Orr Glacier
Rennick Glacier () is a broad glacier, nearly long, which is one of the largest in Antarctica. It rises on the polar plateau westward of Mesa Range and is wide, narrowing to near the coast. It takes its name from Rennick Bay where the glacier reaches the sea. Early exploration The seaward part of the glacier was photographed by United States Navy Operation Highjump, 1946–47. The upper reaches of the Rennick Glacier were discovered and explored by the U.S. Victoria Land Traverse (VLT) in February 1960, and the first ascent made of Welcome Mountain by John Weihaupt, Alfred Stuart, Claude Lorius and Arnold Heine of the VLT party. On February 10, 1960, Lieutenant Commander Robert L. Dale, pilot of U.S. Navy (USN) Squadron VX-6, evacuated the VLT from , on this glacier, and then conducted an aerial photographic reconnaissance to Rennick Bay on the coast before returning the VLT team to McMurdo Station. Course The Rennick Glacier rises to the east of the Tobin Mesa in th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Glacier Morphology
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography Unconstrained Glaciers Ice sheets and ice caps Ice sheets and ice caps cover the largest areas of land in comparison to other glaciers, and their ice is unconstrained by the underlying topography. They are the largest glacial ice formations and hold the vast majority of the world's fresh water. Ice sheets Ice sheets are the largest form of glacial formation. They are continent-sized ice masses that span areas over . They are dome ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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United States Navy
The United States Navy (USN) is the naval warfare, maritime military branch, service branch of the United States Department of Defense. It is the world's most powerful navy with the largest Displacement (ship), displacement, at 4.5 million tons in 2021. It has the world's largest aircraft carrier fleet, with List of aircraft carriers in service, eleven in service, one undergoing trials, two new carriers under construction, and six other carriers planned as of 2024. With 336,978 personnel on active duty and 101,583 in the Ready Reserve, the U.S. Navy is the third largest of the United States military service branches in terms of personnel. It has 299 deployable combat vessels and about 4,012 operational aircraft as of 18 July 2023. The U.S. Navy is one of six United States Armed Forces, armed forces of the United States and one of eight uniformed services of the United States. The United States Navy traces its origins to the Continental Navy, which was established during ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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United States Geological Survey
The United States Geological Survey (USGS), founded as the Geological Survey, is an agency of the U.S. Department of the Interior whose work spans the disciplines of biology, geography, geology, and hydrology. The agency was founded on March 3, 1879, to study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The agency also makes maps of planets and moons, based on data from U.S. space probes. The sole scientific agency of the U.S. Department of the Interior, USGS is a fact-finding research organization with no regulatory responsibility. It is headquartered in Reston, Virginia, with major offices near Lakewood, Colorado; at the Denver Federal Center; and in NASA Research Park in California. In 2009, it employed about 8,670 people. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on its hundredth anniversary, was "Earth Science in the Pub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Serrat Glacier
Rennick Bay () is an embayment of the coastline of Antarctica at the terminus of Rennick Glacier. It is bounded on the west and east by Belousov Point and Stuhlinger Ice Piedmont. Discovery and naming The eastern part of the bay was discovered from the ship '' Terra Nova'', of the British Antarctic Expedition (1910–13) under Scott. It was named by the British Antarctic Expedition for Lieutenant Henry E. de P. Rennick, Royal Navy, an officer on the Terra Nova. The bay was photographed by United States Navy Operation Highjump (1947) and by the Soviet Antarctic Expedition (1958). According to the ''Sailing Directions for Antarctica'', "Cape Cheetham appears to be an isolated pinnacle forming the eastern extremity of Rennick Bay, an embayment about 18 miles wide, the western extremity of which is formed by high cliffs with outcroppings of rock. Location The northwestern end of the bay is defined by Belousov Point on the end of the Anderson Peninsula. The Suvorov Glacier ent ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Explorers Range
Explorers Range () is a large mountain range in the Bowers Mountains of Victoria Land, Antarctica, extending from Mount Bruce in the north to Carryer Glacier and McLin Glacier in the south. Exploration and naming The Explorers Range was named by the New Zealand Antarctic Place-Names Committee (NZ-APC) for the northern party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64, whose members carried out a topographical and geological survey of the area. The names of several party members are assigned to features in and about this range. Location The Explorers Range is south of the Stuhlinger Ice Piedmont, Cape Cheetham and Gannutz Glacier. The Rennick Glacier flows north to the sea along its western side. Glaciers originating in the northern Explorer Range that flow into this glacier include, from north to south, Arruiz Glacier, Alvarez Glacier and Sheehan Glacier. Ob' Bay is to the east of the northern part of the range, which is fed by glaciers ori ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Lanterman Range
The Lanterman Range () is a mountain range about long and wide, forming the southwest part of the Bowers Mountains in Antarctica. It is bounded by the Rennick Glacier, Sledgers Glacier, Black Glacier and Canham Glacier. Exploration and naming The range was mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1960–62. It was named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Commander William Lanterman, an aerological officer for U.S. Navy Operation Deep Freeze, 1959–62. Location The Lanterman Range lies to the east of the Rennick Glacier and its tributary Canham Glacier. The Sledgers Glacier flows past its northeast end. The MacKinnon Glacier drains the range to the north into Sledgers Glacier. Glaciers draining to the west include Orr Glacier, Linder Glacier, Hunter Glacier, Hoshko Glacier, Zenith Glacier and Johnstone Glacier. The Molar Massif lies to the east. The Crown Hills form t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Morozumi Range
The Morozumi Range () is a mountain range in the Usarp Mountains of North Victoria Land, Antarctica. It extends northwest–southeast for , with its northern elevations overlooking the convergence of Gressitt Glacier and Rennick Glacier. Early exploration and name The Morozumi Range was mapped by the United States Geological Survey from surveys and United States Navy air photos in 1960–63. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for Henry M. Morozumi, an aurora scientist at South Pole Station South is one of the cardinal directions or compass points. The direction is the opposite of north and is perpendicular to both west and east. Etymology The word ''south'' comes from Old English ''sūþ'', from earlier Proto-Germanic ''*sunþa ... in 1960, and Station Scientific Leader at Byrd Station in 1963. Geology The Morozumi Range is in the Rennick Graben, separated by the Rennick Faults from the Wilson Group rocks of the USARP mountains. Baseme ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Alamein Range
Alamein Range () is a range lying west of Canham Glacier, in the Freyberg Mountains of Antarctica. It was named in association with Lord Bernard Freyberg and the Second New Zealand Expeditionary Force by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64. Location The Alamein Range runs from northwest to southeast. It lies to the east of the Rennick Glacier and west of the Canham Glacier. The Salamander Range is parallel to it on the east side of the Canham Glaciier. In the north, the Canham Glacier joins the Rennick Glacier past the tip of the Alamein Range. Features, from north to south, include Takrouna Bluff, Benoit Peak and Mount Camelot. Features to the west, between the Alamein Range and Rennick Glacier, include Mount Strandmann, Smiths Bench, Mount Baldwin and the Moawhango Névé. Features Takrouna Bluff . A small but prominent bluff on the east side of Alamein Range, overlooking Canham Glacier from a position west-sout ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Outback Nunataks
The Outback Nunataks () are a series of bare rock nunataks and mountains which are distributed over an area about long by wide. The group lies south of Emlen Peaks of the Usarp Mountains and west of Monument Nunataks and upper Rennick Glacier, adjacent to the featureless interior plateau. Exploration and naming The Outback Nunataks were discovered by the United States Victoria Land Traverse party, 1959–60, and mapped by United States Geological Survey (USGS) from surveys and United States Navy air photos, 1959–64. They were so named by the Advisory Committee on Antarctic Names (US-ACAN) for their remote position at the posterior side of the large mountain belt that extends from the Ross Sea to the interior ice plateau. Location The terrain to the west of the nunataks is a featureless expanse of the polar plateau. The Emlen Peaks of the Usarp Mountains and the Helliwell Hills are to the north. The Rennick Glacier, the Freyberg Mountains, the Monument Nunataks and th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Freyberg Mountains
The Freyberg Mountains () are a group of mountains in Victoria Land, Antarctica, bounded by the Rennick Glacier, Bowers Mountains, Black Glacier, and Evans Névé. They are west of the Victory Mountains and south of the Bowers Mountains. Name The Freyberg Mountains were named for New Zealand's most famous general, Bernard Freyberg, by the Northern Party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1963–64. Location The Freyberg Mountains lie to the east of the Rennick Glacier and to the south of the Bowers Mountains Bowers Mountains () is a group of north–south trending mountains in Antarctica, about long and wide, bounded by the coast on the north and by the Rennick Glacier, Canham Glacier, Black Glacier and Lillie Glacier in other quadrants. They are we .... The Canham Glacier defines their northwest limit. The Black Glacier defines their eastern limit, separating them from the Leitch Massif, Neall Massif and West Quartzite Range further ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Monument Nunataks
The Monument Nunataks () are a group of nunataks in Antarctica that have numerous pinnacles and odd-shaped projections resembling monuments, situated north of Sculpture Mountain in the upper part of Rennick Glacier. The group was named by the Northern Party of the New Zealand Geological Survey Antarctic Expedition (NZGSAE) of 1962–63. Location The Monument Nunataks are on the east side of the upper Rennick Glacier. The Freyberg Mountains are to the east, and the Mesa Range to the south. the Outback Nunataks are to the west. Features Features, from north to south, include: Mount Lorius . A mountain, high, standing north of Mount Allison. Mapped by the United States Antarctic Research Program (USARP) Victoria Land Traverse Party, 1959-60. Named by the United States Advisory Committee on Antarctic Names (US-ACAN) for Claude Lorius, French glaciologist, a member of the traverse party. Mount Allison . A mountain northeast of Mount Stuart. Mapped by the United States Geol ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |