Titlebook: Glacial Geomorphology; A proceedings volume Donald R. Coates Conference proceedings 1982 Donald R. Coates 1982 Geomorphology

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Glacial Grooves and Periglacial Features in the Saharan Ordovicianh-language audiences. (A comprehensive, detailed report is available only in French.) Some special problems are discussed in more detail..Remarkable deep and almost rectilinear glacial grooving can be followed across almost flat terrain for tens of kilometers. Scattered evidences confirming the glac

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intimate

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https://doi.org/10.1007/978-3-030-65912-7he glacial margin (the glacier is frozen to its bed in most places, excess pore-water pressure is dissipated by marginal seepage, and the glacial flow is upward) and an abrasion zone behind the margin (the bed is thawed and the glacier is sliding, excess pore-water pressure is not dissipated, and th

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,Anhang mit Bildtafeln zu den L?tversuchen,position, the tendency is to develop a form which imposes minimum resistance to glacier flow. Erosion commonly precedes deposition, but either may dominate in shaping of a particular drumlin field..Drumlin form is affected by protrusions in the glacially overridden topography and by character and ab