Landing Bluff
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Landing Bluff
Landing Bluff is a rock mass in Antarctica with a steep slope on the eastern side, with several small outcrops just to the south-west. It is located on the south-west part of Sandefjord Bay adjacent to Amery Ice Shelf, about 26 km west of Mount Caroline Mikkelsen. Mapped by Norwegian cartographers from air photographs taken by the Lars Christensen Expedition (1936–37) and called ''Strandknatten'' (The Strand Crag). A survey cairn was erected on the highest point by ANARE in 1968. So named because of its proximity to the landing place for stores and equipment for the ANARE Amery Ice Shelf The Amery Ice Shelf () is a broad ice shelf in Antarctica at the head of Prydz Bay between the Lars Christensen Coast and Ingrid Christensen Coast. It is part of Mac. Robertson Land. The name "Cape Amery" was applied to a coastal angle mapped o ... party in January–March, 1968. In 1987 on Landing Bluff was established Soviet Antarctic base Druzhnaya-4. References {{coord, 69 ...
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Rock (geology)
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's outer solid layer, the crust, and most of its interior, except for the liquid outer core and pockets of magma in the asthenosphere. The study of rocks involves multiple subdisciplines of geology, including petrology and mineralogy. It may be limited to rocks found on Earth, or it may include planetary geology that studies the rocks of other celestial objects. Rocks are usually grouped into three main groups: igneous rocks, sedimentary rocks and metamorphic rocks. Igneous rocks are formed when magma cools in the Earth's crust, or lava cools on the ground surface or the seabed. Sedimentary rocks are formed by diagenesis and lithification of sediments, which in turn are formed by the weathering, transport, and deposition of existing ro ...
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Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ...
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Sandefjord Ice Bay
Sandefjord Ice Bay is an ice bay about 25 nautical miles (46 km) wide which forms the head of Prydz Bay. The feature is bounded on the west by Amery Ice Shelf, on the east by Publications Ice Shelf, and on the south by the mainland. The bay was first discovered in February 1935 by Captain Klarius Mikkelsen on the Norwegian whaling ship '' Thorshavn'', sent out by Lars Christensen. They gave it the name Sandefjordbukta after the town of Sandefjord, Norway Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmost portion of the Scandinavian Peninsula. The remote Arctic island of Jan Mayen and t ..., center of the Norwegian whaling industry. The term "ice bay" is applied to this feature because of its formation in ice, and to reduce confusion with other bays of this name, particularly Sandefjord Bay on Coronation Island. See also * Sansom Islands * Landing Bluff Re ...
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Amery Ice Shelf
The Amery Ice Shelf () is a broad ice shelf in Antarctica at the head of Prydz Bay between the Lars Christensen Coast and Ingrid Christensen Coast. It is part of Mac. Robertson Land. The name "Cape Amery" was applied to a coastal angle mapped on 11 February 1931 by the British Australian New Zealand Antarctic Research Expedition (BANZARE) under Douglas Mawson. He named it for William Bankes Amery, a civil servant who represented the United Kingdom government in Australia (1925–28). The Advisory Committee on Antarctic Names interpreted this feature to be a portion of an ice shelf and, in 1947, applied the name Amery to the whole shelf. In 2001 two holes were drilled through the ice shelf by scientists from the Australian Antarctic Division and specially designed seabed sampling and photographic equipment was lowered to the underlying seabed. By studying the fossil composition of sediment samples recovered, scientists have inferred that a major retreat of the Amery Ice Shelf to ...
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Mount Caroline Mikkelsen
Mount Caroline Mikkelsen is a small coastal mountain discovered on February 20, 1935. Its height is and it is between Hargreaves Glacier and Polar Times Glacier on Ingrid Christensen Coast. The mountain overlooks the southern extremity of Prydz Bay, north-northwest of Svarthausen Nunatak, and is the highest summit in the vicinity. It was discovered by Captain Klarius Mikkelsen in the ''Thorshavn'', a Norwegian whaling ship sent out by Lars Christensen. It is named for Captain Mikkelsen's wife Caroline Mikkelsen Caroline Mikkelsen (20 November 1906 – 15 September 1998, later married Mandel) was a Danish-Norwegian explorer who on 20 February 1935 was the first woman to set foot on Antarctica, although whether this was on the mainland or an island ..., who accompanied her husband on this voyage and became the first woman to set foot on Antarctica. References Mountains of Princess Elizabeth Land Ingrid Christensen Coast {{PrincessElizabethLand-geo-stub ...
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Lars Christensen
Lars Christensen (6 April 1884 – 10 December 1965) was a Norwegian shipowner and whaling magnate. He was also a philanthropist with a keen interest in the exploration of Antarctica. Career Lars Christensen was born at Sandar in Vestfold, Norway. Born into a wealthy family, Christensen inherited his whaling fleet from his father, Christen Christensen. After completing middle school in 1899, he received training in Germany and at Newcastle followed by trade college in Kristiania (now Oslo). He started his career as a ship owner in 1906. He ventured into the whaling industry in 1909, and directed several companies, including Framnæs Mekaniske Værksted, AS Thor Dahl, AS Odd, AS Ørnen, AS Thorsholm and Bryde og Dahls Hvalfangstselskap. Christensen was Danish consul in Sandefjord from 1909. In 1910 Lars Christensen had married Ingrid Dahl (1891–1976), daughter of wholesale merchant and ship owner Thor Dahl (1862–1920). He would later assume control of large part of his fa ...
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ANARE
The Australian National Antarctic Research Expeditions (ANARE ) is the historical name for the Australia: Antarctic Program#Australian Antarctic program, Australian Antarctic Program (AAp) administered for Australia by the Australian Antarctic Division (AAD). History Australia has had a long involvement in South Pole, south polar regions since as early as Douglas Mawson's Australasian Antarctic Expedition in 1911. Further Australian exploration of the Antarctic continent was conducted during the British Australian and New Zealand Antarctic Research Expedition (BANZARE), which was conducted over the years 1929–1931. The Australian National Antarctic Research Expeditions were established in 1947 with expeditions to Macquarie Island and Heard Island. In 1948 the Australian Antarctic Division (AAD) was established to administer the expedition program. ANARE Name The name ANARE fell out of official use in the early 2000s. However current and former Australian Antarctic expedit ...
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Cliffs Of Antarctica
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also featur ...
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