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Geographical Society Island

Island in Greenland

Geographical Society Island

Island in Greenland

FieldValue
nameGeographical Society Island
native_nameGeografisk Samfund Ø
native_name_linkDanish language
sobriquet
image_nameAerial photographs of Greenland ENBLA06.jpg
image_size270px
image_captionView of Geographical Society Island
mapframeyes
mapframe-zoom5
mapframe-stroke-width2
image_map_size270px
image_map_captionMap of Geographical Society Island
pushpin_mapGreenland
pushpin_labelGeographical Society Island
pushpin_map_captionLocation of Geographical Society Island in Greenland
coordinates
etymologyNamed after the Royal Geographical Society
locationGreenland Sea
area_km21717
rank6th largest in Greenland
231st largest in world
coastline_km
elevation_m1730
elevation_footnotes
highest_mountSvedenborg Bjerg
countryGreenland
country_admin_divisions_titleUnincorporated area
country_admin_divisionsNE Greenland National Park
country_area_km2
population0
population_as_of2021
density_km20
ethnic_groupsnone

| mapframe-zoom = 5 | mapframe-stroke-width = 2 231st largest in world

Geographical Society Island () is an island off Foster Bay in northeastern Greenland.

Geography

The island has an area of 1,717 km2. It is mountainous with Svedenborg Fjeld as the highest point at 1,730 m. To the north lies the mouth of the Kaiser Franz Joseph Fjord with Ymer Island to the NW and smaller Bantekoe Island to the NE in Foster Bay. To the south lies Traill Island, separated by a narrow sound, the Vega Sound. In the west, over King Oscar Fjord lies Ella Island.

Map of Northeastern Greenland

Geology

From west to east, the rocks constituting the island are sandstone of roughly Devonian, Carboniferous and Cretaceous age, and some smaller areas with Triassic and Jurassic sandstone.

References

References

  1. {{cite peakbagger
  2. [http://islands.unep.ch/ITP.htm UNEP]
  3. "Segment 12".
Info: Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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