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The Banda Arc is a double island arc formed by the collision of the Indo-Australian plate with the Eurasian plate that commenced around 15 to 12 million years ago. [2] Principal islands include Timor , Flores , and Seram .
Location of the Banda Islands in the center of the Maluku Islands Map of the Banda Islands. The Banda Islands (Indonesian: Kepulauan Banda) are a volcanic group of ten small volcanic islands in the Banda Sea, about 140 km (87 mi) south of Seram Island and about 2,000 km (1,243 mi) east of Java, and constitute an administrative district (kecamatan) within the Central Maluku Regency in the ...
The Outer Banda Arc includes the Kai Islands, Tanimbar Islands, Babar Islands, and Leti Islands. Yamdena in the Tanimbar Islands is the largest island in the ecoregion. Yamdena is mostly low, with a maximum elevation of 120 meters. Yamdena and several other Outer Arc islands have areas of karst where the island's limestone was uplifted and then ...
Banda Arc tectonic map, Weber Deep in the ForeArc basin Location of the Banda Sea in Southeast Asia Banda Sea in the center of Maluku Islands Map of the Banda Sea plate. Weber Deep is at the location of the number 57 on the map. Weber Deep (Indonesian: Kedalaman Weber) is the deepest point in the Banda Sea off Indonesia. Weber Deep maximum ...
Together with Sumba, Babar and associated smaller islands, Timor forms the southern outer archipelago of the Lesser Sunda Islands with the inner islands of Flores, Alor and Wetar to the north, and beyond them Sulawesi. Timor is the principal island of the Outer Banda Arc, which is being uplifted by arc-continent collision with the Australian ...
Mount Manuk is a truncated andesitic volcano on Manuk Island. Rising 3,000 m from the sea floor, it is the easternmost volcano of the Banda Arc chain that forms a volcanic island. No confirmed historical eruptions are known from Manuk. [1]
Leti is an Indonesian island, ... The nature of the Banda Arc-continent; collision in the Timor region. In: D. Brown and P.D. Ryan (eds.) Arc-continent collision ...
This series of islands formed when the northern edge of the Australian continent was upthrust in collision with southeast Asia. These islands are paralleled by the Inner Banda Arc, a series of active and extinct volcanic islands, including neighboring Wetar. The islands in the Banda Arc are arranged in a distinct horseshoe shape and represent a ...