Inglefield Land
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Inglefield Land
Inglefield Land is an unglaciated area along the northwestern coast of Greenland. It was named after English explorer Edward Augustus Inglefield. History Inglefield Land is noted for its archaeological sites, which show evidence of occupation by the Dorset Culture and Thule Culture. Geography The region stretches from Cape Alexander to the southwest to Cape Agassiz at the eastern end. It is bounded by Prudhoe Land in the south, the Humboldt Glacier in the northeast, and the Kane Basin to the north. The Dodge Glacier is located to the southwest and the Hiawatha Glacier Hiawatha Glacier is a glacier in northwest Greenland, with its terminus in Inglefield Land. It was mapped in 1922 by Lauge Koch, who noted that the glacier tongue extended into Lake Alida (near Foulk Fjord). Hiawatha Glacier attracted attention in ... to the east. The McGary and Bonsall Islands are located off the northeastern and the Littleton Islands of the southwestern end. References {{reflist Geography ...
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Smith Sound
Smith Sound ( da, Smith Sund; french: Détroit de Smith) is an uninhabited Arctic sea passage between Greenland and Canada's northernmost island, Ellesmere Island. It links Baffin Bay with Kane Basin and forms part of the Nares Strait. On the Greenland side of the sound were the now abandoned settlements of Etah and Annoatok. History The first known visit to the area by Europeans was in 1616 when the ''Discovery'', captained by Robert Bylot and piloted by William Baffin, sailed into this region. The sound was originally named ''Sir Thomas Smith's Bay'' after the English diplomat Sir Thomas Smythe. By the 1750s it regularly appeared on maps as ''Sir Thomas Smith's Sound'', though no further exploration of the area would be recorded until John Ross' 1818 expedition. By this time it had begun to be known simply as ''Smith Sound''. In 1852 Edward Augustus Inglefield penetrated a little further than Baffin, establishing a new furthest north in North America. References Further ...
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Kane Basin
Kane Basin ( da, Kane Bassin; french: Bassin (de) Kane) is an Arctic waterway lying between Greenland and Canada's northernmost island, Ellesmere Island. It links Smith Sound to Kennedy Channel and forms part of Nares Strait. It is approximately 180 kilometres in length and 130 km at its widest. It is named after the American explorer Elisha Kane, whose expedition in search of Franklin's lost expedition crossed it in 1854. Kane himself had named it "Peabody Bay," in honor of philanthropist George Peabody, the major funder of Kane's expedition. Currently Peabody Bay is a bay at the eastern side of the basin, off the southwestern end of the Humboldt Glacier Humboldt Glacier ( da, Humboldt Gletscher) is one of the major glaciers in northern Greenland. The glacier is named after German naturalist Alexander von Humboldt and is the widest tidewater glacier in the Northern Hemisphere. Geography The Humb ... in northern Greenland. Further reading * Cold Regions Research and ...
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Peabody Bay
Peabody Bay ( da, Peabody Bugt) is a large bay in northwestern Greenland. Administratively it is part of Avannaata municipality. Geography Peabody Bay is located on the eastern side of the Kane Basin off the western end of the Humboldt Glacier. Cape Forbes and the Cass Fjord lie at the northern end of the roughly 80 km wide bay. The McGary Islands lie at the southern end of the bay and the Bonsall Islands lie between that end and Dallas Bay to the SW. Elisha Kane —whose Arctic venture in search of the lost Franklin expedition crossed the area in 1854— had named the Kane Basin itself "Peabody Bay," in honor of philanthropist George Peabody George Peabody ( ; February 18, 1795 – November 4, 1869) was an American financier and philanthropist. He is widely regarded as the father of modern philanthropy. Born into a poor family in Massachusetts, Peabody went into business in dry go ..., the major funder of Kane's expedition. Currently, however, Peabody Bay is this smaller ...
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Unglaciated
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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Edward Augustus Inglefield
Sir Edward Augustus Inglefield (27 March 1820 – 4 September 1894) was a Royal Navy officer who led one of the searches for the missing Arctic explorer John Franklin during the 1850s. In doing so, his expedition charted previously unexplored areas along the northern Canadian coastline, including Baffin Bay, Smith Sound and Lancaster Sound. He was also the inventor of the marine hydraulic steering gear and the anchor design that bears his name. bears his name, as do the Inglefield Land region and the Inglefield Gulf of Greenland. Career First voyage to the Arctic Inglefield set out from Britain on his search in July 1852, commanding Jane Franklin, Lady Franklin's private steamer , seven years after Sir John Franklin had left on his ill-fated search for the fabled Northwest Passage. Once Inglefield had reached the Arctic, a search and survey of Greenland's west coast was made; Ellesmere Island was resighted and named in honour of the president of the Royal Geographic ...
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Dorset Culture
The Dorset was a Paleo-Eskimo culture, lasting from to between and , that followed the Pre-Dorset and preceded the Thule people (proto-Inuit) in the North American Arctic. The culture and people are named after Cape Dorset (now Kinngait) in Nunavut, Canada, where the first evidence of its existence was found. The culture has been defined as having four phases due to the distinct differences in the technologies relating to hunting and tool making. Artifacts include distinctive triangular end-blades, oil lamps () made of soapstone, and burins. The Dorset were first identified as a separate culture in 1925. The Dorset appear to have been extinct by 1500 at the latest and perhaps as early as 1000. The Thule people, who began migrating east from Alaska in the 11th century, ended up spreading through the lands previously inhabited by the Dorset. There is no strong evidence that the Inuit and Dorset ever met. Modern genetic studies show the Dorset population were distinct from later ...
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Thule Culture
The Thule (, , ) or proto-Inuit were the ancestors of all modern Inuit. They developed in coastal Alaska by the year 1000 and expanded eastward across northern Canada, reaching Greenland by the 13th century. In the process, they replaced people of the earlier Dorset culture that had previously inhabited the region. The appellation "Thule" originates from the location of Thule (relocated and renamed Qaanaaq in 1953) in northwest Greenland, facing Canada, where the archaeological remains of the people were first found at Comer's Midden. The links between the Thule and the Inuit are biological, cultural, and linguistic. Evidence supports the idea that the Thule (and also the Dorset, but to a lesser degree) were in contact with the Vikings, who had reached the shores of Canada in the 11th century as part of Norse colonization of North America. In Viking sources, these peoples are called the ''Skrælingjar''. Some Thule migrated southward, in the "Second Expansion" or "Second Phase". B ...
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Cape Alexander, Greenland
Cape Alexander ( kl, Ullersuaq, also ''Uvdlerssuak'' and ''Sarfalik''; da, Kap Alexander) is a headland in the Baffin Bay, northwest Greenland, Avannaata municipality. It is one of the important landmarks of Greenland. Geography Cape Alexander is located in Prudhoe Land, at the western end of Hartstene Bay with the Dodge Glacier to the east and the Storm Glacier to the southeast. This headland is the westernmost point of the island of Greenland. Sutherland Island (Tigssarfik) lies off the shore to the southeast. The small Carey Islands are located further to the west; among them Nordvestø (73°10'W), the westernmost point of Greenland as a territory. See also *List of countries by westernmost point References Alexander Alexander is a male given name. The most prominent bearer of the name is Alexander the Great, the king of the Ancient Greek kingdom of Macedonia who created one of the largest empires in ancient history. Variants listed here are Aleksandar, Al ...< ...
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Cape Agassiz, Greenland
A cape is a clothing accessory or a sleeveless outer garment which drapes the wearer's back, arms, and chest, and connects at the neck. History Capes were common in medieval Europe, especially when combined with a hood in the chaperon. They have had periodic returns to fashion - for example, in nineteenth-century Europe. Roman Catholic clergy wear a type of cape known as a ferraiolo, which is worn for formal events outside a ritualistic context. The cope is a liturgical vestment in the form of a cape. Capes are often highly decorated with elaborate embroidery. Capes remain in regular use as rainwear in various military units and police forces, in France for example. A gas cape was a voluminous military garment designed to give rain protection to someone wearing the bulky gas masks used in twentieth-century wars. Rich noblemen and elite warriors of the Aztec Empire would wear a tilmàtli; a Mesoamerican cloak/cape used as a symbol of their upper status. Cloth and clothing ...
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Prudhoe Land
Prudhoe ( ) is a town in south Northumberland, England, about west of the city of Newcastle upon Tyne and just south of the River Tyne. Situated on a steep, north-facing hill in the Tyne valley, Prudhoe had a population of 11,675 at the 2011 Census. It has largely become a commuter town for nearby Newcastle. Nearby settlements include Ovingham, Ovington, Wylam, Stocksfield, Crawcrook, Hedley on the Hill and Mickley. History The name derives from the Anglo-Saxon personal name Prud (from ''prūd'', meaning proud) and hoe or haugh, a spur of land. There has been a castle at Prudhoe since ancient times, when England was at war with Scotland. The area now known as Castlefields was a fruit orchard, and the Scots were rumoured to have burnt this orchard while attempting to capture Prudhoe Castle. The castle, originally owned by the D'Umfravilles, then the Percys and now English Heritage, is considered to be the only medieval fortification in Northumberland never to have been ...
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Humboldt Glacier
Humboldt Glacier ( da, Humboldt Gletscher) is one of the major glaciers in northern Greenland. The glacier is named after German naturalist Alexander von Humboldt and is the widest tidewater glacier in the Northern Hemisphere. Geography The Humboldt Glacier borders the Kane Basin in North West Greenland. Its front is wide. It has been retreating in the period of observation spanning 1975–2010. Humboldt Glacier fringes the coast of Peabody Bay from north to south. The McGary Islands lie off the glacier at the southern end of the bay.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute'', p. 88 See also *List of glaciers in Greenland *Peabody Bay Peabody Bay ( da, Peabody Bugt) is a large bay in northwestern Greenland. Administratively it is part of Avannaata municipality. Geography Peabody Bay is located on the eastern side of the Kane Basin off the western end of the Humboldt Glacier. Ca ... References External links * Glaciers of Greenland {{arctic ...
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Dodge Glacier
Dodge Glacier ( da, Dodge Gletscher), is a glacier in northwestern Greenland. Administratively it belongs to the Avannaata municipality. The glacier was named by Isaac Israel Hayes (1832 – 1881) after expedition member Henry W. Dodge during the American Arctic Expedition of 1860 – 1861. Geography The Dodge Glacier has its terminus in the Smith Sound, east of Cape Alexander (Ullersuaq), north of the Storm Glacier. The Dodge and Storm glaciers don't discharge directly from the Greenland Ice Sheet, but from an ice cap located at the southwestern end of Inglefield Land which is attached to the Ice Sheet from the southeast. In the same manner as the neighboring Storm Glacier, the Dodge Glacier has retreated significantly in recent years. See also *List of glaciers in Greenland *Operation IceBridge Operation IceBridge is an ongoing NASA mission to monitor changes in polar ice. It is an airborne follow-on mission to the ICESat satellite, continuing until after the IC ...
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