Till
Till or glacial till is unsorted glacial sediment.Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines.
Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Provided by Wikipedia
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2by Kasielke, TillGet access
Published 2016
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