Fluvioglacial landform
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Fluvioglacial landforms or glaciofluvial landforms are those that result from the associated erosion and deposition of sediments caused by glacial meltwater. Glaciers contain suspended sediment loads,
Thórsmörk glacial outwash plain
Esker in Einunndalsranden naturreservat, Hedmark, Norway
Mouth of the Schlatenkees glacier in Austria
Braldu River below the Baltoro Glacier in Pakistan
Kame
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A kame, or knob, is a glacial landform, an irregularly shaped hill or mound composed of sand, gravel and till that accumulates in a depression on a retreating glacier, and is then deposited on the lan
A kame near Kirriemuir, Scotland
A kame in Yellowstone National Park, Wyoming
A kame among the glacial drift on the terminal moraine of the Okanagan Lobe of the Cordilleran Ice Sheet on the Waterville Plateau of the Columbia Plateau in Washington
Kame terraces in the eastern Pyrenees of France: Montfillà (left), above the Porta valley, Cerdagne; and Pla de l'Orri (right), above the Cabrils valley, Conflent