Adolf Hoel Glacier
The area where the glacier flows is remote and uninhabited.
History
This glacier was first mapped in 1931 by the Høygaard and Mehren expedition. It was named after Adolf Hoel (1863–1933), Norwegian geologist and chairman of the Arctic Trading Co.
Geography
The Adolf Hoel Glacier originates in the eastern side of the Greenland ice sheet around the area of Hobb Land, with J. L. Mowinckel Land to the south and Arnold Escher Land to the north. It is joined by the Skråbræ from the north. Then it flows along the northern edge of Andrée Land in a roughly WNW/ESE direction until its terminus in the Nunatak Glacier to the east. It has a flow of 0.3 km (0.19 mi) per year.
The Eyvind Fjeld Glacier flows to the north and the Wilkins Nunataks rise to the NW. The Jakob Kjøde Bjerg, a large 1,850 m (6,070 ft) high nunatak, rises off the northeastern side of the glacier, beyond which flows the Waltershausen Glacier.
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Bibliography
- A. K. Higgins, Jane A. Gilotti, M. Paul Smith (eds.), The Greenland Caledonides: Evolution of the Northeast Margin of Laurentia.
See also
References
- ^ "Adolf Hoels Gletscher". Mapcarta. Retrieved 31 July 2019.
- ^ "Catalogue of place names in northern East Greenland". Geological Survey of Denmark. Retrieved 31 July 2019.
- ^ Ice flow in Greenland for the International Polar Year 2008–2009
- ^ Deeply incised submarine glacial valleys beneath the Greenland ice
- ^ Ocean forcing of the Greenland Ice Sheet
External links