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Moon Bay
Moon Bay is a bay wide which recedes between Edinburgh Hill and Renier Point, on the east side of Livingston Island, in the South Shetland Islands off Antarctica. The glaciers Sopot Ice Piedmont, Iskar, Huron, Struma, Kaliakra, Panega and Debelt feed the bay. Both Half Moon Island and Elemag Reef are lying in Moon Bay. The bay was known to sealers in the area as early as 1821. It was recharted in 1935 by Discovery Investigations personnel on the '' Discovery II'', and probably named by them for nearby Half Moon Island Half Moon Island is a minor Antarctic island, lying in McFarlane Strait north of Burgas Peninsula, Livingston Island in the South Shetland Islands of the Antarctic Peninsula region. Its surface area is . The Argentine Cámara Base is locate ..., which lies in the entrance to the bay. Maps South Shetland Islands.Scale 1:200000 topographic map. DOS 610 Sheet W 62 60. Tolworth, UK, 1968. South Shetland Islands.Scale 1:200000 topographic map. DOS 610 Sheet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Struma Glacier
Struma Glacier ( bg, ледник Струма, lednik Struma, ) is a glacier in eastern Livingston Island in the South Shetland Islands, Antarctica situated south of lower Kaliakra Glacier and north of Huron Glacier. Bounded by Melnik Ridge to the north, Yankov Gap to the west and Bowles Ridge to the south, it is 4.8 km long and 1.5 km wide, and flows eastwards into Moon Bay south of Sindel Point. First crossed by the Bulgarians Lyubomir Ivanov and Doychin Vasilev from Camp Academia on 28 December 2004, as part of Tangra 2004/05 survey. The glacier is named after the Struma River in Bulgaria and forms part of the overland route between Pirdop Gate and Yankov Gap. Location The midpoint is located at . Bulgarian topographic survey Tangra 2004/05 and mapping in 2005 and 2009. See also * List of glaciers in the Antarctic * Glaciology Maps * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
RRS Discovery II
RRS ''Discovery II'' was a British Royal Research Ship which, during her operational lifetime of about 30 years, carried out considerable hydrographical and marine biological survey work in Antarctic waters and the Southern Ocean in the course of the Discovery Investigations research program. Built in Port Glasgow, launched in 1928 and completed in 1929, she was the first purpose-built oceanographic research vessel and was named after Robert Falcon Scott's 1901 ship, RRS ''Discovery''. Career The ship's maiden voyage took place from December 1929 to May 1931 and consisted of a hydrographic survey of the South Sandwich Islands. From October 1932 until May 1933 she operated in the Antarctic, calling at South Africa, Australia and New Zealand. Similar voyages took place from 1934 to 1939 during which she supplied the British Graham Land expedition. Her last voyage before the onset of war was from September 1937 to May 1939. In December 1935 and January 1936 the ship was invo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Discovery Investigations
The Discovery Investigations were a series of scientific cruises and shore-based investigations into the biology of whales in the Southern Ocean. They were funded by the British Colonial Office and organised by the Discovery Committee in London, which was formed in 1918. They were intended to provide the scientific background to stock management of the commercial Antarctic whale fishery. The work of the Investigations contributed hugely to our knowledge of the whales, the krill they fed on, and the oceanography of their habitat, while charting the local topography, including Atherton Peak. The investigations continued until 1951, with the final report being published in 1980. Laboratory Shore-based work on South Georgia took place in the marine laboratory, Discovery House, built in 1925 at King Edward Point and occupied until 1931. The scientists lived and worked in the building, travelling half a mile or so across King Edward Cove to the whaling station at Grytviken to work on w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elemag Reef
Elemag Reef (Rif Elemag \'rif 'e-le-mag\) is the 100 m long in southeast-northwest direction and 40 m wide moraine reef in Moon Bay, Livingston Island in the South Shetland Islands, with a narrow shoal extending for over 400 m eastwards. Surface area 0.33 ha. Situated 5.4 km south-southwest of Edinburgh Hill, 5.95 km west of Half Moon Island, 5.18 km northwest of Rila Point, 3.3 km northeast of Zlatograd Rock and 1.85 km east-southeast of Sindel Point. Formed at the Glacier terminus, terminus of merging Struma Glacier, Struma and Huron Glaciers, it was originally named ''Elemag Point''. The current reef configuration is due to glacier retreat of up to 1.8 km in the area in the late 20th and early 21st century. Bulgarian mapping in 2009. Bulgarian topographic survey Tangra 2004/05 and mapping in 2009. Named after Elemag, governor of Berat during the final years of the First Bulgarian Empire. Maps * L.L. Ivanov et al. :commons:Image:Livingston-Greenwich-map.jpg, Antarctica: Livi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Half Moon Island
Half Moon Island is a minor Antarctic island, lying in McFarlane Strait north of Burgas Peninsula, Livingston Island in the South Shetland Islands of the Antarctic Peninsula region. Its surface area is . The Argentine Cámara Base is located on the island. It is only accessible by sea and by helicopter; there is no airport of any kind. The naval base is operational occasionally during the summer, but is closed during the winter. Geography The island is a series of gravel bars (tombolos) connecting volcanic bedrock islands. The volcanism is not recent and may be millions of years old. The crescent shaped island may be the result of an eroded caldera similar to the much more recent Deception Island volcano complex. The parallel gravel bars are a result of post-glacial (isostatic) uplift of the area after the much larger Pleistocene ice cap melted and the pressure was released. Wildlife Plants found on the island include several lichen and moss species as well as Antarcti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Debelt Glacier
The Debelt Glacier ( bg, ледник Дебелт, lednik Debelt, ) on Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of Rose Valley Glacier and northeast of Panega Glacier. It drains the southeastern slopes of Vidin Heights and flows into Moon Bay between Edinburgh Hill and Helis Nunatak. The glacier extends three km in an east-west direction, and 1.5 km in north-south direction. Debelt glacier is centred at (62.5319° S; 60.0628° W). Bulgarian topographic survey Tangra 2004/05 and mapping in 2005 and 2009. The feature is named after the settlement of Debelt in Southeastern Bulgaria, successor of the ancient town of Deultum. Registered in the SCAR Composite Antarctic Gazetteer. See also * List of glaciers in the Antarctic * Glaciology Maps * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of Bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panega Glacier
Panega Glacier ( bg, ледник Панега, lednik Panega, ) on Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of the northeastern portion of Saedinenie Snowfield, south of Rose Valley Glacier, southwest of Debelt Glacier and north of lower Kaliakra Glacier. It drains the southeast slopes of Vidin Heights and flows into Moon Bay between Helis Nunatak and Perperek Knoll. The glacier extends in the southeast-northwest direction, and in the southwest-northeast direction. It is named after Zlatna Panega River in northern Bulgaria. Location The glacier is centred at (Bulgarian topographic survey Tangra 2004/05 and mapping in 2005 and 2009). See also * List of glaciers in the Antarctic * Glaciology Maps * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of Bulgaria, 2005. * L.L. IvanovAntarctica: Livings ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kaliakra Glacier
Kaliakra Glacier ( bg, ледник Калиакра, lednik Kaliakra, ) is a glacier in northeastern Livingston Island, Antarctica extending in east-west direction and in north-south direction, and situated southeast of Saedinenie Snowfield, southwest of Panega Glacier, north of Struma Glacier and upper Huron Glacier, and northeast of Perunika Glacier. It is bounded by Melnik Ridge and Bowles Ridge to the south, by Hemus Peak, Gurev Gap, Gleaner Heights, Elhovo Gap, Leslie Hill, Leslie Gap and Radnevo Peak to the west, and Miziya Peak and Samuel Peak to the north. The glacier drains eastwards into Moon Bay south of Perperek Knoll and north of Sindel Point. The glacier was first crossed by the Bulgarians Lyubomir Ivanov and Doychin Vasilev from Camp Academia on 24 December 2004. Kaliakra, the name of a cape on the Bulgarian Black Sea Coast, was given to the glacier by the Bulgarian Antarctic Place-names Commission, around 1995. Location The midpoint of the glacier is l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Huron Glacier
Huron Glacier is a } long and wide glacial flow on Livingston Island in the South Shetland Islands of Antarctica, situated east of Perunika Glacier, southeast of Kaliakra Glacier, south of Struma Glacier, west-northwest of Iskar Glacier and northeast of Huntress Glacier. It is bounded by Bowles Ridge to the north, Wörner Gap to the west and the Tangra Mountains to the south, receiving ice influx from several tributary glaciers draining the mountain's northern slopes between Mount Friesland and Helmet Peak, and running east-northeastwards to empty into Moon Bay north of Yana Point. Camp Academia is situated on upper Huron Glacier, in the northwestern foothills of Zograf Peak. The glacier was named by the UK Antarctic Place-names Committee in 1958 after the American ship ''Huron'' (Captain John Davis) of New Haven, Connecticut, which visited the South Shetland Islands in 1820–21 and 1821–22. Location Huron Glacier is centred at (British mapping in 1968, Bulgarian survey ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Huron
Huron may refer to: People * Wyandot people (or Wendat), indigenous to North America * Wyandot language, spoken by them * Huron-Wendat Nation, a Huron-Wendat First Nation with a community in Wendake, Quebec * Nottawaseppi Huron Band of Potawatomi, a band of Potawatomi American Indians, based in Calhoun County, Michigan), are also known as the Huron Potawatomi Bodies of water * Lake Huron, one of the North American Great Lakes * Huron Swamp in Springfield Township, Oakland County, Michigan * Huron Falls, one of 24 named waterfalls in Ricketts Glen State Park in Pennsylvania * Huron Lake, in the parish municipality of Lac-aux-Sables, Mékinac Regional County Municipality, Quebec * Huron River (other) * Rivière des Hurons (other) Places Canada * Lac-Huron, Quebec, an unorganized territory in the Rimouski-Neigette Regional County Municipality * Huron-Kinloss, a township in Bruce County, Ontario * Huron East, Ontario, a municipality in Huron County, Ontario * Rural ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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