
The Fiji islands are in the south-west
Pacific Ocean, where they occupy a central locale 2797 km
north-east of Sydney, Australia, and 1848 km north of Auckland, New
Zealand. Fiji lies wholly in the southern tropics, that is, between
the equator and the tropic of Capricorn. The Fiji archipelago forms
the eastern outpost of the chain of high volcanic islands of
continental origin that extends eastward from Papua New Guinea to
the Solomon Islands and Vanuatu. Fiji’s closest neighbor to the
east is Tonga and to the west Vanuatu (formerly the New Hebrides).
Longitudinally, Fiji is where the new day begins; on the 180th
meridian the International Date Line makes a special eastward bend
around the island group so that all of the country keeps the same
time.
The territorial waters of Fiji are defined in the deed of cession
as all that area ‘lying between the parallels of latitude of 15
degrees south and 22 degrees south of the equator, and between the
meridians of longitude of 177 degrees west and 175 degrees east of
the meridian of Greenwich’. In 1965 the boundary was extended by
one degree to take in Conway Reef, extending the limit to 174 east.
In latitude, the Fiji islands correspond with Tahiti, Townsville in
Australia, Zimbabwe, Rio de Janeiro and northern Chile.
The area included within these limits is approximately 709,660 sq
km, about 97% of which is water. The remaining 3% (18,376 sq km) is
land. The Fiji archipelago includes about 300 islands (depending on
how many reefs and tiny islets you take into consideration) of
which about 100 are inhabited. The largest island, Viti Levu, which
has 70% of the population and an area of 10,388 sq km, is the hub
of the entire archipelago. On it are Suva, the largest city, the
chief port and the capital; Nadi, site of the international
airport; and Lautoka, the second largest city and the second port
of entry.
Vanua Levu, to the north-east of Viti Levu, is the second largest
island which, with an area of 5538 sq km, is slightly more than
half the size of Viti Levu. Although more sparsely settled than
Viti Levu, it is also a center of population. Like Viti Levu, it
produces sugar cane and also has large coconut plantations.

Taveuni lies to the east of Vanua Levu,
being separated from it by the Somosomo Strait. With an area of 435
sq km, it is verdant, mountainous and agriculturally rich.
Tied with Taveuni as the third largest island in the archipelago
(with an area of 409 sq km) is Kadavu, which lies to the south of
Viti Levu. It is a centre of traditional Fijian culture and not
often seen by tourists.
All of the remaining islands of Fiji are small and are divided into
two main groups, Lomaiviti and Lau.
Lomaiviti translates as ‘middle’ or central Fiji, which describes
exactly where this island group is on the map.
It is composed of seven main islands, with smaller ones lying off
the coasts. Their aggregate land area is 425 sq km. Gau, Koro and
Ovalau are large, each being about 100 sq km or more in area.
Ovalau derives its importance from the town of Levuka, which was
the earliest European settlement in Fiji and the original capital.
Gau is the largest, highest and southernmost of the group; Koro is
a high, wedge-shaped island rising abruptly from deep water. Nairai
and Batiki, to the east of Ovalau, are lower than their neighbors
and are surrounded by extensive reefs. Makogai, north-east of
Levuka, was once a leper colony serving the entire south-west
Pacific. Wakaya, once a plantation, is now an exclusive real estate
development. All of the islands can be seen from the old capital of
Levuka on a clear day.

Lau, or eastern Fiji, the area most
heavily influenced by the Tongan culture, includes numerous
limestone islands and others of volcanic or composite structure,
all set among widespread reefs.
For administrative reasons all of Lau is one district, but it is
geographically divided into four subgroups: northern Lau, central
Lau and southern Lau (which together form a chain of islands
stretching 432 km in a north-south direction), and the Moala group,
lying to the south of Lomaiviti.
Northern Lau includes the Exploring Islands (one large island and
eight small ones, all enclosed within a barrier reef) and some 14
others of which Naitauba, Kanacea, Mago and Cicia are the most
important.
Central Lau includes five islands centring on Lakeba, which is the
hereditary seat of the chiefs of Lau and the home of Ratu Sir
Kamisese Mara.
Southern Lau comprises 16 islands as well as some clusters, most of
them grouped within 100 km of Lakeba. Beyond these, in the
attenuated ‘tail’ of the archipelago, lie Vatoa and Ono, isolated
from their nearest neighbours and from one another by wide
stretches of open sea. The most outlying islands of southern Lau
are actually closer to Tonga than they are to Fiji.
The Moala group is composed of three islands having an aggregate
area of 119 sq km and situated about halfway between Kadavu and
southern Lau. Moala is the principal island; Totoya is the rim of
an extinct volcano whose breached and flooded crater forms a
beautiful landlocked lagoon; and Matuku is reckoned to be one of
the garden spots of Fiji.
The Yasawa group, to the north-west of Viti Levu, includes six
principal islands (four of them large) and many small ones, having
a total area of 135 sq km. These islands, which have been compared
to a string of pearls, extend across the sea for 80 km in shallow
water behind the Great Sea Reef. This area is the destination for
Blue Lagoon Cruises. It is a favorite of many tourists and lives up
to the visitor’s idea of what the South Seas ‘should’ look
like.
Rotuma, a Polynesian outlier 386 km north-west of the Fiji group,
was ceded to Britain in 1881 as part of the colony of Fiji.
Although politically part of Fiji, geographically and
ethnologically it has nothing to do with the islands. Most
Rotumans, who are Polynesians related to the Samoans, live on Viti
Levu rather than their ‘home’ island. Rotuma’s policy is to
discourage tourism.

The islands
with which most visitors find themselves familiar are those of the
Mamanuca group, also an archetypal ‘South Pacific’ locale, just
offshore from Nadi and Lautoka on Viti Levu. It is here that many
of the popular resorts such as Beachcomber, Plantation Island,
Castaway and Mana are located.
Some of the other smaller but well-known islands are Beqa, home of
the firewalkers; Vatulele, famous for its sacred prawns; and Rabi,
once inhabited by Fijians, but now the adopted home of Banabans or
Ocean Islanders (Micronesians) who moved there after WW II (see the
Other Ethnic Groups section later in this chapter). Both Beqa and
Vatulele are off the southern coast of Viti Levu, while Rabi is off
the coast of Taveuni.
Political & Administrative Divisions
Politically, the archipelago is divided into four areas or
‘divisions’: the Northern Division which is composed of Vanua Levu
and the neighbouring islands of Taveuni, Rabi and Qamea; the
Western Division which consists of the western half of the main
island of Viti Levu, including the Yasawa group to the north-west
and Vatulele to the south; the Central Division made up of the
eastern half of Viti Levu; and the Eastern Division, composed of
the Lau, Kadavu and Lomaiviti groups.
Types of Islands

Sailors
generally speak of ‘high’ and ‘low’ islands, but to be geologically
correct there are three types of islands in the archipelago. The
majority are high islands of volcanic origin and low islands which
include coral and limestone varieties. The volcanic islands, of
which Viti Levu is an example, have sharply defined, mountainous
landscapes, ancient volcanoes and rocky outcrops and shores.
Inland, the terrain is broken, with few stretches of flat land
except in river valleys. In the windward areas where rains are
frequent, the hills are covered with thick vegetation and are
smothered almost incessantly with rain. Leeward, growth is sparse
and hills are brown. Lively vestiges of the active volcanic period
are hot springs, which are always found at low elevations. The best
known in Fiji are the springs at Nakama, in the old
coconut-plantation town of Savusavu on Vanua Levu.
Coral islands, although low and small, have their own peculiarly
Robinson Crusoesque charm. Generally located near the inner margin
of a broad reef, they are usually only a few metres above sea
level, are flat as a table and have beautiful white-sand beaches.
Despite limited soil, they often support luxuriant vegetation
including vines, grasses, broad-leaved trees and, of course, the
coconut palm. A classic example is the resort on Beachcomber Island
off Lautoka.
Limestone islands may also appear to be low and flat-topped, but
have steep, sharp sides suggesting that they are huge masses of
rock heaved up from the sea. This is exactly what they are – often
surrounded by a succession of precipitous cliffs, undercut by the
surf. Because the limestone erodes easily, the rock may be pitted
and bristling with sharp pinnacles or cut by ravines or narrow
canyons. Inland, central depressions give the islands a basin-like
appearance. The depression floors are commonly cut up into rolling
hills, fertile and well wooded. A good example of a typical
limestone island is Vanua Balavu in the Lau group.
Of the hundreds of islands in the Fiji group, only a few may be
classed as true atolls. The typical atoll, of which so much has
been written in the romantic literature of the South Seas, is
basically long strips of broken coral and sand ranging from a few
metres to half a km forming a circular or ring-like structure that
surrounds a lagoon. Perhaps the best-known example of an atoll in
Fiji is Wailagilala, on the eastern side of the Nanuku Passage, the
main shipping lane through the islands.