New Zealand Official Yearbook 1972

New Zealand is in the south-west section of the Pacific, that great ocean stretching across one-third of the earth's surface. To the west, beyond the Tasman Sea, is Australia, 1,600 kilometres away. From its position on the rim of the Pacific basin, New Zealand is a little over 10,000 kilometres from San Francisco and Panama and a similar distance from Tokyo and Singapore. In area 26.9 million hectares, it is similar in size to the British Isles and Japan.

One of the chief charms of the New Zealand landscape is its infinite variety. Such level lowlands as exist are small in area; contrasts between coastal plain and bordering hard-rock mountains are abrupt. High mountains make up most of the South Island area—often stark and bare or mantled in permanent snow. By contrast, most of the North Island is weak-rock hill country. From Cook Strait to the Bay of Plenty a hard-rock mountain core dominates the North Island scene, forming an effective barrier between cast and west; the only low level gap across it is at the gorge cut by the Manawatu River near Palmerston North.

A peculiar and special feature of the North Island is the volcanic country of the interior. Here are the largest North Island lakes and in a line from Ruapehu to White Island, most of the still active volcanoes, hot springs, and geysers.

The most spectacular mountains are in the South Island; high mountains, deep and narrow valleys, swift rivers, and glacial lakes, large and small, give infinite variety to the scene. It is in this high country, that ice has left its special mark in glacial troughs and fiords and, above all, the noble southern lakes. There is little weak-rock hill country in the South Island; the lowlands are mainly bordering plains, basin plains, and valley plains. Of these the most extensive are the plains of Canterbury and Southland.

New Zealand has large areas of luxuriant forests which are the delight of trampers, campers, and hunters. Forests cover nearly a quarter of the total land area, of which national parks and scenic reserves set aside as permanent forest form 2 million hectares.

The indigenous forests may be grouped broadly into two main formations: mixed temperate evergreen forest and southern beech forest. The former is a mixed community of many species of broad-leaved trees and conifers, and the latter a pure community of one or more of the species of southern beech. Generally, the mixed temperate evergreen forests are the forests of the north and of the warm, wet lowlands and lower mountain slopes. The beeches form the forests of the south, of the high mountains, and of the drier lowlands. But there are extensive areas where the types mingle in forests of extremely varied composition.

Mountains, forests, lakes, rivers, and beaches have influenced the characteristics of the people. New Zealand society has been shaped and subtly tempered by a number of factors—geographical, historical, social, and psychological during more than a century of growth as a nation. New Zealand today represents both an extension and a modification of the European tradition. In addition to its Maori population, New Zealand has experienced in recent years a considerable inflow of Polynesians from its associated territories and elsewhere in the Pacific. Auckland has become the major city of Polynesia, and as such a focal point of the South Pacific. The Polynesian (including Maori) population is of greater significance than its relatively small numbers would suggest. Outside the Pacific area New Zealand may present a basically European face to the world, but the preservation of distinctive life-style by the Maori, together with a close compatibility (extending to frequent intermarriage) between the two races, has doubtless been a determining factor in the evolution of New Zealand society.

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, 1,600 kilometres 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, 850 kilometres to the east of Lyttelton. Dating from 1842 the administrative boundaries ofNew Zealand, including the minor islands, 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, 930 kilometres north-east of the Bay of Islands, and Campbell Island, 590 kilometres south of Stewart Island.

New Zealand is also responsible for the administration of two island groups in the South-west Pacific—Niue and the Tokelau Islands. These are incorporated within the boundaries of New Zealand. Niue is 2,460 kilometres north-east of Auckland, while the Tokelau Islands are 1,130 kilometres further north. The territorial area reaches to within 8 degrees of the Equator.

The Ross Dependency, some 2,300 kilometres 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.

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.

In the North Island, Whangarei, Auckland, Tauranga, and Wellington are natural harbours which have been developed into ports for extensive use by overseas ships. At Napier and Gisborne artificial harbours have been made. On the east coast of the North Auckland Peninsula several other 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 the rugged nature of the terrain they have—with the exception of Queen Charlotte Sound—little or no commercial utility. By dredging and by breakwater construction, ports capable of accommodating overseas vessels have been formed in Lyttelton, Otago, and Bluff Harbours and on the coast at Timaru. On the west coast of both Islands the strong ocean drifts and high seas cause shoaling at river mouths and harbour entrances, although an overseas port has been developed at New Plymouth, 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 the coast by ocean currents.

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(6458 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: Rau-kumara, 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 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. 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-east 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.

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 1 1/4 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 (7 1/4 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 9 3/4 miles and 8 1/2 miles respectively, and terminal faces at altitudes of 670 ft and 690 ft.

Rivers—New Zealand rivers, owing to the high relief of the country, are mostly swift-flowing and difficult to navigate. As sources of hydro-electric power the rivers are of considerable importance, since their rapid rate of flow and dependable volume of water make them eminently suitable for this purpose. The Waikato and the Rangitaiki in the North Island and the Waitaki, Cobb, Clutha, and Waipori in the South are used for major hydro-electric schemes.

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.

The discovery in 1861 that the beds of rivers in the South Island contained extensive deposits of alluvial gold was of considerable importance in the early economic development of the country.

With the very successful acclimatisation of freshwater fish, notably trout, many rivers 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 some of the larger ones of the North Island, situated on a volcanic plateau, have their own particular beauty. As reservoirs the lakes of both Islands are of vital importance for the maintenance of the rivers and 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. In 1965 Lake Benmore, New Zealand's largest artificial lake, was created. It lies on the Waitaki River in North Otago and covers 30 1/2 square miles in area and consists of two arms, the main arm being 18 1/2 miles in length and the Ahuriri Arm 11 1/2 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 intruded into the outer crust in a molten state during mountain building; some, however, may be the products of an intense metamorphism of sediments.

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 land mass. 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, embracing 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.

Erosion during this time has eaten into the major landscape forms that the earth movements have built, carving detailed landscape pattern of peaks, ridges, valleys, and gorges, and has built up alluvial plains, shingle fans, and other construction forms. At the coast, waves have driven back the headlands and built beaches, splits, and bars. The Pleistocene period was the time of the Ice Age, and in the highmountains 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. 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. This is one of the largest and youngest accumulations of acid volcanic rocks in the world.

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; and many small scoria cones can be seen in the locality. Late Tertiary and Quaternary basaltic eruptions in North Auckland have built lava plateaus and many young cones.

Geological maps and an accompanying description were included in issues of the Official Yearbook up to 1971, and are also included in An Encyclopaedia of New Zealand.

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.

EARTHQUAKES: Geophysical Background—Earthquakes are geographically associated with active volcanoes and with major earth movements such as mountain building; these 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 fully understood.

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. It is noteworthy, however, 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, 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 36 1/2°S and 43 1/2°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 169 1/2°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 at 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); Nandi (Fiji); Rarotonga (Cook Islands); Raoul Island (Kermadecs); Cape Reinga, Onerahi, Auckland, East Cape, Karapiro, Whakatane, Wairakei, Gisborne, Tuai, Tarata, Chateau, Taradale, Castlepoint, Mangahao, and Wellington (North Island); Cobb, Kaimata, Christchurch, Gebbies Pass, Mount John, Milford Sound, Oamaru, 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, and 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 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 interior.

Earthquakes during 1971—Earthquakes did not cause any appreciable damage in 1971. The largest New Zealand earthquake during the year was that of 15 April, which occurred at a depth of 170 miles beneath the Bay of Plenty, about 70 miles to the north of Whakatane. Its magnitude was 6.2 on the Richter Scale, and it was felt on the east coast of the North Island, and as far south as Wellington, but because of its depth caused no damage. Two other deep shocks that were felt widely in the North Island originated at a depth of 90 miles beneath the Lake Taupo region on 1 November (magnitude 5.7) and 12 November (magnitude 5.5).

For the third year in succession, no shallow earthquake in New Zealand has reached a magnitude of 6. The largest shallow shock had a magnitude of 5.9, and occurred on 14 August near Maruia, about 25 miles to the east of Reefton. It was felt extensively over the northern part of the South Island, and caused minor damage at Westport, Greymouth, and Reefton. Other shallow earthquakes that were felt widely were those of 16 March, near the northern end of Lake Te Anau (magnitude 5.7) and 29 April, near Cape Turnagain, off the Hawke's Bay coast. The latter earthquake had a magnitude of 5.5 and was felt most strongly at Waipukurau and Dannevirke. A series of earthquakes took place near Lake Benmore on the Waitaki River. The largest, on 7 April, had a magnitude of 5.0, and was felt as far afield as Oamaru and Dunedin. Three other shocks of magnitude between 3 and 4 were recorded from the region within a few days of the main event, and a further earthquake of magnitude 4.1 occurred there on 30 June.

Several earthquakes were also reported felt from the Christchurch area. That of 25 September, with a magnitude of about 4.5, appears to have been located directly under the city, and caused minor damage. An earthquake of magnitude 3.8 on 23 April, also felt in Christchurch, probably originated about 10 miles to the north, near Kaiapoi.

Of scientific interest is an earthquake of magnitude 4.4 that occurred on 31 January, near the Reinga Ridge, about 180 miles to the north-west of North Cape. This is the first earthquake to have been located in this region, and appears to be part of a weakly-active seismic region running through the North Auckland Peninsula to Norfolk Island.

Mt. Ruapehu was again active during April and May. Several eruptions of rock, ash, and steam occurred, the most important being on 8 May and 16 May. No significant earthquake activity was associated with these eruptions.

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 50 in the Pacific islands and collected by telegraph and radio, along with measurements of winds at upper levels made at 9 radio wind stations, and of temperatures made at 8 radiosonde stations. Daily observations are made for climatological purposes at about 250 places in New Zealand and 80 in the islands. Rainfall measurements are made at a total of about 2,000 places within New Zealand and 270 outside the country.

Detailed climatological statistics are published annually by the New Zealand Meteorological Service in the Meteorological Observations, in Rainfall Observations, and in 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 70°S.

The weather pattern from day to day is dominated by a succession of anticyclones, separated by troughs of low pressure, which pass more or less regularly from west to east across the Australia-Tasman Sea - New Zealand area and beyond. In this region there is no semi-permanent anticyclone such as those found in similar latitudes over the Indian Ocean and eastern Pacific Ocean respectively. The troughs normally have a north-west to south-west orientation and are associated with deep depressions centred far to the south. A typical weather sequence commences with a low-pressure trough approaching from the west. Freshening north-westerly winds prevail with increasing cloud, followed by rain for a period during which winds may reach gale force. The passage of the trough, with its associated cold front, is accompanied by a change to cold south-westerly or southerly winds and showery weather, occasionally with some hail and thunder. Barometers then rise with the approach of the next anticyclone from the west. Winds moderate and fair weather prevails for a few days as the anticyclone moves across the country.

While the sequence just described is very common the situation is frequently much more complex. The troughs are very unstable systems where depressions readily form, some of which develop into vigorous storms that may pass over New Zealand at any time of the year. Occasionally in summer a cyclonic storm of tropical origin passes over or near New Zealand accompanied by gales and heavy rain affecting mainly northern and eastern districts of the North Island. The anticyclones vary in size, intensity, and rate of movement. Their centres, on the average, follow a track across the North Island but individual centres may pass either north or south of the country, the more northerly tracks being favoured in spring and the southerly tracks in autumn. At times when little development occurs within the troughs the anticyclones follow each other at intervals of about 6-7 days.

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.

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 ocean, 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 of 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 300 mm in a small area of Central Otago to over 7000 mm in the Southern Alps. The average for the whole country is high, but for the greater part it lies between 600 and 1500 mm, a range regarded as favourable for plant growth in the temperate zone. The only areas with under 600 mm 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 800-1000 mm a year. Of the remainder, much valuable farm land, chiefly in northern Taranaki and Northland, has upwards of 1500 mm. Over a sizeable area of both Islands rainfall exceeds 2500 mm 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. 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 600 mm 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 (2.5 mm 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 560 mm which occurred at Milford Sound where the mean annual rainfall exceeds 6000 mm. 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 north-eastern districts of the Auckland Province. By contrast, in the Manawatu district and in Otago and Southland daily falls reaching 80 mm are very rare.

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 5 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 15°C in the far north to 12°C about Cook Strait, then to 9°C in the south. With increasing altitude, temperatures drop about 2°C 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 exceed 30°C 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 38°C at Ashburton and -19°C 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 8°C. For the remainder of the North Island, and east coast districts of the South Island, it is 9°-10°C. Further inland it exceeds 11°C in places, reaching a maximum of 14°C in Central Otago where there is an approach to a continental type of climate.

Temperatures in the preceding paragraphs are recorded on the Celsius scale (formerly called centigrade), and not the Fahrenheit scale. The degree Celsius (°C) equals 5/9 (°F-32).

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 0°C 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 -12°C 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 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 100 percent during clear nights. As the following table shows, the diurnal variation is greater than the difference between summer and winter.

Very low humidity—between 20 and 30 percent or lower—occurs at times in the lee of the Southern Alps where the Föhn effect is often very marked. In summer the hot, dry “Canterbury Nor'-wester” 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 30°C. 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 a year. 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 a year, 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 a year. 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.

Brief Review of 1971:Year—There were two unusual features of the 1971 weather. The first, which affected all other weather elements, was a persistently high frequency of easterly to north-easterly winds; the only months in which this feature did not occur were September and October. The second special feature of 1971 was its high temperatures, making it the warmest year in New Zealand in 110 years of observations, with an average departure from the 1931-60 normal of 1.0°C. The previous warmest years, all about equal, were 1956, 1962, and 1970. Highest departures from normal were in Westland, and lowest departures in eastern districts of both Islands. The only months in which temperatures were not above normal but only close to it were July, October, and November.

The easterly to north-easterly winds brought excessive cloud to areas east of the ranges in the North Island, to Bay of Plenty and Taupo, and to Nelson and most of Marlborough; and in these areas sunshine was mainly 200-370 hours below normal. Rotorua and Waipukurau both recorded sunshine more than 100 hours below their previous lowest. On the other hand, sunshine was above normal, mainly by 100 hours, on the West Coast, in the Mackenzie basin, and in Wellington and Manawatu.

The greater part of the North Island had rainfall above normal. Highest departures of over 35 percent were in central and northern Hawke's Bay with most of Gisborne, in Bay of Plenty and Rotorua, and in eastern Northland. In the South Island rainfall was somewhat below normal in Canterbury and Westland, and in most of Southland; but somewhat above normal in Nelson, central Marlborough, and parts of Otago. The greatest departures below normal, exceeding 25 percent, were recorded over parts of Canterbury, especially about and south of Christchurch.

Seasonal Notes—Both January and February were very warm, besides being cloudy and wet over a considerable area of the North Island but mainly dry in the South Island. The rainfall at the Hermitage in January of 60 mm was the lowest for that month in 50 years of observations. From 3 to 8 January cyclone Rosie brought upwards of 50 mm of rain to the greater part of the country and this relieved the prevailing very dry conditions. Napier, Blenheim, and Hanmer recorded their lowest January sunshine for at least 45 years. February 1971 was equal with February 1935 as the third warmest month on record, the two warmest being February 1938 and January 1956. In February nearly all the rain fell from the 23rd to the 25th and this was preceded by 6 weeks of dry, hot weather affecting especially the South Island and southern districts of the North Island. Parts of the Southland Plain and western Southland were still very dry by the end of the month. Forest fires were exceptionally frequent in February in Westland, Otago, and Southland.

In March, rainfall was only about half the normal value over the greater part of the country and it was less than a quarter in the north Canterbury high country. A total of 645 mm of rain at Hokitika from November to March was the lowest in over a century of observations. Most of the country was favoured with more sunshine than normal and departures of 50-80 hours were recorded in western districts. In Canterbury and southern districts of the North Island the weather was too dry, causing a shortage of feed in some areas and also affecting crops.

April weather was a continuation of that of March, but with floods and slips in eastern districts from Hawke's Bay to Bay of Islands, while the remainder of the country had sunny, warm, dry weather.

May was rather wet. A small but intense depression off the coast of northern Hawke's Bay caused heavy rain with slips, considerable flooding, and disruption of transport in Gisborne and Hawke's Bay on the 3rd and 4th. Good growth was reported for the time of the year in most areas.

June was the warmest in over a century of observations for a considerable part of the country, especially in the North Island. In the South Island rainfall was mainly above normal but in the North Island it was mainly below normal. Flooding occurred in Bay of Plenty after rainfalls of up to 300 mm in the 4 days, 3-6 June; and it occurred in parts of Otago after rainfalls of 150 mm on the 6th and 7th. The mild weather was appreciated by farmers, who found growth good for the time of year.

In July considerable cloud and rain affected some eastern districts, but rainfall was mainly low elsewhere, with fairly sunny conditions. Depressions over Northland caused severe gales there on the 22nd and 26th and these were reported in other northern districts on the 2nd. In some districts unusually frosty weather cut back growth but stock were healthy. Lambing commenced under mainly favourable conditions.

August was unusually mild, especially in the north. In the North Island rainfall was mainly up to 50 percent above normal but in the South Island it was predominantly 25 percent below normal. Sunshine was mainly below average. In Northland and eastern districts of the North Island and about Cook Strait serious losses of new-born lambs were reported, some in violent south-easterly gales with rain, affecting especially the Cook Strait area from the 16th to the 18th.

In contrast with other months of the year, September and October were marked by an unusually high frequency of westerly and north-westerly winds. In September, Waikato and parts of Bay of Plenty and central Hawke's Bay received more than double the normal rainfall; while sunshine was below normal west of the main ranges from Waikato to Manawatu, and also on the Southland coast. Unusually violent north-westerly gales buffeted Canterbury and Otago on 10 and 11 September, with considerable damage in some inland districts.

October was a wet month over most of the country and too wet for the farmers in the North Island. Violent north-westerly gales buffeted parts of Otago on 27 October, with a gust of 85 knots at Dunedin Airport.

November was a sunny month. Rainfall was somewhat above normal over the greater part of the North Island, but somewhat below normal over the greater part of the South Island. Daily falls of up to 160 mm on the 15th caused flooding on the Taieri Plains. Strong gales from a westerly quarter buffeted most of the North Island on the 26th, causing some damage. Conditions were good for farming except in some eastern districts of the North Island, where it was too wet for the lambs.

December was dry in the South Island. Over most of the North Island and in northern districts of the South Island sunshine was below normal. It was a good month for stock, and there was plenty of growth except in parts of Marlborough and Canterbury, where it was too dry.

Summary of Meteorological Observations for 1971—The observations from which the following summary was compiled for the year 1971 were at 0900 hours New Zealand standard time, i.e., 2100 hours Greenwich mean time.

For 1971 the mean sea level pressure values in millibars at 0900 hours New Zealand standard time were: Auckland, 1015.7; Kelburn, Wellington, 1014.7; Nelson Aerodrome, 1015.1; Hokitika Aerodrome, 1014.3; Christchurch, 1014.0; and Dunedin Airport, 1013.2.

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 Maoris displayed exceptional courage and intelligence.

From the early days of European settlement in the first half of the nineteenth century many Maoris believed that their interests were best served by co-operation with the settlers. For the most part the Europeans adopted a humanitarian attitude to the Maori people, who accepted their assurances and found a satisfactory safeguard for their interests in the exercise of their rights and privileges of British subjects. As the Europeans established a self-contained and aggressively growing society, there grew up a rivalry for land and a clash of power. In the 1860s Maori tribes in Taranaki, Waikato, and Bay of Plenty fought the settlers and Government troops in a series of sporadic campaigns based on loss of land rights and rising Maori nationalism. After 1870 there followed the development of a European colony of settlement with Maori people making further economic adjustments to European ways.

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 though still forming a minority component.

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.

There is no record of any European visit to New Zealand after Tasman's departure until Captain James Cook sighted land on 7 October 1769 near Gisborne. Cook and a party of men from the Endeavour landed at Gisborne on 9 October 1769. On his first voyage Cook spent 6 months exploring the New Zealand coastline, and he completely circumnavigated the North and South Islands. Hisactivities can best be described by saying “he found New Zealand a line on a 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 Maoris. He returned to New Zealand again in 1773, 1774, and in 1777. His careful observations made New Zealand known to the western world; the accounts of his voyages were translated into a dozen languages. The bi-centenary of Cook's first visit to New Zealand was celebrated in 1969; an account of his voyages of discovery in the Pacific is given on pages 1116 to 1128 of the 1969 issue of the Official Yearbook.

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—Whaling stations sprang up along the coast from 1792 onwards 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, was responsible for the establishment of the first mission station in the Bay of Islands. To promote the translation of the Bible into Maori, Thomas Kendall (one of Marsden's assistants) took two Maori chiefs with him to England in 1820. The printing of the Bible in Maori was made possible through the establishment of a printing press by William Colenso at Paihia in the Bay of Islands in 1835.

The growing white population in the Bay of Islands, and the lawlessness of crews of visiting ships led to the appointment by the British Government of James Busby as British Resident at Waitangi in 1833. The Governor of New South Wales in 1837 sent Captain William Hobson, in command of HMS Rattlesnake, from Sydney to the Bay of Islands to report on New Zealand. Among other things, Hobson suggested a treaty with the Maori chiefs and the placing of British subjects under British law. On 29 January 1840 Hobson arrived at the Bay of Islands as Governor to proclaim British sovereignty (see later).

By 1840 numerous mission stations had spread through the northern half of the North Island. Conversion of Maori tribes to Christianity was accompanied by the introduction of new crops and methods of cultivation and pacification of the warring tribes.

The first body of immigrants to reach New Zealand under a definite scheme of colonisation arrived at Port Nicholson, Wellington, on 22 January 1840 to found the initial settlement of the New Zealand Company. The colonists were in the main sturdy resourceful people seeking a better future than was offering in nineteenth century industrial England.

The guiding genius of the company, Edward Gibbon Wakefield, aware of the intention of the British Government to annex New Zealand, had earlier (in 1839), dispatched his agents in order to purchase large areas of land from the Maoris before the Crown could assume a monopoly of land purchase.

Wakefield's scheme of colonisation was based on the sale of land to investors or men of wealth for development by labouring class immigrants. With the profit from land sales the company could bring out more immigrants. Wakefield aimed at a balance between landowners and labourers; in effect he aimed to transplant a cross-section of English society. But, ignorant of the system of tribal ownership of Maori land, the company had bought land from individual Maoris; then Hobson provided that all European land titles should derive from the Crown which would be the only purchaser of land from the Maoris. Title to land remained a difficulty for some years and was a cause of distress to the colonists and, combined with a considerable degree of absentee ownership and land speculation, made most precarious the existence of the early company settlements of Wellington, Wanganui, New Plymouth, and Nelson. The company had brought nearly 10,000 persons to New Zealand by 1848. The later settlements of Otago, in 1848, and Canterbury, in 1850, organised under the aegis of the New Zealand Company in co-operation with the Free Church of Scotland and the Church of England respectively, achieved a much greater measure of success owing to the absence of any large Maori population and to satisfactory land purchase arrangements.

The non-Maori population in the main settlements in 1842 totalled 3,801 in Wellington, 2,895 in Auckland, 2,500 in Nelson, 895 in New Plymouth, 380 in Russell, 263 in Hokianga, and 198 in Akaroa. By 1862 the non-Maori population had reached 125,000 (as against 55,000 Maoris) and by 1866 it had jumped to 200,000 with men from Australia joining in the gold rush to Otago. Migration then dropped away until 1874 when there was a high inflow for several years from Britain with the Vogel policy of public works development.

After the death of Hobson in 1842, subsequent governors, through lack of funds and weak administration, found themselves unable to protect the small and helpless settlements from threatening Maori aggression engendered by strong feelings on land ownership. The response of the Colonial Office was to appoint Captain George Grey as Governor and to provide him with adequate funds and troops so that he soon restored order and won not only the confidence of the Maoris but also for a time that of the settlers. Grey, through his chief land purchase officer, Donald McLean, endeavoured to buy up land in advance of the settlers' needs in order to prevent conflict between settlers and Maoris. By 1858 the census revealed that the settlers outnumbered the Maoris who, fearful that they were being swamped by the settlers, became increasingly reluctant to sell their land. At the same time the intensified settler pressure for more land led McLean to negotiate only with those Maoris still favourably disposed to land sales. This practice alarmed the other Maoris and finally the war broke out in 1860 over a land dispute at Waitara in Taranaki where settler demand for land was strongest. The return of Grey as Governor did not solve the problem for, as an autocrat, he could not work with elected ministers nor could he regain the confidence of the Maoris and finally he quarrelled with the commander of the Imperial troops. Widespread confiscation of Maori land by the settlers' government in order to pay the cost of the war included land belonging to friendly as well as hostile Maoris and aroused further resentment. Although the war had died down by 1870 it was only during the term of Donald McLean as Native Minister that some measure of reconciliation began with the establishment of four Maori electorates in 1876.

Subsequent History and Development (1870 onwards)—The absence of hostilities and the discovery of gold there had allowed the South Island 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.

By 1870 the gold boom had ended in the South Island. To remedy the situation of economic stagnation, Sir Julius Vogel began a policy of extensive borrowing for railway and road construction and for immigrant labour. The results of this policy were to double the population to 500,000 by 1880, to immensely improve transport and communications and to encourage industry in the towns where most of the immigrants had congregated. After Vogel's plans for these loans to be secured against the land were frustrated by the provinces, he decided that the provincial system, begun in 1853, had outlived its usefulness and that parochialism was a hindrance to the development of the colony. The system was abolished in 1875, local administration being provided for by the Counties Act and the Municipal Corporations Act 1876.

When systematic colonisation began, New Zealand's only important trade association was with the cast coast of Australia. It was, however, the inflow of British capital which set the New Zealand economy on a path of growth: that determined by the requirements of markets in the United Kingdom. Britain with a vigorously expanding demand from its working population required from the young colony an assured and increasing supply of food and raw materials, and a guaranteed market for its industrial goods. In accordance with this archetypal pattern of colonial development agricultural trade with the United Kingdom assumed over-riding importance as the land was brought into production. By 1868, in spite of the problem of distance, the United Kingdom had already become New Zealand's principal trading partner.

With the introduction of refrigeration in 1882 and steam navigation in the late 19th century, the development of exports of frozen meat and dairy products assured the dominance of the United Kingdom in New Zealand's external trade. These developments, with a continued substantial investment of British capital, particularly in farming and food processing industries, established that degree of specialisation to meet the needs of the British market, which shaped the entire New Zealand economy during its first hundred years.

The depression of the 1880s, a consequence of a fall in world price levels, resulted in unemployment and large emigration but export prices recovered in the nineties. From 1880 onwards the natural increase of births over deaths exceeded the net inflow from migration.

In 1891 John Ballance, as leader of the Liberal Party, became Premier to be followed on his death in 1893 by Richard John Seddon, who remained Premier until his death in June 1906. The Government pursued a vigorous legislative programme in which the main emphasis was that of social justice, the principal manifestations of which were the breaking up of the large estates, the establishment of the Court of Arbitration, and the introduction of old age pensions. The policy of subdivision of large estates to produce closer settlement included the compulsory purchase of large holdings bythe State, but more important were the effects of refrigeration, which encouraged the smaller dairy and fat-lamb farms, the accelerated Government purchase of Maori lands and the widespread introduction of systems of Crown leasehold with subsequent loans to small farmers 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 under the influence of William Pember Reeves.

The expansion of the exports in dairy produce and frozen meat during the 1890s produced more intensive settlement and the rise of a new farming class in which the “cow-cockie” was the dominant figure. These farmers, having benefited by the spread of prosperity, were in 1911 mainly responsible together with the city businessmen for the overthrow of the Liberal regime. The new Reform Government under Massey, in order to strengthen the primary producer, introduced measures of which the extension of rural credit was typical. Industrial conflict on the waterfront and with the Waihi miners ended in a victory for Massey who relied on the use of troops and special constables to repress the strikes.

Three years after the advent of the Reform Party, the First World War, 1914-1918, broke out, leading to a coalition Government and an Imperial commandeer of exports which created the precedent for the establishment after the war of central boards to regulate the exports of pastoral products. War activities were marked by heavy casualties in proportion to the population while the landing at Gallipoli signified the growing awareness of a sense of nationhood.

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 on the administrative side, the period was characterised by extensive public works expenditure, with particular attention to hydro-electric schemes and highways.

Land values rose steeply, accelerated by Government efforts to settle returned servicemen on the land, and between 1915 and 1925 forty percent of the occupied land had changed hands. New Zealand was extremely vulnerable to the overseas price fluctuations of the pastoral products. With the advent of the depression by 1930, farmers, despite greatly increased production, were faced with a serious decline in income (over forty percent) together with heavy mortgage commitments on land bought at high prices so that many were faced with foreclosure. In the towns, tradesmen and shopkeepers faced bankruptcy, and wage earners unemployment or reduction in wages. A coalition Government, formed in 1931 to meet the crisis had, as its leading figure, Coates, who was Minister of Finance from 1933. In order to produce balanced budgets and cope with the effects of the depression, enactments 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. Partly as a consequence of these measures and of a rise in overseas price levels a general economic revival was taking place by 1935.

Development as a Nation—The election of a Labour Government in 1935 (with notable politicians including Savage, Fraser, and Nash, who successively became Prime Ministers) reflected the general climate of opinion and led to change in administrative policy, the preoccupation being mainly with social problems. These attitudes were reflected in certain distinctive trends in legislation.

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.

Another 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.

Shaken by conflict with its industrial left-wing, and faced with increasing public impatience at the continued existence of some wartime controls and concern at inflation, the Labour Government was defeated at the 1949 election after holding office since 1936. The National Party took office under the leadership of Sidney Holland and its first term was marked by a conflict with the Waterside Workers' Union. This dispute in 1951 ended in a complete victory for the Government after it introduced most stringent emergency regulations to deal with the situation. For the first time this century, Holland held an emergency election before parliament had run its full 3-year term. The result was to return the National Government with an increased majority.

In 1952, continued inflation and a balance of payments crisis produced restrictions on exchange allocation to importers in an effort to build up overseas reserves. The 1954 election reduced National's majority and was marked by the appearance of a third party, the Social Credit Party which gained 11 percent of the votes.

During his time as Prime Minister, Holland initiated a constitutional change with the abolition of the Legislative Council on the grounds that it no longer possessed any effective function. Illness caused Holland's retirement in 1957 when he was replaced as leader by Keith Holyoake.

In 1957, the Labour Party gained a narrow victory at the polls under the leadership of Walter Nash. Budgetary policy to meet a recurrence of the balance of payments crisis proved unpopular and at the 1960 election, the National Party under the leadership of Keith Holyoake was returned to power, as it was in subsequent elections in 1963, 1966 and 1969.

International affairs have assumed growing importance in recent decades. It was evident when peace returned to the Pacific area in 1945 that New Zealand found itself in a different world, where its relations with the countries geographically closest to it would grow rapidly in importance. This did not, however, alter the extent to which New Zealand identified itself as a European nation. New Zealand took part in the Paris Peace Conference and it was not until 1955 that it altered the planning commitments of its defence forces from security arrangements in the Middle East to similar arrangements in the South-east Asia and Pacific areas.

The most far-reaching reorientation required of New Zealand in this new situation was the need to obtain a guarantee of its security from the United States rather than the United Kingdom to which it had traditionally turned. With Australia it signed the ANZUS pact with the United States in 1951 and this provides the cornerstone of New Zealand's security arrangements. It also gives New Zealand a common interest with the nations of Western Europe in encouraging the United States to maintain outward-looking policies and a global defence capability.

New Zealand's growing regional awareness has been expressed partly in its defence relationships through SEATO, and through the collective defence arrangements with Malaysia and Singapore; but more widely in its participation in the Colombo Plan and other arrangements for extending development aid to South-east Asia, the South-west Pacific and the Indian subcontinent. The stability and well-being of these areas are vital to New Zealand's interests and relationships with the countries of the region are becoming closer every year.

Contemporaneously with the expansion of the field of political interest, the economic and industrial development of the country has proceeded. Expansion and diversification of manufacturing and servicing industries have provided avenues of employment for the growing labour force.

Agricultural development has continued to be based on the principle of the family farm, and the New Zealand farmer remains typically both labourer and manager, as well as landowner. The present level of efficiency has been won by hard effort, skilled management, the application of the results of scientific research, and a heavy personal investment in farm improvement. Dairy producers are now faced with problems of maintaining overseas markets as a result of Britain's move to join the European Economic Community.

Farm production has constantly expanded so that New Zealand has become one of the world's greatest exporters of pastoral produce. The bulk of this produce still goes to the British market.

The advantages of a closely bilateral trading relationship with the United Kingdom were not one-sided. The association was grounded in economic logic, and enabled New Zealand to develop its only major natural asset into a pastoral system of unmatched economic efficiency, which, to the present day would, under free trading conditions, enable its primary products to meet any competition.

The pattern of economic dependence developed in accordance with a series of mutually agreed decisions extending over a long period, and these were formalised by the Ottawa Agreement of 1932 between the British and New Zealand Governments which provided preferential access to each other's markets. The advantages of this economic rationalisation were demonstrated most strikingly in the Second World War, 1939-45 when, apart from the New Zealand military contribution, its continued substantial supply of food to a beleaguered Britain was vital to the continuation of the Allied war effort.

Settlers came originally to New Zealand because of some dissatisfaction with the conditions of life they knew in their country of birth. They sought to build a new society which, while retaining what was good in Britain and Europe, would exclude the pressures which they had found damaging to the quality of their own lives. It is perhaps ironic that, to the extent which a new society has been created, this has been achieved by means of, and is contingent upon, continued strong economic ties with Europe.

Increasing interest has been taken in the last decade 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.

New Zealand has experienced in recent years a considerable inflow of Polynesians from its associated territories and elsewhere in the Pacific. Auckland has become the major city for Polynesians, and as such a focal point of the South Pacific.

The Polynesian (including Maori) population is of greater significance than its relatively small numbers would suggest. Outside the Pacific area New Zealand may present a basically European face to the world, but the preservation of distinctive life-style by the Maori, together with a close compatibility (extending to frequent intermarriage) between the two races, has doubtless been a determining factor in the evolution of New Zealand society. As such it is complementary to the basic evolutionary drive in that society, based as it is on the inheritance of European liberal ideas.

In early days, the New Zealand Government saw its role in the country's overseas territories as that of providing direction and guidance to less-developed areas. 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 section New Zealand Books in this Yearbook. A useful reference is the Encyclopaedia of New Zealand, published in 1966.

Sovereignty—On 29 January 1840 Captain William Hobson, R.N., arrived in the Bay of Islands. His instructions from the British Government required him to take possession of the country with the consent of the Maori chiefs, this policy being designed by the Colonial Office strongly influenced by missionary opinion, to safeguard the well-being of the native people. Hobson read his commission at Kororareka on 30 January and on 6 February 46 chiefs signed the Treaty of Waitangi, a compact whereby all rights and powers of sovereignty were ceded to the Queen, all territorial rights were secured to the chiefs and their tribes (with the Crown having the sole right of purchase) and in return the Queen extended her protection and all the rights and privileges of British subjects. Other chiefs throughout both Islands later adhered to this Treaty.

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 madefor 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.

One aspect, that of native affairs, was withheld from the responsible Ministers and the Governor, as representative of the Crown, continued to act independently of his elected advisors in this sphere. In 1861 Grey attempted unsuccessfully to hand over this responsibility but the Ministers were unwilling to assume responsibility for the cost of the war. Finally in 1864 Sir Frederick Weld instituted the “self-reliant policy” whereby the colony accepted responsibility for the settlement of difficulties with the Maoris and consented to the withdrawal of troops by the Imperial Government.

In recognition of a nascent sense of nationality and of an increasing desire for self-reliance in political matters 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 member 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 Westminster.

NEW ZEALAND'S INTERNATIONAL RELATIONS—Few pressures existed prior to the early 1930s to impel New Zealand towards enunciating an independent foreign policy. Successive Governments 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. 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. The Labour Government 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, it pressed for the restoration of the authority of the League of Nations 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. 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. Also 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 career foreign affairs 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 in 1941 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.

From 1955 New Zealand contributed forces to a Commonwealth Far East reserve stationed in Malaya. In 1959 New Zealand, with Australia, became associated with the Anglo-Malayan Defence Agreement, concluded in 1957, which subsequently became the Anglo-Malaysian Defence Agreement with the formation of Malaysia in 1963. When the United Kingdom decided to withdraw its forces east of Suez by the end of 1971, New Zealand, in association with Australia, indicated its intention to maintain a military presence in Malaysia and Singapore after British withdrawal. Subsequently, with a change of government in the United Kingdom in June 1970, the British decided to retain forces in the area although they upheld the earlier decision to revoke AMDA. A new five-power defence arrangement involving Australia, Malaysia, New Zealand, Singapore, and the United Kingdom replaced the Anglo-Malaysian Defence Agreement on 1 November 1971.

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 countries is reflected not only in its membership of such regional organisations as the South Pacific Commission, but also in 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. In 1968 Nauru achieved independence as did Fiji and Tonga in 1970. In August 1971, at the request of these five countries New Zealand hosted the first meeting of the South Pacific Forum. New Zealand's liberal tradition of friendship for emergent peoples, and the fact that large numbers of Polynesian people have settled here, means that the islanders tend to look to New Zealand for leadership and encouragement. Inevitably, New Zealand is going to be increasingly involved in the South Pacific region.

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 and civilian police in various peace-keeping operations, and has endeavoured to assist all efforts to attain the political and social objectives outlined in the Charter.

The historic links with Britain and with Western Europe and North America remain as close as ever; and the economic links with Britain, New Zealand's best customer, remain strong. One of the key problems of external political and economic policy for New Zealand remains the movement towards political and economic integration in Europe and the likelihood that Britain will join the European Economic Community at the beginning of 1973.

Ministry of Foreign Affairs—The primary responsibility of the Ministry of Foreign Affairs is for the formulation and execution of New Zealand foreign policy. It conducts relations with other countries and communications with their governments and representatives in New Zealand. It operates New Zealand's aid programme and maintains diplomatic and consular representation abroad. Its overseas functions are discharged through a network of 27 diplomatic and consular posts consisting of embassies, high commissions, consulates-general, and other permanent missions. At home, the preparation and co-ordination of foreign policy recommendations is carried out in close association with a number of other Government departments. The ministry is administered jointly with the Prime Minister's Department. Prime Ministers have found it appropriate on occasions to hold the Foreign Affairs portfolio. The Secretary of Foreign Affairs is also Permanent Head of the Prime Minister's Department.

In economic and commercial matters the ministry works closely with the Department of Industries and Commerce and with the Treasury. The ministry has a special role too as a clearing house for material provided by New Zealand posts overseas for other departments, and through its posts it performs numerous services on behalf of departments without representatives abroad.

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. While the Commonwealth association no longer reflects the similarity of outlook that was formerly apparent among its members, it has taken on new importance as a broadly-based grouping of nations that hold certain elements of their heritage in common and that adhere to the same fundamental principles, such as mutual respect and tolerance, in their dealings with others.

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 5 members, in 1971 there were 31 full members and one “special member”, Nauru. The accession to full membership in 1970 of Tonga, Western Samoa and Fiji has greatly increased South Pacific representation in Commonwealth forums. The Commonwealth has thus become an entity embracing several continents and its relationships have taken on a new scope and emphasis. As Commonwealth heads of government affirmed in the Commonwealth Declaration adopted in Singapore in January 1971, the association “provides many channels for continuing exchanges of knowledge and vowson professional, cultural, economic, legal, and political issues among member states. These relationships we intend to foster and extend for we believe that our multi-national association can expand human understanding and understanding among nations, assist in the elimination of discrimination based on differences of race, colour or creed, maintain and strengthen personal liberty, contribute to the enrichment of life for all and provide a powerful influence for peace among nations”. New Zealand, itself a country where two races live in harmony, sees in the Commonwealth a special opportunity for multi-racial co-operation and understanding.

New Zealand contributes to the budgets of the Commonwealth Secretariat and the Commonwealth Foundation, which were both established at the Commonwealth heads of government meeting in 1955. The Commonwealth Foundation, an independent fund administered by a board of trustees consisting of representatives of “member nations”, has contributed greatly to the growing areas of common endeavour. It has sponsored official and non-official Commonwealth organisations that provide links between administrators, engineers, lawyers, accountants, scientists, and private individuals in the different Commonwealth countries. Similarly, the Commonwealth Secretariat, under the leadership of its Secretary-General, has provided a focus for Commonwealth activities, and a basis for extending co-operation between Commonwealth Governments.

New Zealand and the South Pacific—The South Pacific is New Zealand's immediate environment, its Polynesian peoples are 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.

Through the South Pacific Commission the Governments administering territories in the South Pacific—Britain, the United States, France, Australia, and New Zealand—have made a concerted effort to promote the economic and social development of the area and its peoples. In the 24 years of its existence the commission has, within its budgetary limits (its budget for 1971, $1,096,954), 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. Its membership has grown to include Western Samoa and Nauru. At the same time the importance of the South Pacific Conference has increased. The territorial representatives who attend the conference now have a decisive voice in determining the commission's work programme. Close working links are maintained with United Nations specialised agencies which take an active 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 New Zealand to administer 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. On 4 August 1965 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.

Progress in the constitutional field has also been made in Niue and the Tokelau Islands, New Zealand's remaining dependent territories. On 1 November 1968, at the request of the Niue Assembly, a full-member system of government was introduced, giving the Executive Committee responsibility for the portfolios controlling all Government departments. Under the Niue Amendment Act 1971 the Executive Committee has general direction and control of the executive government of Niue. There is a Resident Commissioner responsible to the Executive Committee who acts as a liaison officer between the Governments of New Zealand and Niue.

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 (as have the people of Niue) 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 Niue are indicative of broader developments in the South Pacific, developments which included in 1970 the attainment of full independence by the Kingdom of Tonga and by Fiji. Economic, social, and educational development has made the peoples of the area more self-reliant. Students from certain English-speaking territories in the South Pacific undertake courses at the University of the South Pacific in Fiji under the New Zealand bursary scheme.

New Zealand in the United Nations—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 Nations' regular budget is 0.32 percent, in 1971 this meant a New Zealand contribution to the organisation of $433,784.

United Nations Security and Peace-keeping Activities—New Zealand Governments have acted upon the conviction that the United Nations, and it alone, contains the rudiments of a universal collective 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. At San Francisco in 1945 the Right Hon. Peter Fraser argued forcibly but unsuccessfully to eliminate the veto and to strengthen the collective security provisions of the United Nations Charter. Within the United Nations 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; and 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. New Zealand has been prepared to play its part; forces were supplied to the United Nations Force in Korea and military observers to the United Nations observer groups in Palestine, Kashmir, and Lebanon; and a civilian police unit has served in Cyprus.

New Zealand has recognised that the objective of developing the United Nations' potential in security and peacekeeping is a long-term one.

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 recognises 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 reapingtangible rewards. First the '60s and now the '70s have been designated as “development decades” and an international development strategy—an overall plan setting targets for development during the second decade—was adopted by the Twenty-fifth Anniversary Commemorative Session in 1970.

The United Nations Organisation 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 autonomous specialised agencies.

The biggest single task now facing ECOSOC is to promote and direct programmes for economic development in the less-developed countries. New Zealand had 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; and it was again elected by the General Assembly to serve over the period 1971-73. 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. Most recently, it served on the Commission on Human Rights for two consecutive terms covering the period 1966-71, and it is currently serving on the Population Commission for the period 1969-72.

Specialised Agencies—New Zealand is a member of all 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, exists 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 assessment similar to that used in the United Nations itself, range from $2,700 to $216,000 annually and totalled some $767,000 in 1971-72. 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. The ILO is concerned with protecting the basic dignities and freedoms of the wage earner and brings together representatives of governments, employers, and workers to frame international conventions on working and living conditions.

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 service of experts to developing countries (for example in physiotherapy, police work, forestry, and education) and donations of equipment or commodities.

Two major fields for this sort of additional assistance are the contributions made to the United Nations Development Programme and to the World Food Programme. New Zealand has given annual contributions to UNDP (in 1971-72 $500,000), 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 and FAO in 1961 and administered jointly by them. In 1963-70 New Zealand made total grants of US$1,670,000, of which US$610,000 was in cash and US$1,060,000 in commodities. For 1971-73, New Zealand has pledged a further US$840,000, of which US$280,000 will be in cash and US$560,000 in commodities. New Zealand is a member of the inter-governmental committee which supervises the programme.

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 is also a foundation member of the Asian Development Bank, established in 1967 under the auspices of ECAFE “to foster economic growth and co-operation in the ECAFE region”.

New Zealand has supported agency activity which will help the social and economic development of the Pacific Islands and some projects are now listed. WHO has assisted in the past in the eradication of yaws and tuberculosis; FAO is at present the executing agency for a UNDP project designed to control the rhinoceros beetle which ravages much of the islands' coconut crops, and has also established a regional fisheries development agency; UNESCO has set up a curriculum development unit at the University of the South Pacific; a development assistance team, backed by ECAFE and the specialised agencies, is being established in Suva.

New Zealand has in the past served on the governing bodies of WHO, FAO, UNESCO, and UPU, and is a member of the FAO Council for 1970-72. 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.

Conference on Trade and Development (UNCTAD)—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 held its second session in New Delhi early in 1968. UNCTAD is the United Nations body generally responsible for all matters relating to trade development. It is open to all United Nations members and other states who are 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, manufacturers, finance invisibles, and shipping. New Zealand held a seat on the Committee on Commodities from 1967 to 1969, and the Committee on Shipping from 1969 to 1971. The second UNCTAD conference was held in Delhi in 1968 and the third conference was convened in Santiago, Chile, in April 1972.

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 some of 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 Collective Security—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 the provisions of the United Nations Charter 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 to collective security action on several occasions both within the United Nations and under other arrangements. From 1955, military units were based in Malaya as part of the Commonwealth Strategic Reserve, where they took part in actions during the emergency. New Zealand forces later supported Malaysia in itssuccessful resistance to Indonesian Confrontation. In 1965 an artillery battery was sent to South Vietnam under the Manila Treaty. It was subsequently joined by two infantry companies and a small Special Air Services troop. Force strengths rose to 560 before the beginning of withdrawals in 1970. All combat forces were withdrawn from South Vietnam at the end of 1971. Some 30 army personnel remained in a training role.

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. It assured New Zealand and Australia of American support in the event of aggression in the Pacific.

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 the 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”.

In keeping with the close ties between the three countries, the machinery for consultation has been kept as simple and flexible as possible. Meetings of a council of ministers are generally held once a year to review situations affecting the treaty area.

SEATO—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 came into force 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 process. 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 (SEATO) established under the treaty is headed by a council, made up of the foreign ministers of the signatory governments, which meets annually in members' capitals. Between meetings a body known as the Council Representatives provides continuity with representation generally provided by 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. The civil and military secretariat has its headquarters at Bangkok.

The Manila Treaty 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”. The military planning and exercises carried out under the treaty are valuable in improving the capacity of the members to act together against aggression.

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 recognised by making provision in the treaty for the parties, separately and jointly, to increase their capacity to counter subversion and to co-operate in economic measures to promote economic progress and social well-being. While most of this action is taken outside the framework of SEATO, the organisation 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 ofthe farming problems of the South-east Asian member governments has recently been initiated; New Zealand has contributed one expert to this programme. Seminars and study groups have been organised to consider particular problems. Cultural exchanges have been promoted. The New Zealand Government funded $20,000 a year from which to contribute to SEATO aid programmes.

Commonwealth Arrangements—Throughout the past two decades a defence arrangement known as ANZAM provided a further basis for New Zealand's co-operation in defence matters with Britain and Australia. In November 1971, following changes in Britain's role east of Suez, ANZAM was succeeded by an arrangement known as ANZUK. Unlike SEATO and ANZUS, ANZAM and ANZUK are not organisations established by formal treaty but have gradually evolved from the practice of close defence co-ordination among the three countries. ANZUK provides an important forum for consultation on defence matters of common concern to Australia, New Zealand, and the United Kingdom. The three Governments, however, retain full control over their individual defence policies. ANZUK meetings are usually held in Canberra.

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 its formation in September 1963 and renamed the Anglo-Malaysian Defence Agreement (AMDA). Under its provisions, the United Kingdom undertook to assist in the defence of Malaysia and was accorded the right to maintain such forces in Malaysia, including a Commonwealth Strategic Reserve, as were agreed to be necessary for the defence of Malaysia and for the fulfilment of Commonwealth and international obligations. The agreement was accepted as applying generally to Singapore when it acceded to independence in 1965. In 1959 New Zealand, together with Australia, was associated with AMDA by an exchange of letters, placing on record that the provisions of the agreement applicable to the Commonwealth Strategic Reserve, in particular the provisions dealing with the status of forces, applied in respect of New Zealand forces in the reserve.

In January 1968 the British Government announced that its forces in South-east Asia would be withdrawn by the end of 1971. In February 1969 the New Zealand Prime Minister announced that the Government had decided to retain, in conjunction with Australia, a military presence in Malaysia and Singapore after the British withdrawal. A series of five-power meetings were held at official and ministerial level to discuss defence questions arising from the British decision to withdraw. During these meetings Malaysia and Singapore declared that the defence of the two countries was indivisible and Britain outlined the form its continuing interest would take, including its capability to assist in the event of a threat to peace and its intention to continue exercises and training in the area.

With the change of government in Britain in June 1970 the decision was taken to retain a British ground presence in Malaysia and Singapore. This presence was, however, to be on a smaller scale than previously and, in view of the nature of the continuing arrangement, the British upheld the earlier decision that AMDA should be revoked in 1971.

In place of AMDA, a new five-power defence arrangement for Malaysia and Singapore came into being on 1 November 1971. The new arrangement is less formal than AMDA and is based on the concept of partnership of the five participating countries. The basis of the five-power defence arrangement is not a formal treaty or agreement but a statement incorporated in the communique of the meeting of ministers of the five-power countries held in London in April 1971. At that meeting the ministers declared, in relation to the external defence of Malaysia and Singapore, “that in the event of any form of armed attack externally organised or supported or the threat of such attack against Malaysia or Singapore, their governments would immediately consult together for the purpose of deciding what measures should be taken jointly or separately in relation to such attack or threat”. The Ministers agreed to establish an Air Defence Council to provide direction to the Commander of an Integrated Air Defence System for Malaysia and Singapore which was established on 1 September 1971; they also decided to set up a Joint Consultative Council to provide a forum for regular consultation at senior official level on matters relating to the defence arrangement.

New Zealand's military contribution to the five-power defence arrangement includes one battalion, a frigate regularly stationed at Singapore, medium-range transport aircraft and helicopters; and strike aircraft periodically deployed to the area from New Zealand. Underlying New Zealand's participation in the five-power defence arrangement is the belief that defence co-operation of thiskind contributes significantly to the maintenance of stability and the continuation of development in the region as a whole. The five-power defence arrangement contributes to the security of Malaysia and Singapore. ANZUK forces are helping Malaysia and Singapore to build up their own defence establishments by supplementing their capabilities in the field of sophisticated equipment and by providing training assistance. It has always been made clear that the New Zealand presence will be maintained only as long as it has the consent and encouragement of the Governments of Malaysia and Singapore. New Zealand forces will not be involved in internal security problems and their deployment on active operations will require the express consent of the New Zealand Government.

New Zealand Aid—New Zealand's aid to developing countries takes many forms—capital aid (cash grants and equipment), technical assistance (the provision of experts and student training), food aid, and loans. It is channelled through a number of diverse programmes; multilateral, bilateral, and non-Governmental.

New Zealand has for many years played an active role in multilateral schemes initiated by the United Nations and its specialised agencies, e.g., the United Nations Development Programme, the World Food Programme, the United Nations Children's Fund and the programmes of aid to refugees.

The largest individual bilateral programme is the Colombo Plan, the main vehicle for the New Zealand Government's civil aid to South and South-east Asia. Other bilateral programmes undertaken by New Zealand include those involving the Cook Islands, Niue Island, the Tokelau Islands, and Western Samoa. Bilateral aid to Asia under the Colombo Plan amounted to $4,621,741 in the 1970-71 financial year, while aid to the islands of the south-west Pacific totalled $4,317,838.

Contributions to the Asian Development Bank amounted to $1,007,143 in the 1970-71 financial year and formed an important adjunct to New Zealand's bilateral aid to Asia.

Other programmes in which the New Zealand Government participates include the Special Commonwealth African Assistance Plan under which African students are brought to New Zealand for higher education and special training courses; the Commonwealth Education Scheme under which students and scholars from developing countries study in New Zealand; the Commonwealth Medical Scheme and the Commonwealth Programme for Technical Co-operation.

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 an 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 1971, New Zealand has made available under the Colombo Plan capital aid and technical assistance amounting to $43,114,362.

The major capital aid projects with which New Zealand has been associated in 1970-71 include dairy schemes in India, a road building programme in north-east Thailand, aviation assistance to Indonesia and Thailand, the Indus Basin Development Scheme in Pakistan and provision of equipment to trade training schools in Burma. Total expenditure on capital aid has amounted to $25,495,378 including $2,033,864 in the 1970-71 financial year.

Up to 31 March 1971 New Zealand has spent a total of $10,851,213 on student training and $6,767,711 on the provision of experts, advisers, and consultants. The number of students and trainees brought to New Zealand under Colombo Plan awards had reached 3,218, of whom 578 were in New Zealand on 31 March 1971. Experts who have served in Asia under the Colombo Plan had reached 513 by the same date. Major technical assistance projects overseas include the provision of a road construction team in north-east Thailand, a civilian surgical team in Vietnam, and teachers for Malaysia. Consultants from the private sector have also been engaged under the Colombo Plan on a wide range of technical assistance projects of a substantial nature. These include forestry, water reticulation, road design, beef cattle development, port surveys, architectural design, and prefabricated buildings.

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. At 31 March 1971 there were 120 volunteers in the field. The Government grant to VSA during the 1970-71 year was $71,665.

Distribution of New Zealand Aid—The distribution of New Zealand Government aid to overseas countries during the two latest financial years is set out in the following table. The aid is shown as bilateral where the arrangements were concluded directly between the New Zealand Government and the government of the recipient country or countries 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 in cash and kind through CORSO and other private organisations.

General Aims—New Zealand's foreign policy has changed in emphasis and scope. It has 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.

New Zealand has accepted a growing involvement in the problems of the South Pacific region because of its close ties with the island people. 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 Pacific power, New Zealand has sought security in friendship and formal defensive arrangements with Australia and the United States. 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. 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 monarchial State; it is also a constituent member of the Commonwealth, sharing with other members in “their recognition of the Crown as the Symbol of their free association and of the Sovereign as the Head of the Commonwealth...” (Preamble to Royal Titles Act 1953.)

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.

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 stead 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, in 1963 and in 1970. 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 of the Statute of Westminster in 1947 laws could not be made 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.

The Electoral Act 1956 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:

These reservations have become a formal convention associated with the fundamental character of the system of government.

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 and caucus.

With the increasing range and complexity of the statutory field, there has been a growth in delegated legislation with detailed procedural steps and other amplifying matter becoming the subject of regulations made by Order in Council under the authority of a particular statute, rather than being incorporated in the statute itself. The power to make such regulations lies with the Executive Councilwhich comprises all the members of Parliament who have been appointed Ministers, together with the Governor-General, who presides over the Council. 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. The Standing Orders of the House of Representatives, enable 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 has traditionally covered 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 adjournments.

In session parliamentary privileges 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 but lost it at the 1969 election. At any general election these parties, together with any other political parties and also those candidates standing as independents, state their respective policies before the electors. Each main party normally puts forward one candidate for each of the 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 has a mandate to govern and the minority party has a responsibility to challenge Government measures in debate and to demonstrate to the electors that it can provide a viable alternative government.

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. The election of the 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 the possibility of the Opposition mustering sufficient support to pass a resolution of no-confidence in the Government on a vital issue, thus forcing it to resign. With only two main disciplined political parties contending for office, changes of government are now rare except at the time of general elections. In the representation and formation of public opinion the major general debates are of principal importance. Special inquiries by select committees also provide a useful forum in which interests and opinions can make themselves heard. The major general debates are the address in reply to the speech from the Throne at the opening of Parliament, the debate on the Budget or financial statement, and the various debates on Imprest Supply Bills.

The first two of these give ordinary members an opportunity to air their views freely on any subject they choose from the national interest to the special aspirations of their constituents. Imprest supply debates are more specialised. On such Bills, the British principle of raising grievances before granting supply has been applied by allowing the Opposition to choose the subject for debate.

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.

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 decisions taken in Cabinet. 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 which is a debate on its general principles, followed by a clause-by-clause consideration of the Bill which may be by the whole House sitting in Committee. The Bill is then reported to the House, and later read a third time. 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 as an Act of Parliament. To facilitate detailed informal discussion, and so that evidence from experts and interested parties may be heard by the House on legislation which is before it, a number of select committees are appointed regularly each year. Their terms of reference indicate areas of legislative interest corresponding to the various ministries. There are normally 10 members on each committee and party strength roughly reflects party strength in the House. Bills which are to go to select committees are given only a pro forma second reading before being referred. Committees have power only to report their opinions to the House. They cannot amend, though they can recommend amendments. The House as a whole thus retains its responsibility for approving legislation or rejecting it.

Apart from legislation, select committees deal with petitions, and, from time to time, ad hoc select committees are set up with some specific matter referred to them.

There are special procedures for dealing with local Bills and private Bills. Local Bills are those affecting a particular locality only, normally introduced at the request of a local authority. All such Bills stand referred to a select committee, the Local Bills Committee, after their first reading. The committee holds hearings at which interested parties appear, and it reports to the House on the merits of the Bill. The committee's report is often the decisive factor in local government legislation and always carries considerable weight with the Government and the House. Private Bills are those which apply specifically to a person or group of persons. They are initiated, after public notice, by a petition presented to the House by a member.

Duration of Parliaments—Quinquennial Parliaments, instituted under the Constitution Act, were abolished by the Triennial Parliaments Act 1879, which fixed the term at 3 years. General elections have been held at 3-yearly intervals since 1881, with a few exceptions. The term of the nineteenth Parliament was during the First World War extended to 5 years by special legislation, and that of the twenty-fourth (1931-35) to 4 years under the Electoral Amendment Act 1934. By the Electoral Amendment Act 1937 the 3-year term was restored, but on account of war conditions the term of the twenty-sixth Parliament was extended to nearly 5 years before dissolution on 30 August 1943. Since then the duration of Parliament has been of 3 years, with the exception that the twenty-ninth Parliament was dissolved in 1951 after the expiration of approximately 20 months. The 3-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 3 years.

Number of Representatives—In 1969 84 electorates (80 European and four Maori) returned 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 37 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; 870, at 74; in 1875, at 84; in 1881, at 91; in 1887, at 70; in 1900, at 76; and in 1969 at 80. 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 thequota fixed for the South Island. In 1967 the Commission considered the results of the 1966 census and fixed the number of electorates in the North Island at 55 (an increase of three). Thus there were 84 electorates for the general election in 1969, and the number was increased to 87 for the 1972 election.

Qualifications of Members—Under the Electoral Act 1956 every registered elector of either sex is qualified to be a parliamentary candidate. If a public servant is elected to Parliament he must vacate 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 5 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 3 months after the date of every general election of members of Parliament. At April in the intervening years adjustments are made on a basis matching that for the State Services Remuneration and Conditions of Employment Act 1969; the Government Statistician provides the Prime Minister with a certificate specifying the percentage movements in average weekly ordinary time earnings outside the State Services (as ascertained from the April half-yearly survey of industries in the private sector conducted by the Department of Labour) and adjustments may be made by Order-in-Council to the salaries of Ministers and members.

The following table sets out the salaries and allowances payable from 1 April 1971 in accordance with the recommendations of the Royal Commission upon Parliamentary Salaries and Allowances 1970, as amended by the 1971 review conducted in accordance with the procedure outlined in the preceding paragraph.

There is an additional allowance depending on classification of electorates: (a) electorates which are wholly urban, $90; (b) electorates which are substantially urban, $230; (c) electorates which are partially urban and partially rural, $250, (d) electorates which are ordinary rural, $920; (e) electorates which are predominantly rural, $1,150. The special additional allowance for Southern Maori electorate is $350 and for each of the other Maori electorates is $175. The daily sessional allowance is $3 and the night allowance for members entitled thereto is $8. In addition to the salary and allowances, members are entitled to certain travel concessions and a stamp 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.

Under the Superannuation Act 1956 there is a compulsory contributory superannuation scheme for members of the House of Representatives. The scheme provides that a retiring allowance shall be payable to a member after 9 years' 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 11 percent of an ordinary member's salary, and the Government subsidises the fund. The rate of contribution was increased by 1 percent from 1 April 1970 to provide for cost-of-living adjustments to be made to retiring allowances. 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 60 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.

A Minister may have more than one portfolio and in addition responsibility for the supervision of one or more Government departments in which the activities carried out, though important, do not rank as portfolios. Occasionally a Minister is appointed without portfolio, as in 1969 when the Associate Minister of Finance had no portfolio responsibility.

Executive Council—In the legal sense those members of Parliament who have been appointed Ministers comprise the Executive Council. The Governor-General normally presides over meetings of the 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.

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 January 1972 the Executive Council consisted of 18 members. Two members, exclusive of His Excellency or the presiding member, constitute a quorum.

His Excellency the Governor-General receives a salary and an allowance which are determined from time to time by the Civil List Act 1950 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—The membership of the Executive Council and Cabinet is identical but Cabinet, unlike the Executive Council, is not a body created by any legal document. The existence of Cabinet was not recognised by statute until a passing reference was made in the Parliamentary Commissioner (Ombudsman) Act 1962.

The fact that the Juridical Acts 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 or a Statutory Commission—does not diminish the power and authority of Cabinet. Cabinet is the top committee of the administrative system, with responsibility for co-ordinating the work of the various Ministers and taking those decisions which largely determine the nature of the legislation put before Parliament and the regulations which the Executive Council is asked to approve.

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. 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.

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, Ministry of Foreign 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 Welfare 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.

OMBUDSMAN—The Parliamentary Commissioner (Ombudsman) Act 1962 has become an important addition to the parliamentary checks on departmental administration. The Act created the office of Ombudsman, who is able to investigate, on complaint or on his own initiative, any administrative decision, recommendation, act, or omission of a Government department or related organisation as it affects any individual. Local authorities are outside his jurisdiction. The Ombudsman does not have power to reverse departmental decisions, but he may make his recommendations to the department and to the Minister, and if, in his opinion, no appropriate action is taken he may report to the Prime Minister and then to Parliament. He has very wide powers to call for documents and files. The Government cannot refuse information, except in matters relating to the security of the State or to Cabinet proceedings.

JUDICIARY—The hierarchy of courts in New Zealand comprises the Court of Appeal, the Supreme Court, and the Magistrate's 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.

PARLIAMENTARY ELECTIONS—The law on elections is contained in the Electoral Act 1956 Following each population census, which is normally taken every 5 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. 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 1 month is given during 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 define the new electoral districts.

All general elections and by-elections are held on a Saturday. Polling hours in all electorates are from 9 a.m. to 7 p.m.

Any serviceman aged 20 years or over serving overseas is qualified to vote as an elector of the electoral district in which he last resided before he left New Zealand.

Franchise—Since 1969, persons 20 years of age and over have had the right to vote in the election of members of the House of Representatives. (From 1893 onwards all persons aged 21 years had voting rights.)

Registration of Electors—Registration as an elector is compulsory, although it is not compulsory to vote. To be qualified for registration as a parliamentary elector in New Zealand a person must have attained the age of 20 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 3 months or more in the electoral district in respect of which application for registration is made, and not have subsequently resided for 3 months or more in any other electoral district. Broadly speaking the qualifications restrict the right to vote to permanent residents. Persons of more than half Maori ancestry register in one of the four Maori electoral districts and persons of half Maori ancestry have the option of registering on either a European or Maori roll.

Voting at parliamentary elections is by secret ballot. 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.

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 for reasons of distant travel on polling day, sickness, etc.

LOCAL GOVERNMENT—In 1876 territorial local government assumed the form it still basically retains. The Counties Act 1876 divided the country into 63 counties, with provision for administration by elective 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.

Boroughs—Dealing with the needs of concentrated urban populations, boroughs are concerned with a wide range of functions. With the growth and urbanisation of population the number of boroughs, despite numerous amalgamations of adjacent boroughs, steadily increased until 1955 when the total was 146. In April 1971 the total was 137.

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.

Counties—Counties are now governed under the Counties Act 1956. With increasing settlement the original 63 counties were gradually subdivided until they reached 129 in 1920, although the number of councils formed and actively functioning never exceeded 126. The number of counties has since been reduced by amalgamations and mergers by the Local Government Commission. At April 1971 there were 109 counties constituted, of which 108 were actively functioning, Fiord being a sparsely populated county in which the Counties Act is not wholly in force.

County Towns and County Boroughs—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 3 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. The county council may conduct a poll in the county town to ascertain the wishes of the electors of the county town in respect of the persons to be appointed to this committee. There was a total of 100 county towns at April 1971. Twenty-nine of these had populations of over 1,000 the largest being Glenfield with a population of over 22,000. The Counties Amendment Act 1968 contains provisions for the constitution of county boroughs. This unit of local government can only be formed from an existing county town or borough or town district. It remains an integral part of the parent county, but the county borough council, which is a fully elected body, has a statutory right to exercise some, but not all, the powers of the county council within the district of the county borough. The minimum population required for a county borough is 1,500. At April 1971 there was only one county borough.

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. Where it remains subject to county control (mainly for roads) it is a dependent town district. Town districts on reaching a population of more than 500 may become independent. 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 requires that the area 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. The number of town districts in April 1971 was 16 (10 independent and 6 dependent).

Remuneration of Members—The remuneration of members of local authorities is governed by the statutes constituting the various types of local authorities. Most authorities may pay their chairman an annual allowance with a maximum fixed for each type of authority. The maximum payable to mayors and town council chairmen varies according to the population of the municipality. Ordinary members of territorial authorities may be paid for each meeting attended. All local authorities may reimburse members for expenses incurred whilst travelling on official business.

Special-purpose Authorities—Special-purpose authorities differ from territorial authorities in that each is charged with only one major function. The need for the most efficient and economic discharge of the major function being the prime consideration, their boundaries may either extend beyond or fall within those of territorial authorities in the same geographical area. Only rarely do the boundaries coincide. Sometimes, as is the case with a number of urban fire authorities, territorial authorities themselves are also constituted as and perform the functions of special-purpose authorities. The more important special-purpose authorities are those administering harbours, hospitals and the retail distribution of electricity. Others are engaged in fire fighting, water supply, urban drainage and transport, soil conservation and rivers control, pest destruction, nassella tussock control, land drainage, and underground water usage.

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.

A local authority has no legislative powers beyond the authority to make bylaws within limits defined in its constituting Act, but it can promote legislation on matters which affect the government of the area under its jurisdiction and which it is not already empowered to deal with. If the subject is transient and not contentious and is approved by Government it is usually dealt with by the inclusion of an appropriate section in the annual Local Legislation Act passed by Parliament for this purpose. If, on the other hand, the local authority seeks powers of a permanent or major nature additional to those conferred on it by general Acts it must submit to Parliament a special local Bill. The extent to which the foregoing privileges are used may be gauged from the fact that the annual Local Legislation Act usually contains 40 to 45 sections, while about 15 local Acts are passed each year.

Number of Local Authorities—The number of local authorities actively functioning at 1 April 1971 was 640 made up as follows: county councils, 108; borough (including city) councils, 137; town councils (independent), 10; town councils (dependent), 6; catchment authority, 1; river boards (2 boards also have the power of land-drainage board), 8; catchment boards, 13; catchment commissions, 4; land-drainage boards, 37; electric power boards, 39; water-supply boards, 2; urban drainage boards, 4; transport board, 1; local railway board, 1; museum authority, 1; power and gas boards, 2; 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), 149; independent fire boards, 60; independent harbour boards, 17: and hospital boards, 31. Borough and county councils also function as fire authorities in 199 cases, as harbour boards in 9 cases, as underground water authorities in 2 cases and as county pest destruction boards in 40 cases. In addition, there were 22 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 geographical boundaries of a county, are regarded as separate entities.

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.

Apart from a few special-purpose authorities some of whose members are appointed by other local authorities, by Government, or, in the case of fire authorities, by insurance interests, members of local authorities are elected triennially, any qualified elector being eligible to seek election. In general the franchise extends to all persons aged 20 years or over who either possess a rating qualification or who, being British subjects, possess a residential qualification in the district of the local authority concerned. The right to vote for members of land drainage and river boards is, however, restricted to those who possess rating qualifications. Plural voting on the basis of the value of rateable property is permitted in elections for county councils and several types of special-purpose authorities. Where pest destruction boards rate on the basis of livestock or acreage, plural voting is also permitted.

Voting Procedures—Franchise could only be exercised by personal attendance at the polling booth, but the Local Elections and Polls Act 1966 was amended in 1970 to permit local authorities to use postal voting. (Authority to use postal voting is limited to county councils. Other local authorities are able to use this method only on approval being granted by Order in Council.)

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 or as soon as possible thereafter. 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.

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 3 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.

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.

By 31 March 1971 there were 127 operative schemes with a further 70 schemes at the recommendation stage; although 59 councils had yet to submit schemes, more than 90 percent of the population are living in areas where councils have brought down recommended, proposed, or operative district schemes.

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 5 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.

POPULATION GROWTH—New Zealand's first million of population was recorded in 1908, 68 years after the signing of the Treaty of Waitangi. In 1952, 44 years later, the second million was reached, and the third million is expected to be reached in the mid-1970s.

Population has two sources of gain—natural increase (excess of births over deaths) and net migration (excess of arrivals over departures). In the early years in New Zealand, as in every young country, the bulk of the increase was through migration. From the late 1870s natural increase permanently displaced immigration as the chief contributor to population growth. At the census of 1881 the percentages of the total population born in New Zealand and born overseas were approximately equal (50.2 percent New Zealand born to 49.8 percent overseas born), and each succeeding census until 1961 recorded an increased proportion of the population as having been born in New Zealand. In 1966 it dropped from 86 to 85.2 percent, partly as a result of international travel and tourism; more New Zealanders were overseas and more tourists were in New Zealand.

During the present century, natural increase has accounted for over three-quarters of the growth of population.

The natural increase rate has, in the main, closely reflected the changes in the birth rate, with a low point of 8.68 per 1,000 in 1935 and high points of 18 per 1,000 in 1947 and 1961. The 1966 figure of 13.57 was the lowest since 1944. In more recent years it has been 13.98 in 1967, 13.72 in 1968, 13.79 in 1969 and 13.23 in 1970. Like the low birth rate of the thirties, the fall in the birth rate in recent years is a feature that New Zealand has shared with a number of other developed countries, and notably with Australia, Canada, and the United States.

Details are given in the following table.

Migration, however, has continued to add to the population quite substantially except during depression and war periods and the recession conditions of 1968-69. Gains from external migration are 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. A changed economic climate in the country brought a net migration loss to population for 1967, 1968, and 1969 calendar years.

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, e.g., cities and boroughs, also take into account local economic developments, housing schemes, 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 6 years of international war, and of 1966-71 mainly attributable to a marked change in migration patterns.

COMPARISON WITH OTHER COUNTRIES—The annual average percentage increases of population for the period 1963-68 are given in the following table for certain selected countries. (Source: United Nations Statistical Yearbook.)

INTERCENSAL RECORDS—Intercensal estimates of total population are prepared from the records of vital statistics and of external migration. The figures in the tables following have been revised in line with 1971 Census results.

The 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 New Zealand Maoris.

The following table shows the New Zealand Maori population.

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

The following diagram presented on a ratio scale shows the growth of actual population from 1880 to 1968 and projections through to 2000

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 NZ 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 NZ 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 1966 and 1971 Censuses. At the 1971 Census the North Island population was 2,051,363, including 213,577 NZ Maoris, and the South Island population 811,268, inclusive of 13,837 NZ Maoris. The increase since the 1966 Census was 158,037 for the North Island and 27,675 for the South Island.

Between the 1966 and 1971 Censuses, births in the South Island numbered just over 82,000, and deaths almost 38,000, giving a net natural increase of just over 44,000. The fact that the total population increase is under 28,000 indicates a net migration outflow from the South Island during the intercensal period. This is in contrast to the 1961-66 intercensal period when a small net migration inflow of approximately 5,000 was recorded.

Statistical Areas—The boundaries of statistical areas are shown on the map inside the back cover.

In the following table are shown the approximate areas and the populations of the statistical areas as at the Censuses of March 1966 and March 1971.

Statistical Divisions and Urban Areas—Statistical divisions and 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. Statistical divisions are a new concept. The basic criterion for a statistical division is a population of 75,000 or more within the area of economic and social interests of a heavily populated centre. Seven statistical divisions have been established, namely, Auckland, Hamilton, Napier-Hastings, Palmerston North, Wellington (including Hutt), Christchurch, and Dunedin. The division, like the urban area, does not have any administrative functions, but embraces areas of unified community, economic, and social interests. In addition to the central city or borough, urban areas include neighbouring boroughs and town districts and parts of counties which are regarded as suburban to the centre of population. Maps of statistical boundaries are available at Government bookshops.

Previously there have been 18 statistically defined urban areas; there are now 24 urban areas. The additional areas result from splitting the Auckland, Wellington, and Hutt urban areas and adding Masterton. Adjustments of urban area boundaries have been made because of the peripheral growth of population in some of the urban centres.

In the following table the populations of statistical divisions and urban areas are given.

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 1971 Census. The parent county is shown in parentheses. The populations of county towns are included in the administrative county populations given in the table following.

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 5,317 people at 1971 Census (23 March).

Counties—The following table gives the population of individual counties at the 1971 Census of Population on 23 March, 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.