacific; to the Cook Islands, Niue, the Tokelau Islands and Western Samoa; and the Colombo Plan, the main vehicle for civilian aid to South and South-East Asia. Bilateral aid to the islands of the South West Pacific amounted to $3,281,000 for the year ended 31 March 1968, while aid to Asia under the Colombo Plan alone amounted to $3,058,000.

Contributions to the Asian Development Bank, some $1,622,000 in 1967, form an important adjunct to New Zealand's bilateral aid to Asia.

Other programmes in which New Zealand participated included the Special Commonwealth Aid to Africa Programme, under which over 80 Africans are studying in New Zealand and a number of New Zealand experts are working in Africa, and the Commonwealth Education Scheme, under which up to 21 Scholarships and Fellowships are offered each year. Over $325,000 was spent under these programmes in the 1967-68 financial year.

New Zealand and the Colombo Plan—New Zealand was a foundation member of the Colombo Plan which had its origin in, and takes its name from, a meeting of Commonwealth Foreign Ministers held in January 1950 in Colombo to exchange views on world problems, particularly on the economic needs of the countries of South and South-East Asia. The Colombo Plan is not a single plan but rather the aggregation of a series of separate plans drawn up and administered by each country in the region. The external assistance required and made available to help implement these plans is negotiated on a bilateral basis. What was once a Commonwealth idea has grown into a truly international co-operative effort with 24 member countries.

Up to 31 March 1968 New Zealand has made available under the Colombo Plan capital aid and technical assistance amounting to $32,142,000. The sum of $3,058,000, the highest annual total to date, was spent during the 1967-68 financial year.

Total expenditure on capital aid has amounted to $20,488,000 including $1,532,000 in the 1967-68 financial year. Major capital aid projects assisted during the year included dairy projects at Bombay and Dehra Dun in India; a milk condensory at Polunnaruwa in Ceylon; a feeder road project and a Faculty of Agriculture at Khon Kaen in Thailand; the Nam Ngum Dam in Laos; and the Indus Waters Scheme.

Up to 31 March 1968 New Zealand has spent a total of $7,591,000 on technical assistance. The number of students and trainees brought to New Zealand under the Colombo Plan awards has reached 2,432, of whom 493 were in New Zealand on 31 March 1968. The number of experts who have served in Asia under the Colombo Plan had reached 372 by the same date. The two current major technical assistance projects are the 23-member road construction team in North-East Thailand and the 15-member civilian surgical team in Vietnam.

Volunteer Service Abroad—The Council for Volunteer Service Abroad, although a non-governmental organisation, receives Government assistance in carrying out its programme of dispatching volunteer workers for assignments in many Asian and Pacific countries. As of 31 March 1968 there were 105 volunteers in the field. The Government grant during the 1967-68 year was $23,010 for administrative purposes and fare costs amounting to $16,136. The grant for 1968-69 is $28,000 plus fare costs estimated at $22,500.

Distribution of New Zealand Aid—The distribution of the total aid given by the New Zealand Government to developing countries during the two latest financial years ended 31 March is set out in the following table. Aid is shown as bilateral where the arrangements were concluded directly between New Zealand and the country or countries assisted, and multilateral where the aid was contributed to an international agency or fund. The table lists only Government aid. It does not take into account the substantial aid given privately in cash and kind through CORSO, religious missions, the Red Cross, organisations assisting lepers, the Save the Children Fund, and by other means.

General Aims—It is clear that, as New Zealand has assumed the international responsibilities appropriate to an independent country, its foreign policy has changed in emphasis and scope. The foundations of New Zealand's pre-war position in international affairs—its identification with Britain and its membership of the Commonwealth—have been modified and extended to meet the demands of an international situation greatly changed from that of 1939. As a country of predominantly European settlement, New Zealand retains its traditional loyalties to the United Kingdom and a sense of identity with Europe and of involvement in its destiny. As a Pacific power, it has sought security in friendship and formal defensive arrangements with Australia and the United States of America. New Zealand's growing involvement in the problems of the South Pacific region and its close ties with the island people are giving rise to a new recognition of the importance of the role it will have to play in this area in the future. New Zealand is in a unique position to encourage the growth of a regional consciousness in the South Pacific which is essential if the problems of the area are to be seen and tackled as a whole. At the same time it has recognised the importance of regional developments in Asia and the future security of that region, and has sought to develop its associations with Asian countries. As a country concerned with the preservation of world peace and the organisation of defence against aggression it has placed prime importance upon development of the United Nations as an agency for peaceful settlement of international disputes and for the achievement of collective security. Pending the establishment of a broadly based United Nations security system, however, New Zealand has been prepared, in respect of South-East Asia, to participate in a protective grouping concerned with the defence of a single area. Moreover, while it sees aggressive Communism as the greatest threat to individual liberty at the present time, it is well aware of the powerful stirrings of other forces—the yearning for political emancipation, the antagonism to systems of racial discrimination, the demand of underprivileged countries for a greater share of the world's prosperity, or social advancement and opportunity. New Zealand's action in the international field are designed to take account of these forces and, where possible, to assist the people of other countries in their striving for a better life. The limits of what it is able to do are those imposed by its size and capacity; its disposition is towards peaceful and friendly relations with all nations and (whatever the modifications which the needs of national security may impose) it is to that ultimate goal that its foreign policy is directed.

CONSTITUTION OF NEW ZEALAND: General—New Zealand is a monarchical State; it is also a constituent member of the Commonwealth. It is in this context that the preamble to the Royal Titles Act 1953 is significant “. . . whereas it is expedient that the style and titles at present appertaining to the Crown should be altered so as to reflect more clearly the existing relationships of the Members of the Commonwealth to one another and their recognition of the Crown as the Symbol of their free association and of the Sovereign as the Head of the Commonwealth ...”

Constitutional elements besides that of the titular head, the Monarch, can be reviewed under the categories of legislative authority, the executive and administrative structure, and the judiciary. This division is a convenient one, even though there is no absolute line of demarcation between the three phases (e.g., legislation may and often does arise through the day-to-day experience of those responsible for administration and execution of policy, or through difficulties or anomalies made explicit in the course of dispensing justice or interpreting law). Conversely, in the exercise of the powers and functions of industrial and other tribunals, commissions, authorities, etc., both administrative and judicial elements may be discerned.

THE MONARCH—The New Zealand Parliament in the Royal Titles Act 1953 gave its assent to the use of the Royal style and titles as follows: Elizabeth the Second, by the Grace of God of the United Kingdom, New Zealand, and Her Other Realms and Territories Queen, Head of the Commonwealth, Defender of the Faith.

While the seat of the Monarch is normally in the United Kingdom, the Queen is represented in New Zealand by the Governor-General appointed by the Crown on the advice of Her New Zealand Ministers. The Governor-General has, however, an official existence, even in the country to which he has been appointed, only in the absence of the Queen from that country. In the island territories the Crown is represented by the Resident Commissioner or Resident Agent. These officials carry out the constitutional functions of the Crown, but they also possess in varying degrees certain executive and legislative powers, being responsible to the New Zealand Government for the administration and good government of the islands concerned.

Many powers held by the Monarch (or her representative) comprise but the means of giving effect to the public will. In New Zealand the Governor-General acts on the advice of the Ministers, which cannot constitutionally be ignored. Despite the long-term trend for powers to be assigned directly to Ministers without any necessity for vice-regal consultation, there are still many phases of Government which require Royal participation.

The Queen (in her absence the Governor-General) gives consent or approval prior to a Minister taking office or the formation of a Ministry; summons, prorogues, and dissolves Parliament; delivers the Speech from the Throne at the opening of a session; gives the Royal Assent to measures which have passed all stages in the House of Representatives, without which they have not the force of laws; makes appointments to most important State offices; confers knighthoods and other honours, etc.; and also provides that background of stability, continuity, and experience in many facets of government which is so desirable whenever there are sweeping changes in the dominance of political parties.

Besides those duties associated with the constitutional role, the Royal personage or representative makes an important contribution to the ceremonial life of the nation. This was particularly well illustrated during the sojourn of the Royal visitors in New Zealand in 1953-54 and in 1969. Both as the symbol of the nation and in virtue of her identification with the life and interests of her people, the Queen becomes the focus for all State occasions, as does the Governor-General in her absence.

LEGISLATIVE AUTHORITY—The supreme law-making body with power to legislate for the whole country is the General Assembly, which now consists of the Governor-General and the House of Representatives, the former Legislative Council having been abolished since the close of 1950.

The powers of Parliament to make laws are legally untrammelled. This was not always so, for prior to the adoption by New Zealand to the Statute of Westminster in 1947 there was incapacity to make laws on certain matters which conflicted with United Kingdom statutes extending to New Zealand. There was also some doubt as to New Zealand's power to make laws possessing extra-territorial effect.

Although they do not limit the legal powers of Parliament as stated earlier, the provisions of the Electoral Act 1956 creating reserved sections in that Act are of great constitutional significance. The Act provides that certain of its sections may not be repealed except by a 75 percent majority of the House of Representatives or following a referendum. These sections are those relating to:

This innovation is not legally effective in the sense that it does not prevent a subsequent Parliament from repealing it, since one Parliament cannot bind its successors. It should not be thought, however, that the provision is a mere gesture. It records the unanimous agreement of both parties represented in Parliament that certain provisions have a fundamental character in the system of Government and should not be altered at the whim of a bare majority. Considered in this light the provision creating reserved sections introduces something in the nature of a formal convention which could not constitutionally be ignored.

While the law-making function is the prerogative of Parliament, it must be remembered that, as in most democracies, laws are passed because of their acceptability to the majority party in Parliament—i.e., the Government party. Furthermore the initial acceptance will have probably been made in the deliberations of Cabinet.

With the increasing range and complexity of the statutory field, the multifarious concerns of a modern twentieth century government, and the necessity of conserving time for consideration of more important issues, much of the detailed procedural steps and other amplifying matter must become the subject of regulations made by Order in Council under the authority of some statute, rather than being incorporated in the statute itself. The power to make such regulations lies with the Executive Council which comprises those senior members of the majority party in Parliament who are appointed thereto, together with the Governor-General. Regulations, though originating in Cabinet and becoming effective in the formal proceedings of the Executive Council, rest fundamentally on the will of Parliament as a whole and are now subject to its supervisory jurisdiction. A general provision contained in the Regulations Amendment Act 1962 requires all such regulations to be laid before Parliament, though most empowering Acts contained a similar provision prior to that date. An amendment to the Standing Orders of the House of Representatives, also passed in 1962, enables the House or any member thereof to refer any regulation to the Statutes Revision Committee, a Select Committee of the House, which is empowered to consider the regulation and to determine whether the special attention of the House should be drawn to it on any of the following grounds: (a) That it trespasses unduly on personal rights and liberties: (b) That it appears to make some unusual or unexpected use of the powers conferred by the statute under which it is made: (c) That for any special reason its form or purport calls for elucidation.

Meeting of Parliament—Parliament is summoned, prorogued, or dissolved by Proclamation issued by the Governor-General. A session is that period between the summoning of Parliament and its prorogation. Its length varies, but it usually occupies the months from June to November. When Parliament is prorogued all the business on hand lapses, and if this is to be proceeded with in the next session it must be re-introduced.

The course of a session may be interrupted by an adjournment.

Parliamentary Privileges—While in session these include freedom of speech and freedom from arrest in civil cases, and also the right to engage in secret debate, if required, etc.

The Party System—The two main political parties represented in Parliament are National and Labour. A third party—Social Credit—obtained a seat for the first time at the 1966 General Election. At any general election these parties, together with any other political parties which may be desirous of so doing and also those candidates standing as independents, state their respective policies before the electors. Each party normally puts forward one candidate for each of the 80 electorates into which the country is divided. The party which wins the majority of seats, although not necessarily the majority of votes, at the general election forms the Government. The leader of the elected members of the majority party becomes the Prime Minister, who makes Ministerial appointments from elected members of his party. The leader of the minority party in Parliament becomes the Leader of the Opposition. The effectiveness of the party system relies largely on the general agreement that the majority party is to govern and the minority is to criticise—so that there is ample time allocated for debate on Government measures in Parliament. While party control is exercised by national and local organisations outside Parliament, within the latter it is maintained by the respective party Whips.

Parliamentary Procedure—The House of Representatives has its Standing Orders, which govern its procedure and which are administered by Mr Speaker in the exercise of his control of the House. Mr Speaker's rulings on interpretation of the Standing Orders are followed in a similar manner to judicial decisions in the ordinary Courts of law. The main means by which Parliament does its work is through the system of debate and committees. The election of a Speaker is the first business of a new House after the members have been sworn. A Chairman of Committees is elected as soon afterwards as is convenient. Twenty members, inclusive of the Speaker, constitute a quorum.

Parliamentary Functions and Control—The Parliament controls the Government in power in the last resort by its power to pass a resolution of no confidence in the Government, or to reject a proposal which the Government considers so necessary that it is made a matter of confidence, and thus force the Government to resign.

Financial control is exercised by the fact that expenditure of public money must be authorised by the House of Representatives in the form of an Appropriation Act, which authorises or grants money to the Government for the purposes approved. The authority for the raising of revenue by taxation or borrowing must also be given by Parliament. The functions of Parliament are, of course, the passing of legislation and taking action to make available finances or funds as required for State expenditure, while it also controls the Government. Legislation can be initiated by any member of Parliament, but in practice almost all Bills are introduced by the Government in power as a result of policy taken in Cabinet, sometimes at the instigation of those Government Departments which will be responsible for their administration when the Bills become law. The chief exceptions are private Bills, which are designed for the particular interest or benefit of a person or body of persons, whether incorporated or not, and local Bills which relate largely to matters of local (as distinct from central) government business. The process of passing a public Bill is as follows: it receives a formal first reading on introduction, is then printed, and after some time it is given a second reading as a result of a debate on its general merits or principles. It may then be referred to one of the Select Committees, for consideration in the closest detail, before being considered by the whole House sitting in Committee. During these stages members have opportunities to suggest amendments which may be incorporated in the Bill if the majority so decide. The Bill is then reported to the House, and later read a third time; debate rarely occurs at these stages. The final stage is to send the Bill to the Governor-General for the Royal Assent and, unless provision is made for commencement on another date, it then becomes law. Bills providing for receipt of moneys, such as the Finance Bill, and expenditure of moneys, such as the Appropriation Bill, are introduced only by a Minister of the Crown, normally the Minister of Finance. No Bill involving an appropriation of public moneys or affecting the rights of the Crown can be passed without the recommendation of the Crown, which is given by Message from the Governor-General.

Duration of Parliaments—Quinquennial Parliaments, instituted under the Constitution Act, were abolished by the Triennial Parliaments Act 1879, which fixed the term at three years. General elections have been held at three-yearly intervals since 1881, with a few exceptions. The term of the nineteenth Parliament was during the First World War extended to five years by special legislation, and that of the twenty-fourth (1931-35) and subsequent Parliaments to four years under the Electoral Amendment Act 1934. By the Electoral Amendment Act 1937 the three-year term was restored, but on account of war conditions the term of the twenty-sixth Parliament was extended to four years by the Prolongation of Parliament Act 1941. The Prolongation of Parliament Act 1942 extended the term still further to one year from the termination of the war, but with a proviso for a motion to be moved in the House of Representatives each year after the year 1942 either approving the continuation of the House or fixing an earlier date for its expiry. During the 1943 session a motion in favour of dissolution was carried, and Parliament was dissolved on 30 August 1943. Since then the duration of Parliaments has been of three years, with the exception that the twenty-ninth Parliament was dissolved after the expiration of approximately 20 months. The three-year limit was re-enacted in the Electoral Act 1956, this being one of the reserved provisions referred to earlier. A referendum on 23 September 1967 favoured the continuation of terms of three years.

Number of Representatives—From the next election there will be 84 electorates (80 European and four Maori) returning members to the House of Representatives. The number was originally fixed by the Constitution Act as not more than 42 and not less than 24, and the first Parliament called together in 1854 consisted of 40 members. Legislation passed in 1858 fixed the number of European members at 41; in 1860, at 53; in 1862, at 57; in 1865, at 70; in 1867, at 72; in 1870, at 74; in 1875, at 84; in 1881, at 91; in 1887, at 70; and in 1900, at 76. Since 1867 there have been four Maori representatives, and provision for this number was retained in the Electoral Act 1956. In 1954 the boundaries of the Maori electoral districts, which had remained unaltered since 1867, were changed by Proclamation so as to give a greater degree of equality of population among the four districts (in effect the Southern Maori Electoral District now includes a considerable area of the North Island). The Electoral Amendment Act 1965 fixed the number of European electorates in the South Island at 25 (an increase of one) and provided that the number of European electorates in the North Island shall be ascertained by the Representation Commission after each quinquennial census of population on the basis of the quota fixed for the South Island. In 1967 the Electoral Boundaries Commission considered the results of the 1966 census and fixed the number of electorates in the North Island at 55 (an increase of three).

Qualifications of Members—Under the Electoral Act 1956 every registered elector of either sex, but no other person, is qualified to be a parliamentary candidate. It is provided, however, that a person shall not be so elected who is disqualified as an elector under any of the provisions of the Act (see under “Franchise” later); or is an undischarged bankrupt; or is a contractor to the Public Service of New Zealand to whom any public money above the sum of $400 is payable, directly or indirectly (but not as a member of a registered company or incorporated body), in any one financial year. Although women have had the vote since 1893, they were not eligible as parliamentary candidates until the passing of the Women's Parliamentary Rights Act 1919. Prior to 1936 a public servant was prohibited from being elected, but this prohibition was removed by the Political Disabilities Removal Act 1936. The present law is that if a public servant is elected to Parliament he vacates his office forthwith and he cannot resume employment in the Public Service within 12 months of ceasing to be a member of Parliament unless he had previously been a public servant for at least five years.

Salaries, etc.—Section 27 of the Civil List Act 1950 provides that on the recommendation of a Royal Commission the Governor-General may from time to time, by Order in Council, fix the salaries and allowances to be paid to the Prime Minister and other Ministers of the Crown or members of the Executive Council, to Parliamentary Under-Secretaries, and to the Speaker and Chairman of Committees and other members of the House of Representatives,and that a Royal Commission shall be appointed for this purpose within three months after the date of every general election of members of Parliament. The 1967 Royal Commission has been set up but in view of existing economic conditions the time for submission of its report was extended until 30 April 1968.

In accordance with the recommendations contained in the report (issued in 1968) of the Royal Commission upon Parliamentary Salaries and Allowances, the Prime Minister's salary, as from 1 April 1968 was increased to $12,400 with a tax-free allowance of $3,500 for the expenses of his office and a Ministerial residence. In addition, while travelling on official business he receives $12 per day to meet expenses, and by virtue of his office is entitled to free cars, secretarial assistance, and free postage. The Deputy Prime Minister's salary is $9,150 with a tax-free expense allowance of $1,400. The salary of each other Minister holding a portfolio is $8,600 with a tax-free expense allowance of $1,300 and that of each Minister without portfolio $7,000 with $1,100 tax-free allowance. Where the office of Minister of External Affairs is held by a Minister other than the Prime Minister the expense allowance is increased by $450. Any Minister not occupying a Ministerial residence receives an allowance in lieu at the rate of $600 a year. This allowance, or the assessed value of the residence where one is provided, is subject to income tax. Ministers also receive an allowance of $12 per day when travelling on official business within New Zealand, and in addition are entitled to free cars, secretarial assistance, and free postage. For Parliamentary Under-Secretaries the rate of salary is $6,450, with the same house provision or allowances, and travel allowance while on official business, as for Ministers; an expense allowance of $1,100 is also payable. After the general election of November 1954 no appointments were made until 1960, when two Parliamentary Under-Secretaries were appointed. In 1967 there was only one Parliamentary Under-Secretary.

The basic salary paid to members of the House of Representatives is now $4,650 a year. Members are also paid an allowance to provide for expenses incurred in connection with parliamentary duties ranging from $900 to $1,450 a year subject to the classification of their electorates by the Representation Commission into the five classes of (a) a wholly urban electorate, or (b) a substantially urban electorate, or (c) a partially urban and partially rural electorate, or (d) an ordinarily rural electorate, or (e) a predominantly rural electorate. An additional expense allowance of $300 a year is paid to the member for Southern Maori, and an allowance of $150 to the members representing the other three Maori Electorates. A sessional accommodation allowance is paid at the rate of $2.25 for each day and $6 for each night on which a member is in Wellington and attends the sittings of Parliament, or of a Select Committee of Parliament of which he is a member. The sessional accommodation allowance is not payable to any member representing a Wellington urban electorate. (For full details see Parliamentary Salaries and Allowances Order 1968.) In addition to the salary and allowances, members are entitled to certain privileges in respect of air and other forms of travel, a stamp allowance of $14 a month, and certain other concessions regarding telegrams and telephone services. If a member is defeated at an election he continues to receive salary to the end of the month following the month in which the election took place. A similar payment is made in the case of the death of a member leaving a widow or dependent children.

Both the Speaker and Chairman of Committees hold office until a dissolution and receive payment until the first meeting of a new Parliament. The Speaker's remuneration is $7,350 a year in addition to which he receives an expense allowance of $1,000 plus normal member's allowance a year and residential quarters in Parliament House. The salary of the Chairman of Committees is $5,950 a year. In addition, he receives the electoral and sessional allowances appropriate to his electorate, increased by the sum of $600, and is provided with sessional accommodation.

The Leader of the Opposition is paid a salary of $7,350 a year with an expense allowance of $1,300 a year. In addition, a secretary, an assistant secretary, and a typist are provided by the State, and an allowance of $1,100 is payable for travel outside his electorate. His stamp allowance is $35 per month. In addition, the Leader of the Opposition is entitled to an official residence on the same basis as a Minister, or to an allowance of $600 a year in lieu thereof. The Deputy Leader of the Opposition receives a salary of $5,200 a year in addition to his appropriate electorate allowance and the sessional accommodation allowance where this is payable.

The Chief Whip of each party receives a salary of $5,050 a year, and the Junior Whip of each party receives a salary of $4,850 a year, together with the appropriate expense allowance in each case in accordance with the classification of his electorate and where applicable accommodation allowance.

Former Prime Ministers receive an annual payment of $400 for each full year in office, with a maximum of $2,000 a year, after retirement, defeat at the polls, or when a member only. This is subject to a two-year minimum period having been served as Prime Minister.

Part V of the Superannuation Act 1947, as amended by the Superannuation Amendment Act 1955, consolidated in 1956 and amended in 1961, introduced a compulsory contributory superannuation scheme for members of the House of Representatives. The scheme now provides that a retiring allowance shall be payable to a member after nine year's service and the attainment of 50 years of age, and shall be calculated at the rate of one thirty-second of the basic salary for a member as at the date of his ceasing to be a member, for each year of service with a maximum of two-thirds of that basic salary, or alternatively the member may elect to take a variable retiring allowance so as to secure a level income, or he may elect to receive a refund of his contributions. The annual contribution is 10 percent of an ordinary member's salary, and the Government subsidises the fund by an equal amount. In the case of a male member dying and leaving a widow surviving she becomes entitled during her widowhood to receive an annuity of half of the retiring allowance to which her husband would have been entitled had he retired aged 50 years at the time of his death, or $260 a year, whichever is the greater.

ADMINISTRATION AND EXECUTIVE RESPONSIBILITY—After the election of a new Parliament, it is the responsibility of the leader of the party, which is most likely to secure and retain the support of the majority of members in the House, to form a Government. Although procedures for the selection of new Ministers have varied between the two principal parties, the Prime Minister has the final responsibility for allocating portfolios. A portfolio comprises a specific field of Government activity—for instance all matters relating to education will be allocated to one Minister who is henceforth known as the Minister of Education.

He may also have other portfolios and the supervision of one or more Government Departments in which the activities carried out, though important, either do not rank as portfolios or are subsidiary aspects of the field—in these cases the Minister's responsibility will extend to being in charge of the named Department. One or other of the appointed Ministers in this way is responsible for the direction of activities and executive acts of each of the Government Departments and offices, etc., embracing the entire range of State activities. Occasionally a Minister is appointed without portfolio.

Executive Council—In the legal sense those members of Parliament who have been appointed Ministers, together with the Governor-General, comprise the Executive Council, The powers, duties, and responsibilities of the Governor-General and the Executive Council under the present system of responsible government are set out in Royal Letters Patent and Instructions thereunder of 11 May 1917, published in the New Zealand Gazette of 24 April 1919. The Royal Powers Act 1953 provides that the statutory powers conferred on the Governor-General may be exercised either by Her Majesty the Queen in person or by the Governor-General. In the execution of the powers and authorities vested in him the Governor-General must be guided by the advice of the Executive Council; but, if in any case he sees sufficient cause to dissent from the opinion of the Council, he may act in the exercise of his powers and authorities in opposition to the opinion of the Council, reporting the matter to Her Majesty without delay, with the reasons for his so acting.

In any such case any member of the Executive Council may require that there be recorded in the minutes of the Council the grounds of any advice or opinion that he may give upon the question.

A point of interest is that the Civil List Act 1950, in section 6, provided that no person shall be appointed a Minister or a member of the Executive Council unless he is a member of Parliament and that a person who ceases to be a member of Parliament cannot continue to be a Minister or a member of the Executive Council for more than 21 days. This gave statutory recognition for the first time to what had long been the convention.

At August 1968 the Executive Council consisted of 17 members in addition to the Governor-General. Two members, exclusive of His Excellency or the presiding member, constitute a quorum.

Under the Civil List Act 1950 and its amendments, His Excellency the Governor-General receives a salary of $18,000, and an allowance of $11,000 a year for the salaries and expenses of his personal establishment, plus all expenditure incurred in respect of the transport to and from New Zealand and the travel within or outside New Zealand of the Governor-General and his family and staff.

Cabinet—There is a close relationship between the Executive Council and the Cabinet. There are however, significant differences in membership and functions.

The Council consists of all Ministers and is presided over by the Governor-General. Cabinet may or may not comprise all the Ministers, including a Minister without portfolio; the Governor-General is not a member. The Council is one of the instruments for giving the imprint of legal form to policy determined by Cabinet which had been recognised only by constitutional convention until legislative reference to Cabinet was made in the Parliamentary Commissioner (Ombudsman) Act 1962.

Cabinet has been described as the directing body of national policy whose nature is more easily explained by analogy than by definition. It determines the policy to be submitted to Parliament. In it is vested the supreme control of national policy within the limits of Parliamentary approval. It co-ordinates and delineates the activities of the several Departments of State.

The juridical acts which are necessary to give legal force to certain of the decisions of Cabinet are taken by others—the Crown, the Executive Council, a Minister of the Crown, a Statutory Commission and the like. The preliminary review of proposed policy or of current administrative developments, which takes place in the informal atmosphere of Cabinet meetings, implies both deliberative or selective and administrative procedures on the part of this body.

Cabinet discussions are informal and confidential, anonymity being maintained as to the individual advocacy or opposition to particular proposals. The Cabinet system enables general agreement to be reached on any line of action proposed by either an individual Minister or by the Government as a whole. As a result the Executive Council confirmation can proceed smoothly and expeditiously. In Parliament a Minister can be confident that his legislative or other proposals will have the unqualified support of the Government no matter what divergences of opinion may have been apparent before general agreement was reached in Cabinet. A consistent and agreed course of action on any particular issue can be determined. The work of Cabinet thus exemplifies the concept of the collective responsibility of the Government.

Certain questions are considered by committees of Cabinet, the membership of which includes those Ministers primarily concerned with the subject matters. Authority to determine some issues may be delegated to a Cabinet committee by Cabinet. In other cases a committee may be called upon to study a particular question and submit its recommendations to Cabinet for determination. Some Cabinet committees are established on a permanent basis for the consideration of matters arising in broad fields of Government policy. Examples are the Cabinet Economic Committee and the Cabinet Works Committee. Several of these committees are supported by inter-departmental committees of officials. Other committees are of a temporary nature; they are established to consider particular problems and after having studied the question in detail, normally with appropriate officials advising, the committee reports back to Cabinet with its recommendations; and after the final decision has been made by Cabinet, the committee's work is completed.

The Cabinet Secretariat is responsible for the servicing of Cabinet and its committees to ensure their smooth functioning. It is its purpose also to assist in the co-ordination and review of the work of the Departments of State.

Government Departments—The Minister as the political head of a Department of State may in fact have several Departments under his control. There are, however, some 40 different Departments with separate functions in New Zealand. Each of these have a permanent head who is responsible for the work and administration of the Department. He is of course responsible to the Minister in charge of the Department, while he also acts as adviser to the Minister on all matters within his appointed competence. Besides ensuring that the ministerial policy and directions communicated to him are effectively put into practice, his functions as the adviser include assessing the consequences of any executive action resulting from his departmental activity, evaluating the merits and demerits, whether political, social, or financial, of various modes of action, and making suggestions for improvements and for new policy measures as derived from departmental experience in the day-to-day execution of policy.

Departments can be broadly classified according to the administrative or regulatory, developmental, or social nature of their activities. Within the first group are the servicing subgroup, such as the Legislative, Prime Minister's, External Affairs, Printing Office, Law Drafting, Valuation, Statistics, and Audit; the finance subgroup—Treasury, Customs, Inland Revenue; the regulatory subgroup—State Services Commission, Internal Affairs, Labour, Marine; the defence and law and order subgroup—Ministry of Defence, Justice, Crown Law, and Police; the publicity and research subgroup—Tourist and Publicity, Scientific and Industrial Research.

In the second group are the transport and communications subgroup, such as Ministry of Transport, Post Office, and Railways; the developmental—Ministry of Works, Agriculture, Lands and Survey, Forest Service, Mines, Electricity, Maori and Island Affairs, and Industries and Commerce; the commercial—Public Trust, Government Life Insurance, State Advances Corporation, and State Insurance.

The third group comprises the Education, Health, and Social Security Departments.

This broad division serves merely to indicate the field of the dominant activity or purpose of the particular Department. Most Departments have servicing, informative, and regulatory functions, and many are equally regulatory and developmental in nature.

In addition to the system of direct administration in the form of Government Departments, there are other activities over which the State exercises some ultimate measure of control or ownership, though divorced in varying degrees from immediate supervision. The Reserve Bank of New Zealand (the central bank), and one trading bank, are entirely State-owned, although the actual administration is quite independent, subject in the case of the Reserve Bank to the proviso that it must give effect to the monetary policy of the Government, as communicated to the bank by the Minister of Finance, and to any resolution of Parliament in respect of Government monetary policy.

Further instances of this principle are shown by the National Airways Corporation, which, although owned by the State, is administratively self-contained, and by the Tourist Hotel Corporation. In certain other avenues the type of administration is in between the normal departmental form and that evident in the corporation type; of such is the National Roads Board, which, though determining policy to a large degree, yet makes use of departmental administrative structures for implementation of policy.

Some administrative organisations have also quasi-judicial functions. Examples of this class are the Price Tribunal, Transport Charges Authority, Licensing Control Commission, and Local Government Commission.

JUDICIARY—The hierarchy of Courts in New Zealand comprises the Court of Appeal, the Supreme Court, and the Magistrates' Court. Apart from these Courts of general jurisdiction there are other Courts dealing with specific fields. In the latter category are the Court of Arbitration concerned with awards and general orders governing wage determination and conditions of employment in industry; the Compensation Court dealing with workers' compensation. For further details refer to Section 8 (Justice) of this issue.

ELECTORAL PROVISIONS—The law on these matters is now contained in the Electoral Act 1956. Following each population census, which is normally taken every five years, the boundaries of European electorates are revised. In addition, there are four Maori electoral districts, three in the North Island and one covering a portion of the North Island together with the whole of the South Island, where the Maori population is comparatively small. The Governor-General may at any time by Proclamation alter the boundaries of the Maori electoral districts, and, as in the case of European electoral districts, any alterations are to come into force at the expiry of the Parliament existing when the Proclamation is issued.

The Government Statistician is required to supply population figures to the Surveyor-General as soon as possible after the census. The population used as the basis in obtaining the quota for each European electoral district is defined in section 2 (1) of the Electoral Act 1956.

The term “European population” means total population with the following exceptions:

After the population figures are supplied by the Government Statistician it is then the responsibility of the Representation Commission to define new electoral districts for Europeans. The Commission is constituted by virtue of section 15 of the Electoral Act 1956 and comprises seven members. Four of these, the Surveyor-General, the Government Statistician, the Chief Electoral Officer, and the Director-General of the Post Office, are official members. Two are unofficial members, being persons nominated by the House of Representatives, one nominated to represent the Government, and one to represent the Opposition. The seventh member is appointed, on the nomination of the official and unofficial members of the Commission or a majority of them, to be the Chairman of the Commission. The Chairman and unofficial members cease to be members on the date on which the first periodical census is taken after the date of their appointment.

The European population of the South Island is divided by 25 and the quotient so obtained is the quota for the South Island. Then the European population of the North Island is divided by the quota for the South Island, and the quotient so obtained is the number of European electoral districts in the North Island. The quota for North Island is obtained by dividing the European population of that Island by the number of electoral districts in that Island. In applying the quota the Commission may make an allowance by way of addition or subtraction of 5 percent of the quota to enable districts to be adjusted to meet considerations of topography, community of interest, communications, and existing electoral boundaries.

When the boundaries have been provisionally determined, maps are prepared illustrating the proposed electoral districts, and descriptions of each electoral district are published in the New Zealand Gazette. A time limit of one month is given thereafter in which objections to the proposed boundaries may be lodged. These objections are then considered by the Representation Commission and a final decision reached on boundaries which then become the new electoral districts.

In addition to determining new European electoral districts the Representation Commission is also charged with the responsibility of classifying them for the purpose of allowances as provided by the current Parliamentary Salaries and Allowances Order. Under this order provision is made for an allowance based on the size, topography, and transport facilities of the electorate, the nature of its roads, the distribution of its population, and all other considerations that the Commission deems relevant.

The Act provides that all general elections and by-elections shall be held on a Saturday and for both European and Maori elections to be held on the same day. Polling hours in all electorates are from 9 a.m. to 7 p.m.

The Act provides that, if at any time Parliament is dissolved before it has been two years in existence, the main and supplementary rolls used in the previous general election, together with a further supplementary roll, may be used if in the opinion of the Chief Electoral Officer it is impracticable to print new main rolls. The same rolls, together with a further supplementary roll, are to be used for any by-election occurring before the next following general election.

Provision is made for the voting at elections and licensing polls by servicemen serving overseas, who are or will be of, or over the age of, 21 years before the date of the election or poll, whether or not registered as electors of any electoral district. Each such serviceman shall be qualified to vote as an elector of the electoral district in which he last resided before he left New Zealand.

FRANCHISE—Since the abolition of plural voting in 1889 and the introduction of women's suffrage in 1893, every person 21 years of age or over (with certain obvious exceptions) has had the right to exercise one vote and one vote only in the election of members of the House of Representatives. Some of the more important provisions of the Electoral Act 1956 are now given.

Qualification for Registration as Elector—To be qualified for registration as a parliamentary elector in New Zealand a person must have attained the age of 21 years and must (a) be a British subject or Irish citizen, (b) be ordinarily resident in New Zealand, (c) at some period have resided continuously in New Zealand for at least a year, and (d) except in special cases have resided continuously for three months or more in the electoral district in respect of which application for registration is made, and not have subsequently resided for three months or more in any other electoral district.

The Act defines what is meant by the term “ordinarily resident”. To be ordinarily resident in New Zealand, a person must be or have been actually resident in New Zealand with the intention of residing there indefinitely. If he is absent from New Zealand he must have had, even since he left New Zealand, an intention to return to reside there indefinitely, and (except in the case of a public servant or the wife or husband of a public servant) must not have been absent from New Zealand for more than three years. Broadly speaking, the qualifications restrict the right to vote to permanent residents, the test laid down being similar to the legal concept of domicile.

The following persons are disqualified from registration as electors: (a) Those in respect of whom reception orders under the Mental Health Act 1911 are in force, (b) those detained pursuant to a conviction in any penal institution, and (c) those whose names are on the Corrupt Practices List for any district.

These qualifications and disqualifications apply alike to Maoris and Europeans.

Registration of Electors—A system of compulsory registration of electors has been in operation in respect of Europeans since 1924 and was introduced in respect of Maoris in 1948. Every person qualified to be registered as an elector of any district must, if he is in New Zealand, apply for registration within one month after the date on which he first becomes qualified to be registered as an elector. He must also apply for registration within three months after the issue of every Proclamation proclaiming the names and boundaries of electoral districts or within such later period as may be provided by Order in Council. Qualified electors who are outside New Zealand may apply for registration if they wish.

A European is not entitled to be registered as an elector of a Maori district and a Maori (other than a half-caste) is not entitled to be registered as an elector of a European district. A half-caste Maori may choose to be registered either for a Maori or European district, and special rules are laid down to govern a change from one to the other.

Voting at Elections—Voting at parliamentary elections is by secret ballot, a method which was first introduced in New Zealand in 1870. Recognition of the fundamental character which the secret ballot has attained in New Zealand was given in the Electoral Act 1956, which included the section providing for this method of voting among the reserved sections which may be repealed only by a 75 percent majority vote of all the members of the House of Representatives or following a referendum.

In general, only those persons whose names are lawfully on the main and supplementary rolls of electors compiled prior to an election may vote at that election. The following classes of persons whose names are not on the roll are, however, entitled to vote:

Special Voters—A vote is normally cast by the elector at a polling booth within his district. An elector may, however, vote as a “special voter”, either at a polling booth outside his district or by post, in the following cases:

These latter conditions replace the former classes of absentee, postal and declaration voters, including servicemen outside New Zealand.

LOCAL GOVERNMENT—In 1876, following the abolition of the provinces, local government assumed the form it still basically retains. The Counties Act of 1876 divided the country into 63 counties, with provision for administration by elective councils having powers considerably less than those enjoyed by the Provincial Councils. In the same year the Municipal Corporations Act provided for the incorporation of the 36 boroughs then in existence and for the creation of new boroughs.

A description of the development of counties, boroughs, and town districts follows.

Counties—Counties are now constituted under the Counties Act 1956, which consolidated legislation relating to counties and road districts. In general, the county organisation makes provision for the primary needs of a scattered population within a large area. With increasing settlement the original 63 counties were gradually subdivided until in 1920 the maximum of 129 was reached, although the number of councils formed and actively functioning never exceeded 126. The number of counties has been reduced by amalgamations and mergers by the Local Government Commission. At October 1968 there were 108 counties constituted, of which 107 were actively functioning, Fiord being a sparsely populated county in which the Counties Act is not wholly in force. The Local Government Commission operates under the Local Government Commission Act 1967.

County councils may, under the provisions of the Counties Act 1956, declare areas within counties to be county towns. To qualify, the areas concerned must have a population of at least 200, with an average density of not less than one person to the acre or not less than 60 houses with an average density of not less than one house to three acres. After the constitution of a county town the county council is required to appoint a county town committee of not less than three nor more than seven members, to advise it on the administration of the county town. Membership is restricted to electors having a ratepayer's or residential qualification in respect of property or an address within the county town, or members of the council for the riding in which the county town is sited.

The Counties Amendment Act 1968 contains provisions for county councils to declare an existing county town, or a borough or town district which is abolished and added to a county, to be a county borough. The minimum population stipulated for a county borough is 1,500.

Boroughs—Dealing with the needs of a concentrated population, the borough organisation is concerned with a wide range of functions of a purely local nature. With the growth and centralisation of population the number of boroughs, despite numerous amalgamations of adjacent boroughs, steadily increased until 1955 when the total was 146. In October 1968 the total was 139.

Under the Municipal Corporations Act 1954 for the constitution of a borough there must be a population of at least 1,500 with an average density of population of at least one person per acre. A borough containing a population of 20,000 or more may be proclaimed a city, although the corporation remains unaltered.

Town Districts—The town district represents a form of local government intermediate between the county and the borough. It implies a certain concentration of population and the presence of interests which, from their purely local nature, cannot be satisfactorily met by the county organisation. In its early stages a town district usually remained subject to county control, although such control was practically confined to the main and county roads in the town district; in such circumstances it was known as a dependent town district. The Town Boards Amendment Act 1908 enabled town districts on reaching a population of more than 500 to become independent. On attaining its independence a town district becomes in all respects a separate entity, and, apart from its smaller population, is not essentially different from a borough. The constitution and powers of town districts have been brought into closer relationship to boroughs over the years, and independent town districts are now constituted under the Municipal Corporations Act 1954. The Act required that the area should not be more than 2 square miles, within which no two points are more than 4 miles distant and with a density of population of not less than one person to the acre. No new dependent town districts can be constituted. The number of town districts in October 1968 was 16 (10 independent and 6 dependent).

General Powers—Local authorities in New Zealand derive their powers from the Acts under which they are constituted, and also from special empowering Acts. In addition to legislation providing for particular types of local authority or for individual local authorities, there are several statutory measures which are more or less applicable to all local authorities, such as the Local Elections and Polls Act 1966 and the Local Authorities Loans Act 1956. For most harbour boards, there is in addition to the general Harbours Act a special Act for each board, which is subordinate to the general Act. Certain types of local authority—urban drainage boards, transport boards, the Auckland Regional Authority, the Auckland Harbour Bridge Authority, the Christchurch-Lyttelton Road Tunnel Authority, and the Waikato Valley Authority—derive their principal powers from special constituting Acts.

Local authorities have general powers of entering into contracts for any of the purposes for which they are constituted; of selling and leasing land; and of taking or purchasing any land which may be necessary or convenient for any public work.

Number of Local Authorities—The number of local authorities actively functioning at 12 October 1968 was 677 made up as follows: County councils, 107, borough (including city) councils, 139; town councils (independent), 10; town councils (dependent), 6; road board, 1; regional authority, 1; river boards (2 boards also have the power of land-drainage boards), 8; catchment boards, 13; catchment commissions, 3; land-drainage boards, 34; electric power boards, 39; water-supply boards, 2; urban drainage boards, 4; transport board, 1; local railway board, 1; electric power and gas boards, 2; independent milk boards, 15; nassella tussock boards, 2; harbour bridge authority, 1; road tunnel authority, 1; valley authority, 1; plantation board, 1; underground water authorities, 3; pest destruction boards (separately elected), 171; independent fire boards, 62; independent harbour boards, 18; and hospital boards, 31. Borough and county councils also function as fire authorities in 190 cases, as harbour boards in 9 cases, and as county pest destruction boards in 42 cases. In addition, there were 21 district councils of the National Roads Board constituted under the National Roads Act 1954. Although these district roads councils are not local authorities in the strict sense of the term they are intimately connected with certain aspects of local government providing an advisory service to the National Roads Board concerning the roading needs and the allocation of national roading funds within their respective districts.

Administratively, boroughs and independent town districts, which are contained within the areas of the several counties, are regarded as separate entities. From an administrative point of view, therefore, the fundamental districts are counties, boroughs, and independent town districts. Upon this foundation a considerable superstructure of districts of other types has been erected. These overlapping districts may be divided into two broad classes, viz: (1) Districts formed from parts of counties, e.g., road districts; and (2) those which are composed of a group of adjacent districts of other types united for a common purpose, e.g., electric power districts.

Local Government Commission—The Local Government Commission Act 1967, which replaced the Local Government Commission Act 1961, set up a revised Local Government Commission which is a permanent institution deemed to be a Commission of Inquiry under the Commissions of Inquiry Act 1908.

The Act provides that the Commission shall consist of a Chairman with knowledge of local Government, one member with a special knowledge of finance and economics, and another member with a special knowledge of administration.

The functions of the Commission are to carry out investigations, prepare reorganisation schemes, and make recommendations and reports for the purpose of ensuring that the system of local government in any locality will best provide for the needs and continued development of the locality, that local authorities have such district boundaries and such functions and powers as will enable them to provide most effectively and economically essential or desirable local government services and facilities, that local authorities shall have such resources as will enable them to engage adequate services and to obtain and operate adequate technical facilities, plant, and equipment, and that districts shall be of such size and nature as will promote efficient local government and avoid the necessity of uneconomic expenditure.

The Commission has a duty to prepare local government area schemes to cover the whole of New Zealand by 31 December 1972. These schemes are to come into force as final schemes after the hearing of objections to publicly notified provisional schemes. These schemes will have no immediate effect on the local authorities in the local government area, but will set the general pattern to which individual local schemes will be required to conform.

Franchise—Under the Local Election and Polls Act 1966, elections are held on the second Saturday in October every third year. Enrolment of residential electors is compulsory. On any proposal relating to loans or rates a rate paying or a freehold qualification is necessary. Details of the franchise as it affects each type of local district are now given.

Counties—Any person of 21 years of age and over who possesses either of the following qualifications is entitled to be enrolled on the county electors roll:

Boroughs—Any person of 21 years of age and over who possesses any of the following qualifications is entitled to enrolment:

Town Districts—The franchise is the same as for boroughs, except that for county electoral purposes in dependent town districts the county qualification is necessary.

Pest Destruction Districts—Where the rates of the district are based on the acreage and rateable value of land occupied by the ratepayer, the franchise is the same as that exercised for county council elections. Where the franchise is based on stock ownership, from one to five votes are allowed according to the number of stock units owned. In the case of county pest destruction districts, no separate elections are held as the county council is also the board.

Land Drainage Districts—Where the rates of the district are based on the acreage of land occupied by the ratepayer, the franchise is one vote where the area of rateable property does not exceed 50 acres, two votes where it exceeds 50 acres but does not exceed 100 acres and three votes where it exceeds 100 acres. Where the rates are based on rateable value of the land, the franchise is the same as that derived from a rating qualification in a county.

Other Districts—Road districts, river districts, water-supply districts, and the local railway district all have a franchise similar to that of counties except that the residential qualification applies to road districts only.

Districts composed of a grouping of districts of other types united for a common purpose have a franchise as for the component districts. Such districts are urban drainage districts, electric power districts, harbour districts, hospital districts, urban transport districts, and catchment districts. In some cases—e.g., the Auckland Metropolitan and Hutt Valley Drainage Boards—the members are appointed or elected by the territorial local authorities included in the district.

TOWN AND COUNTRY PLANNING—The Town and Country Planning Act 1953 provides for the making and enforcement of regional and district planning schemes, and the detailed procedure to be followed in each case is amplified by the Town and Country Planning Regulations 1960. The Government administers the Act through the Minister of Works who may delegate his authority to the Commissioner of Works.

Regional Planning—Regional Planning Authorities may be established under provisions of the Town and Country Planning Act 1953. As provided in the Act the authorities consist of representatives of the several councils whose districts are wholly or partly within the region. Every local authority within the region, other than the constituent councils, is entitled to be represented by at least one associate member. The Regional Planning Authority may also appoint any person who may be possessed of special knowledge, or representatives of any Department of State, to be associate members. Authorities are now operating in the four main centres and in Northland and Marlborough.

Finance for administration purposes is provided for by way of a maximum rate of one-sixtieth of a cent in the dollar on the rateable capital value of those portions of the councils' territories inside the regional area. The Act also makes provision whereby any of the constituent councils may enter into and carry out agreements for the execution of combined works.

Regional planning schemes must be preceded by a comprehensive survey of the natural resources of the areas concerned, and of the present and potential uses and values of all lands in relation to public utilities or amenities. Regional schemes envisage the conservation and economic development of natural resources by classification of lands according to their best uses and by the co-ordination of all such public improvements, utilities, and amenities as are not limited to the territory of any one local authority. Every regional planning scheme is intended to be a guide to councils engaged in the preparation of district planning schemes and to public authorities and all persons in relation to conservation and development within the region. Regional schemes are required to be reviewed at intervals of not more than 10 years.

District Planning—Every district scheme is required to have for its general purpose the development of the area to which it relates (including where necessary the replanning and reconstruction of an area already built on) in such a way as will most effectively tend to promote and safeguard the health, safety and convenience, the economic and general welfare of its inhabitants, and the amenities of every part of the area. The council of every city, borough, county, and independent town district must provide and maintain a district scheme whether or not a regional planning scheme including its district has been prepared or become operative.

While a district scheme is being prepared a council may refuse its consent to the carrying out of any development that would be in contravention of the scheme and falls within the definition of a “detrimental work”, but the owner or occupier affected may appeal against such a decision to the Town and Country Planning Appeal Board. The Minister can require the council to exercise these powers where the development would or might adversely affect Government works or the public interest, and local authorities have similar rights in respect of their works. Any appeal proceedings lie against the Minister or the local authority concerned.

In the period before a district scheme becomes operative, any change of use of land that detracts or is likely to detract from the amenities of the neighbourhood is required to have the prior consent of the council. Where an application is made to the council for consent, the applicant and every person who claims to be affected by the proposed use has a right to be heard by the council and may appeal to the Appeal Board against the council's decision.

When completed and recommended by the council, copies of a district scheme are submitted to the Minister of Works and to adjoining councils and to local authorities within the area covered by the scheme for consideration, particularly in relation to their public works. When the Minister and each local authority is satisfied that all their respective public works have been properly provided for in the scheme and have certified accordingly, the district scheme is publicly notified for inspection for three months. Any owner or occupier of land affected may object to any provision of the scheme, and the Minister, other local authorities, professional, business, sporting or other such organisations, may also object to the scheme on grounds of public interest. In the event of an objection not being sustained by the council the objector may appeal to the Appeal Board whose decision is final.

Where any council has not an operative district scheme for its district by 1 January 1971, the Minister of Works is empowered to take such steps as he may consider necessary to have such a district scheme made operative as quickly as possible. The costs and expenses incurred by the Minister are recoverable from the local authority, or they may be deducted from any moneys payable to the local authority by the Crown.

When a district scheme has been finally approved and made operative the council and all local authorities having jurisdiction in the district are bound to observe, and enforce observance of, the requirements of the scheme. The provisions of an operative regional planning scheme are also obligatory, but a constituent council has a right of appeal to the Town and Country Planning Appeal Board where a provision of a proposed or operative district scheme conflicts with the regional scheme; the Minister has, incidentally, a similar right of appeal so far as the regional scheme conflicts with the public interest.

Operative district schemes may be changed at any time, and must be reviewed when any part of the scheme has been operative for a period of five years. In preparing, recommending, and approving a change or a review of a district scheme the proposed change or review is publicly notified for inspection by owners and occupiers of property and simultaneously submitted to the Minister, to the Regional Planning Authority, and to the local authorities within the district for their consideration and objection where necessary in the light of their respective public works and other responsibilities.

Once a district scheme has been made operative it cannot be cancelled unless it is replaced at the same time by another operative district scheme. Furthermore, once a proposed change to an operative district scheme has been publicly notified for inspection and objection by owners and occupiers of property, no development work, subdivision, or change of use of land or buildings that would conflict with the proposed change may be carried out without permission by order of the Appeal Board.

Where a district scheme is operative the local authority may take, under the Public Works Act 1928, any land in its district if in accordance with the scheme it considers it is necessary or expedient to do so for the proper development or use of the land, or for the provision or preservation of amenities, or for the improvement of areas that are too closely subdivided or are occupied by decadent buildings.

POPULATION GROWTH—Throughout the main period of European settlement in New Zealand, which lasted from 1850 to 1880, the rate of population growth was very rapid. The 1858 Census recorded 115,462 inhabitants of whom one-half were Maoris. At the 1886 Census the population had reached 620,487, though the Maori population had in the meantime fallen from 56,049 to 43,927.

Thereafter, as the wave of immigration subsided, the rate of growth slowed down. The average annual increase has varied between 0.8 and 2.8 percent, with low rates during the depression periods of 1886-1891 and 1929-1936, and also during the two World Wars. In the 20 years from 1945 the annual rate of growth was over 2 percent a year. The lower birth rate since 1964 together with changes in migration flow has resulted in a lower rate of growth in recent years.

During the present century, natural increase has been the principal element in the growth of population; and in the following table the natural increase of non-Maoris is given.

A comparable table for the Maori population is not available but the following table shows the inter-censal increases in the Maori population. Since the Maori birth rate has exceeded that of the population of European origin very considerably, while the death rate has fallen, the natural increase of Maoris has made an increasingly important contribution to the growth of the total population.

The other element in the population growth—the gains from external migration—is shown in the following table. Movements of the armed forces are not included.

Most of the inward migration has been from the United Kingdom, Australia, and the Netherlands; in more recent years increasing numbers have come from the Pacific islands, notably Western Samoa.

CENSUS STATISTICS—Population statistics are based primarily on the five-yearly population census. Intercensal population estimates are based on the most recent census data available, adjusted in accordance with later figures of births, deaths, and migration. Estimates of the populations of particular localities, ....... and boroughs, also take into account local economic developments, housing scheme the numbers on school rolls, changes in boundaries, and any other factors leading to, or indicating, changes in population.

The basis adopted for the population census, and virtually throughout population statistics in New Zealand, is that of population physically present in the place of enumeration at the time of enumeration.

All references to New Zealand relate solely to geographic New Zealand, i.e., island territories are omitted except where their inclusion is specifically stated. Though Niue Island and Tokelau Islands are constitutionally part of New Zealand, for geographical reasons they are administered separately. The Cook Islands are self-governing but the islanders are New Zealand citizens.

PRESENT POPULATION—The following table gives a summary of population. A 50-year time series is given in the Statistical Summary towards the back of this Yearbook.

INCREASE OF POPULATION—The growth of population has been substantial in each intercensal period. The lowest rates are those of 1926-36, which included some years of economic depression, and of 1936-45, which included six years of international war.

COMPARISON WITH OTHER COUNTRIES—The annual average percentage increases of population for the period 1963-66 are given in the following table for certain selected countries. (Source: United Nations Statistical Yearbook.)

INTERCENSAL RECORDS—Intercensal statements of total population are prepared from the records of vital statistics and of external migration and are relatively accurate.

The following population figures exclude members of New Zealand armed forces who were overseas, and also members of the armed forces of other countries who were in New Zealand.

The figures given in the preceding table are for total population inclusive of Maoris. The following table shows the Maori population.

POPULATION PROJECTIONS—An indication of future population growth, including Maoris, in New Zealand is given by the detailed projections for the period 1967-2000.

Projections of future population involve an element of uncertainty owing to incomplete knowledge of the factors underlying changes in fertility, mortality, and migration levels, coupled with the difficulty of accurately forecasting the future course of the factors which are known to affect these components of population change. It should be understood, therefore, that these projections merely show the effect of the assumptions stated below the table on the future growth of the existing population. The assumptions, however, have been adopted only after careful studies of trends in the patterns of fertility, mortality, and migration and, in the light of available current information, are regarded as those most likely to produce realistic projections over the length of the projection period.

PROJECTED NEW ZEALAND POPULATION

Assumptions—The projections are linked to actual population numbers as at 31 December 1967. The assumptions on which the projections depend are as follows:

The following diagram presented on a ratio scale shows the growth of actual population from 1880 to 1967 and projections through to 1990.

Figure 3.1. POPULATION

DISTRIBUTION OF POPULATION—Detailed population statistics are compiled for each census and are published in Volume 1, Increase and Location of Population, of the Census of Population and Dwellings.

North and South Islands—In 1858 the North Island had a larger population than the South, but this position was reversed at the succeeding enumeration, and the South Island had the larger population (exclusive of Maoris) at each census from 1861 to 1896. In 1901 the North Island was found to have slightly the larger total and since then has steadily increased its lead.

The following table gives the population, excluding Maoris, of the North and South Islands as disclosed by each census since 1901.

The population of the North Island increased at a greater proportionate rate than that of the South Island between the 1961 and 1966 censuses. At the 1966 census the North Island population was 1,893,326, including 190,524 Maoris, and the South Island population 783,593, inclusive of 10,635 Maoris. The increase since the 1961 census was 208,541 for the North Island and 53,394 for the South Island.

The natural increase of population (i.e., excess of births over deaths) for the North Island during the 1961-66 intercensal period was 152,942, and for the South Island the natural increase was 48,312. External migration has also added to the population and there has been population movement between the islands.

Statistical Areas—The boundaries of statistical areas are shown on the map inside the back cover. Northland comprises the northern counties from Mangonui to Otamatea; central Auckland, the counties from Rodney to Franklin (including islands in the Hauraki Gulf); East Coast, the area north of Wairoa; while South Auckland - Bay of Plenty comprises the remainder of the provincial district. Hawke's Bay, Taranaki, and Wellington statistical areas are the same as the provincial districts of the same names.

In the South Island the statistical areas coincide with the provincial district boundaries, except for the transfer of Amuri and Cheviot counties from Nelson to Canterbury, and the transfer of all that area of Grey county north of Grey River from Nelson to Westland.

In the following table the approximate areas and the populations as at the census of March 1966 and estimated at 1 April 1968 of the statistical areas are shown.

Urban Areas—Urban areas are statistical conceptions and not administrative units. Their purpose is to provide definite, stable, and comparable boundaries for the larger centres of population. In addition to the central city or borough, they include neighbouring boroughs and town districts and parts of counties which are regarded as suburban to the centre of population. The present boundaries of urban areas have been in use since 1951.

For the 1961 Census, three new urban areas were defined at Whangarei, Tauranga, and Rotorua and comparable figures have been compiled for past years.

In the following table statistics of urban areas are given; 62.5 percent of the population lived in these areas in 1966.

The next table gives the component parts of the five largest centres of population as estimated at 1 April 1968.

Cities and Boroughs—The population of cities and boroughs is now given.

Town Districts—The population of independent town districts—i.e., those contained in section (a) of the following table—is not included with that of the county in which the town district is located, but the population of dependent town districts—section (b) — is included in that of the respective parent county.

County Towns—The following table lists those county towns with populations of 1,000 or more at the time of the 1966 census. The parent county is shown in parentheses. The populations of county towns are included in the administrative county populations given previously.

Extra-county Islands and Shipboard Population—In addition to the populations quoted for administrative counties, cities and boroughs, and independent town districts, the New Zealand totals include shipboard population and persons located on islands not within the boundaries of any county. The two latter categories comprised a total of 6,252 people as at 1 April 1968.

Of the islands concerned, Waiheke, with a population of 2,020, was the only one of any size.

Counties—The following table gives the population of individual counties at 1 April 1968, together with the approximate area of each. It should be noted that “Administrative Counties” do not include boroughs or town districts independent of county control, but include town districts and county towns which form parts of counties.