Traveling Luck for Ahlmannfonna Svalbard (general), Svalbard and Jan Mayen Svalbard and Jan Mayen flag

Alternatively known as Ahlmann Ice

The timezone in Ahlmannfonna is Arctic/Longyearbyen
Morning Sunrise at 04:42 and Evening Sunset at 17:56. It's light
Rough GPS position Latitude. 80.0833°, Longitude. 22.8333°

Satellite map of Ahlmannfonna and it's surroudings...

Geographic features & Photographs around Ahlmannfonna in Svalbard (general), Svalbard and Jan Mayen

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

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

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

hill a rounded elevation of limited extent rising above the surrounding land with local relief of less than 300m.

Accommodation around Ahlmannfonna

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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.

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

island a tract of land, smaller than a continent, surrounded by water at high water.

peninsula an elongate area of land projecting into a body of water and nearly surrounded by water.

plain(s) an extensive area of comparatively level to gently undulating land, lacking surface irregularities, and usually adjacent to a higher area.

valley an elongated depression usually traversed by a stream.

nunatak a rock or mountain peak protruding through glacial ice.

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

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

snowfield an area of permanent snow and ice forming the accumulation area of a glacier.

icecap a dome-shaped mass of glacial ice covering an area of mountain summits or other high lands; smaller than an ice sheet.


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