Tisobis Valley

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Tisobis Valley ( 80°11′S156°20′E / 80.183°S 156.333°E / -80.183; 156.333 Coordinates: 80°11′S156°20′E / 80.183°S 156.333°E / -80.183; 156.333 ) is an ice-free valley just northeast of Mount Henderson in Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Tisobis is a historical name used in Roman Britain for the River Dwyryd.

Geographic coordinate system Coordinate system

A geographic coordinate system is a coordinate system that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are often chosen such that one of the numbers represents a vertical position and two or three of the numbers represent a horizontal position; alternatively, a geographic position may be expressed in a combined three-dimensional Cartesian vector. A common choice of coordinates is latitude, longitude and elevation. To specify a location on a plane requires a map projection.

Valley Low area between hills, often with a river running through it.

A valley is a low area between hills or mountains typically with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, at least with respect to the cross section of the slopes or hillsides.

Mount Henderson is a prominent mountain. It is 2,660 metres (8,730 ft) high, and stands 5 nautical miles (9 km) west of Mount Olympus in the Britannia Range of Antarctica. It was discovered and named by the British National Antarctic Expedition, 1901–04.

PD-icon.svg This article incorporates  public domain material from the United States Geological Survey document "Tisobis Valley" (content from the Geographic Names Information System ).

United States Geological Survey scientific agency of the United States government

The United States Geological Survey is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization has four major science disciplines, concerning biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility.

Geographic Names Information System geographical database

The Geographic Names Information System (GNIS) is a database that contains name and locative information about more than two million physical and cultural features located throughout the United States of America and its territories. It is a type of gazetteer. GNIS was developed by the United States Geological Survey in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names.


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Byrd Glacier glacier in Antarctica

The Byrd Glacier is a major glacier in Antarctica, about 136 km long and 24 km wide, draining an extensive area of the polar plateau and flowing eastward between the Britannia Range and Churchill Mountains to discharge into the Ross Ice Shelf at Barne Inlet. Its valley below the glacier is the lowest point not to covered by water on Earth which reaches 2,780 m below sea level. It was named by the NZ-APC after Rear Admiral Byrd, US Navy, American Antarctic explorer.

Sabrina Ridge is a bare rock ridge between Sabrina Valley and Tamarus Valley, 5 miles (8 km) south of Derrick Peak in Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Sabrina is a historical name formerly used in Roman Britain for the River Severn.

Sabrina Valley is an ice-free valley between Pontes Ridge and Sabrina Ridge in the Britannia Range. Named in association with Sabrina Ridge by a University of Waikato geological party, 1978-79.

Ituna Valley is a narrow ice-free valley between Isca Valley and Lemanis Valley in the Britannia Range, Antarctica. The valley opens northward to Hatherton Glacier, 8 miles (13 km) west-northwest of Derrick Peak. It was named in association with "Britannia" by a University of Waikato geological party, 1978–79, led by Michael Selby. "Ituna" is a historical name used in Roman Britain for the River Eden, Cumbria.

Onnum Ridge is a mountain spur that descends northeast to McCraw Glacier, 3 nautical miles (6 km) south of Derrick Peak in the Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.), geological party, 1978–79, led by Michael Selby. Onnum is a historical placename formerly used in Roman Britain.

Onnum Valley is an ice-free valley between Derrick Peak and Onnum Ridge in Britannia Range. Named in association with Onnum Ridge by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby.

Operose Peak is a peak above Onnum Valley to the southwest of Derrick Peak in the Britannia Range of Antarctica. The steep lower slopes of the peak are of Beacon sandstone; the top is made up of a thick dolerite sill. The Latin name means laborious or requiring great pain reflecting the steepness of the slopes.

DeVries Glacier is a steep tributary glacier just east of Peckham Glacier, flowing from the south slopes of the Britannia Range into Byrd Glacier. It was named by the Advisory Committee on Antarctic Names for Arthur L. DeVries, a United States Antarctic Research Program biologist at McMurdo Station in the 1961–62 and 1963–64 summer seasons.

Pontes Ridge is a mountain spur that descends eastward to McCraw Glacier, 4 nautical miles (7 km) south of Derrick Peak in Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Pontes is a historical placename formerly used in Roman Britain.

Metaris Valley is a small, rounded cirque valley with steep sides and residual névé, lying west of Derrick Peak in the Britannia Range in Antarctica. It was named in association with Britannia by a University of Waikato geological party, 1978–79, led by Michael Selby. "Metaris" is the historical name of a bay in Roman Britain, known today as The Wash.

McCraw Glacier is a glacier in the Britannia Range, Antarctica, draining the northwest slopes of Mount Olympus and flowing north, westward of Johnstone Ridge, to enter Hatherton Glacier. It was named by a University of Waikato geological party, 1978–79, led by Michael Selby, and named for John D. McCraw, Dean of Science at the university, a member on a 1959–60 field party to the McMurdo Dry Valleys.

Menster Ledge is a relatively level benchlike feature which rises to 1,800 metres (5,900 ft) 6 nautical miles (11 km) southwest of Mount Olympus in Hughes Basin, Britannia Range, Antarctica. The feature is 2.5 nautical miles (5 km) wide and is smoothly ice covered in the central and northern portions; an abrupt ice and rock cliff forms the south end of the ledge. It was named after Chaplain William Menster of the flagship USS Mount Olympus in Operation Highjump, 1946–47. The location of the ledge is in proximity to Byrd Glacier, Mount Olympus, and other features that memorialize leaders and ships of Operation Highjump.

Tamarus Valley is an ice-free valley lying south of Sabrina Ridge and 2.5 nautical miles (4.6 km) northeast of Mount Henderson in the Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Tamarus is the historical name used in Roman Britain for the River Tamar.

Magnis Ridge is a rock ridge 1.5 nautical miles (3 km) west of Derrick Peak, forming the divide between Magnis Valley and Metaris Valley in the Britannia Range, Antarctica. It was named in association with Magnis Valley by a University of Waikato geological party, 1978–79, led by Michael Selby.

Magnis Valley is a broad ice-free valley, 5 nautical miles (9 km) long, lying 3 nautical miles (6 km) west of Derrick Peak in the Britannia Range, Antarctica. It was named in association with Britannia by a University of Waikato geological party, 1978–79, led by Michael Selby; Magnis is a historical placename formerly used in Roman Britain.

Stahl Peak is a peak 2 nautical miles (3.7 km) east of Saburro Peak in the Ravens Mountains, Britannia Range. It rises to over 1800 meters. Named after CMSgt. Alfred E. Stahl who served with the 109 Airlift Wing as a Flight Engineer Superintendent during the transition of LC-130 operations from the U.S. Navy to the Air National Guard

Mount Selby is a mountain rising over 2,200 m between Mount Henderson and Mount Olympus in Britannia Range. Named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for Michael Selby, Professor of Earth Sciences, University of Waikato, Hamilton, New Zealand. Selby was a member of field parties in Antarctica, 1969–70, 1971–72, and 1978–79, the last doing geological work in Britannia Range.

Ravens Mountains is a symmetrical group of mountains on the west side of Hughes Basin in Britannia Range. The mountains are 12 nautical miles (22 km) long and rise to 2130 m in Doll Peak. Named after the 109 Airlift Wing of the New York Air National Guard which has provided logistical support to the United States Antarctic Program (USAP) for several years beginning in 1988. Ravens is a nickname associated with the Airlift Wing.

Lieske Glacier is a tributary glacier draining the north slopes of Mount Olympus in the Britannia Range, Antarctica, and flowing north between Johnstone Ridge and Dusky Ridge into Hatherton Glacier. It was named by the Advisory Committee on Antarctic Names for Bruce J. Lieske, a meteorologist who wintered at Little America V in 1957.