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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    Glacial motion can be fast (up to 30 metres per day (98 ft/d), observed on Jakobshavn Isbræ in Greenland) [1] or slow (0.5 metres per year (20 in/year) on small glaciers or in the center of ice sheets), but is typically around 25 centimetres per day (9.8 in/d).

  3. Ice stream - Wikipedia

    en.wikipedia.org/wiki/Ice_stream

    An ice stream is a region of fast-moving ice within an ice sheet. It is a type of glacier , a body of ice that moves under its own weight. [ 2 ] They can move upwards of 1,000 metres (3,300 ft) a year, and can be up to 50 kilometres (31 mi) in width, and hundreds of kilometers in length. [ 3 ]

  4. Subglacial stream - Wikipedia

    en.wikipedia.org/wiki/Subglacial_stream

    The glacier encounters more bumps due to its higher speed and, since ice moving at a higher speed is less able to maintain connection with the bedrock, faster moving glaciers are more likely to form cavities when passing over bumps. [2] [1] This increases the subglacial space which can be filled with water, decreasing basal water pressure. [7]

  5. 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]

  6. Plucking (glaciation) - Wikipedia

    en.wikipedia.org/wiki/Plucking_(glaciation)

    As a glacier moves down a valley, friction causes the basal ice of the glacier to melt and infiltrate joints (cracks) in the bedrock. The freezing and thawing action of the ice enlarges, widens, or causes further cracks in the bedrock as it changes volume across the ice/water phase transition (a form of hydraulic wedging), gradually loosening ...

  7. Overdeepening - Wikipedia

    en.wikipedia.org/wiki/Overdeepening

    The glacier does not move uniformly, but rather shows changing patterns of motion as the season progresses, which result from the seasonal evolution of the subglacial drainage system. The largest glacial movements were observed during periods of transition, as increasing water was released into the glacier.

  8. Antarctic ice sheet - Wikipedia

    en.wikipedia.org/wiki/Antarctic_ice_sheet

    [115] [117] Then, the subglacial basins would gradually collapse over a period of around 2,000 years, although it may be as fast as 500 years or as slow as 10,000 years. [ 115 ] [ 117 ] Their loss would ultimately add between 1.4 m (4 ft 7 in) and 6.4 m (21 ft 0 in) to sea levels, depending on the ice sheet model used.

  9. Minecraft server - Wikipedia

    en.wikipedia.org/wiki/Minecraft_server

    A Minecraft server is a player-owned or business-owned multiplayer game server for the 2011 Mojang Studios video game Minecraft. In this context, the term "server" often refers to a network of connected servers, rather than a single machine. [ 1 ]