| Rimfaxe | |
|---|---|
| Rimfaxe Gletscher | |
 Kattertooq and Sehested Fjords map section | |
  Location within Greenland | |
| Location | Greenland |
| Coordinates | 63°18′N42°25′W / 63.300°N 42.417°W Coordinates: 63°18′N42°25′W / 63.300°N 42.417°W |
| Terminus | Sehested Fjord, North Atlantic Ocean |
Rimfaxe (Danish : Rimfaxe Gletscher [1] ) is a glacier of the King Frederick VI Coast in the Sermersooq municipality, southeastern Greenland.
This glacier is named after Hrimfaxi, the cosmic horse of Norse mythology.
Rimfaxe is a large, active glacier flowing from the eastern side of the Greenland ice sheet. [2]
The Rimfaxe glacier flows roughly southeastward between high peaks and has its terminus in the Sehested Fjord shortly after its confluence with the Guldfaxe Glacier that joins it from the west. The smaller Ygdrasil glacier flows to the east, running parallel to it, and has its terminus in a lake that discharges right by the terminus of the Rimfaxe. [3]
The Greenland ice sheet is a vast body of ice covering 1,710,000 square kilometres (660,000 sq mi), roughly 79% of the surface of Greenland.
Glacial motion is the motion of glaciers, which can be likened to rivers of ice. It has played an important role in sculpting many landscapes. Most lakes in the world occupy basins scoured out by glaciers. Glacial motion can be fast or slow, but is typically around 25 centimetres per day (9.8 in/d).
Jakobshavn Glacier, also known as Ilulissat Glacier, is a large outlet glacier in West Greenland. It is located near the Greenlandic town of Ilulissat and ends at the sea in the Ilulissat Icefjord.
Glacier ice accumulation occurs through accumulation of snow and other frozen precipitation, as well as through other means including rime ice, avalanching from hanging glaciers on cliffs and mountainsides above, and re-freezing of glacier meltwater as superimposed ice. Accumulation is one element in the glacier mass balance formula, with ablation counteracting. With successive years in which accumulation exceeds ablation, then a glacier will experience positive mass balance, and its terminus will advance.
Waltershausen Glacier is one of the major glaciers in Greenland. It has its terminus on the east coast of the Greenland ice sheet.
Wordie Glacier is a glacier in northeastern Greenland. It has its terminus on the east coast of the Greenland ice sheet.
Sehested Fjord ) is a fjord of the King Frederick VI Coast in the Sermersooq municipality, southeastern Greenland.
Ryder Glacier, is one of the major glaciers in northern Greenland.
Fimbul Glacier, is a glacier in eastern Greenland.
Farquhar Glacier, is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality.
Melville Glacier, is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality.
Hart Glacier, is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality.
Sharp Glacier, is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality.
Leidy Glacier, is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality.
Adolf Hoel Glacier, also known as Hoel Glacier(Hoels Gletscher), is one of the major glaciers in King Christian X Land, Northeast Greenland. Administratively it lies in the Northeast Greenland National Park zone.
Heim Glacier, is a glacier in eastern Greenland. It is named after Swiss geologist and glacial phenomena expert Albert Heim (1849–1937).
Skinfaxe is a glacier of the King Frederick VI Coast in the Sermersooq municipality, southeastern Greenland.
Guldfaxe is a glacier of the King Frederick VI Coast area in the Sermersooq municipality, southeastern Greenland.
Tjasse is a glacier of the King Frederick VI Coast area in the Sermersooq municipality, southeastern Greenland.
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