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Tamarus Valley
Tamarus Valley () is an ice-free valley lying south of Sabrina Ridge and 2.5 nautical miles (4.6 km) northeast of Mount Henderson in the Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Tamarus is the historical name used in Roman Britain for the River Tamar. Valleys of Oates Land {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valley
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sabrina Ridge
Sabrina Ridge () is a bare rock ridge between Sabrina Valley and Tamarus Valley, 5 miles (8 km) south of Derrick Peak in Britannia Range. Named in association with Britannia by a University of Waikato (N.Z.) geological party, 1978–79, led by Michael Selby. Sabrina is a historical name formerly used in Roman Britain for the River Severn. External links Sabrina Ridgeon USGS website Sabrina Ridgeon SCAR A scar (or scar tissue) is an area of fibrous tissue that replaces normal skin after an injury. Scars result from the biological process of wound repair in the skin, as well as in other organs, and tissues of the body. Thus, scarring is a na ... website Sabrina Ridge area map References Ridges of Oates Land {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Henderson (Britannia Range)
Mount Henderson is a prominent mountain. It is high, and stands west of Mount Olympus in the Britannia Range of Antarctica. It was discovered and named by the British National Antarctic Expedition, 1901–04 The ''Discovery'' Expedition of 1901–1904, known officially as the British National Antarctic Expedition, was the first official British exploration of the Antarctic regions since the voyage of James Clark Ross sixty years earlier (1839–184 .... References Mountains of Oates Land Britannia Range (Antarctica) {{OatesLand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Britannia Range (Antarctica)
The Britannia Range is an Antarctic mountain range bounded by the Hatherton and Darwin glaciers on the north and the Byrd Glacier on the south, westward of the Ross Ice Shelf. Discovered by the British National Antarctic Expedition (1901–04) under Scott. Named after HMS ''Britannia'', a vessel utilized as a naval college in England, which had been attended by several officers of Scott's expedition. Features * Abus Valley * Adams Crest * Banna Peak * Beale Peak * Bellum Valley * Benson Bluff * Berry Bastion * Borowski Peak * Brier Icefalls * Casatelli Peak * Cohn Bluff * Danum Platform * Darnell Nunatak * Dartmouth Peak * DeGalan Peak * Doll Peak * Dubris Valley * Dusky Ledge * Dusky Ridge * Forbes Ridge * Hourihan Glacier * Hughes Basin * Icenhower Ridge * Jacobs Peak * Johnson Spire * Johnstone Ridge * Krissek Peak * Lemanis Valley * Lucia Peak * Magnis Ridge * Marty Nunataks * Menster Ledge * Metaris Valley * Moore Pinnacle * Mount Aldrich * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Michael Selby
Michael John Selby (13 January 1936 – 21 January 2018) was a New Zealand geomorphologist, academic, and university administrator. Mount Selby in Antarctica's Britannia Range is named for him. Biography Born in Luton, Bedfordshire, England, on 13 January 1936, Selby studied at Keble College, Oxford, gaining a BA(Hons), MA, and DipEd. Selby came to New Zealand on the RMS ''Rangitata'' in 1960, and was appointed as a junior lecturer at the Waikato branch of the University of Auckland. On the establishment of the University of Waikato in 1964, he joined the new Department of Geography, and then the Department of Earth Sciences when it was formed in 1970. The following year, he completed a DPhil: the title of his doctoral thesis was ''Runoff, infiltration and soil erodibility studies in the Otutira catchment''. He was later awarded a Doctor of Science degree from the University of Oxford on the basis of his research linking concepts in geomorphology with quantitative mea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roman Britain
Roman Britain was the period in classical antiquity when large parts of the island of Great Britain were under occupation by the Roman Empire. The occupation lasted from AD 43 to AD 410. During that time, the territory conquered was raised to the status of a Roman province. Julius Caesar invaded Britain in 55 and 54 BC as part of his Gallic Wars. According to Caesar, the Britons had been overrun or culturally assimilated by other Celtic tribes during the British Iron Age and had been aiding Caesar's enemies. He received tribute, installed the friendly king Mandubracius over the Trinovantes, and returned to Gaul. Planned invasions under Augustus were called off in 34, 27, and 25 BC. In 40 AD, Caligula assembled 200,000 men at the Channel on the continent, only to have them gather seashells ('' musculi'') according to Suetonius, perhaps as a symbolic gesture to proclaim Caligula's victory over the sea. Three years later, Claudius directed four legi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Tamar
The Tamar (; kw, Dowr Tamar) is a river in south west England, that forms most of the border between Devon (to the east) and Cornwall (to the west). A part of the Tamar Valley is a World Heritage Site due to its historic mining activities. The Tamar's source is less than from the north Cornish coast, but it flows southward and its course runs across the peninsula to the south coast. The total length of the river is . At its mouth, the Tamar flows into the Hamoaze before entering Plymouth Sound, a bay of the English Channel. Tributaries of the river include the rivers Inny, Ottery, Kensey and Lynher (or ''St Germans River'') on the Cornish side, and the Deer and Tavy on the Devon side. The name Tamar (or Tamare) was mentioned by Ptolemy in the second century in his ''Geography''. The name is said to mean "great water."Furneaux, Robert. The Tamar: A Great Little River. Ex Libris Press. 1992. Foot, Sarah. ''The River Tamar''. Bossiney Books. 1989.Neale, John. Discovering ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
