Traveling Luck for Payer Land Østgrønland, Greenland Greenland flag

Alternatively known as Payers Land

The timezone in Payer Land is America/Danmarkshavn
Morning Sunrise at Sun never rises on the specified date at the specified location and Evening Sunset at 00:00. It's light
Rough GPS position Latitude. 74.5000°, Longitude. -22.4167°

Satellite map of Payer Land and it's surroudings...

Geographic features & Photographs around Payer Land in Østgrønland, Greenland

mountain an elevation standing high above the surrounding area with small summit area, steep slopes and local relief of 300m or more.

glacier(s) 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.

nunatak a rock or mountain peak protruding through glacial ice.

area a tract of land without homogeneous character or boundaries.

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peak a pointed elevation atop a mountain, ridge, or other hypsographic feature.

fjord a long, narrow, steep-walled, deep-water arm of the sea at high latitudes, usually along mountainous coasts.

point a tapering piece of land projecting into a body of water, less prominent than a cape.

cove(s) a small coastal indentation, smaller than a bay.

cape a land area, more prominent than a point, projecting into the sea and marking a notable change in coastal direction.

stream a body of running water moving to a lower level in a channel on land.

gorge(s) a short, narrow, steep-sided section of a stream valley.

mountains a mountain range or a group of mountains or high ridges.

valley an elongated depression usually traversed by a stream.

nunataks rocks or mountain peaks protruding through glacial ice.

reef(s) a surface-navigation hazard composed of consolidated material.

upland an extensive interior region of high land with low to moderate surface relief.

delta a flat plain formed by alluvial deposits at the mouth of a stream.

bay a coastal indentation between two capes or headlands, larger than a cove but smaller than a gulf.


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