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  2. 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.

  3. Glaciology - Wikipedia

    en.wikipedia.org/wiki/Glaciology

    Collective name for the morphologic structures in/on/under/around a glacier. Moraine Accumulated debris that has been carried by a glacier and deposited at its sides (lateral moraine) or at its foot (terminal moraine). Névé Area at the top of a glacier (often a cirque) where snow accumulates and feeds the glacier. Nunatak/Rognon/Glacial Island

  4. 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

  5. Fluvioglacial landform - Wikipedia

    en.wikipedia.org/wiki/Fluvioglacial_landform

    Lateral Moraine: moraine in upper Engadin left by retreating glacier Lateral moraines are ridges of sediment deposited alongside the glacier running parallel to the long axis of the glacier. These sediments are typically deposited on top of the ice ( supraglacial till) at the margin of the glacier and as such do not experience the same amount ...

  6. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Lateral moraines are formed on the sides of the glacier. Medial moraines are formed when two different glaciers merge and the lateral moraines of each coalesce to form a moraine in the middle of the combined glacier. Less apparent are ground moraines, also called glacial drift, which often blankets the surface underneath the glacier downslope ...

  7. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    The stream issuing from the glacier will then become clearer as glacial flour diminishes. Lakes and ponds can also be caused by glacial movement. Kettle lakes form when a retreating glacier leaves behind an underground chunk of ice. Moraine-dammed lakes occur when a stream (or snow runoff) is dammed by glacial till.

  8. What causes earthquakes? The science behind why seismic ... - AOL

    www.aol.com/causes-earthquakes-science-behind...

    What causes earthquakes? Earthquakes occur when the plates that make up the Earth's crust move around. These plates, called tectonic plates, can push against each other. ... Earthquakes occur when ...

  9. Moraine-dammed lake - Wikipedia

    en.wikipedia.org/wiki/Moraine-dammed_lake

    A moraine-dammed lake, occurs when the terminal moraine has prevented some meltwater from leaving the valley. When a glacier retreats, there is a space left over between the retreating glacier and the piece that stayed intact which holds leftover debris . Meltwater from both glaciers seep into this space creating a ribbon-shaped lake due to the ...