Geography
The Andaman Archipelago is an oceanic continuation of the Burmese Arakan Yoma range in the North and of the Indonesian Archipelago in the South. It has 325 islands which cover an area of 6,408 km2 (2,474 sq mi), with the Andaman Sea to the east between the islands and the coast of Burma. North Andaman Island is 285 kilometres (177 mi) south of Burma, although a few smaller Burmese islands are closer, including the three Coco Islands.
The Ten Degree Channel separates the Andamans from the Nicobar Islands to the south. The highest point is located in North Andaman Island (Saddle Peak at 732 m (2,402 ft)).
The subsoil of the Andaman islands consists essentially of Late Jurassic to Early Eocene ophiolites and sedimentary rocks (argillaceous and algal limestones), deformed by numerous deep faults and thrusts with ultramafic igneous intrusions. There are at least 11 mud volcanoes on the islands.
The climate is typical of tropical islands of similar latitude. It is always warm, but with sea-breezes. Rainfall is irregular, but usually dry during the north-east, and very wet during the south-west, monsoons.
Read more about this topic: Andaman Islands
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