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  2. Glacial motion - Wikipedia

    en.wikipedia.org/wiki/Glacial_motion

    This type of motion is enhanced if the bed is soft sediment, if the glacier bed is thawed and if meltwater is prevalent. Bed deformation is thus usually limited to areas of sliding. Seasonal melt ponding and penetrating under glaciers shows seasonal acceleration and deceleration of ice flows affecting whole icesheets. [3]

  3. 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]

  4. Regelation - Wikipedia

    en.wikipedia.org/wiki/Regelation

    Melting curve of ice Molecular structure of ice near the surface. For a normal crystalline ice far below its melting point, there will be some relaxation of the atoms near the surface. Simulations of ice near to its melting point show that there is significant melting of the surface layers rather than a symmetric relaxation of atom positions.

  5. Scientists discover hidden impact of melting water from ...

    www.aol.com/scientists-discover-hidden-impact...

    The impact of so-called “meltwater” on how fast Antarctic glaciers melt is not yet taken into account. The study, from The Scripps Institution of Oceanography, suggests that glacier melting ...

  6. Fluvioglacial landform - Wikipedia

    en.wikipedia.org/wiki/Fluvioglacial_landform

    At the interface of the glacier and the underlying land surface, the immense weight of the glacier causes ice to melt and produces subglacial meltwater streams. These streams under immense pressure and at high velocities along with the overlying weight of the glacier itself are able to carve into landscapes and pluck sediment from the ground. [6]

  7. Ice calving - Wikipedia

    en.wikipedia.org/wiki/Ice_calving

    Melting at the waterline is an important second order calving process as it undercuts the subaerial ice, leading to collapse. Other second order processes include tidal and seismic events, buoyant forces and melt water wedging. When calving occurs due to waterline melting, only the subaerial part of the glacier will calve, leaving a submerged ...

  8. Swiss start measuring latest glacier melts after hot summer - AOL

    www.aol.com/news/swiss-start-measuring-latest...

    Fields of white snow and ice are giving way to grey rocky outcrops in the Swiss Alps as glaciers melt after another hot summer. And another wave of melting is expected to be confirmed this year ...

  9. Alpine glaciers melt at record rate after heatwaves - AOL

    www.aol.com/news/alpine-glaciers-melt-record...

    STORY: Heatwaves across Europe have claimed another kind of victim.The Alps' glaciers are melting at a record rate in at least 60 years' worth of record keeping.That's according to data shared ...