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  2. Glacial stream - Wikipedia

    en.wikipedia.org/wiki/Glacial_stream

    A glacier stream is a channelized area that is formed by a glacier in which liquid water accumulates and flows. [1] Glacial streams are also commonly referred to as "glacier stream" or/and "glacial meltwater stream". The movement of the water is influenced and directed by gravity and the melting of ice. [1]

  3. Subglacial stream - Wikipedia

    en.wikipedia.org/wiki/Subglacial_stream

    Subglacial streams can transport, deposit, and remove sediment from the glacier bed; this process is influenced by water supply and the amount and characteristics of the available sediment. [12] The size of sediment particles, the slope of the subglacial stream’s channel, and the roughness of the bed all contribute to whether sediment is ...

  4. Sediment transport - Wikipedia

    en.wikipedia.org/wiki/Sediment_transport

    Sediment transport due to fluid motion occurs in rivers, oceans, lakes, seas, and other bodies of water due to currents and tides. Transport is also caused by glaciers as they flow, and on terrestrial surfaces under the influence of wind .

  5. Marine sediment - Wikipedia

    en.wikipedia.org/wiki/Marine_sediment

    Marine sediment, or ocean sediment, or seafloor sediment, are deposits of insoluble particles that have accumulated on the seafloor.These particles either have their origins in soil and rocks and have been transported from the land to the sea, mainly by rivers but also by dust carried by wind and by the flow of glaciers into the sea, or they are biogenic deposits from marine organisms or from ...

  6. Sediment - Wikipedia

    en.wikipedia.org/wiki/Sediment

    Sediment is a solid material that is transported to a new location where it is deposited. [1] It occurs naturally and, through the processes of weathering and erosion, is broken down and subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles.

  7. Ice rafting - Wikipedia

    en.wikipedia.org/wiki/Ice_rafting

    Ice rafting was a primary mechanism of sediment transport during glacial episodes of the Pleistocene when sea levels were very low and much of the land was covered by large masses (sheets) of ice. The rafting of various size sediments into deeper ocean waters by icebergs became a rather important process.

  8. EXPLAINER: How glaciers can burst and send floods downstream

    www.aol.com/news/explainer-glaciers-burst-send...

    The floods that slammed into two hydroelectric plants and damaged villages in northern India were set off by a break on a Himalayan glacier upstream. A large cluster of glaciers are in the ...

  9. Subaqueous fan - Wikipedia

    en.wikipedia.org/wiki/Subaqueous_fan

    Ice is a more efficient agent of erosion compared to wind and water. Glaciers can carry a heavy load of sediment to the ice front of the glacier. At the ice front, as the glacier melts, sediment is deposited. As the glacier moves through a landscape, it begins to form a U-shaped valley which is characteristic of a glacier. [5] These valleys are ...