THE NEW ZEALAND OFFICIAL YEAR-BOOK, 1944

LOCATION, AREA, AND BOUNDARIES.–Consisting of two large and several smaller islands, the Dominion of New Zealand lies in the South Pacific Ocean some 1,200 miles to the eastward of Australia. With South America some 6,000 miles distant to the east and the Antarctic Continent 1,600 miles distant to the south, the Islands are, for their size, among the world's most isolated. For statistical purposes, the following classification of the administrative area is the most convenient:–

The total area of the foregoing groups is 103,935 square miles. Elsewhere in this issue (viz., in the section on land tenure, settlement, &c.) the aggregate area of the Dominion appears as 66,390,697 acres—i.e., 103,735 square miles. The latter area does not include the Cook and other Pacific Islands annexed in 1901.

As well as exercising jurisdiction over the areas already mentioned, the Dominion also administers the Union Islands, the Ross Dependency, and Western Samoa (which is held on a mandate from the League of Nations). Jointly with the Imperial Government and the Government of Australia, New Zealand is responsible for the mandate over the Island of Nauru. The administrative appointments for the island are made by the Australian Government, but New Zealand appoints a representative to the British Phosphates Commission, which controls the working of the phosphate deposits.^*

The Island Territories Act, 1943, provides for the appointment of a member of the Executive Council as Minister of Island Territories. This Minister is charged with the administration of the government of any territory out of New Zealand which may at any time be a dependency or mandated territory of the Dominion, or otherwise be under the jurisdiction of the Government or Parliament of the Dominion.

The relevant Proclamations, &c., defining from time to time the administrative area of the Dominion are given in the following paragraphs.

The Proclamation of British sovereignty over New Zealand, dated the 30th January, 1840, gave as the boundaries of what was then the colony the following degrees of latitude and longitude: On the north, 34° 30´ S. lat.; on the south, 47° 10´ S. lat.; on the east, 179° 0´ E. long; on the west, 166° 5´ E. long. These limits excluded small portions of the extreme north of the North Island and of the extreme south of Stewart Island.

In April, 1842, by Letters Patent, and again by the Imperial Act 26 and 27 Vict., c. 23 (1863), the boundaries were altered so as to extend from 33° to 53° of south latitude and from 162° of east longitude to 173° of west longitude. By Proclamation bearing date the 21st July, 1887, the Kermadec Islands, lying between the 29th and 32nd degrees of south latitude and the 177th and 180th degrees of west longitude, were declared to be annexed to and to become part of the then colony of New Zealand.

By Proclamation of the 10th June, 1901, the Cook Group of islands, and all the other islands and territories situate within the boundary-lines mentioned in the following schedule, were included as from the 11th June, 1901:–

A line commencing at a point at the intersection of the 23rd degree of south latitude and the 156th degree of longitude west of Greenwich, and proceeding due north to the point of intersection of the 8th degree of south latitude and the 156th degree of longitude west of Greenwich; thence due west to the point of intersection of the 8th degree of south latitude and the 167th degree of longitude west of Greenwich; thence due south to the point of intersection of the 17th degree of south latitude and the 167th degree of longitude west of Greenwich; thence due west to the point of intersection of the 17th degree of south latitude and the 170th degree of longitude west of Greenwich; thence due south to the point of intersection of the 23rd degree of south latitude and the 170th degree of longitude west of Greenwich; and thence due east to the point of intersection of the 23rd degree of south latitude and the 156th degree of longitude west of Greenwich.

By Imperial Order in Council of the 30th July, 1923, the coasts of the Ross Sea (in the Antarctic regions), with the adjacent islands and territories, were declared a British settlement within the meaning of the British Settlements Act, 1887. This region was named the Ross Dependency and placed under the administration of the Governor-General of New Zealand. The dependency is uninhabited.

By Imperial Orders in Council of the 4th November, 1925, the Union or Tokelau Islands (consisting of the islands of Fakaofu, Nukunono, and Atafu, and the small islands, islets, rocks, and reefs depending on them, a total area of only four square miles) were excluded from the Gilbert and Ellice Islands Colony, and placed under the administration of the Governor-General of New Zealand. In accordance with a provision of the second of these Orders in Council, the Governor-General's authority and power in connection with the administration of the islands were, by New Zealand Order in Council of the 8th March, 1926, delegated to the Administrator of Western Samoa.

* The island of Nauru is at present (April, 1944) under Japanese occupation.

GEOGRAPHICAL FEATURES–Coast-line.–By reason of its elongated shape, New Zealand possesses a very lengthy coast-line in proportion to its area. With the exception of the low-lying North Auckland peninsula, the length of the New Zealand land-mass lies along a south-westerly-north-easterly axis, parallel to the direction of its mountain-chains.

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

Mountains.–The mountainous nature of New Zealand is one of its most striking physical characteristics. In the North Island the higher mountains occupy approximately one-tenth of the surface; but, with the exception of the four volcanic peaks of Egmont (8,260 ft.), Ruapehu (9,175 ft.), Ngauruhoe (7,515 ft.), and Tongariro (6,458 ft.), they do not exceed an altitude of 6,000 ft. Of these four volcanoes only the first-named can be classed as extinct. 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 South Island is much more mountainous than the North, but shows fewer manifestations of recent volcanic activity. Along almost the entire length of the Island runs the massive chain known as the Southern Alps, which attains its greatest height in Mount Cook (12,349 ft.), while no fewer than seventeen peaks exceed 10,000 ft.

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

In the 1931 issue of the Year-Book was given a list, not claimed as exhaustive, of 223 named peaks of 7,500 ft. or more in altitude, while the 1942 and intervening issues of the Year-Book have contained a list of the more important mountains, together with details of height in each case.

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Glaciers.–In keeping with the dimensions of her 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, this glacier has a length of 18 miles and a width of 1 ¼ 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 ¼ 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 ¾ miles -and 8 ½ miles respectively, and terminal faces at altitudes of 670 ft. and 690 ft.

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

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

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

In the 1932 Year-Book appears an account of the rivers of New Zealand by Professor R. Speight, M.Sc., F.G.S., Curator of the Canterbury Museum. The 1942 issue contains a list of the more important rivers, with details of their length and, in some cases, the approximate rate of discharge.

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

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

Lakes.–In considering New Zealand's numerous lakes, a distinction can be made, especially from the scenic viewpoint, between the lakes of the two Islands. Surrounded by extremely rugged country the larger lakes of the South Island are distinguished by the grandeur of their alpine settings, while those of the North Island, situated on a volcanic plateau, are of interest by reason of the neighbouring thermal activity. Due to the excellence of their fishing, the latter possess an added tourist attraction. In both Islands the larger lakes are situated at high altitudes, and their consequent remoteness renders them unsuitable as a means of communication. In their functions as reservoirs the lakes of both Islands are of vital importance for the maintenance of the streams draining them and as a means of flood-prevention. More especially is this the case where hydro-electric schemes are involved, Lakes Waikaremoana and Taupo in the North Island, and Lakes Coleridge, Pukaki, and Tekapo in the South Island, being of particular significance in this respect.

An article on the lakes of New Zealand, also by Professor R. Speight, will be found in the 1932 Year-Book, while the 1942 issue contains particulars of the more important lakes.

GEOLOGY.–An article on the geology of New Zealand prepared by Dr. J. Henderson, M.A., F.R.S.N.Z., Director of the Geological Survey, is contained in the 1940 and earlier editions of the Year-Book. For more detailed information the reader is referred to the treatises of Professors Park and Marshall, the bulletins of the Geological Survey, and the many papers that have appeared in the “Transactions of the New Zealand Institute” (now the Royal Society of New Zealand).

EARTHQUAKES.–An article on earthquakes in New Zealand appeared in the 1942 and earlier issues of the Year-Book. The information given below has been supplied by Mr. R. C. Hayes, Acting-Director of the Dominion Observatory.

Seismicity and Earthquake Distribution.–A comparison between the records of destructive earthquakes in New Zealand and those in other seismic countries shows that the seismicity of New Zealand, on the whole, is surprisingly high. However, this is due to the occurrence of a large number of earthquakes of the semi-destructive type (R.-F. 8) with comparatively few major destructive shocks (R.-F. 9, 10).

During the period 1835-1934 sixty-nine destructive earthquakes are known to have occurred in New Zealand, forty-nine of which were of the semi-destructive type (not exceeding intensity R.-F. 8). Of the remainder, fourteen were of intensity 9, and six of intensity 10.

The total number of earthquakes of all intensities, and the maximum intensity, reported felt in New Zealand in each of the years 1922 to 1942 were as follows:–

The abnormally large number of earthquakes reported in the year 1922 was due to the swarm of local shocks in the Taupo region in the latter half of that year. Abnormally large numbers of shocks also occurred in 1929-30, due to aftershocks of the Buller earthquake of 17th June, 1929.

Earthquakes in 1942.—The seismic disturbances in the Wairarapa region in the latter half of 1942 commenced with a severe shock on the night of 24th June. This shock reached intensity R.-F. 9+ at places east and south-east of Masterton. The epicentre was located at a point approximately eight miles east of Masterton, where surface evidence of fault-movement was discovered. The shock was felt with diminishing intensity over most of New Zealand, from Auckland to near Dunedin. The intensity in Wellington varied between R.-F. 7 and 8.

On 2nd August a very severe shock occurred in the same region. This shock was nearly equal in magnitude to that on 24th June, but its slightly greater depth of origin rendered the surface effects less severe.

A third severe aftershock occurred on 2nd December. In addition, a very large number of smaller subsidiary shocks occurred. Up to 31st December approximately six hundred were recorded on the seismograph at Wellington. Only 7 per cent, of these were perceptible in Wellington.

Regional Distribution.—New Zealand earthquake statistics over the past hundred years or so show that certain parts of the country are subject to almost continuous seismic activity with occasional destructive shocks, while other parts are more or less free from seismic disturbances. By combining early earthquake records with the more precise data of recent years it is possible to divide the country roughly into four seismic regions.

These regions are classified below, in order of seismicity:—

The following table shows the average frequency of earthquakes in each of the four regions defined above.

The boundaries between the seismic regions are not well defined, since one region generally merges more or less imperceptibly into another. Further, seismic frequency is not uniform. This leads to the number of shocks being considerably above the average in some years and below it in others. The normal irregularity is increased by the occasional occurrence of earthquake swarms in certain regions. Probably the most notable swarm in New Zealand was that which occurred in the Taupo region in the latter half of 1922. The number of minor local shocks in this swarm was so great that only the stronger ones, or those affecting the adjacent region, were used in determining the average frequency of region I. Major earthquakes occur chiefly in the eastern and southern parts of region I.

Deaths due to Earthquakes.—During the period 1848-1942 the number of deaths recorded in New Zealand as due directly or indirectly to earthquakes was 284. Of these, 255 were due to the Hawke's Bay earthquake of 3rd February, 1931.

CLIMATE.—An article on the climate of New Zealand, supplied by Dr. M. A. F. Barnett, M.Sc., Ph.D., F.Inst.P., Director of Meteorological Services, was included in the 1942 and earlier issues of the Year-Book, but considerations of space preclude its repetition in this issue.

A Brief Review of 1942.—Frequent rains during the 1941-42 summer gave benefit to crops, but ripening and harvesting were delayed. Drier conditions in the north, however, caused the milk-production to decline rather early. There was excellent autumn growth, and fodder-supplies were more than ample for the favourable winter. Autumn-sown wheat made steady progress also. A cold snap towards the end of July checked pastures temporarily, and wet conditions on the east of the North Island near the end of August caused some deaths among new lambs. Lambing percentages, on the whole, were up to, or above, average. By October all young stock were thriving well. Some crops ripened earlier than desirable during the dry spell in the month of November, and a considerable amount of harvesting was successfully completed during December.

For the year as a whole mean temperatures were slightly milder than normal in all districts except Taranaki, Nelson, and Westland. Sunshine was below average, especially in the districts mentioned, as well as in the Waikato and Central Otago districts. North Auckland and Hawke's Bay were, however, sunnier than usual. The districts of the North Island where the rainfall exceeded the annual average were a belt extending from Cape Egmont across the central plateau to East Cape and the Wellington Provincial District south of the Manawatu Gorge. Rainfall was excessive over most of the South Island, especially in South Westland. Deficiencies occurred, however, in eastern districts from Christchurch to Invercargill and locally about Tasman Bay, the percentage departures being greatest in South Canterbury.

Seasonal Notes.—January was cool and changeable with frequent, but not excessive, rain. Cool temperatures continued during February, which was dull and humid for Hawke's Bay, where rainfall was heavy, while conditions were dry in Auckland, Taranaki, and Nelson. Towards the end of March temperatures became milder, and there was excessive rain, but North Auckland and South Canterbury were dry. April was a typical autumn month, being rather dry, except west of the Southern Alps. Several long-standing rainfall records were broken by the excessive falls in May, which was also an exceptionally dull month. Flooding occurred in the vicinity of Christchurch on the 24th. June, in contrast to May, was the driest on record for most places. The rest of the winter was comparatively mild, rain being frequent, particularly in July. Several districts in central New Zealand experienced severe flooding on the 13th and 14th July. September was a changeable spring month, with windy periods and frequent showers. Some hard frosts followed widespread snow showers on the 10th and 11th, and there was considerable thunderstorm activity on the 23rd and 24th. October was a mild, sunny month, with ample rain in the South Island, falls being very heavy there on the 23rd, when Central Otago received also a steady snowfall. Thunderstorms accompanied the final rains of November, which was a month of little really settled weather, and, for the fifth month in succession, mean temperatures over the Dominion were above normal. December was quite cool, with several windy spells. Except for the seriousness of the continued dryness prevailing in Hawke's Bay and the Manawatu, it was a fairly good month.

Summary of Meteorological Observations.—The observations from which the following summary was compiled for the year 1942 were taken at 09.00 hrs., N.Z. standard time.

For 1942 the mean sea-level pressure at 09.00 hrs., in millibars, was: Auckland, 1,017.4; Wellington, 1,015.2; Nelson, 1,015.3; Hokitika, 1,015.2; Christchurch, 1,013.2, Dunedin, 1,011.7.

PLANTS OF NEW ZEALAND.—Those desiring information on the flora and plant covering of New Zealand are referred to the article by Dr. W. R. B. Oliver, D.Sc., F.R.S.N.Z., which appeared in the 1940 and previous issues of the Year-Book, while a brief reference to the geographical distribution of the forest trees is made in the section of this Year-Book dealing with Forestry (Section 18). For more detailed information the following works may also be consulted: “Plants of New Zealand,” by R. M. Laing and E. W. Blackwell, ed. 4, 1940; “Manual of the New Zealand Flora,” by T. F. Cheeseman, ed. 2, 1925; “The Trees of New Zealand,” by L. Cockayne and E. Phillips-Turner, 1928; “The Forest Flora of New Zealand,” by T. Kirk, 1889; “New Zealand Trees and Shrubs and how to Identify Them,” by H. H. Allan, 1928; “New Zealand Ferns,” by H. B. Dobbie, ed. 3, 1931; “New Zealand Plants and their Story,” by L. Cockayne, ed. 3, 1927; “The Vegetation of New Zealand,” by L. Cockayne, ed. 2, 1928; “The Cultivation of New Zealand Plants,” by L. Cockayne, 1923; “The New Zealand Nature Book,” Vol. 2, by W. Martin, 1929; and numerous articles published in the Transactions of the Royal Society of New Zealand.

FAUNA.—A brief article on the fauna of New Zealand, originally prepared by the late Mr. James Drummond, F.L.S., F.Z.S., and revised by him in 1935, is contained in the 1940 and earlier editions of the Year-Book.

EXECUTIVE COUNCIL.—The powers, duties, and responsibilities of the Governor-General and the Executive Council under the present system of responsible government are set out in Royal Letters Patent and Instructions thereunder of 11th May, 1917, published in the New Zealand Gazette of 24th April, 1919 (p. 1213). 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 His 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.

At present (April, 1944), the Executive Council consists of thirteen members in addition to the Governor-General, and also in addition to the two members of the War Cabinet who are not members of the Government Cabinet, and one member of the Legislative Council holding a special war portfolio. Two members, exclusive of His Excellency or the presiding member, constitute a quorum.

Under the Civil List Act, 1920, His Excellency the Governor-General receives an honorarium of £5,000 per annum, an allowance of £2,000 per annum for the salaries and expenses of his establishment (exclusive of the Official Secretary), and an allowance of £500 per annum for travelling-expenses.

The Prime Minister's salary is at the rate of £1,800 per annum and that of other Ministers £1,170 per annum. In addition Ministers of the Crown occupy a Ministerial residence, or receive house allowance at the rate of £200 per annum.

Authority is also given in the Civil List Act for the appointment of either one or two Maoris or half-castes as members of the Executive Council representing the Native race. One such appointment was made on 21st January, 1941, the salary being £990 per annum, plus £200 per annum house allowance.

The present Government, shortly after assuming office, instituted a scheme whereby the services of all parliamentary representatives of the Government party might be co-opted to assist Ministers in bringing the Government's policy into effect. As part of this plan, Ministers are sharing a portion of their authorized salaries with other Government parliamentary representatives.

The Finance Act, 1940, authorized the payment to every member of the Executive Council who is a member of the War Cabinet, and does not hold any of the Ministerial offices, a salary at the rate of £1,170 per annum. The Finance Act (No. 2), 1942, gave similar authority for the payment of members of the Executive Council and War Administration.

In providing for the appointment of Parliamentary Under-Secretaries, by the Civil List Amendment Act, 1936, an innovation was made in executive control in New Zealand. For service rendered as Parliamentary Under-Secretary a salary of £000 is provided. At the present time (April, 1944) two such appointments are current.

LEGISLATIVE COUNCIL.—The Imperial Act under which the earliest appointments were made to the Legislative Council under a system of responsible government provided that the first appointees should be not less than ten in number. The number actually summoned for the first session (held at Auckland from 24th May, 1854) was sixteen, of whom only fourteen attended. The number increased irregularly for thirty years. In 1885 and 1886 it stood at fifty-three, but has not since reached that limit. The number of members at present (April, 1944) is 36.

An Act of the Imperial Parliament in 1868 provided that future appointments of Councillors should be made by the Governor (not by the Sovereign). Until 1891 members were appointed for life, but since that year appointments have been made for seven years only, members, however, being eligible for reappointment. Prior to 1891 the Speaker was appointed by the Governor, but the Council now elects its own Speaker, who holds office for five years. The Chairman of Committees was formerly elected every session, but in 1928 the standing orders were amended to provide for a three years' term of office. Speaker and Chairman are both eligible for re-election.

Provision for an elective Legislative Council is contained in the Legislative Council Act, 1914, which may be brought into operation at a date to be specified by Proclamation.

The qualifications for membership of the Legislative Council are the same as for the House of Representatives (see post), with the proviso that a person may not at the same time be a member of both Houses. Prior to 1941 women were not eligible for appointment to the Legislative Council, but this restriction was removed by section 40 of the Statutes Amendment Act, 1941. Up to the present, no women members have been appointed.

Before the year 1892 the honorarium of Councillors was understood to be for the session, not for the year, and formed the subject of a special vote every session, the amount varying in different sessions. By the Payment of Members Act, 1892, the honorarium was made annual, not sessional, and was fixed at £150 a year. There have been several alterations since that date, and the present rate is £315 per annum. The Speaker receives £720 per annum and free sessional quarters, and the Chairman of Committees £450. Besides the honorarium, members receive certain concessions in regard to travelling-expenses actually incurred in going to and from Parliament, and also privileges in respect of postages, &c.

Subject to certain exemptions, members not attending the Council are liable to be fined.

HOUSE OF REPRESENTATIVES—The number of members constituting the House of Representatives is eighty—seventy-six Europeans and four Maoris. They are designated “Members of Parliament.” The number was originally fixed by the Constitution Act as not more than forty-two and not less than twenty-four, and the first Parliament called together in 1854 consisted of forty members. Legislation passed in 1858 fixed the number of European members at forty-one; in 1860, at fifty-three; in 1862, at fifty-seven; in 1865, at seventy; in 1867, at seventy-two; in 1870, at seventy-four; in 1875, at eighty-four; in 1881, at ninety-one; in 1887, at seventy; and in 1900, at seventy-six. By the Maori Representation Act, 1867, which is still in force, as embodied in the Electoral Act, 1927, four Maori members were added, three for the North Island and one for the South.

After each population census the Dominion is divided anew into seventy-six European electorates, according to population distribution. In the allocation of electorates an addition is made to rural populations so that the number of rural electorates, in proportion to their population, is higher than urban electorates. The “country quota,” as this allowance is called, is computed on the basis that 28 per cent. is added to the rural population, which for electoral purposes means population other than that contained in a city or borough of over 2,000 inhabitants or in any area within five miles of the chief post-offices at Auckland, Wellington, Christ-church, or Dunedin. The “country quota” first appeared in 1881, to the equivalent of an addition of 33 ⅓ per cent. to the country population. It was reduced in 1887 to 18 per cent., but was increased in 1889 to the present 28 per cent.

Quinquennial Parliaments, instituted under the Constitution Act, were abolished by the Triennial Parliaments Act, 1879, which fixed the term at three years. General elections have been held at three-yearly intervals since 1881, with a few exceptions. The term of the nineteenth Parliament was during the 1914-18 War extended to five years by special legislation, and that of the twenty-fourth (1931-35) and subsequent Parliaments to four years under the Electoral Amendment Act, 1934. By the Electoral Amendment Act, 1937, the three-year term was restored, but on account of war conditions, the term of the twenty-sixth Parliament was extended to four years by the Prolongation of Parliament Act, 1941. The Prolongation of Parliament Act, 1942, extended the term still further to one year from the termination of the war, but with a proviso for a motion to be moved in the House of Representatives each year after the year 1942 either approving the continuation of the House or fixing an earlier date for its expiry. This proviso was put into operation during the 1943 session, and a general election was held on 25th September, 1943.

Under the Electoral Act, 1927, every registered elector of either sex, but no other person, is qualified to be a Parliamentary candidate. It is provided, however, that a person shall not be so elected who is disqualified as an elector under any of the provisions of the Act (see under “Franchise” post); or is an undischarged bankrupt; or is a member of the Legislative Council; or is a contractor to the public service of New Zealand to whom any public money above the sum of £50 if payable, directly or indirectly (but not as a member of a registered company or incorporated body), in any one financial year. Though women's suffrage has been operative since 1893, women were not eligible as Parliamentary candidates until the passing of the Women's Parliamentary Rights Act, 1919, the provisions of which are now embodied in the Electoral Act, 1927. Under the Electoral Act public servants were prohibited from being elected, but this prohibition has been removed by the Political Disabilities Removal Act, 1930, which provided that if elected they immediately cease to be public servants.

The payment made to members of the House of Representatives is £450 per annum, subject to certain deductions for absence not due to sickness or other unavoidable cause. In addition to the honorarium, members are entitled to certain privileges in respect of railway and other forms of travel, &c.

The election of a Speaker is the first business of a new House after the members have been sworn. A Chairman of Committees is elected as soon afterwards as is convenient. Both Speaker and Chairman of Committees hold office until a dissolution, and receive payment until the first meeting of a new Parliament. The Speaker's remuneration is £900 per annum, plus sessional allowance of £100 and free sessional quarters, and that of the Chairman of Committees £075 per annum.

Twenty members, inclusive of the Speaker, constitute a quorum.

FRANCHISE.—Since the abolition of plural voting in 1889 and the introduction of women's suffrage in 1893 every person twenty-one years of age or over has had the right to exercise a vote in the election of members for the House of Representatives. To be registered as an elector a person must have resided for one year in the Dominion, and for three months in the electoral district for which he claims to vote. A system of compulsory registration of electors was introduced at the end of 1924, but for Maori electors a Proclamation is necessary before registration becomes operative. Up to the present this Proclamation has not been made.

There are, of course, slight exceptions to the foregoing, for, if a person is classified as one of the following, he or she is not entitled to register as an elector or to vote:—

Maoris are qualified to vote only at elections of the four members representing the Maori race. A Maori half-caste may register on the roll of a European electoral district; and, if so, may not then vote at an election of Maori members.

By the Electoral Amendment Act, 1937, which made provision for a secret ballot in Maori elections, Maori electors were granted the same privileges, in the exercise of their vote, as European electors.

For the system of local-government administration a modified form of franchise exists, property qualification being necessary for the exercising of votes on financial issues. Further reference to this aspect of franchise will be found in Section 25 of this Year-Book.

POPULATION censuses were taken during 1936 in New Zealand and in all its inhabited dependencies. For New Zealand proper the census related to the night of Tuesday, 24th March, 1936, and recorded a total of 1,573,810, inclusive of 82,326 Maoris. The annexed Kermadec Islands had a population of 2. For the Cook Islands and Niue Island the effective date of the census was 30th April, 1936, and the population was 16,350 (Cook Islands, 12,246; Niue Island, 4,104). The Tokelau (Union) Islands, where a census was taken by the Western Samoan Administration for 4th November, 1936, had a population of 1,170. The same date was selected by the Administration for its census of the mandated territory of Western Samoa, the population being recorded as 55,946. All the outlying islands (vide page 1) were uninhabited, as was also the Ross Dependency situated in Antarctic regions. The total population of New Zealand, dependencies, and mandated territory at the 1936 censuses was 1,647,278.

Further 1936 census figures will be found later in this section or in other portions of this volume, but for details it will be necessary to refer to the census volumes published separately. The following summary gives, where available, figures more recent than those of the census.

METHOD OF COMPILATION.—In common with almost all countries, the chief instrument in compiling population data in New Zealand is the census, which in this country in normal times is taken quinquennially. The minutiæ of the distribution of population, together with analyses of various population characteristics, compiled from census data will be found in the official publications compiled after each census.

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

Intercensal figures of total population are based on the customary equation:—

Population = Population (census) + Births and immigration - Deaths and emigration.

The first interruption in the sequence of New Zealand censuses was caused by the abandonment, for reasons of financial stringency resulting from the world-wide economic depression, of the census proclaimed for 21st April, 1931. Owing to the outbreak of war and its subsequent effect on population no census was taken in 1941, the necessary legislative sanction being provided by section 36 of the Finance Act, 1940. The effect of this section is not necessarily to eliminate the 1941 census, as was the case with the census due in 1931. The section authorizes the census due in 1941 to be taken in any year not earlier than 1941 nor later than 1945.

The comparative shortness of the interval between the census enumerations in normal times, combined with New Zealand's insular position and the completeness of her registration system, prevents serious intercensal errors in statements of the total population of New Zealand.

The distance of the Dominion from other countries, combined with the fact that overseas migration centres in a few ports or air-ports, facilitates the compilation of accurate statistics of external migration. Records of passenger traffic by sea and air between the North and South Islands are also maintained.

Population figures for war years are exclusive of New Zealand soldiers, &c., overseas, and of members of forces of overseas countries who may be in New Zealand. New Zealand troops within the Dominion, whether intended for overseas service or for home defence, are counted in the population totals.

Residents of the Kermadec Islands, Cook Islands, Niue, Western Samoa, and the Tokelau Group are not included in the population statistics quoted throughout this section, except in the first table. Further information will be found in the section entitled “Dependencies.” Separate statistics of the Maori population are given towards the end of this section.

INCREASE OF POPULATION.—The outstanding note of the history of population movement in New Zealand is that of unbroken growth. That it has not been invariably regular is well attested by the accompanying table, and by the long-term comparison shown in a later section of this Year-Book entitled. “Statistical Summary.”

Commencing with the 1926 census all half-caste European-Maoris were included with the Native population in lieu of the previous practice of treating as Europeans such half-castes as were living in European fashion, and as Maoris those half-castes who were living in Native fashion. The figures in the preceding table have been corrected from 1861 onwards, to accord with the present practice. Lack of data prevents adjustment for years prior to 1861. The increase from 1858 to 1861 is, therefore, very slightly understated.

The “European” population now looks in retrospect down a vista of well over one hundred years. At the opening of the nineteenth century there existed a more or less fluctuating population of perhaps one hundred; by 1839 it had swelled to a total of about a thousand whalers, sealers, traders, missionaries, adventurers, and settlers. Activities of the colonizing companies and societies in the “forties” brought rapid changes and swiftly rising numbers, to be enhanced in the “sixties” by the gold rushes of the period.

The most significant period is possibly that of the “seventies,” marked by a vigorous developmental policy of public works and assisted immigration. The record year 1874, which saw a rise in population of 46,000 (including 32,000 assisted immigrants), was, and still is, the high-water mark of population gains. Both 1874 and 1875 shewed a ratio of growth far in advance of any level subsequently attained.

In the late “eighties” and early “nineties” came economic depression and, consequently, comparative stagnation in population. In the four “March” years 1887-88, 1888-89, 1890-91, and 1891-92, and also in 1927-28, emigrants exceeded immigrants, these being the only such occasions in the history of the country, until the cent depression years, when departures exceeded arrivals in the six “March” years 1931-32 to 1936-37.

Up to the “seventies” New Zealand was dependent on migration for the greater portion of her increase of population, but since then natural increase—i.e., excess of births over deaths—has been the principal factor.

A table is appended showing for each five-yearly period from 1861 the excess of births over deaths and of immigration over emigration. Maoris are not included, nor, prior to 1921, are crews of vessels. Figures for years later than 1920 have not been adjusted consequent upon the censuses. While there thus exist discrepancies with total population increases given elsewhere, such discrepancies do not invalidate the use of the table.

Trend of Population.—While the population of New Zealand has been growing, the rate of increase has declined substantially, the lowest point being reached in 1935. The next four years showed steady improvement until 1939, when the percentage increase recorded was the highest since 1927. Since the outbreak of war, however, the check on migration and the movement of members of the Armed Forces, &c., have introduced abnormal features.

Immigration now contributes relatively small increments to the population; indeed, in the five depression years 1931-35 there was a net exodus from New Zealand of 9,918. With the passing of the depression the net inward flow resumed, but, largely owing to war conditions, the excess of arrivals for the seven years 1936-42 was only 14,106.

In recent years natural increase (excess of births over deaths) reached a critical position. The natural increase rate (per 1,000 of mean population) reached a low point of 7.89 in 1936. It is obvious that this meant that the population was still increasing at a moderate rate, but owing to the time-lag it was less obvious to many that a rate as low as this meant, in the near future, a stationary or, more probably, a declining population. In other words, the population was failing to reproduce itself in sufficient numbers for growth and even for the maintenance of a stationary population.

One method of measuring the status of a population is that of the net reproduction index, which is based on female children born and probably surviving. Gross and net reproduction rates in recent years are:—

Though economic factors are not the only, and possibly not even the most important, cause of the decline in the birth-rate, the immediate cause of the low level reached in 1935 was almost certainly the economic depression from 1931 onwards. As economic conditions recovered there was some improvement in the birth-rate (though accompanied by higher death-rates), and the net reproduction index has returned to a level indicating a modest margin of growth. This index is not, and cannot be, an exact measure, but it does afford a close and fairly reliable approximation in normal circumstances. In its use it is necessary to remember, inter alia, that the probability of survival of the children born is calculated on past mortality experience in more or less normal conditions; no allowance is made for wars, major epidemics, or other factors which may result in abnormal losses of population.

The foregoing observations necessarily omit any forecast of the trend of external migration; also they do not take into account the Maori section of the population, which is increasing fairly rapidly.

SEX PROPORTIONS.—The following table is interesting as showing the early excess of males and the gradual equalization of the sexes in New Zealand. The figures quoted are exclusive of Maoris.

The preponderance of males in the early years of New Zealand was doubtless due to the fact that the difficulties of pioneering and the remoteness of the country from Europe were such as to deter female immigration to a greater extent than male. This was accentuated by the character of the early industries.

Of the two sources from which the Dominion's population has been recruited—viz., migration and natural increase—the effect of the former has hitherto been to give in the aggregate a considerable preponderance of males, and of the latter to give a regular preponderance of females.

INTERCENSAL RECORDS.—As already noted, the intercensal statements of total Dominion population, prepared from the records of vital statistics and of external migration, have been by virtue of the favourable position of the Dominion in this respect relatively accurate, and the 1936 census results have afforded a further demonstration of this. The same degree of accuracy does not persist, however, for Maori and European elements. Results for the censuses of 1921 and 1926 suggested that numbers of Maori-European children of at least half Maori blood have been counted in birth statistics as Europeans. In consequence, the Maori population had been slightly understated, and the European population overstated to a corresponding degree. The 1936 census results afforded further support to this view. Accordingly the statements of population at intercensal dates, 1921-36, were revised. For fuller details of revised statements (including the annual estimates of population of towns, provincial districts, &c.) reference should be made to the 1936-37 edition of the annual Statistical Report on Population and Buildings.

As population figures for the calendar year are in demand for numerous purposes, figures are given also for years ending 31st December.

The figures given in the two preceding tables show the population exclusive of Maoris. The following table shows the population inclusive of Maoris.

EXTERNAL MIGRATION.—Statistics of external migration have been recorded in New Zealand since 1860. Since 1st April, 1921, they have been compiled from individual statements obtained from each person entering or leaving the Dominion.

Commencing with the year 1933-34, the year ending 31st March has been adopted as a standard for the statistical expression of external migration in place of the calendar year formerly in use. The principal reason for the change was to avoid the partition of a season's migration movement into two statistical years as was inevitable with the calendar year ending in the middle of the summer flow of tourists and immigrants.

Including crews of vessels, 43,096 persons from overseas arrived in New Zealand during the year ended 31st March, 1943, which, compared with 1941-42, shows a decrease of 10,899. During the same period 44,117 persons departed. This figure, compared with the corresponding one for 1941-42, shows a decrease of 8,734.

Wartime restrictions on migration, diversion of ships, and use of passenger-liners as troop-carriers and hospital ships have inevitably led to a considerable decrease in the migration figures, which in 1942-43 reached their lowest ebb for over eighty years.

In addition to the figures just quoted there were also 845 “through” passengers who called at a port of New Zealand en route to their destination.

The excess of total departures over total arrivals for 1942-43 was 1,021, compared with an excess of arrivals of 1,144 during 1941-42.

The numbers of arrivals and departures during the last eleven years are given in the table following. Crews of vessels, “through” passengers, tourists on cruising liners, and members of the Armed Forces, &c. (1939-40 to 1942-43), have not been taken into account in this table.

The excess of “crew” arrivals over “crew” departures, neither of which are included above, normally provide an average annual increment of some hundreds to the population of New Zealand.

Classes of Arrivals and Departures.—The following table gives an analysis of all classes of passenger arrivals during the last five years, including “through” passengers and tourists on cruising liners.

The succeeding table gives a similar analysis of passenger departures.

Ages.—The following table gives the age-distribution of immigrants and emigrants for the twelve months ended 31st March, 1943.

ASSISTED IMMIGRATION.—The general scheme of Governmental assistance to immigrants has been restricted in varying degrees since May, 1927. Further details will be found in the 1931 or preceding issues of the Year-Book.

Various systems of assisted immigration have been in force since 1871, with the exception of the period 1892 to 1903 (inclusive).

The numbers of assisted immigrants during each of the last eleven years were as follows:—

The total to 31st March, 1943, was 226,274, of which number all came from the United Kingdom, with the exception of 3,969 from the Continent of Europe, spread over the five years 1874 to 1878 (inclusive).

PASSPORTS—Permission to enter New Zealand.—With certain specified exceptions, no person of sixteen years of age or over may land in New Zealand unless in possession of a passport or some other document satisfactorily establishing nationality and identity. Exemption (which is additional to the requirements of the Immigration Restriction and Undesirable Immigrants Exclusion Acts) may be granted by the Minister of Internal Affairs.

With certain exceptions, all aliens require a visa.

For persons from tho Cook Islands and Western Samoa the only requirement is a permit to visit New Zealand granted by the Resident Commissioner of the Cook Islands or the Administrator of Samoa, as the case may be. The regulations, further, do not apply to a British subject who is the master or a member of the crew of the vessel in which he arrives, or to a British subject arriving from Australia.

Departure from New Zealand.—All persons sixteen years of age or over travelling overseas require a permit from the Minister or Under-Secretary of Internal Affairs.

British subjects travelling between New Zealand and Australia do not require passports, but permits are necessary.

IMMIGRATION RESTRICTION.—Detailed information under this head will be found on pp. 44-45 of the 1942 number of the Year-Book.

NATIONALITY AND NATURALIZATION.—The British Nationality and Status of Aliens (in New Zealand) Act, 1928, which was reserved for Royal assent, came into force on tho 1st July, 1929. This Act made important alterations in the naturalization law of New Zealand, and made provision for the adoption of Part II of the British Nationality and Status of Aliens Act, 1914 (Imperial). A fairly detailed account of its effects will be found on pp. 92-95 of the 1931 issue of the Year-Book.

The British Nationality and Status of Aliens (in New Zealand) Amendment Act, 1934-35, was assented to on 26th March, 1935. This Act does two things: in the first place, it brings the New Zealand law into conformity with the law of the United Kingdom relative to the nationality of married women (see p. 70 of 1940 Year-Book). In the second place, a woman who has lost her British nationality by reason of her marriage to an alien has the right, while she remains in New Zealand, to claim the same privileges as if she had remained a British, subject. The legislation does not seek to alter the fact that such a woman has in law ceased to be a British subject: it merely says that upon making the prescribed declaration she is, while she remains in New Zealand, entitled to all the rights and privileges and is subject to all the duties and obligations of a natural-born British subject.

The British Nationality and Status of Aliens (in New Zealand) Amendment Act, 1943, brings the nationality laws of New Zealand into conformity with the United Kingdom law in the matter of declarations of alienage and in the British nationality of persons born abroad. The Act also makes provision for naturalization to be granted to aliens serving with the Armed Forces, notwithstanding that the provisions of the principal Act may not have been complied with. Provision is also made in the Act for the recognition in New Zealand of any certificates which may be granted under similar provisions in the United Kingdom or in any other British Dominion.

During 1942, 29 women took advantage of section 3 of the 1934-35 Act and made the necessary declaration. The nationalities of the husbands were as follows: German, 9; Danish, 4; Norwegian, 3; Italian, Dutch, and Polish, 2 each; Czechoslovak, Chinese, French, Hungarian, Swiss, Yugoslav, 1 each. Two persons made declarations renouncing their nationality as British subjects—i.e., declaration of alienage.

DISTRIBUTION OF POPULATION—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 retained until 1901. In that year the North Island was found to have slightly the larger total and since then has steadily increased its lead. The Maori War which broke out in 1860 retarded settlement in the North, while a large area of land reserved for the Maoris was for many years a serious hindrance to the development, by Europeans, of this portion of the Dominion. The South Island was practically free from Maori troubles, and settlement was more rapid, though much of the land was disposed of in large areas. The discovery of gold in Otago in 1861 and on the West Coast in 1864 attracted to these localities considerable numbers of miners.

At 30th June, 1943, the North Island population was estimated as 1,085,519, inclusive of 93,461 Maoris; and the South Island population as 547,179, inclusive of 3,478 Maoris.

The natural increase of European population (i.e., excess of births over deaths) for the South Island during the 1926-36 intercensal period was 47,181, but the total net increase was only 39,889. For the North Island the natural increase was 92,130, and the total net increase 107,126. Allowing for the fortuitous presence in the South Island in 1926 of 2,000 or 3,000 North Island residents visiting the Dunedin Exhibition the margin is reduced, but the existence of a northward drift of population is still evident.

Internal Migration.—Particulars of passenger movement between the North and South Islands are available and are of use in the compilation of population statements. During the year ended 31st March, 1943, the North Island showed a gain of 5,093 from the South Island, compared with 10,776 in 1941-42.

Provincial Districts.—The approximate areas and the populations, inclusive of Maoris, of the various provincial districts are as follows:—

The foregoing table illustrates the wide disparities in the size of the provincial districts, whether measured by area or by population. The growth of population during the interval between 1926 and 1936 is given below both in absolute numbers and as a percentage of the 1926 totals. The figures include Maoris.

Urban and Rural Population.—On 24th March, 1936, somewhat over one-third (38.5 per cent.) of the population of the Dominion (excluding Maoris) was included in the four principal urban areas—Auckland, Wellington, Christchurch, and Dunedin—and over one-half (51.7 per cent.) in these or in the ten secondary urban areas. In the following table urban population means the population in cities and boroughs, while rural population covers counties, all town districts, and extra-county islands. The continuance of urban drift is noticeable, but with a marked slackening in pace.

Another conception of urban and rural population is presented in the next table, which covers the last seven censuses. Maoris are omitted, as data are not available over the whole period. The great bulk of Maoris inhabit rural communities. In the case of the larger centres there are numerous suburban boroughs and town districts; consequently, as regards the fourteen urban areas the centre has been taken as including all cities, boroughs, and town districts within the territory of the present urban area. In other instances the “centre” is a borough or town district.

The comparison is not an exact one, but is sufficiently accurate to indicate the general trend of urbanization. For instance, it is noticeable that in 1901 29 per cent. of the population were in towns of 10,000 population or over; by 1936 the proportion had become 47 per cent.

An important characteristic of the distribution of urban population in New Zealand is what may be termed its decentralization. In place of one great metropolis containing a huge proportion of the population, as in the case of the Australian States—e.g., Victoria, whose capital city (Melbourne) contains over one-half of the total population of the State—the more highly urbanized portion of the community is localized in four widely separated centres. These four centres have always existed more or less on the same plane, a fact which has played no small part in the development of the country. An interesting feature is the wide gap which has long existed between the four major centres and the next largest towns.

Urban and rural communities are not evenly distributed. The South Island, for example, contains proportionately more rural population than does the North Island.

RECENT MOVEMENTS IN TOWNS.—Urban areas afford the best basis of comparison of population-growth in the case of the largest towns, since their boundaries are stable and, of greater significance, they include the suburbs as well as the central city or borough. The following table excludes Maoris—data being lacking in earlier years—but their numbers are too small to exercise any significant effect.

POPULATION ESTIMATES.—It has been the practice, in years in which a census is not taken, to compile estimates of population for provincial districts, urban areas, counties, cities, boroughs, and town districts, these relating to 1st April. Owing to various factors arising out of the war, it has now been found impossible to compile accurate estimates, and authority has been granted, by the Population Estimates Emergency Regulations 1942, to discontinue these until after the next census.

The latest estimates, which relate to 1st April, 1941, are now given, and these have been adjusted to 1st April, 1943, where necessary, for any alterations to population and area in cases where boundaries have been changed.

Urban Areas.—The population of each of the fourteen urban areas (cities or boroughs, plus their suburbs), as estimated for 1st April, 1941, was as follows:—

Urban Areas.—Estimated Population (including Maoris), 1st April, 1941

Counties.—Estimated Population (including Maoris) and Area, 1st April, 1941

(NOTE.—"Administrative Counties" do not include boroughs or town districts independent of county control, but include dependent town districts.)

Boroughs.—Estimated Population (including Maoris) and Area, 1st April, 1941

Town Districts.—Estimated Population (including Maoris) and Area, 1st April, 1941

AGE DISTRIBUTION.—The following table shows the estimated age distribution of the population at 31st December, 1942. The figures are based on the 1936 Census data and brought up to date from statistics of births, ages of persons dying, and ages of persons arriving in or departing from New Zealand.

DENSITY OF POPULATION.—The total area of the Dominion of New Zealand is approximately 103,935 square miles. Omitting the annexed islands and certain uninhabited outlying islands, the area of the land-mass remaining is 103,416 square miles. This calculation, it should be explained, includes all inland waters—viz., lakes, rivers, harbours, estuaries, &c. It should be noted also that there is a great deal of high mountainous country in New Zealand, particularly in the South Island, while there are also great areas of broken, swampy, or hilly country which is either incapable of effective use or which can be used profitably only for pastoral purposes, afforestation, or the like.

The density of population in 1943 may be quoted as 15.80 persons to the square mile. This figure would be higher if members of the Armed Forces serving overseas were included in the population.

The area and population of individual towns and counties will be found in preceding tables in this section. At the 1936 census density of population in the various provincial districts was:—

Attention must be drawn to the necessity for the exercise of discretion in the use of data concerning density of population, particularly in comparing one country with another. Areas may be calculated in many ways, while area itself may have little relationship to potentiality of use. In the case of urban population, it is impossible to obtain the aggregate area of sites actually in occupation by business premises, residences, &c. Many boroughs contain within their boundaries large reserves which, with farming and other unbuilt-on land, tend to disguise the actual relation of population to area.

MAORI POPULATION.—A record of early statistics of Maoris is given in Vol. III of the 1936 Census Results. The first official general census was taken in 1857-58, and others occurred in regular sequence from 1874 onwards. Owing to inherent difficulties the earlier census records make no pretence towards complete accuracy, and even some later enumerations hardly claim to be more than approximations.

Available statistical evidence points to a decline in the numbers of the Native race following the advent of Europeans, but this decline was commonly exaggerated by early writers. Of later years an unmistakable and now fairly rapid increase has been noted. This gain, however, has been accompanied by a very considerable dilution of blood.

The Maori population recorded at the census of 24th March, 1936, was 82,326, which is an increase of 18,656 on the 1926 total. The percentage increase was 29.30, equivalent to an average annual increase of 2.60 per cent. These percentages, it will be noted, are considerably higher than the corresponding figures for the non-Maori population—viz., 10.93 per cent. and 1.05 per cent. For the year 1942–43 the net increase of the Maori population was 2,777, or 2.99 per cent., as compared with a decrease of 3,021 (0.20 per cent.) for the non-Maori population. Movements of troops tend to invalidate this comparison; the natural increase ratios for the year 1942-43 afford a better illustration. These are:—

The Census record of Maori population is as follows:—

Of the 96,939 Maoris at 30th June, 1943, 93,461 were in the North Island. Auckland Provincial District contains the bulk of the Maoris, particularly in the Auckland Peninsula and Poverty Bay regions. In the South Island Maoris do not attain any numerical significance.

The records of the 1926 and 1936 censuses permit of a statement of the total numbers wholly or partly of Maori blood.

In 1936 there were recorded in New Zealand some 94,156 persons wholly or partly of Maori origin. Of these, some 59 per cent. were recorded as of unmixed Maori descent. There is some reason to believe that the degree of miscegenation is understated, and it is unlikely that the proportion of pure Maori descent is more than 50 per cent.