Traveling Luck for Forbindelsegletscher, Østgrønland, Greenland

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Where is Forbindelsegletscher?

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Also known as Forbindelsesgletscher
The timezone in Forbindelsegletscher is America/Danmarkshavn
Sunrise at 12:41 and Sunset at 15:54. It's Dark

Latitude. 68.1667°, Longitude. -31.6333°

Satellite map around Forbindelsegletscher

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Geographic features & Photographs around Forbindelsegletscher, in Østgrønland, Greenland

a land area, more prominent than a point, projecting into the sea and marking a notable change in coastal direction.
a mass of ice, usually at high latitudes or high elevations, with sufficient thickness to flow away from the source area in lobes, tongues, or masses.
a rock or mountain peak protruding through glacial ice.
a small coastal indentation, smaller than a bay.
a long, narrow, steep-walled, deep-water arm of the sea at high latitudes, usually along mountainous coasts.
a tract of land, smaller than a continent, surrounded by water at high water.
an elevation standing high above the surrounding area with small summit area, steep slopes and local relief of 300m or more.
a coastal indentation between two capes or headlands, larger than a cove but smaller than a gulf.
a pointed elevation atop a mountain, ridge, or other hypsographic feature.
a small, narrow, deep, steep-sided stream channel, smaller than a gorge.
a break in a mountain range or other high obstruction, used for transportation from one side to the other [See also gap].
conspicuous, isolated rocky masses.
a high, steep to perpendicular slope overlooking a waterbody or lower area.
an elongate area of land projecting into a body of water and nearly surrounded by water.
a mountain range or a group of mountains or high ridges.
a tapering piece of land projecting into a body of water, less prominent than a cape.
an elongated depression usually traversed by a stream.
marine channel;
that part of a body of water deep enough for navigation through an area otherwise not suitable.
a bluff or prominent hill overlooking or projecting into a lowland.

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