2021
DOI: 10.1007/s12665-021-09561-2
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Fluvial response to active tectonics: analysis of DEM-derived longitudinal profiles in the Rangit River Basin, Eastern Himalayas, India

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Cited by 9 publications
(1 citation statement)
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“…The main river of the valley, Rangeet originates in the glaciers of Mount Kabru at an elevation of 7412 m, at the southern flank of the Khangchendzonga Massif. On its way downstream, it merges with river Teesta (another major river system of Sikkim) at around 200 m. The Rangeet river catchment has an area of 2132 km 2 and is stretched 98 km in length (Sarkar et al., 2021). This area includes the river's source in the Rathong Glacier on the southern slopes of the Kabru Massif near Mount Khangchendzonga and the numerous tributaries that join it along its course before it flows into the Teesta river.…”
Section: Methodsmentioning
confidence: 99%
“…The main river of the valley, Rangeet originates in the glaciers of Mount Kabru at an elevation of 7412 m, at the southern flank of the Khangchendzonga Massif. On its way downstream, it merges with river Teesta (another major river system of Sikkim) at around 200 m. The Rangeet river catchment has an area of 2132 km 2 and is stretched 98 km in length (Sarkar et al., 2021). This area includes the river's source in the Rathong Glacier on the southern slopes of the Kabru Massif near Mount Khangchendzonga and the numerous tributaries that join it along its course before it flows into the Teesta river.…”
Section: Methodsmentioning
confidence: 99%