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  2. Moraine - Wikipedia

    en.wikipedia.org/wiki/Moraine

    End moraine size and shape are determined by whether the glacier is advancing, receding or at equilibrium. The longer the terminus of the glacier stays in one place, the more debris accumulate in the moraine. There are two types of end moraines: terminal and recessional. Terminal moraines mark the maximum advance of the glacier.

  3. Terminal moraine - Wikipedia

    en.wikipedia.org/wiki/Terminal_moraine

    Terminal moraine of Wordie Glacier, Greenland Map of the Salpausselkä terminal moraines in Southern Finland. A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this point, debris that has accumulated by plucking and abrasion, has been pushed by ...

  4. Valparaiso Moraine - Wikipedia

    en.wikipedia.org/wiki/Valparaiso_Moraine

    PPhysiography of the Valparaiso Moraine. Valparaiso Moraine at Mink Lake, north of Valparaiso, Indiana. The Valparaiso Moraine is a recessional moraine (a landform left by receding glaciers) that forms an immense U around the southern Lake Michigan basin in North America. It is a band of hilly terrain composed of glacial till and sand.

  5. Fluvioglacial landform - Wikipedia

    en.wikipedia.org/wiki/Fluvioglacial_landform

    A recessional moraine is a ridge of deposited debris that occurs when the glacier is stationary for an extended length of time. [27] This occurs when a glacier meaning the glacier is in equilibrium or has halted during retreat . The occurrence of end moraines can be useful for determining a pattern of advance, retreat, and equilibrium of a ...

  6. Glacial landform - Wikipedia

    en.wikipedia.org/wiki/Glacial_landform

    Moraine: Built up mound of glacial till along a spot on the glacier. Feature can be terminal (at the end of a glacier, showing how far the glacier extended), lateral (along the sides of a glacier), or medial (formed by the merger of lateral moraines from contributory glaciers). Types: Pulju, Rogen, Sevetti, terminal, Veiki

  7. Glacier terminus - Wikipedia

    en.wikipedia.org/wiki/Glacier_terminus

    Tracking the change in location of a glacier terminus is a method of monitoring a glacier's movement. The end of the glacier terminus is measured from a fixed position in neighboring bedrock periodically over time. The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record ...

  8. List of glacial moraines - Wikipedia

    en.wikipedia.org/wiki/List_of_Glacial_Moraines

    1.5 Moraines of the Great Plains of the United States. 1.6 Moraines of the U.S. and Canadian Rocky Mountains. 2 Europe. 3 Antarctica. Toggle Antarctica subsection.

  9. Tiefwarensee Ice Age Trail - Wikipedia

    en.wikipedia.org/wiki/Tiefwarensee_Ice_Age_Trail

    The terms ground moraine (Grundmoräne), ablation moraine (Ablationsmoräne) and push moraine (Stauchendmoräne) are explained. A distinction is made between recessional or deposited end moraines ( Satzendmoräne , material left behind by the inland ice when the ice melts) and push moraines ( Stauchendmoräne , till heaped up ahead of the ...