Fiji has a complex geologic history. In light of a lowered foundation of old development, the Fiji islands are to a great extent the result of volcanic activity, sedimentary store, and arrangements of coral. Viti Levu has an area of around 4,000 square miles (10,000 square km) and records for the greater part of Fiji’s territory region. A rough isolating reach running from north to south has a few tops over 3,000 feet (900 meters), including Tomanivi (previously Mount Victoria), at 4,344 feet (1,324 meters) the most elevated point in Fiji. The primary waterway frameworks — the Rewa, Navua, Sigatoka (Singatoka), and Ba (Mba) — all have their headwaters in the focal mountain region. Toward the southeast and southwest, as well concerning the south where the reach partitions, the mountains give way to levels and afterward swamps. The waterfront fields in the west, northwest, and southeast record for short of what one-fifth of Viti Levu’s region however are the fundamental communities of farming and settlement.

Waya Island, Yasawa Gathering, Fiji.
Vanua Levu, the second biggest island, has an area of around 2,140 square miles (5,540 square km). It is separated along its length by a mountain range with tops ascending to in excess of 3,000 feet. On the island’s northern coast, away from the mouth of the Dreketi (Ndreketi) Stream, the waterfront fields are thin. The greater part of different islands, including the Lomaiviti, Lau, and Yasawa gatherings, are volcanic in beginning, in any case, similar to the significant islands, they are limited by coral reefs, seaward shakes, and sandbars that make the Koro Ocean perilous for route.