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Physical geography of Assam
This article discusses the geological origin, geomorphic characteristics, and climate of the northeastern Indian state of Assam.
Assam, extending from 89° 42′ E to 96° E longitude and 24° 8′ N to 28° 2′ N latitude, has an area of 78,438 km², similar to that of Ireland or Austria.
==Geologic and geomorphic origin==
Geologically, as per the plate techtonics, Assam is in the eastern most projection of the Indian Plate, where it thrusts underneath the Eurasian Plate creating a subduction zone. It is postulated that due to the northeasterly movement of the Indian plate, the sedimentary layers of an ancient geocyncline called the Tethys (in between Indian and Eurasian Plates) were pushed upward to form the Himalayas. It is estimated that the height of the Himalayas is increasing by 4 cm each year. Therefore, Assam possesses a special geomorphic environment, with large plains and dissected hills of the South Indian Plateau system abutting the Himalayas to the north, north-east and east.
Geomorphic studies also conclude that the Brahmaputra is a paleo-river, older than the Himalayas, which often crosses higher altitudes in the Himalayas eroding at a greater pace than the increase in the height of the mountain range to sustain its flow. The height of the surrounding regions still increasing forming steep gorges in Arunachal.
抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』
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