| Adolf Hoel Glacier | |
| Other Name: | Adolf Hoels Gletscher |
| Type: | Piedmont glacier |
| Location: | Greenland |
| Map: | Greenland |
| Coordinates: | 74°N -71°W |
| Mark: | Blue_pog.svg |
| Length: | 45km (28miles) |
| Width: | 7km (04miles) |
| Terminus: | Nunatak Glacier Geologfjord Kaiser Franz Joseph Fjord Greenland Sea |
Adolf Hoel Glacier (Danish: Adolf Hoels Gletscher), 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.
The area where the glacier flows is remote and uninhabited.
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.[1]
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 0.3km (00.2miles) per year.[2]
The Eyvind Fjeld Glacier flows to the north and the Wilkins Nunataks rise to the NW. The Jakob Kjøde Bjerg, a large 1850m (6,070feet) high nunatak, rises off the northeastern side of the glacier, beyond which flows the Waltershausen Glacier.[3] [4] [5]