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- W2766882010 abstract "Abstract The laterite-capped Mysore Plateau is bordered both on the east and west sides by ruggedly high and linear mountain ranges rising 500–1000 m above its 700- to 900-m-high planation surface of the plateau. Characterized by planar scarps with sparse gullies and a few planation surfaces, the high laterite-topped mountain ranges are dissected by N–S- and NNW–SSE-trending fractures and faults, whereas the main part of the plateau is broken into blocks by long, deep curvilinear shear zones of Precambrian antiquity. The mature old River Kaveri that consistently flows eastwards abruptly swerves left or right along the N–S fault planes and then drops into a canyon that is characterized by channel-in-channel geomorphology before leaving the mountain domain. Like the Kaveri (Cauvery), most of the rivers cross hills and ridges as antecedent rivers. Ponding of the Kaveri and its tributaries gave rise to a huge lake that stretched as much as 45 km upstream. The lake is now represented by a thick pile of black clay deposits of Late Quaternary age, forming the granary of Karnataka state. Demarcated by E–W-trending, two continent-wide shear zones of Precambrian age, the laterite-capped, 2670 m-high, Nilgiri massif is characterized by many planation surfaces, steep to nearly vertical scarps on all sides, and meandering streams descending through canyons as water falls. These features imply fast uplift and attendant exhumation of the Precambrian terrane that rose up like a horst." @default.
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- W2766882010 date "2017-01-01" @default.
- W2766882010 modified "2023-09-27" @default.
- W2766882010 title "Mysore Plateau and Nilgiri Massif" @default.
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- W2766882010 doi "https://doi.org/10.1016/b978-0-444-63971-4.00012-8" @default.
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