description Clark Esker Overview
Clark Esker is a named glacial ridge in Manitoba, Canada, composed of stratified sand and gravel deposited by meltwater during the last glaciation. Its elongated form records the movement of water within or beneath glacial ice and remains as a visible part of the postglacial landscape. The feature is relevant to the study of eskers, glacial deposits, and the geological history of Manitoba. It is a landform rather than a built structure or inhabited place.
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