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Niue
by Eroarome Martin Aregheore and Tom Misikea |
| 1. INTRODUCTION
The Island of Niue is in the South Pacific (190 S and 1690 W) in the middle of a triangle formed by Tonga, Samoa and the Cook Islands. Niue is a raised coral atoll, the largest and highest in the world with a coral reef fringing its elevated coastline. It has a total land mass of 258 square kilometres in area with a coastline circumference of 64 km (Douglas and Douglas, 1989) see Figure 1. Of the total land area in Niue about 20,400 ha are available for agriculture. Niue is a self-governing Commonwealth country with an elected 20-member Parliament, in free Association with New Zealand. The administrative centre is Alofi, on the west coast. Niueans are Polynesians, and the provisional population estimate is about 1,700 (Niue Statistics, 2001) although the 2006 World Factbook (July 2006) estimate was 2, 166 with a 0.01% growth rate. However, the population of the island continues to drop, from a peak of 5,200 in 1966 to 2,100 in the late 1990s, with substantial emigration to New Zealand. The number of Niueans living in New Zealand and other countries is about treble those resident in the island. The population of Alofi, the administrative centre was estimated to be about 900 (Crocombe 2001). Niueans are bilingual, speaking Niuean and English. Niue relies greatly on agriculture for its income and food security. The productive ventures in agriculture and livestock are carried out by the public sector, under the guidance of the Department of Agriculture, Forestry and Fisheries (DAFF). The Niue Development Board has been responsible for planning and execution of schemes for the production of lime juice, passion fruit pulp and juice, honey, copra and reconstituted milk. During the last 5 years focus has been on vanilla (Vanilla tahitiensis), kava, Nonu (Morinda citrifolia) etc. and DAFF has been very active in assisting farmers with these crops by facilitating them to become certified organic producers, as overseas markets are very attractive for these organic foods. Honey production has been managed by a private entrepreneur and this product is also on the verge of receiving organic status. The main livestock owned by islanders are pigs, poultry and a few cattle. In the past (1960s) cattle in fenced blocks were used to control weeds under coconuts or on unoccupied homestead areas. These cattle, mainly Bos indicus crosses were managed for beef. 20 Herefords from New Zealand were imported in 1992 for cross-breeding with local stock (mainly crossbred Friesians, Brahmans, Santa Gertrudis etc.), but this was not successful. In 1996 the government cattle farm at Vaiea was relinquished to a private company (Niue Alpaca Quarantine Station) and most cattle at the farm distributed to potential growers in the public sector. Some sheep were imported as sentinels for the newly formed Quarantine Station. Table 1 presents statistics of ruminant livestock numbers and imports for the period 1995 - 2005. Table 1 - Niue statistics of livestock numbers,
fresh milk and cattle and beef
* Livestock numbers from Niue data except numbers in ( ) from FAOSTAT
Figure 1. Map of Niue |
| 3. SOILS AND TOPOGRAPHY
Niue Island is an elevated coral atoll uplifted by a series of volcanic disturbances to form terraces of exposed coral limestone that subsequently were partly covered by a thin layer of volcanic ash. There are four main soil types in Niue and these are: (1) Hikutavake: outer fringe of the island (2) Hakupu: coconut/pasture soil (3) Fonuakula: pasture soil, and (4) Palai: forestry soil, root crops. For a generalized picture of the soils of Niue see Figure. 2 and Wright and van Westerndorp (1965). The soils differ in texture and colour but have similar pedological organization comprising a thin layer of topsoil over subsoil with makatea floaters of limestone outcrops. The soil series can be differentiated by the subsoil colours. These colours range from very dark grey, through brown and reddish brown to dark red. All soils have low water holding capacity due to high porosity of the soil and the nature of the substrata material - clay content, low bulk density and shallow depth. The soils of Niue in general are well supplied with phosphorous and potassium, but there are a few areas that are deprived of these nutrients for plant growth which makes crop production difficult. Some soils also lack nitrogen as can be seen by the yellowing of leaves on some vegetation. Burning of some areas for cropping is common and this may be the reason why some areas are deprived of nitrogen. The supply of calcium, magnesium and many of the trace elements seems adequate for plant growth in most areas. Wright and van Westerndorp (1965) also observed that the soil of Niue is probably derived from volcanic ash. Niue is an upthrust coral atoll which was raised to the surface during underground volcanic action centuries ago.
Figure 2. Generalized Soil Map
of Niue (Copyright Government of Niue) The soils are very well drained. Indeed so porous is the limestone of the island that there are no surface streams, no surface water or any areas of impeded drainage. The shape of the land surface has a strong influence on the soil and land use possibilities. Niue can be regarded overall as flat, though in micro-topography it is uneven and broken. Coral limestone outcrops are recognized on roadsides and on the sea line of the island and these show the roughness of the island. Wright's survey concluded that 48 percent of the surface is occupied by outcrops of hard reef rock. |
| 9. CONTACTS
This profile was written and will be updated from time to time by: Eroarome Martin Aregheore The University of the South Pacific School of Agriculture Alafua Campus, Apia, Samoa. Tel: 685 21 671 Fax: 685 22 933 E-mail: aregheore_m@samoa.usp.ac.fj and Tom Misikea, Chief Livestock Officer Department of Agriculture, Forestry and Fisheries, Niue E-mail: tomanogi_t@yahoo.com [The profile was edited by J.M. Suttie and S.G. Reynolds in May 2002 and revised by S.G. Reynolds in May 2006]. |