The islands of Fiji are centrally located in the southwest Pacific. Over
three hundred islands and islets make up the archipelago, which spreads
between latitudes 15' and 22' south of the equator for 300 miles. The
international date line runs through Fiji at the Koro Sea and the Moala
Island group.
The total land area of the islands is about the equivalent of the state
of Delaware, somewhat over 7,000 square miles. Two great islands account
for nearly 95 per cent of the total area: Viti Levu, the largest, is
over 4,000 square miles, and Vanua Levu, about half as large. Over 90
per cent of the native population lives on these two islands although
nearly a hundred other islands are inhabited.
Most of the islands are made up of volcanic and sedimentary rocks. The
largest islands rest on a submerged portion of an ancient land mass,
sometimes called the Melanesian continent, which goes back in time to
the Paleozoic and, in its prime, intermittently connected Fiji with
southeastern Asia and Australia. Subsequent submergence, followed by
cycles of volcanic upbuilding, erosion, and more submergence over eons
of time, gave the big islands their upper foundations. The last
extensive volcanic activity and land uplift occurred in the Pleistocene
and accounts for many of the present mountain masses. The final touches
to the Fiji profile have been wrought by more recent weathering and
erosion. Sedimentation is still going on at river mouths and along the
coasts, where deltas are being built and mangrove thickets flourish.
Many of the smaller islands are old limestone masses that were pushed up
from the sea. Unlike the high craggy volcanic islands, these are lower
and flat-topped. Typically, they contain a basin-shaped depressed area
that is surrounded by a rim. These depressions are usually fertile and
heavily forested.
Coral islands make up the third variety of land forms. These are always
small and low. Their small size, thinner soil, and lack of fresh water
make them much less suitable for human habitation. But even a thin layer
of soil produces a luxurious vegetation.
Fringing and barrier reefs are abundant throughout the archipelago,
surrounding nearly every island. The most striking of these formations
is the Great Sea Reef, which forms an arc of nearly 300 miles along the
western fringe of Fiji and encloses large areas of coral-infested sea.
Moderately high mountains give to the larger islands a generally rugged
terrain. The more extensive ranges lie across the path of the prevailing
south and easterly winds producing windward and leeward climatic areas.
On the windward side rainfall is heavy and rather evenly distributed
over the year. Here the valleys and mountain slopes support a typical
dense tropical growth. The leeward side, however, receives much less
moisture and has wet and dry seasons. Scattered patches of trees and
grasses cover the ground, whereas heavy stands of forest are confined to
valley bottoms and higher mountain slopes. The mountainous interior of
Viti Levu contains a number of peaks over 3,000 feet, the highest of
which is Mt. Victoria, 4,341 feet.
Surface water is abundant on the bigger islands. Several large and
navigable rivers drain Viti Levu and Vanua Levu. The Rewa River, on the
east side of Viti Levu is the largest and is navigable for small craft
for 70 miles. Smaller rivers and hundreds of streams are important
sources of food and drink for the people of the interior.
Great flood plains are formed at the mouths of the larger rivers. These
and the fertile flats that run back along the valleys contain the
greatest population densities.
The climate is generally pleasant and healthful. Tropical extremes of
heat and humidity are moderated by the prevailing trades, which usually
supply cool and pleasant breezes from the east. Still, days of
uncomfortable heat and oppressive humidity are not unknown; however,
such periods are protracted only in the interior. The climate is far
from uniform throughout the islands. The windward sides, where rainfall
often exceeds a hundred inches, have a more even temperature and
sunshine is more moderate. On the leeward sides there is less general
cloudiness and more sunshine, especially during the dry season. The
smaller islands generally resemble the leeward areas in climate.
Native plant and animal life, like much of the southwest Pacific, is
southeastern Asiatic in type and in origin. In the more profuse and
varied windward sides there are several general vegetation zones. Along
the coasts and in the larger river basins occur alluvial vegetation
largely dominated by several kinds of mangrove, which is densest in mud
flats washed by the tide. In this zone trees are scattered, and many of
them bear useful nuts and fruits. On the slopes and ridges behind the
coastal belts are the great tropical rain forests. They make up a dense
cover of evergreen trees interwoven with wild creepers and vines. Thick
stands of shrubs and smaller trees add to the tropical profusion. Above
2,000 feet the forests thin out and become more heavily coated with moss
and lichens, and ferns and orchids attach themselves to the branches.
Beyond 3,000 feet is the cloud belt, and above this trees become stunted
and are finally replaced by hardy shrubs that cling to the rocks and
crags.
On the leeward sides, patches of rain forest are found only in the
moister areas. More typical of this zone are thin-leaved trees
interspersed in large expanses of meadow and grassland.
A number of native plants are very vital to the Fijian livelihood and
some have modern economic importance. Several timber trees are essential
to house building, canoe construction, and wood carving. The ubiquitous
palms, here as elsewhere in the Pacific, are vital sources of food,
drink, building, and weaving materials and cordage. The mangrove
provides firewood, house poles, fishing fences, and traps, laths for
bows and black dye for their hair and tapa. Valuable starch is secured
from the sago palm, which is cut just before flowering, and the leaves
are a common thatching material. Various reeds, canes, and bamboos and
lianas are useful to Fiji economy. In the drier areas reeds and grasses
provide material for house walls, thatch, fish fences, and arrow shafts.
Several kinds of trees yield edible nuts and fruits.
Like other central-Pacific island groups, Fiji is poorly provided with
indigenous mammals. A small gray rat is a considerable pest in gardens
and homes, and a large nocturnal bat, which is called a flying fox,
lives in tree colonies and is often seen at dusk in banana groves or
other feeding places. All the economically important animals of Fiji
have been introduced, such as pigs, fowl, dogs, cattle, horses, sheep,
and goats.
Bird life is diverse and interesting, although in a number of places
introduced forms, like mynahs and turtle doves, have forced the native
varieties back into the jungle. Several game birds such as doves,
pigeons, and ducks are occasionally hunted.
Snakes and lizards are fairly common on the islands; none is poisonous.
Some are eaten, but the practice is not usual. Snakes had a more
important place in the former religious and totemic practices.
Much more vital to the native economy is the abundant and varied marine
life. This, with gardening, provides the foundation of Fijian
subsistence. Turtles, crabs, prawns, eels, to say nothing of scores of
fishes, are hunted, trapped, poisoned, speared, and netted. The cycle of
the balolo worm has here the same importance as in other Pacific
islands.