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Kappen Cliffs
The Kappen Cliffs () are steep rock cliffs that form the south edge of Kar Plateau on Scott Coast, Victoria Land, Antarctica. The cliffs are long and rise to . They were named by the New Zealand Geographic Board (1999) after Professor Ludger Kappen of Kiel University Kiel University, officially the Christian-Albrecht University of Kiel, (german: Christian-Albrechts-Universität zu Kiel, abbreviated CAU, known informally as Christiana Albertina) is a university in the city of Kiel, Germany. It was founded in ..., Germany, who conducted extensive lichen ecophysiology in the Cape Geology area. References Cliffs of Victoria Land Scott Coast {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kar Plateau
Granite Harbour () is a bay in the coast of Victoria Land, Antarctica, about long, entered between Cape Archer and Cape Roberts. It was discovered and named by the British National Antarctic Expedition (1901–04) in the ''Discovery'' in January 1902, while searching for safe winter quarters for the ship. The name derives from the great granite boulders found on its shores. See also *First View Point *Stevens Cliff Granite Harbour () is a bay in the coast of Victoria Land, Antarctica, about long, entered between Cape Archer and Cape Roberts. It was discovered and named by the British National Antarctic Expedition (1901–04) in the ''Discovery'' in January 19 ... References Bays of the Ross Dependency Landforms of Victoria Land Scott Coast Ports and harbours of the Ross Dependency {{ScottCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scott Coast
Scott Coast () is the portion of the coast of Victoria Land, Antarctica between Cape Washington and Minna Bluff. It was named by the New Zealand Antarctic Place-Names Committee in 1961 after Captain Robert Falcon Scott, Royal Navy, leader of the ''Discovery'' Expedition (1901–1904) and the British Antarctic Expedition (1910-1913), who died on the return journey from the South Pole. Much of the early exploration of this coastline was accomplished by Scott and his colleagues, and many of the names in the region were bestowed by him. See also * Blue Glacier * Dreschhoff Peak * Nostoc Flats * Robbins Hill * Stoner Peak * Thoreson Peak * Weidner Ridge * Mount Band Mount Band () is a mountain on the Scott Coast of Victoria Land. Its name stems from the profusion of colored lichens appearing in bands on brown rocks in the mountains of Victoria Land in Antarctica Antarctica () is Earth's southernmost ... External links Coasts of Victoria Land {{Sco ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Zealand Geographic Board
The New Zealand Geographic Board Ngā Pou Taunaha o Aotearoa (NZGB) was established by the New Zealand Geographic Board Act 1946, which has since been replaced by the New Zealand Geographic Board (Ngā Pou Taunaha o Aotearoa) Act 2008. Although an independent institution, it is responsible to the Minister for Land Information. The board has authority over geographical and hydrographic names within New Zealand and its territorial waters. This includes the naming of small urban settlements, localities, mountains, lakes, rivers, waterfalls, harbours and natural features and may include researching local Māori names. It has named many geographical features in the Ross Sea region of Antarctica. It has no authority to alter street names (a local body responsibility) or the name of any country. The NZGB secretariat is part of Toitū Te Whenua Land Information New Zealand (LINZ) and provides the board with administrative and research assistance and advice. The New Zealand Geograph ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ludger Kappen
Ludger Kappen is an ecophysiologist, botanist and lichenologist. He was Director of the Botanic Institute and Botanical Garden at the University of Kiel, and Chairman and Director of the University's Polar Ecology Institute. Early life and education Kappen studied within the biological sciences at Freiburg and Göttingen, and was awarded a doctorate in 1963 for his work on the effects of environmental stress on ferns. Career Kappen's first academic post was at the Forest Botanical Institute of the University of Göttingen investigating cold tolerance in fir trees, grape vines, lichens and marine algae. In 1974 he gained his habilitation at University of Würzburg for his further research into the mechanisms of cold tolerance in plants. In 1981 he joined University of Kiel as the established Professor of Ecophysiology and Director of the Botanic Institute, which included the University's botanical garden. In 1984 Kappen became the Chair and Director of the new Polar Ecology Ins ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kiel University
Kiel University, officially the Christian-Albrecht University of Kiel, (german: Christian-Albrechts-Universität zu Kiel, abbreviated CAU, known informally as Christiana Albertina) is a university in the city of Kiel, Germany. It was founded in 1665 as the ''Academia Holsatorum Chiloniensis'' by Christian Albert, Duke of Holstein-Gottorp and has approximately 27,000 students today. Kiel University is the largest, oldest, and most prestigious in the state of Schleswig-Holstein. Until 1864/66 it was not only the northernmost university in Germany but at the same time the 2nd largest university of Denmark. Faculty, alumni, and researchers of the Kiel University have won 12 Nobel Prizes. Kiel University has been a member of the German Universities Excellence Initiative since 2006. The Cluster of Excellence The Future Ocean, which was established in cooperation with the GEOMAR Helmholtz Centre for Ocean Research Kiel in 2006, is internationally recognized. The second Cluster of Excel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Geology
Cape Geology is a low, gravel-covered point marking the western limit of Botany Bay, in the southern part of Granite Harbour, Victoria Land, Antarctica. It was charted and named by the Western Geological Party of the Terra Nova Expedition (1910–13) who established their base there. Historic site The rock shelter known as Granite House was built in 1911, for use as a field kitchen, by Griffith Taylor’s second geological excursion in the course of the Terra Nova expedition. It was enclosed on three sides with granite boulder walls and used a sled to support a sealskin roof. The stone walls of the shelter have partly collapsed. It contains the corroded remains of tins, a sealskin and some cord. The sled lies 50 m seaward of the shelter and consists of a few scattered pieces of wood, straps and buckles. The site has been designated a Historic Site or Monument (HSM 67), following a proposal by New Zealand, Norway and the United Kingdom to the Antarctic Treaty Consultative Meet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliffs Of Victoria Land
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 featu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
