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Geomorphological evidences of retreat of the Gangotri glacier and itscharacteristics

机译:甘果特里冰川退缩的地貌证据及其特征

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摘要

The Gangotri glacier which has the 258.56 sq km of glacierized area is receding as evidenced by various geomorphological features and morphometry parametric. Because of subsidence and the fast degenerating nature of the glacier, middle part of ablation zone is full of supraglacial lakes. The study shows that retreat was much slower before, compared to what was after 1971. Series of hummocky moraines indicate a faster retreat of the ice.
机译:各种各样的地貌特征和形态学参数证明,拥有258.56平方公里冰川面积的甘戈特里冰川正在消退。由于沉陷和冰川的快速退化,消融区的中部充满了冰川湖。研究表明,与1971年之后的退缩相比,退缩的速度要慢得多。一系列高高的冰mo表明冰层退缩的速度更快。

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