Map - Palace - Fiji

A palace is a grand residence, especially a royal residence, or the home of a head of state or some other high-ranking dignitary, such as a bishop or archbishop. The word is derived from the Latin name pal?tium, for Palatine Hill in Rome which housed the Imperial residences. Most European languages have a version of the term (palais, palazzo, palacio, etc.), and many use it for a wider range of buildings than English. In many parts of Europe, the equivalent term is also applied to large private houses in cities, especially of the aristocracy; often the term for a large country house is different. Many historic palaces are now put to other uses such as parliaments, museums, hotels, or office buildings. The word is also sometimes used to describe a lavishly ornate building used for public entertainment or exhibitions such as a movie palace. A palace is distinguished from a castle while the latter clearly is fortified or has the style of a fortification, whereas a palace does not.

Fiji (, ; Viti, ; Fiji Hindi: ?????, Fij?), officially the Republic of Fiji, is an island country in Melanesia, part of Oceania in the South Pacific Ocean. It lies about 1100 nmi north-northeast of New Zealand. Fiji consists of an archipelago of more than 330 islands—of which about 110 are permanently inhabited—and more than 500 islets, amounting to a total land area of about 18300 km2. The most outlying island group is Ono-i-Lau. About 87% of the total population of live on the two major islands, Viti Levu and Vanua Levu. About three-quarters of Fijians live on Viti Levu's coasts: either in the capital city of Suva; or in smaller urban centres such as Nadi—where tourism is the major local industry; or in Lautoka, where the sugar-cane industry is dominant. The interior of Viti Levu is sparsely inhabited because of its terrain.

The majority of Fiji's islands were formed by volcanic activity starting around 150 million years ago. Some geothermal activity still occurs today on the islands of Vanua Levu and Taveuni. The geothermal systems on Viti Levu are non-volcanic in origin and have low-temperature surface discharges (of between roughly 35 and 60 C).