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Browning Pass (Antarctica)
Browning Pass () is an ice-covered pass, long, lying between the main mass of Deep Freeze Range and the Northern Foothills in Victoria Land, Antarctica. The pass facilitates movement between the lower ends of Priestley Glacier and Campbell Glacier. The feature was first mapped as a part of Campbell Glacier by the Northern Party of the British Antarctic Expedition, 1910–13 (BrAE). It was remapped by the Southern Party of the New Zealand Geological Survey Antarctic Expedition, 1962–63, and named for Frank V. Browning, a member of the BrAE Northern Party, for whom nearby Mount Browning is also named. See also * List of airports in Antarctica __TOC__ List , 18/36Ice , - valign=top , Palmer SkiwayHeliport , , NZ12 , , Anvers Island , , 01/19Snow , - valign=top , Patriot Hills Blue-Ice Runway , , SCPZ , , Ellsworth Mountains , , 24MIce , - valign=top , Pegasu ... References Mountain passes of Victoria Land Scott Coast {{ScottCoast ...
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Terra Nova Bay
Terra Nova Bay is a bay which is often ice free, about long, lying between Cape Washington and the Drygalski Ice Tongue along the coast of Victoria Land, Antarctica. It was discovered by the British National Antarctic Expedition (known as the ''Discovery'' Expedition) under Robert Falcon Scott, 1901–1904, and named by him after '' Terra Nova'', one of the relief ships for the expedition. The Italian permanent Zucchelli Station is located in the bay, as is the Jang Bogo Station of South Korea. Relief Inlet can be found in the south west corner of the Bay. Antarctic Specially Protected Area A marine area of of the bay comprising a narrow strip of coastal waters about long, to the immediate south of Zucchelli Station, and extending to a maximum of from the shore, has been designated an Antarctic Specially Protected Area (ASPA 161). It is an important site for long-term research on the marine ecology of benthic communities. As well as rich and complex sponge and anthozoan comm ...
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Deep Freeze Range
The Deep Freeze Range () is a rugged mountain range, over long and about wide, rising between Priestley and Campbell Glaciers in Victoria Land, Antarctica, and extending from the edge of the polar plateau to Terra Nova Bay. Peaks in the low and mid portions of the range were observed by early British expeditions to the Ross Sea. The range was mapped in detail by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos, 1955-63. It was named by the Advisory Committee on Antarctic Names in recognition of the support to research provided by the U.S. Navy's Operation Deep Freeze expeditions to Antarctica for many years beginning in 1954. __NOTOC__ Geological features Mount Adamson Mount Adamson () is a peak, high, rising east-northeast of Mount Hewson. It was named by the northern party of New Zealand Geological Survey Antarctic Expedition (NZGSAE), 1965–66, for R. Adamson, a geologist with this party. Mount Dickason Mount Dickason () is a promin ...
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Northern Foothills
Northern Foothills () is a line of coastal hills on the west side of Terra Nova Bay, Victoria Land, Antarctica, lying southward of Browning Pass and forming a peninsular continuation of the Deep Freeze Range. It was named by the Northern Party of the British Antarctic Expedition, 1910–13, because during field operations Inexpressible Island Inexpressible Island is a small, rocky island in Terra Nova Bay, Victoria Land, Antarctica. Description The island is bounded in the east by Evans Cove and the Hells Gate Moraine, and in the west by the Nansen Ice Sheet. The eastern side is re ..., close southward, was originally referred to as the "Southern Foothills." Hills of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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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 was discovered by Captain James Clark Ross in January 1841 and named after Queen Victoria. The rocky promontory of Minna Bluff is often regarded as the southernmost point of Victoria Land, and separates the Scott Coast to the north from the Hillary Coast of the Ross Dependency to the south. The region includes ranges of the Transantarctic Mountains and the McMurdo Dry Valleys (the highest point being Mount Abbott in the Northern Foothills), and the flatlands known as the Labyrinth. The Mount Melbourne is an active volcano in Victoria Land. Early explorers of Victoria Land include James Clark Ross and Douglas Mawson. In 1979, scientists discovered a group of 309 meteorites in Antarctica, some of which were found near the Allan Hills in ...
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Priestley Glacier
The Priestley Glacier is a major valley glacier, about long, originating at the edge of the Polar Plateau of Victoria Land, Antarctica. The glacier drains southeast between the Deep Freeze and Eisenhower Ranges to enter the northern end of the Nansen Ice Sheet. It was first explored by the Northern Party of the British Antarctic Expedition, 1910–13, and named for Raymond E. Priestley, a geologist with the Northern Party. Priestley Névé () is the névé at the head of Priestley Glacier in Victoria Land. It was named by the New Zealand Antarctic Place-Names Committee New Zealand Antarctic Place-Names Committee (NZ-APC) is an adjudicating committee established to authorize the naming of features in the Ross Dependency on the Antarctic continent. It is composed of the members of the New Zealand Geographic Board p ... in about 1966 in association with Priestley Glacier. See also * List of glaciers in the Antarctic * Ogden Heights * Szanto Spur * Wasson Rock Gla ...
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Campbell Glacier
Campbell Glacier () is a glacier, about long, originating near the south end of Mesa Range and draining southeast between the Deep Freeze Range and Mount Melbourne to discharge into north Terra Nova Bay. The lower end of the glacier was observed by the Northern Party, led by Lieutenant Victor Campbell, Royal Navy, of the British Antarctic Expedition, 1910–13; it was named for the leader of this party. The extent of the glacier and its discharge into north Terra Nova Bay, rather than the Nansen Ice Sheet, was determined by United States and New Zealand New Zealand ( mi, Aotearoa ) is an island country in the southwestern Pacific Ocean. It consists of two main landmasses—the North Island () and the South Island ()—and over 700 smaller islands. It is the sixth-largest island count ... survey parties to the area in 1961–62 and 1962–63. The steep bluff along the east side of the glacier is known as Hades Terrace, Bier Point is a projecting headland on the east ...
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British Antarctic Expedition, 1910–13
The ''Terra Nova'' Expedition, officially the British Antarctic Expedition, was an expedition to Antarctica which took place between 1910 and 1913. Led by Captain Robert Falcon Scott, the expedition had various scientific and geographical objectives. Scott wished to continue the scientific work that he had begun when leading the ''Discovery'' Expedition from 1901 to 1904, and wanted to be the first to reach the geographic South Pole. He and four companions attained the pole on 17 January 1912, where they found that a Norwegian team led by Roald Amundsen had preceded them by 34 days. Scott's party of five died on the return journey from the pole; some of their bodies, journals, and photographs were found by a search party eight months later. The expedition, named after its supply ship, was a private venture financed by public contributions and a government grant. It had further backing from the Admiralty, which released experienced seamen to the expedition, and from the Royal ...
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New Zealand Geological Survey Antarctic Expedition
The New Zealand Geological Survey Antarctic Expedition (NZGSAE) describes a series of scientific explorations of the continent Antarctica. The expeditions were notably active throughout the 1950s and 1960s. Features named by the expeditions 1957–1958 expedition The 1957–1958 expedition went to the Ross Dependency and named the Borchgrevink Glacier. Other features named include: * Carter Ridge * Felsite Island * Halfway Nunatak * Hedgehog Island * Moraine Ridge 1958–1959 expedition * Cadwalader Beach * Cape Hodgson * Carter Ridge * Isolation Point * Mountaineer Range * Mount Aurora * Mount Hayward * Mount Henderson (White Island) * Mount Bird. 1960–1961 expedition * Deverall Island * Lonewolf Nunataks 1961–1962 expedition * Aurora Heights * The Boil * Ford Spur * Graphite Peak * Half Century Nunatak * Half Dome Nunatak * Hump Passage * Last Cache Nunatak * Lookout Dome * Montgomerie Glacier * Mount Fyfe * Mount Macdonald * Snowshoe Pass * Turret Nu ...
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Frank V
This is a list of characters in the series of fantasy novels by C. S. Lewis called ''The Chronicles of Narnia''. See also a list of portrayals. A *Ahoshta: a 60-year-old Tarkaan of Calormen who later becomes the Grand Vizier, chief adviser to the Tisroc (king). Aravis' stepmother arranged for her to marry him, but Aravis hated him because of his age, appearance, character, and base birth. (HHB) *Alambil: "Lady of Peace", a planet (moving star) in the heavens above Narnia (PC) *Alimash: Calormene nobleman, cousin of Aravis (HHB) *Anradin Tarkaan: Calormene nobleman, former owner of Bree, who wants to buy Shasta (HHB) * Aravis Tarkheena: the daughter of a Calormene nobleman; she flees when her stepmother attempts to marry her to Ahoshta. She escapes from Calormen with Shasta, and becomes Queen of Archenland after marrying him. (HHB) *Ardeeb Tisroc: Great-great-great-great-grandfather of Aravis. (HHB) * Argoz, Lord: One of the Seven Great Lords of Narnia. (VDT) *Arlian, Lord ...
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Mount Browning
Mount Browning () is a mountain, high, which rises opposite the terminus of Boomerang Glacier in the Northern Foothills, on the coast of Victoria Land. It was first roughly mapped by the British Antarctic Expedition, 1907–09. This area was explored and mapped in greater detail by the Northern Party of the British Antarctic Expedition, 1910–13, and the mountain named for Petty Officer Frank V. Browning, Royal Navy The Royal Navy (RN) is the United Kingdom's naval warfare force. Although warships were used by English and Scottish kings from the early medieval period, the first major maritime engagements were fought in the Hundred Years' War against F ..., a member of the Northern Party. References * Mountains of Victoria Land Scott Coast {{ScottCoast-geo-stub ...
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List Of Airports In Antarctica
__TOC__ List , 18/36Ice , - valign=top , Palmer SkiwayHeliport , , NZ12 , , Anvers Island , , 01/19Snow , - valign=top , Patriot Hills Blue-Ice Runway , , SCPZ , , Ellsworth Mountains , , 24MIce , - valign=top , Pegasus Field(serving McMurdo Station and Scott Base) , , NZPG , , Ross Island , , 15/33Ice08/26Ice (skiway) , - valign=top , Perseus RunwayTemporary Airfield , , , , , , 10/28Blue Ice , - valign=top , Petrel Skiway , , SA47 , , Dundee Island , , 08/26Ice , - valign=top , Phoenix Airfield(serving McMurdo Station and Scott Base) , , NZFX , , Ross Island , , 15/33Compacted Snow , - valign=top , Plateau Station Skiway , , AT20 , , Queen Maud Land , , 18/36Ice , - valign=top , Plog Island Skiway(serving Davis) , , , , Plog Island , , (variable)Ice , - valign=top , Princess Elisabeth Skiway , , QAP , AT99 , Utsteinen Nunatak , , Blue Ice , - valign=top , Progress Skiway , , , ...
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Mountain Passes Of Victoria Land
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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