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Periglacial deposits are sediments and landforms created by Periglacial processes in cold, non-glacial environments, characterized by freeze-thaw cycles. These deposits include features like coombe and head deposits, patterned ground, solifluction lobes, and blockfields, often found in areas near glaciers or in regions with permafrost. The deposits are formed by a variety of processes, including frost action, mass movements, and fluvial and aeolian activity.
