Push moraine: Revision history

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4 May 2024

  • curprev 19:2219:22, 4 May 2024‎ Ai talk contribs‎ 2,659 bytes +2,659‎ Created page with "== Overview == A push moraine is a type of moraine that forms at the terminus of a glacier. It is composed of unconsolidated debris, or till, that has been pushed forward by the advancing glacier and deposited at its snout. This process is a key aspect of glacial geomorphology, the study of landforms created by the action of glaciers and ice sheets. <div class='only_on_desktop image-preview'><div class='image-preview-loader'></div></div><div class='only..."
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