Nanuuseq Fjord

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Nanuuseq Fjord
Oyfjord
Greenland edcp relief location map.jpg
Red pog.svg
Nanuuseq Fjord
Location
Location Arctic
Coordinates 60°31′N43°40′W / 60.517°N 43.667°W / 60.517; -43.667 Coordinates: 60°31′N43°40′W / 60.517°N 43.667°W / 60.517; -43.667
Ocean/sea sources North Atlantic Ocean
Basin  countries Greenland
Max. length 14 km (8.7 mi)
Max. width 2 km (1.2 mi)
Surface area SE Greenland
References [1]

Nanuuseq Fjord, [2] old spelling Nanûseq, is a fjord in the King Frederick VI Coast, Kujalleq municipality, southern Greenland. [3]

Fjord A long, narrow inlet with steep sides or cliffs, created by glacial activity

Geologically, a fjord or fiord is a long, narrow inlet with steep sides or cliffs, created by a glacier. There are many fjords on the coasts of Alaska, Antarctica, British Columbia, Chile, Greenland, the Faroe Islands, Iceland, Kamchatka, the Kerguelen Islands, New Zealand, Norway, Novaya Zemlya, Labrador, Nunavut, Newfoundland, Quebec, Scotland, South Georgia Island, and Washington state. Norway's coastline is estimated at 29,000 kilometres (18,000 mi) with nearly 1,200 fjords, but only 2,500 kilometres (1,600 mi) when fjords are excluded.

King Frederick VI Coast Region in Greenland

King Frederick VI Coast is a major geographic division of Greenland. It comprises the coastal area of Southeastern Greenland in Sermersooq and Kujalleq municipalities fronting the Irminger Sea of the North Atlantic Ocean. It is bordered by King Christian IX Land on the north and the Greenland Ice Sheet to the west.

Kujalleq Municipality in Greenland, Kingdom of Denmark

Kujalleq is a municipality on the southern tip of Greenland, operational from 1 January 2009. The administrative center of the municipality is in Qaqortoq. The municipality consists of the former municipalities of southern Greenland, each named after the biggest settlement:

Contents

Geography

Nanuuseq, formerly known as Oyfjord, is a short fjord lying between Nattoralik to the north and Lindenow Fjord to the south. It extends in a roughly east/west direction from its mouth in the North Atlantic Ocean for about 20 km until its head. Its entrance is on the northern side of Nanuuseq Island and there is another 5 km long and narrow island within the fjord itself close to its northern shore. Noret is a short tributary fjord branching northwards off the western end of the long island. [4]

Nattoralik

Nattoralik, old spelling Nagtoralik, is a fjord in the King Frederick VI Coast, Kujalleq municipality, southern Greenland.

Lindenow Fjord

Lindenow Fjord or Kangerlussuatsiaq, is a fjord in the King Frederick VI Coast, Kujalleq municipality, southern Greenland. The fjord is named after Godske Lindenov, admiral of the Danish Navy noted for his role in King Christian IV's expeditions to Greenland.

Nanuuseq

Nanuuseq, also known as Nanûseq or Nanusek is an uninhabited island in the Kujalleq municipality in southern Greenland.

In the same manner as in the fjords further north, dark-hued mountains rise steeply from the shore on both sides. However, there are no glaciers reaching down to the waterline. [1]

Glacier Persistent body of ice that is moving under its own weight

A glacier is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landforms such as cirques and moraines. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water.

Map of Greenland section showing Nanuuseq Fjord. Lindenow-Greenland-onc d 16-map-section.jpg
Map of Greenland section showing Nanuuseq Fjord.

See also

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References

  1. 1 2 GoogleEarth
  2. Den grønlandske Lods - Geodatastyrelsen
  3. Prostar Sailing Directions 2005 Greenland and Iceland Enroute, p. 100
  4. "Nanûseq Fjord". Mapcarta. Retrieved 2 June 2016.