Deformation of the Hidden Creek Lake ice dam: evidence for faulting through the entire thickness of a glacier (original) (raw)

Abstract

As a glacier-dammed lake fills, a large volume of water may be stored beneath the ice dam (the part of the glacier adjacent to the lake) and then released during a subsequent jökulhlaup. The surface of the ice dam rises and falls accordingly. At Kennicott Glacier, Alaska, the kinematics of such motion during the annual jökulhlaup cycle of Hidden Creek

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