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McMurdo Dry Valleys
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- "Dry valleys" redirects here. For other uses, see dry valley
The McMurdo Dry Valleys are a row of valleys in Antarctica located within Victoria Land west of McMurdo Sound. The region includes many interesting geological features including Lake Vida and the Onyx River, Antarctica's longest river. It is also one of the world's most extreme deserts.
Dry Valleys are so named because of their extremely low humidity and their lack of snow or ice cover.

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Encyclopedia
- "Dry valleys" redirects here. For other uses, see dry valley
The McMurdo Dry Valleys are a row of valleys in Antarctica located within Victoria Land west of McMurdo Sound. The region includes many interesting geological features including Lake Vida and the Onyx River, Antarctica's longest river. It is also one of the world's most extreme deserts.
Climate
The Dry Valleys are so named because of their extremely low humidity and their lack of snow or ice cover. Together, at 4800 square kilometers, they constitute around 0.03 % of the continent, and form the largest relatively ice-free region in Antarctica. The valley floors are covered with a loose gravelly material, in which ice-wedge polygons may be observed.
The unique conditions in the Dry Valleys are caused by katabatic winds (from the Greek word for 'going down'). These occur when cold, dense air is pulled downhill simply by the force of gravity. The winds can reach speeds of 320 km/h (200 mph) evaporating all moisture - water, ice and snow - in the process.
Geology
The valleys cut through the Beacon sandstone. The gravel appears to be derived from two sources. The first is terminal moraines which have formed at the end of glaciers which descend into the Dry Valleys. These glaciers sublime directly to air, for the most part, adding very little liquid water to the valleys. The second potential source of gravel is a rather unusual source. It is believed that during some glacial periods, the quantity of ice in the nearby Ross Sea was so great that it forced its way inland into some of the Dry Valleys, in a kind of reverse glacier and deposited its own terminal moraine.
Biota
Endolithic photosynthetic bacteria have been found living in the Dry Valleys, sheltered from the dry air in the relatively moist interior of rocks. Summer meltwater from the Valleys' overhanging glaciers provides the primary source of soil nutrients. Scientists consider the Dry Valleys perhaps the closest of any terrestrial environment to Mars, and thus an important source of insights into possible extraterrestrial life.
Part of the Valleys was designated an environmentally protected area in 2004.
Major geographic features
Valleys
- Alatna Valley (sometimes incorrectly spelled Atlanta Valley is the northernmost, north of Benson Glacier.
From north to south, the three main valleys are
West of Victoria Valley are, from north to south,
Stretching south from Balham Valley are, from west to east:
West of Taylor Valley is
- Pearse Valley (sometimes incorrectly spelled Pearce Valley).
Further south, between Royal Society Range in the west and the west coast of McMurdo Sound at the lobe of Koettlitz Glacier are, from north to south:
Lakes
Some of the lakes of the Dry Valleys rank among the world's most saline lakes, with a higher salinity than Lake Assal (Djibouti) or the Dead Sea. The most saline of all is small Don Juan Pond.
- Lake House (Pearse Valley)
- Lake Joyce (Pearse Valley)
- Lake Garwood (Garwood Valley)
- Lake Miers (Miers Valley)
Rivers
- Kite Stream (Victoria Valley)
- Onyx River (Wright Valley]
- Vincent Creek (Taylor Valley)
- Crescent Stream (Taylor Valley)
- Harnish Creek (Taylor Valley)
- Huey Creek (Taylor Valley)
See also
External links
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- (USGS)
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- , Antarctic Sun, January 26 2003
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- - The New York Times/International Herald Tribune, November 2006
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