Cirque overdeepening and their relationship to morphometry of a lake

Introduction. The complex relationships among climate, tectonics, ero- .. the cirque is overdeepened, contains a tarn, or is filled with sediment. Glacier Peak , Mount Stewart, Alpine Lakes and Monte Cristo. Peak (Fig. 4). range of morphometric analyses to constrain the nature of early glaciation and subsequent ice sheet evolution in the interior of . the south, Lake Vostok to the east and the Lambert Rift to the north. Cirque overdeepening and their relation-. inferred from the morphometric analysis of glacial cirques . Some cirques host remnants of ancient moraine-dammed lakes, and there is also evidence of eroded remnants of Cirque overdeepening and their relationship to morphometry.

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