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Flade Isblink
Flade Isblink is an ice cap on the Crown Prince Christian Land peninsula, King Frederick VIII Land, NE Greenland. Station Nord, the only inhabited place in the region, lies to the northwest, off the ice cap area. History The Flade Isblink was named by Lauge Koch in 1933. He was the first to map the area in the course of survey flights during the 1931–34 Three-year expedition to East Greenland.''Catalogue of place names in northern East Greenland'', Geological Survey of Denmark and Greenland Geography This large and flat ice cap is separated from the Greenland ice sheet and is the largest independent ice cap in Greenland. It is located between the Wandel Sea to the north and Amdrup Land and Antarctic Bay to the south. Romer Lake and the Princess Elizabeth Alps extend southwestwards at the western end and to the east lies the Fram Strait and the Greenland Sea. The ice cap covers most of the northern part of Crown Prince Christian Land and is about in area. The underlying bedroc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland
Greenland ( kl, Kalaallit Nunaat, ; da, Grønland, ) is an island country in North America that is part of the Kingdom of Denmark. It is located between the Arctic and Atlantic oceans, east of the Canadian Arctic Archipelago. Greenland is the world's largest island. It is one of three constituent countries that form the Kingdom of Denmark, along with Denmark and the Faroe Islands; the citizens of these countries are all citizens of Denmark and the European Union. Greenland's capital is Nuuk. Though a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers) for more than a millennium, beginning in 986.The Fate of Greenland's Vikings , by Dale Mackenzie Brown, ''Archaeological Institute of America'', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Romer Lake
Romer Lake ( da, Romer Sø) is a land-locked freshwater fjord at the northern end of King Frederick VIII Land, near Greenland's northeastern coast. The Danish military base/weather station Nord —the only inhabited place in the area— lies to the northeast. The lake and its surroundings are part of the Northeast Greenland National Park zone. Romer Lake was first mapped in 1933 by Lauge Koch during aerial surveys made during the 1931–34 Three-year Expedition to East Greenland ''(Treårsekspeditionen)''. It was likely named after the Danish Astronomer/Inventor Ole Rømer (1644–1710). Geography Romer Lake is located at the western end of the Crown Prince Christian Land peninsula to the west of the Princess Elizabeth Alps. It lies in long and narrow depression running parallel to the Denmark Fjord system further north and stretching roughly from NE to SW for about . A glacier has its terminus at the northern end and the Nunataami Elv river valley flows out of the southern e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordostrundingen C 501 Map Sheet
Nordostrundingen (corrupted from da, Nordøstrundingen which means Northeastern rounding, in English Northeast Foreland), is a headland located at the northeastern end of Greenland. Administratively it is part of the Northeast Greenland National Park. This headland was named by the Denmark expedition 1906–1908. It is an inconspicuous point where the ice slope of the Flade Isblink meets the frozen sea. Easterly point At 11°19'W it is the most easterly point of land relative to either of the Americas (North and South America). Nordøstrundingen is further east than three countries in Africa and even further east than the westernmost point in Europe (excluding the Azores), which is Látrabjarg in Iceland. It is only 1° 49′ from the westernmost point of the European mainland which is in Portugal. Greenland is not part of North America politically, which leads some people to assert that the most easterly point of the continent is the easternmost point in Canada − Cape Spear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordostrundingen
Nordostrundingen (corrupted from da, Nordøstrundingen which means Northeastern rounding, in English Northeast Foreland), is a headland located at the northeastern end of Greenland. Administratively it is part of the Northeast Greenland National Park. This headland was named by the Denmark expedition 1906–1908. It is an inconspicuous point where the ice slope of the Flade Isblink meets the frozen sea. Easterly point At 11°19'W it is the most easterly point of land relative to either of the Americas (North and South America). Nordøstrundingen is further east than three countries in Africa and even further east than the westernmost point in Europe (excluding the Azores), which is Látrabjarg in Iceland. It is only 1° 49′ from the westernmost point of the European mainland which is in Portugal. Greenland is not part of North America politically, which leads some people to assert that the most easterly point of the continent is the easternmost point in Canada − Cape Spear ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outlet Glacier
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography Unconstrained Glaciers Ice sheets and ice caps Ice sheets and ice caps cover the largest areas of land in comparison to other glaciers, and their ice is unconstrained by the underlying topography. They are the largest glacial ice formations and hold the vast majority of the world's fresh water. Ice sheets Ice sheets are the largest form of glacial formation. They are continent sized ice masses that span areas over . They are dome s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Dome
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories: * Ice flow is constrained by the underlying bedrock topography * Ice flow is unrestricted by surrounding topography Unconstrained Glaciers Ice sheets and ice caps Ice sheets and ice caps cover the largest areas of land in comparison to other glaciers, and their ice is unconstrained by the underlying topography. They are the largest glacial ice formations and hold the vast majority of the world's fresh water. Ice sheets Ice sheets are the largest form of glacial formation. They are continent sized ice masses that span areas over . They are dome s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Greenland Sea
The Greenland Sea is a body of water that borders Greenland to the west, the Svalbard archipelago to the east, Fram Strait and the Arctic Ocean to the north, and the Norwegian Sea and Iceland to the south. The Greenland Sea is often defined as part of the Arctic Ocean, sometimes as part of the Atlantic Ocean. However, definitions of the Arctic Ocean and its seas tend to be imprecise or arbitrary. In general usage the term "Arctic Ocean" would exclude the Greenland Sea. In oceanographic studies the Greenland Sea is considered part of the Nordic Seas, along with the Norwegian Sea. The Nordic Seas are the main connection between the Arctic and Atlantic oceans and, as such, could be of great significance in a possible shutdown of thermohaline circulation. In oceanography the Arctic Ocean and Nordic Seas are often referred to collectively as the "Arctic Mediterranean Sea", a marginal sea of the Atlantic. The sea has Arctic climate with regular northern winds and temperatures rarely ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fram Strait
The Fram Strait is the passage between Greenland and Svalbard, located roughly between 77°N and 81°N latitudes and centered on the prime meridian. The Greenland and Norwegian Seas lie south of Fram Strait, while the Nansen Basin of the Arctic Ocean lies to the north. Fram Strait is noted for being the only deep connection between the Arctic Ocean and the World Oceans. The dominant oceanographic features of the region are the West Spitsbergen Current on the east side of the strait and the East Greenland Current on the west. Description Fram Strait is the northernmost ocean area having ice-free conditions throughout the year. The width of the strait is about 450 km, but because of the wide continental shelves of Greenland and Spitsbergen, the deep portion of Fram Strait is only about 300 km wide. The ocean over the Greenland continental shelf is often covered with ice. Within Fram Strait, the sill connecting the Arctic and Fram Strait is 2545 m deep. The Knipo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Princess Elizabeth Alps
The Princess Elizabeth Alps ( da, Prinsesse Elisabeth Alper) is a mountain range in King Frederick VIII Land, northeastern Greenland. Administratively this range is part of the Northeast Greenland National Park zone. The range was named by Eigil Nielsen during the 1938–39 Mørkefjord Expedition after Princess Elisabeth of Denmark (1935–2018), daughter of Prince Knud. Geography The Princess Elizabeth Alps run roughly from north to south across the western half of the large Crown Prince Christian Land peninsula with an average elevation of . The range begins abruptly at the Ingolf Fjord in the south, with the mountains rising steeply from the shore. Towards the northern end the elevations decrease until the range becomes a chain of small nunataks barely rising above the surrounding ice sheet. Google Earth The area of the range is bounded in the north by the Flade Isblink, a massive ice sheet, to the west by the Nunataami Elv valley, to the south by the Ingolf Fjord, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Bay (Greenland)
Antarctic Bay ( da, Antarctic Bugt) is a bay in the Greenland Sea coast of the Crown Prince Christian Land peninsula, King Frederick VIII Land, Northeastern Greenland. Administratively the bay and its surroundings belong to the Northeast Greenland National Park. The area of the bay is uninhabited. History The bay was named by the 1906-1908 Denmark expedition after Alfred Gabriel Nathorst's ship ''Antarctic''.''Catalogue of place names in northern East Greenland''. Geological Survey of Denmark and Greenland. Geography Antarctic Bay opens to the Fram Strait of the Greenland Sea. It lies between Amdrup Land to the west and the Flade Isblink ice cap to the north. It is a fairly wide bay, with the Nordostrundingen about to the northeast of its unnamed northeastern point. Sophus Müller Naes is the southwestern point of the bay.''Prostar Sailing Directions 2005 Greenland and Iceland Enroute,'' p. 128. Kilen lies just a few km north of the ice-covered head and northeastern shore of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Cap
In glaciology, an ice cap is a mass of ice that covers less than of land area (usually covering a highland area). Larger ice masses covering more than are termed ice sheets. Description Ice caps are not constrained by topographical features (i.e., they will lie over the top of mountains). By contrast, ice masses of similar size that ''are'' constrained by topographical features are known as ice fields. The ''dome'' of an ice cap is usually centred on the highest point of a massif. Ice flows away from this high point (the ice divide) towards the ice cap's periphery. Ice caps have significant effects on the geomorphology of the area that they occupy. Plastic moulding, gouging and other glacial erosional features become present upon the glacier's retreat. Many lakes, such as the Great Lakes in North America, as well as numerous valleys have been formed by glacial action over hundreds of thousands of years. On Earth, there are about of total ice mass. The average temperature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
