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A simplified map of the geological structures of Indonesia. The tectonics of Indonesia are very complex, as it is a meeting point of several tectonic plates.Indonesia is located between two continental plates: the Sahul Shelf and the Sunda Plate; and between two oceanic plates: the Pacific Plate and the Philippine Sea Plate.
Tourism is now the largest single industry in terms of income, and as a result, Bali is one of Indonesia's wealthiest regions. In 2003, around 80% of Bali's economy was tourism related. [ 13 ] By the end of June 2011, the rate of non-performing loans of all banks in Bali were 2.23%, lower than the average of Indonesian banking industry non ...
English: Location map of Bali, Indonesia Geographic Coordinate System WGS 1984 (EPSG: 4326) Equirectangular Projection Geographic limits of the map: N: 7.6553417° S;
Map of Sahul and Sunda. Geologically, the Sunda Shelf (/ ˈ s ʌ n d ə / [1]) is a south-eastern extension of the continental shelf of Mainland Southeast Asia.Major landmasses on the shelf include the Indonesian islands of Bali, Borneo, Java, Madura, and Sumatra, as well as their surrounding smaller islands. [2]
In geology, a continent is defined by continental crust, which is a platform of metamorphic and igneous rocks, largely of granitic composition. Continental crust is less dense and much thicker than oceanic crust, which causes it to "float" higher than oceanic crust on the dense underlying mantle. This explains why the continents form high ...
Nusa Lembongan is an island located southeast of Bali, Indonesia. It is part of a group of three islands that make up the Nusa Penida district, of which it is the most famous of the three islands of Nusa Penida, Nusa Lembongan, and Nusa Ceningan - known together as the "Nusa Islands". [ 1 ]