| Rhine Glacier | |
|---|---|
 Reconstruction of the front of the Rhine glacier near Sigmaringen showing blockage the Danube course during the Riss glaciation. | |
  Rhine Glacier | |
| Location | Bavaria top |
| Coordinates | 48°05′12″N9°12′59″E / 48.08667°N 9.21639°E |
| Status | melted |
 | |
The Rhine Glacier was a glacier during the last glacial period and was responsible for the formation of the Lake Constance. [1]
The Last Glacial Period (LGP), also known as the Last glacial cycle, occurred from the end of the Last Interglacial to the beginning of the Holocene, c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the timespan of the Late Pleistocene.
The Nimitz Glacier is an Antarctic glacier, 40 nautical miles long and 5 nautical miles wide, draining the area about 10 nautical miles west of the Vinson Massif and flowing southeast between the Sentinel Range and Bastien Range to enter Minnesota Glacier, in the central Ellsworth Mountains.
The Dater Glacier is a steep valley glacier in Antarctica, 24 nautical miles long and from 1 to 3 nautical miles wide, flowing northeast in a sinuous course from the eastern slopes of the Vinson Massif between Sullivan Heights and Veregava Ridge to Rutford Ice Stream which borders the eastern flank of the Sentinel Range, Ellsworth Mountains. At the lower end the Dater Glacier coalesces with the terminus of the Ellen Glacier, the two emerging from the Sentinel Range as one stream just north of the Flowers Hills.
The Ellen Glacier is a glacier in the central Sentinel Range of the Ellsworth Mountains of Antarctica. It drains the eastern slopes of Mount Anderson and Long Gables and flows generally southeast for 22 nautical miles to Barnes Ridge, where it leaves the range and enters the south flowing Rutford Ice Stream.
Shirase Glacier is a large glacier entering Havsbotn, the bay that forms the head of Lutzow-Holm Bay in Antarctica. The area occupied by this feature was first mapped as a bay and named Instefjorden by the Lars Christensen Expedition (LCE) of 1936–37. Surveys by Japanese Antarctic Research Expedition (JARE) of 1957–62, revealed the large glacier in this position which they named after Lt. Nobu Shirase, leader of the Japanese Antarctic Expedition of 1911–12. Its nearby features were also charted and named by JARE unless otherwise noted.
The Scott Glacier is a major glacier, 120 nautical miles long, that drains the East Antarctic Ice Sheet through the Queen Maud Mountains to the Ross Ice Shelf. The Scott Glacier is one of a series of major glaciers flowing across the Transantarctic Mountains, with the Amundsen Glacier to the west and the Leverett and Reedy glaciers to the east.
Isbrecht Glacier is a small glacier flowing south from Thurston Island in Antarctica between Cox Glacier and Hale Glacier. It was named by the Advisory Committee on Antarctic Names after JoAnn Isbrecht of the United States Geological Survey (USGS), Flagstaff, Arizona, a satellite image processing specialist who was part of the USGS team that compiled the 1:5,000,000-scale Advanced Very High Resolution Radiometer maps of Antarctica and the 1:250,000-scale Landsat image maps of the Siple Coast area in the 1990s.
Haas Glacier is a steep tributary glacier draining northward from Rawson Plateau to enter the south side of Bowman Glacier, in the Queen Maud Mountains of Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1960–64, and was named by the Advisory Committee on Antarctic Names for Charles G. Haas, a meteorologist in the South Pole Station winter party, 1960.
Union Glacier, is a large, heavily crevassed glacier which receives the flow of several tributaries and drains through the middle of the Heritage Range, Ellsworth Mountains, Antarctica. The glacier drains from the plateau at Edson Hills on the west side of the range and flows east between Pioneer Heights and Enterprise Hills. Union Glacier was mapped by U.S. Geological Survey (USGS) from surveys and U.S. Navy (USN) air photos, 1961–66. The name was applied by Advisory Committee on Antarctic Names (US-ACAN) in association with the name Heritage Range.
Rippon Glacier is a small glacier located in Kemp Land, East Antarctica. It is close east of Seaton Glacier, flowing southward into Edward VIII Ice Shelf.
Benbrook Glacier is a glacier 5 nautical miles (9 km) long in the Churchill Mountains. It flows south-southeast from Egress Peak, Carlstrom Foothills, into the Flynn Glacier. It was named after James R. Benbrook of the Department of Physics, University of Houston, Texas, a United States Antarctic Program team member in balloon-borne investigation of the ionosphere and magnetosphere over the Geographic South Pole, 1985–95.
Crosswell Glacier is a glacier 10 nautical miles long, flowing north-northeast from Mount Shinn between Sullivan Heights and Bearskin Ridge, in the central part of the Sentinel Range, Ellsworth Mountains, Antarctica. Together with Patton and Pulpudeva Glaciers, it enters Ellen Glacier northwest of Mamarchev Peak and southeast of Mount Jumper.
Dobbratz Glacier is a broad tributary glacier which drains the south part of the White Escarpment and flows northeast between the Watlack Hills and the Webers Peaks into Splettstoesser Glacier, in the Heritage Range. It was named by the University of Minnesota Geological Party, 1963–64, for Major Joseph Dobbratz, a United States Marine Corps pilot who supported the party.
Goodell Glacier is a glacier about 5 nautical miles long flowing east and north from Fletcher Peninsula into the Williams Ice Stream, Antarctica. It was named by the Advisory Committee on Antarctic Names after Janice G. Goodell of the United States Geological Survey, Woods Hole, Massachusetts, a support member of the Glacier Studies Project Team from the early 1990s onwards.
The Meteorite Hills are a group of hills, 11 nautical miles long, forming the western portion of the Darwin Mountains in Antarctica. The hills are located between the heads of Darwin Glacier and Hatherton Glacier.
Lucchitta Glacier is a glacier about 20 nautical miles (37 km) long flowing south from the Hudson Mountains of Antarctica into Pine Island Bay. It was named by the Advisory Committee on Antarctic Names after geologist Baerbel K. Lucchitta of the United States Geological Survey, Flagstaff, Arizona, a specialist in the use of satellite imagery for geological and glaciological studies from the early 1980s to the early 2000s (decade), and one of the pioneers in the use of imagery for glacier velocity measurements in Antarctica.
Hudman Glacier is a glacier draining south of Mount Landolt between Marze Peak and Miller Peak in Petvar Heights at the south end of the Sentinel Range, in the Ellsworth Mountains of Antarctica, flowing south-southeast to Minnesota Glacier. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for Captain Rayburn A. Hudman, United States Marine Corps, who died in the crash of a Lockheed P2V-2n Neptune, modified for extreme range, flying in sub zero temperatures and Ski equipped for landing on the Ice runways at McMurdo Sound Antarctica on October 18, 1956.
Hyde Glacier is a short glacier flowing east through the Edson Hills to join Union Glacier, in the Heritage Range, Antarctica. It was mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1961–66, and was named by the Advisory Committee on Antarctic Names for William H. Hyde, an ionospheric scientist at Little America V Station in 1958.
Thomas Glacier is a roughly Z-shaped glacier which drains the southeast slopes of Vinson Massif and flows for 17 nautical miles (31 km) through the south part of the Sentinel Range, Ellsworth Mountains, leaving the range between Doyran and Petvar Heights south of Johnson Spur.
Hough Glacier is a glacier in central Doyran Heights in the Sentinel Range of Ellsworth Mountains, Antarctica, rising just south of Mount Tuck and flowing east-southeast for 10 nautical miles between Guerrero Glacier and Remington Glacier. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for William S. Hough, who made ionosphere studies at South Pole Station in 1957.
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