Land tenure in the Cook Islands : with special reference to the Southern Cook Group
Abstract
This study is set in the Cook Group, an archipelago
of fifteen tiny islands totalling only 88 square miles in
area, yet scattered over 850,000 square miles of the Pacific Ocean between Tonga and Samoa on the one hand, and French Polynesia on the other. Since 1901 the group has been
included within the boundaries of New Zealand, and its
18,000 people, who are culturally close relatives of the Maoris of New Zealand, are therefore citizens of that country. The islands are divided physically into two groups. The
Northern Group consists of seven islands of coral formation which constitute the central segment of that scattered band
of atolls that sweeps across the Pacific from French Oceania
to the Marshalls. The Southern Croup islands are, with two
minor exceptions, of volcanic origin, and all eight islands
lie within a radius of one hundred and fifty miles of
Rarotonga, the administrative headquarters of the Government
of the Cook Islands. In area the islands range from Nassau
which is only 300 acres, to Rarotonga which covers 16,602
acres. The population of the permanently settled islands
ranges from 92 on Palmerston to 7,827 on Rarotonga; the total
for the whole group being 18,041. The total population of
the group was approximately 18,000 at the time of first
European contact but declined rapidly thereafter until it
reached about 8,000 at the turn of this century. Since that
time, however, it has regained its former level.
The group lacks mineral deposits of commercial value,
and its principal natural resources are the soil and the
sea - though the potential of the latter is as yet little
known. The soils vary considerably in their productive
potential, but only 9,523 acres or 16 per cent of the total
1
land area of the group is considered suitable for agriculture.
Of the balance, approximately 17 per cent is taken up by the
infertile rubble and sand of the coral islands which can
support little in the way of commercial crops other than the
coconut, 27 per cent is taken up by second class soils which
are suited to certain tree crops but which are at present
relatively little utilized, and the remaining 40 per cent
comprises the mountainous interior of Rarotonga and the
makatea (upraised coral) outcrops of the other Southern
Group islands which are at present completely unproductive.
The climate of the group is tropical and shows little
seasonal variation. The mean annual temperature lies in the
mid-seventies. Annual rainfall is about seventy to eighty
inches and in general is well distributed throughout the
year, except in the Northern Group where periods of drought
are sometimes experienced. Hurricanes usually strike some
part of the group once or twice in each decade, and the
commercial productivity of the islands hit is severely disrupted
for a year or more thereafter.
Of the wealth of truly indigenous vegetation found in
the group, very little indeed makes any significant contribution
to human welfare. The coconut, banana, breadfruit, taro
and most of the other subsistence crops were introduced by
the Polynesian immigrants to the islands in centuries past,
and other crops like citrus, coffee and tomatoes came with the wave of European expansion across the Pacific during the last two centuries.
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