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Qinnguata Kuussua
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Geliefert zwischen Mi., 26.11.2025 und Do., 27.11.2025
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High Quality Content by WIKIPEDIA articles! Qinnguata Kuussua is a river in the Qeqqata municipality in central-western Greenland. Its source is a large meltwater outflow from Russell Glacier flowing from the Greenland Ice Sheet. It is the main river in the Kangerlussuaq area. For most of its run, the river is very wide, up to 2 km (1.2 mi) in the upper reaches. The climate is polar continental, with the area receiving very little rainfall. Several meltwater outflow streams from the southern base of the Russell Glacier (66°57 45 N 50°00 00 W / 66.9625°N 50°W / 66.9625; -50) form the Qinnguata Kuussua river. The valley is 31 km (19 mi) long, oriented east-south-east to west-north-west. From the north it is bounded by an exposed, barren, and flattened ridge of Akuliarusiarsuk. From the south, the river valley is delimited by a sequence of tundra ranges, culminating in Tasersuatsiaap Kinginnera at 591 m (1,939 ft), and petering out near Kangerlussuaq in the form of a low, wide ridge of Qaarsorsuaq.
Weitere Informationen
- Allgemeine Informationen
- GTIN 09786131394935
- Genre Geowissenschaften
- Editor Lambert M. Surhone, Mariam T. Tennoe, Susan F. Henssonow
- Anzahl Seiten 88
- Herausgeber Betascript Publishing
- EAN 9786131394935
- Titel Qinnguata Kuussua
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