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Geological Formation

Frederikshåb Glacier

Glaciers and Ice Formations

Frederikshåb Glacier, also called Sioqqap Sermia in Greenlandic and Frederikshåb Isblink or Frederikshåb Gletscher in Danish, is a glacier on the southwest coast of Greenland in the Sermersooq municipality. It flows down from the Greenland ice sheet to a terminus where meltwater collects in ponds and channels before draining into the Davis Strait. The nearest significant settlement is Paamiut, about 110 kilometers to the south; Frederikshåb is itself the historical Danish name for Paamiut. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

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Glaciation, Processes
Source Frederikshåb Glacier (Wikipedia)

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Source Frederikshåb Glacier (Wikipedia)
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Frederikshåb Glacier (Wikipedia)
  • In Discipline: Glaciology, Lead section (in-discipline Glaciology)
    Frederikshåb Glacier (Greenlandic: Sioqqap Sermia, Danish: Frederikshåb Isblink or Frederikshåb Gletscher) is a glacier on the southwest coast of Greenland in the Sermersooq municipality.
  • Caused By: Glaciation, Lead section (caused-by Glaciation)
    Frederikshåb Glacier (Greenlandic: Sioqqap Sermia, Danish: Frederikshåb Isblink or Frederikshåb Gletscher) is a glacier on the southwest coast of Greenland in the Sermersooq municipality.
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