Skjoldungen
Native name: <span class="nickname" ">Saqqisikuik | |
---|---|
Skjoldungen | |
Geography | |
Location |
Irminger Sea North Atlantic Ocean |
Coordinates | 63°19′N 41°30′W / 63.317°N 41.500°WCoordinates: 63°19′N 41°30′W / 63.317°N 41.500°W |
Area | 450.3 km2 (173.9 sq mi) |
Length | 49 km (30.4 mi) |
Width | 14 km (8.7 mi) |
Coastline | 158.8 km (98.67 mi) |
Highest elevation | 1,738 m (5,702 ft) |
Highest point | Azimuthbjerg |
Administration | |
Greenland | |
Municipality | Sermersooq |
Demographics | |
Population | 0 |
Skjoldungen (Greenlandic: Saqqisikuik)[1] is a large uninhabited island in the King Frederick VI Coast, southeastern Greenland. Administratively it is part of the Sermersooq municipality. The weather of the island is characterized by tundra climate.[2]
The island was named by Wilhelm August Graah (1793–1863) after Skjoldungen or Skioldungen, a honorific title for the successors (Scyldings) of legendary King Skjold to the ancient Danish throne in Norse mythology.[3]
Geography
Skjoldungen is a coastal island in the southeastern shores of Greenland. It is located between two fjords, the Southern Skjoldungen Fjord (Danish: Sonder Skjoldungesund; Greenlandic: Inugsuarmiut), to the southwest, and the Northern Skjoldungen Fjord (Danish: Nordre Skjoldungesund) to the northeast[4] between Skjoldungen and one of the arms of the Thorland Peninsula. The Morke Sound (Danish: Mørkesund) is a 700 metres (2,297 feet) wide sound that joins both fjords in the NW, separating the island from the mainland.[5]
The island stretches 49 kilometres (30 miles) in a NE/SW direction. Its highest point is Azimuthbjerg, a 1,738 m high ultra-prominent peak at the NW end of the island.[6] Skjoldungen's maximum width is 14 kilometres (9 miles).[7] Skjoldungen Island has a rugged terrain, which includes the Skjoldmøen, Bjarje and Hjalte glaciers and the Gedebukken, Pandebrasken, Skuren and Sfinksen nunataks.[5] The southern part divides into two peninsulas jutting southeastwards, the Roar Peninsula (Danish: Roar Halvø) and the Helge Peninsula (Danish: Helges Halvø). Skjoldungen's southernmost headland is Cape Niels Juel, a narrow cape of reddish-brown rock at the end of the Helge Peninsula. 3.5 kilometres (2 miles) long Anarnitsoq island lies just to the west of the cape.[5]
History
Since the eastern coast of Greenland was inhabited by Paleo-Eskimo people around 4,000 years ago, the Skjoldungen Fjords were likely inhabited or visited by nomadic hunters.[8] At the Qoornoq site, located on a small headland by the shore of the Southern Skjoldungen Fjord, there are archaeological remains of later historical periods.[9] These include Thule culture graves[10] indicating that Inuit people lived on the island after the 13th century.[11]
There are remains of relatively recent abandoned Inuit dwellings inside the fjord on Skjoldungen's western shore. These date back to 1938 when one hundred and fifty Inuit from Ammassalik were convinced by the Danish authorities to settle in this large island. During World War II a weather station was built and run by the Allies on Skjoldungen, as well as another one on Cape Adelaer further south down the coast at 61°50′N 42°5′W / 61.833°N 42.083°W.[12] The inhabitants of the Inuit settlement were relocated in 1965 following a nationwide program to concentrate the population of Greenland in a few larger towns.[13]
Currently the island is a popular destination with tourists on cruise ships to Greenland owing to its impressive landscapes.[14]
See also
Bibliography
- Mette Felbo, Grønlandske sommertelte, Grønland, Årg. 41, nr. 1 (1993), p. 19-29
- Hans Christian Gulløv, Thulekulturen i Sydøstgrønland - set fra Skjoldungen, Forskning i Grønland, 1994, nr. 1/2, pp. 21–31
- Hans Christian Gulløv, Minik T. Rosing, Projekt Skjoldungen 1990-92 : baggrund og feltarbejde, Forskning i Grønland, 1994, nr. 1/2, pp. 8-12, on the 1992 ethnographic/archaeological expedition 'Projekt Skjoldungen'; background to the fieldwork
- Jette Lewinsky, Mosses of the Skjoldungen Area, Southeast Greenland, Lindbergia Vol. 1, No. 1/2 (1971), pp. 83-90
- Spencer Apollonio, Lands That Hold One Spellbound: A Story of East Greenland, 2008
- Hans Christian Gulløv, Archaeological Commentary on the Isotopic Study of the Greenland Thule Culture, Journal of the North Atlantic, Special Volume 3 (2012): 65–76
References
- ↑ Den grønlandske Lods - Geodatastyrelsen
- ↑ "Skjoldungen Weather". AccuWeather. Retrieved 8 April 2016.
- ↑ Friedrich Christoph Dahlmann, Forschungen auf dem Gebiete der Geschichte, p. 386
- ↑ Prostar Sailing Directions 2005 Greenland and Iceland Enroute, p. 101
- 1 2 3 "Skjoldungen". Mapcarta. Retrieved 8 April 2016.
- ↑ "Azimuthbjerg". Mapcarta. Retrieved 16 April 2016.
- ↑ GoogleEarth
- ↑ "Jensen, Jens Fog. Paleo-Eskimo sites in Skjoldungen District, South East Greenland". eHRAF Archaeology. Retrieved 18 April 2016.
- ↑ "Qoornoq". Mapcarta. Retrieved 18 April 2016.
- ↑ Koch, Anders; Felbo, Mette (1994). "Thulekulturens grave". Forskning i Grønland (1/2): 35–45.
- ↑ "Site 32. Archaeological remains -- Ancient Site: Qoornoq (63.35, -41.68333)". Distribution Map of Archaeological, Historic, Cultural and Ancient Sites in Greenland. Retrieved 18 April 2016.
- ↑ "Skjoldungen - Weather Station". Warcovers - Greenland Units. Retrieved 18 April 2016.
- ↑ "Skjoldungen or the cementery of shoes". MV FRAM's Expedition Blog. Retrieved 18 April 2016.
- ↑ "Arctic Journey: Skjoldungen Island, Greenland". Another Side of this Life. Retrieved 8 April 2016.
External links
- Skjoldungen pictures
- Geochemical Constraints on the Origin of the Late Archean Skjoldungen Alkaline Igneous Province, SE Greenland
- New insights on the north-eastern part of the Ketilidian orogen in South-East Greenland