Kames

thumb|A kame near Kirriemuir, Scotland thumb|A kame in Yellowstone National Park, Wyoming thumb|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]] 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 land surface with further melting of the glacier. Kames are often associated with kettles, and this is referred to as kame and kettle

river in Nunavut, Canada

The Tüttensee (Lake Tütten) is a small lake in the Chiemgau region, the Bavarian Alpine foothills of the Traunstein district, within the municipalities of Grabenstätt and Vachendorf. With an area of and a maximum depth of , it is one of many Kettle-Lakes in the alpine foothills, that resulted from remnants of dead ice after a glacier retreated.