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  2. Glacial till plains (Ohio) - Wikipedia

    en.wikipedia.org/wiki/Glacial_till_plains_(Ohio)

    The Glacial till plains are a till plain landform in Northern Ohio, located near the shore of Lake Erie and produced by the retreat of the Wisconsin glaciation. Since glacial till is highly fertile soil, agriculture on the glacial till plains is very productive. The region has gently rolling moraine hills left over from the retreating glaciers ...

  3. Till - Wikipedia

    en.wikipedia.org/wiki/Till

    Till after avalanche, Norway. 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 ...

  4. Till plain - Wikipedia

    en.wikipedia.org/wiki/Till_plain

    Till plains are large flat or gently sloping areas of land on which glacial till has been deposited from a melted glacier. In some areas, these depositions can be up to hundreds of feet thick. The morphology of the till plain is generally reflective of the topography of the bedrock below the glacier. Another term for till plain is ground ...

  5. Withrow Moraine and Jameson Lake Drumlin Field - Wikipedia

    en.wikipedia.org/wiki/Withrow_Moraine_and...

    47°41′15″N 119°37′29″W  /  47.68750°N 119.62472°W  / 47.68750; -119.62472. Designated. 1986. The Withrow Moraine and Jameson Lake Drumlin Field is a National Park Service –designated privately owned National Natural Landmark located in Douglas County, Washington state, United States. [1] Withrow Moraine is the only Ice ...

  6. Moraine - Wikipedia

    en.wikipedia.org/wiki/Moraine

    The snow-free debris hills around the lagoon are lateral and terminal moraines of a valley glacier in Manang, Nepal.. A moraine is any accumulation of unconsolidated debris (regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet.

  7. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Glacial landform. Glacial landforms are landforms created by the action of glaciers. Most of today's glacial landforms were created by the movement of large ice sheets during the Quaternary glaciations. Some areas, like Fennoscandia and the southern Andes, have extensive occurrences of glacial landforms; other areas, such as the Sahara, display ...

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