The McMurdo Dry Valleys are a row of largely snow-free valleys in Antarctica, located within Victoria Land west of McMurdo Sound. The Dry Valleys experience extremely low humidity and surrounding mountains prevent the flow of ice from nearby glaciers. The rocks here are granites and gneisses, and glacial tills dot this bedrock landscape, with loose gravel covering the ground.
The region is one of the world's most extreme deserts, and includes many features including Lake Vida, a saline lake, and the Onyx River, a meltwater stream and Antarctica's longest river. Although no living organisms have been found in the permafrost here, endolithic photosynthetic bacteria have been found living in the relatively moist interior of rocks and anaerobic bacteria, with a metabolism based on iron and sulfur, live under the Taylor Glacier.
The Dry Valleys are so named because of their extremely low humidity and lack of snow or ice cover. They are also dry because, in this location, the mountains are sufficiently high that they block seaward-flowing ice from the East Antarctic Ice Sheet from reaching the Ross Sea. At 4,800 square kilometres (1,900 sq mi), the valleys constitute around 0.03% of the continent and form the largest ice-free region in Antarctica. The valley floors are covered with loose gravel, in which ice wedge polygonal patterned ground may be observed.
Precipitation averages around 100 millimetres (3.9 in) per year over a century of records, all in the form of snow. The dry wind rapidly evaporates the snow and little melts into the soil. During the summer, this process can take only hours.
The unique conditions in the Dry Valleys are caused, in part, by katabatic winds; these occur when cold, dense air is pulled downhill by the force of gravity. The winds can reach speeds of 320 kilometres per hour (200 mph), heating as they descend and evaporating all water, ice and snow.
The McMurdo Oasis constitutes approximately 4,000 square kilometres (1,500 sq mi) of "deglaciated mountainous desert", according to McKelvey, bounded by the coastline of south Victoria Land and the Polar Plateau. The Taylor and Wright Valleys are major ice-free valleys within the Transantarctic Mountains. These "dry valleys" include hummocky moraines, with frozen lakes, saline ponds, sand dunes, and meltwater streams. Basement rocks include the Late Precambrian or Early Palaeozoic Skelton Group metamorphic rocks, primarily the Asgard Formation, which is a medium-high-grade marble and calc schist. The Palaeozoic Granite Harbour intrusives include granitoid plutons and dykes, which intruded into the metasedimentary Skelton Group in the Late Cambrian-Early Ordovician during the Ross orogeny. The basement complex is overlain by the Jurassic Beacon Supergroup, which is itself intruded by Ferrar Dolerite sheets and sills. The McMurdo Volcanic Group intrudes, or is interbedded with, the Taylor and Wright Valleys' moraines as basaltic cinder cones and lava flows. These basalts have ages between 2.1 and 4.4 Ma. The Dry Valley Drilling Project (1971–75) determined the Pleistocene layer within the Taylor Valley was between 137 and 275 m thick, and composed of interbedded sandstones, pebble conglomerates, and laminated silty mudstones. This Pleistocene layer disconformably overlies Pliocene and Miocene diamictites.
Endolithic 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 glaciers provides the primary source of soil nutrients. Scientists consider the Dry Valleys perhaps the closest of any terrestrial environment to the planet Mars, and thus an important source of insights into possible extraterrestrial life.
Canadian and American researchers conducted a field expedition in 2013 to University Valley in order to examine the microbial population and to test a drill designed for sampling on Mars in the permafrost of the driest parts of the valleys, the areas most analogous to the Martian surface. They found no living organisms in the permafrost, the first location on the planet visited by humans with no active microbial life.
Part of the Valleys was designated an environmentally protected area in 2004.
Major geographic features
- Alatna Valley (sometimes incorrectly spelled Atlanta Valley) is the northernmost, north of Benson Glacier.
From north to south, the three main valleys are
- Victoria Valley (between St. Johns Range in the north and Olympus Range in the south)
- Wright Valley (between Olympus Range in the north and Asgard Range in the south)
- Taylor Valley (between Asgard Range in the north and Kukri Hills in the south)
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).
- Clark Glacier
- Wright Upper Glacier (Wright Valley)
- Wright Lower Glacier (Wright Valley)
- Rhone Glacier (Taylor Valley)
- Suess Glacier (Taylor Valley)
- Hughes Glacier (Taylor Valley)
- Taylor Glacier (Taylor Valley)
- Canada Glacier (Taylor Valley)
- Commonwealth Glacier (Taylor Valley)
- Howard Glacier (Taylor Valley)
- Doran Glacier (Taylor Valley)
- Lake Vida (Victoria Valley)
- Lake Vanda (Wright Valley)
- Lake Brownworth (Wright Valley) (freshwater)
- Don Juan Pond (Wright Valley)
- Lake Fryxell (Taylor Valley)
- Lake Hoare (Taylor Valley)
- Lake Chad (Taylor Valley)
- Parera Pond (Taylor Valley) (freshwater)
- Lake Bonney (Taylor Valley)
- Lake Joyce (Pearse Valley)
- Lake Garwood (Garwood Valley)
- Lake Miers (Miers Valley)
- Kite Stream (Victoria Valley)
- Onyx River (Wright Valley)
- Doran Stream (Taylor Valley)
- Vincent Creek (Taylor Valley)
- Crescent Stream (Taylor Valley)
- Harnish Creek (Taylor Valley)
- Huey Creek (Taylor Valley)
- Lost Seal Stream (Taylor Valley)
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