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  2. Ice calving - Wikipedia

    en.wikipedia.org/wiki/Ice_calving

    Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. [1] It is a form of ice ablation or ice disruption . It is the sudden release and breaking away of a mass of ice from a glacier , iceberg , ice front , ice shelf , or crevasse .

  3. Larsen Ice Shelf - Wikipedia

    en.wikipedia.org/wiki/Larsen_Ice_Shelf

    The Larsen Ice Shelf is a long ice shelf in the northwest part of the Weddell Sea, extending along the east coast of the Antarctic Peninsula [1] from Cape Longing to Smith Peninsula. It is named after Captain Carl Anton Larsen , the master of the Norwegian whaling vessel Jason , who sailed along the ice front as far as 68°10' South during ...

  4. Ice shelf - Wikipedia

    en.wikipedia.org/wiki/Ice_shelf

    Some named Antarctic iceshelves. Ice shelf extending approximately 6 miles into the Antarctic Sound from Joinville Island. An ice shelf is "a floating slab of ice originating from land of considerable thickness extending from the coast (usually of great horizontal extent with a very gently sloping surface), resulting from the flow of ice sheets, initially formed by the accumulation of snow ...

  5. Chunks of Argentina's Perito Moreno Glacier break off - AOL

    www.aol.com/news/2016-03-11-chunks-of-argentinas...

    Massive chunks of Argentina's Perito Moreno Glacier, which is known as the "White Giant," collapsed into the water on Thursday as tourists and locals watched from an observation deck.

  6. Icefall - Wikipedia

    en.wikipedia.org/wiki/Icefall

    Perhaps the most conspicuous consequence of glacier flow, icefalls occur where the glacier bed steepens and/or narrows. Most glacier ice flows at speeds of a few hundred metres per year or less. However, the flow of ice in an icefall may be measured in kilometres per year. Such rapid flow cannot be accommodated by plastic deformation of the ice.

  7. Moulin (geomorphology) - Wikipedia

    en.wikipedia.org/wiki/Moulin_(geomorphology)

    Moulins are parts of the internal structure of glaciers, that carry meltwater from the surface down to wherever it may go. [7] Water from a moulin often exits the glacier at base level, sometimes into the sea, and occasionally the lower end of a moulin may be exposed in the face of a glacier or at the edge of a stagnant block of ice .

  8. 'Glacial outburst flood' sweeps away homes in Alaska capital

    www.aol.com/weather/glacial-outburst-flood...

    A group of people take in the views of the Mendenhall Glacier on June 8, 2023, in Juneau, Alaska. The glacier in the summer is accessible by kayak or canoe, by foot on a challenging trail or by ...

  9. Today's Wordle Hint, Answer for #1256 on Tuesday, November 26 ...

    www.aol.com/lifestyle/todays-wordle-hint-answer...

    Today's Wordle Answer for #1256 on Tuesday, November 26, 2024. Today's Wordle answer on Tuesday, November 26, 2024, is WITCH. How'd you do? Next: Catch up on other Wordle answers from this week.