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Schirmacher Oasis

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Through Plateau, Fresh water and Saline water

Geography

The oasis is located between the edge of the Antarctic Ice Sheet and the Novolazarevskaya Nivl Ice Shelf. The approximately 100 m (330 ft) high plateau of the Schirmacher Oasis is a barrier to the northwards-running ice stream. On the northern edge of the oasis are so-called epishelf lakes, bays separated from the ocean which are connected with the ocean underneath the surface of the ice. Thus, tidal effects can be observed in the lakes. The epishelf lakes can contain either mere freshwater or saltwater which is overlaid by freshwater. The Antarctic Ice Sheet, southwards of the Schirmacher Oasis, reaches heights of 1,500 m (4,900 ft). The nunataks Skaly Instituta Geologii Arktiki (Skaly IGA) and Basisny-Kit protrude from the ice sheet. Between the offshore ice sheet and the Wegener Ice Sheet Plateau are the Wohlthat Mountains.

The highest part of the Schirmacher Oasis is Mount Rebristaya, with a height of 228 m (748 ft). At a depth of 34.5 m (113 ft), Lake Glubokoye is the deepest inland lake of the oasis. Spatially, the largest lake within the oasis is Lake Sub, with an area of 0.5 km2 (0.19 sq mi).

A number of theories exist about the formation of the oasis that include geothermal heating, intense insolation, or the hypothesis that the ice flow is blocked by a geological feature such as a mountain.

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