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Taylor Valley is the southernmost of the three large
McMurdo Dry Valleys 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 ...
in the
Transantarctic Mountains The Transantarctic Mountains (abbreviated TAM) comprise a mountain range of uplifted (primarily sedimentary rock, sedimentary) rock in Antarctica which extend, with some interruptions, across the continent from Cape Adare in northern Victoria La ...
,
Victoria Land Victoria Land is a region in eastern Antarctica which fronts the western side of the Ross Sea and the Ross Ice Shelf, extending southward from about 70°30'S to 78°00'S, and westward from the Ross Sea to the edge of the Antarctic Plateau. It ...
, Antarctica, located west of
McMurdo Sound McMurdo Sound is a sound in Antarctica. It is the southernmost navigable body of water in the world, and is about from the South Pole. Captain James Clark Ross discovered the sound in February 1841, and named it after Lt. Archibald McMurdo o ...
at approximately . The valley extends from
Taylor Glacier __NOTOC__ The Taylor Glacier is an Antarctic glacier about long, flowing from the plateau of Victoria Land into the western end of Taylor Valley, north of the Kukri Hills, south of the Asgard Range. The middle part of the glacier is bounded on ...
in the west to McMurdo Sound at Explorers Cove at the northwest head of New Harbour in the east and is about long. It was once occupied by the receding Taylor Glacier, from which it derives its name. Taylor Valley contains Lake Bonney in the west (inward), and
Lake Fryxell Lake Fryxell is a frozen lake long, between Canada Glacier and Commonwealth Glaciers at the lower end of Taylor Valley in Victoria Land, Antarctica. It was mapped in the early 1900s and named during Operation Deep Freeze in the 1950s. There are se ...
in the east (coastward), and
Lake Hoare Lake Hoare is a lake about long between Lake Chad and Canada Glacier in Taylor Valley, Victoria Land, Antarctica. Its surface area measures . The lake was named by the 8th Victoria University of Wellington Antarctic Expedition (VUWAE), 1963–64, ...
,
Lake Chad Lake Chad (french: Lac Tchad) is a historically large, shallow, endorheic lake in Central Africa, which has varied in size over the centuries. According to the ''Global Resource Information Database'' of the United Nations Environment Programme, ...
, Lake Popplewell, Mummy Pond and
Parera Pond Parera Pond is a pond lying south of Andrews Ridge in Taylor Valley, Victoria Land. It was named by the New Zealand Geographic Board in 1998. ''Parera'' is the Maori (language), Maori word for wild duck. Further reading * W. Andrew Jackson, Alfon ...
close together between the two. Further east of Lake Bonney is
Pearse Valley Pearse Valley () is an ice-free valley long, lying immediately west of Catspaw Glacier, at the south side of the Asgard Range in Victoria Land. Named by Advisory Committee on Antarctic Names The Advisory Committee on Antarctic Names (ACAN or US-AC ...
. Taylor Valley is separated from Wright Valley in the north by
Asgard Range The Asgard Range is a mountain range in Victoria Land, Antarctica. It divides Wright Valley from Taylor Glacier and Taylor Valley, and was named by the Victoria University of Wellington Antarctic Expedition (1958–59) after Asgard, the home o ...
, and from
Ferrar Glacier __NOTOC__ Ferrar Glacier is a glacier in Antarctica. It is about long, flowing from the plateau of Victoria Land west of the Royal Society Range to New Harbour in McMurdo Sound. The glacier makes a right (east) turn northeast of Knobhead, where ...
in the south by
Kukri Hills Kukri Hills () is a prominent east-west trending range, about long and over high, forming the divide between Ferrar Glacier on the south and Taylor Glacier and Taylor Valley on the north, in Victoria Land, Antarctica. The hills were discovered b ...
. At its southernmost end, Taylor Valley becomes Quinn Gully, a mainly ice-free
gully A gully is a landform created by running water, mass movement, or commonly a combination of both eroding sharply into soil or other relatively erodible material, typically on a hillside or in river floodplains or terraces. Gullies resemble lar ...
, which descends between
MacDonald Hills The MacDonald Hills () are a compact group of exposed rock hills in the Asgard Range, east of Commonwealth Glacier on the north side of lower Taylor Valley, Victoria Land, Antarctica. They are separated from Hjorth Hill by Quinn Gully. The hil ...
and
Hjorth Hill Hjorth Hill () is a rounded, ice-free mountain, high, standing just north of New Harbour and south of Hogback Hill, in Victoria Land, Antarctica. The hill is separated from the MacDonald Hills by Quinn Gully. It was charted by the British Antar ...
to Explorers Cove in New Harbour. It was named by the
Advisory Committee on Antarctic Names The Advisory Committee on Antarctic Names (ACAN or US-ACAN) is an advisory committee of the United States Board on Geographic Names responsible for recommending commemorative names for features in Antarctica. History The committee was established ...
(1997) after Thomas Quinn, supervisor of
Continental Air Operations Continental may refer to: Places * Continent, the major landmasses of Earth * Continental, Arizona, a small community in Pima County, Arizona, US * Continental, Ohio, a small town in Putnam County, US Arts and entertainment * ''Continental'' (al ...
,
Antarctic Support Associates The Antarctic ( or , American English also or ; commonly ) is a polar region around Earth's South Pole, opposite the Arctic region around the North Pole. The Antarctic comprises the continent of Antarctica, the Kerguelen Plateau and other ...
.
Scar Peak Scar Peak () is a peak ( high) surmounting the northern wall of Taylor Valley immediately east of the Lacroix Glacier in Victoria Land. It was named by the New Zealand Geographic Board in 1998 after the Scientific Committee on Antarctic Research ...
overlooks the valley's northern wall, east of the
Lacroix Glacier Lacroix Glacier () is a glacier between Suess Glacier and Matterhorn Glacier, which flows southeast into Taylor Valley in Victoria Land, Antarctica. It was mapped by the British Antarctic Expedition, 1910–13, under Robert Falcon Scott Ca ...
. Taylor Valley was discovered by the
British National Antarctic Expedition The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–18 ...
(1901–04), it was more fully explored by the BrAE (1907–09) and the BrAE (1910–13), and named after Australian geologist
Thomas Griffith Taylor Thomas Griffith "Grif" Taylor (1 December 1880 – 5 November 1963) was an English-born geographer, anthropologist and world explorer. He was a survivor of Captain Robert Scott's Terra Nova Expedition to Antarctica (1910–1913). Taylor was a se ...
. In the oblique aerial photo at right, the tan bands are sandstone layers from the
Beacon Supergroup The Beacon Supergroup is a geological formation exposed in Antarctica and deposited from the Devonian to the Triassic (). The unit was originally described as either a formation or sandstone, and upgraded to group and supergroup as time passed. It ...
, a series of sedimentary rock layers formed at the bottom of a shallow sea between 250 million and 400 million years ago. Throughout that period, Earth's southern continents were locked into the supercontinent
Gondwana Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages ...
. The dark band of rock that divides the sandstone is
dolerite Diabase (), also called dolerite () or microgabbro, is a mafic, holocrystalline, subvolcanic rock equivalent to volcanic basalt or plutonic gabbro. Diabase dikes and sills are typically shallow intrusive bodies and often exhibit fine-grained ...
(sometimes called diabase), a volcanic rock that forms underground. The distinctive dolerite intrusion—or sill—is a remnant of a massive volcanic plumbing system that produced major eruptions about 180 million years ago. The eruptions likely helped tear Gondwana apart.Taylor Valley, Antarctica
at
NASA Earth Observatory NASA Earth Observatory is an online publishing outlet for NASA which was created in 1999. It is the principal source of satellite imagery and other scientific information pertaining to the climate and the Environment (biophysical), environment whi ...
. Article includes
public domain The public domain (PD) consists of all the creative work A creative work is a manifestation of creative effort including fine artwork (sculpture, paintings, drawing, sketching, performance art), dance, writing (literature), filmmaking, ...
text from this US government website.


See also

* Commonwealth Stream * McMurdo Dry Valleys geology *
Victoria Valley Victoria Valley is one of the larger McMurdo Dry Valleys in Antarctica. Lake Vida is the largest lake of the valley. The Victoria River drains the Victoria Upper Glacier, with Upper Victoria Lake just below it and northwest of Lake Vida, into ...
(far north) *
Lake Washburn (Antarctica) Lake Washburn is a lake that formerly existed in the Taylor Valley, McMurdo Dry Valleys, Antarctica. It formed when climatic changes and an expansion of ice caused the flooding of the valley, between 23,000 and 8,340 radiocarbon years ago. Its exte ...
*
Wright Valley The Wright Valley, named for Sir Charles Wright, is the central one of the three large Dry Valleys in the Transantarctic Mountains, located west of McMurdo Sound at approximately . Wright Valley contains the Onyx River, the longest river in Ant ...
(north)


References


External links


USGS Geographic Names Database - Taylor Valley
McMurdo Dry Valleys Valleys of Victoria Land Transantarctic Mountains {{McMurdoDryValleys-geo-stub