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Nordre Sermilik
Ikersuaq, old spelling ''Ikerssuak'', ( da, Bredefjord) is a fjord in southwestern Greenland. Administratively it is part of the Kujalleq municipality. Geography The Ikersuaq fjord is oriented in a roughly NE/SW direction and to the southwest its mouth opens into the Julianehab Bay, Labrador Sea, North Atlantic Ocean. There is a vast ice field on the northwestern side of the fjord, where there are three branches, Qaleragdlit Imâ, Kangerlua and Kangerluarsuk. The Northern Sermilik (Nordre Sermilik) fjord is the inner section of Ikersuaq fjord. On its southern side the 1,440 m high Ilimaussaq peak rises in the peninsula to the east of the fjord. Northern Sermilik has two branches in the north with large glaciers at their heads. Elongated Tuttutooq Island is a prolongation of the southwestern end of the peninsula forming the southern shore of Northern Sermilik. The Narsaq Sound separates the peninsula from the island on the southern shore, connecting with neighbouring Tunu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arctic
The Arctic ( or ) is a polar regions of Earth, polar region located at the northernmost part of Earth. The Arctic consists of the Arctic Ocean, adjacent seas, and parts of Canada (Yukon, Northwest Territories, Nunavut), Danish Realm (Greenland), Finland, Iceland, Norway, Russia (Murmansk Oblast, Murmansk, Siberia, Nenets Autonomous Okrug, Nenets Okrug, Novaya Zemlya), Sweden and the United States (Alaska). Land within the Arctic region has seasonally varying snow and sea ice, ice cover, with predominantly treeless permafrost (permanently frozen underground ice) containing tundra. Arctic seas contain seasonal sea ice in many places. The Arctic region is a unique area among Earth's ecosystems. The cultures in the region and the Arctic indigenous peoples have adapted to its cold and extreme conditions. Life in the Arctic includes zooplankton and phytoplankton, fish and marine mammals, birds, land animals, plants and human societies. Arctic land is bordered by the subarctic. De ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Labrador Sea
The Labrador Sea (French: ''mer du Labrador'', Danish: ''Labradorhavet'') is an arm of the North Atlantic Ocean between the Labrador Peninsula and Greenland. The sea is flanked by continental shelf, continental shelves to the southwest, northwest, and northeast. It connects to the north with Baffin Bay through the Davis Strait. It is a marginal sea of the Atlantic. The sea formed upon separation of the North American Plate and Greenland Plate that started about 60 million years ago and stopped about 40 million years ago. It contains one of the world's largest turbidity current channel systems, the Northwest Atlantic Mid-Ocean Channel (NAMOC), that runs for thousands of kilometers along the sea bottom toward the Atlantic Ocean. The Labrador Sea is a major source of the North Atlantic Deep Water, a cold water mass that flows at great depth along the western edge of the North Atlantic, spreading out to form the largest identifiable water mass in the World Ocean. History The Labrad ... [...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] |
Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kujalleq
Kujalleq ( Greenlandic: , da, Den Syden, lit=The South) is a municipality on the southern tip of Greenland, operational from 1 January 2009. The administrative center of the municipality is in Qaqortoq (formerly called Julianehåb). Creation The municipality consists of the former municipalities of southern Greenland, each named after the biggest settlement: * Nanortalik Municipality * Narsaq Municipality * Qaqortoq Municipality In addition to the area of these municipalities, uninhabited parts of the former municipalities of Paamiut and Ammassalik were added to the new administrative entity. In the case of Paamiut Municipality, it was exclusively a part of the ice sheet including a few nunataks, while in the case of Ammassalik Municipality, it included the coast from the fjord Kangerlussuatsiaq (in Danish ''Lindenow Fjord'') on the old border with Nanortalik Municipality in the south to north of Timmiarmiut. Coat of arms The coat of arms of the municipality depicts a ram's h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julianehab Bay
Qaqortoq, formerly Julianehåb, is a city in the Kujalleq municipality in southern Greenland, located near Cape Thorvaldsen. With a population of 3,050 in 2020, it is the most populous town and the municipal capital in southern Greenland and the fourth or fifth-largest town on the island. History The area around Qaqortoq has been inhabited since prehistoric times. Beginning with the Saqqaq culture roughly 4,300 years ago, the area has had a continuous human presence. Saqqaq culture The earliest signs of population presence are from roughly 4,300 years ago. While Saqqaq-era sites are generally the most numerous of all the prehistoric sites in Greenland, around Qaqortoq the Saqqaq presence is less prominent, with only sporadic sites and items such as chipped stone drills and carving knives. Dorset culture The Dorset people arrived in the Qaqortoq area around 2,800 years ago. Several rectangular peat dwelling structures, characteristic of the early Dorset culture, can b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the "Old World" of Africa, Europe and Asia from the "New World" of the Americas in the European perception of the World. The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and North and South America to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Atlantic Ocean is divided in two parts, by the Equatorial Counter Current, with the North(ern) Atlantic Ocean and the South(ern) Atlantic Ocean split at about 8°N. Scientific explorations of the Atlant ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ice Field
An ice field (also spelled icefield) is a mass of interconnected valley glaciers (also called mountain glaciers or alpine glaciers) on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and higher altitudes of the world where there is sufficient precipitation for them to form. The higher peaks of the underlying mountain rock that protrude through the icefields are known as nunataks. Ice fields are larger than alpine glaciers, but smaller than ice caps and ice sheets. The topography of ice fields is determined by the shape of the surrounding landforms, while ice caps have their own forms overriding underlying shapes. Formation Ice fields are formed by a large accumulation of snow which, through years of compression and freezing, turns into ice. Due to ice's susceptibility to gravity, ice fields usually form over large areas that are basins or atop plateaus, thus allowing a continuum of ice to form over the landscape uninterrupted b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tunulliarfik
Tunulliarfik Fjord (old spelling: ''Tunugdliarfik'') is a fjord near Qaqortoq in the Kujalleq municipality in southern Greenland. It is the inner section of Skovfjord (Skovfjorden). In times of the Norse settlement in southern Greenland, it was known as ''Eiriksfjord''. Geography The fjord head at approximately is formed by the estuary of a river flowing from the glacial outflow lake in Johan Dahl Land. At approximately , south of the Narsarsuaq settlement, the fjord is joined by its tributary Qooroq Fjord from the northeast, changing direction from southern into southwestern. Bounded by long peninsulas and low-lying islands from the southeast and the northwest, it has its mouth in the Skovfjord which empties in Labrador Sea at approximately .Ivittuut/Narsarsuaq/Qaqortoq, Saga Map, Tage Schjøtt, 1992 The Narsaq Sound, between the peninsula forming the northern shore of Tunulliarfik Fjord and Tuttutooq and Illutaliq islands, connects with neighbouring Bredefjord and Nord ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Skovfjord
Tunulliarfik Fjord (old spelling: ''Tunugdliarfik'') is a fjord near Qaqortoq in the Kujalleq municipality in southern Greenland. It is the inner section of Skovfjord (Skovfjorden). In times of the Eastern Settlement, Norse settlement in southern Greenland, it was known as ''Eiriksfjord''. Geography The fjord head at approximately is formed by the estuary of a river flowing from the glacial outflow lake in Johan Dahl Land. At approximately , south of the Narsarsuaq settlement, the fjord is joined by its tributary Qooroq Fjord from the northeast, changing direction from southern into southwestern. Bounded by long peninsulas and low-lying islands from the southeast and the northwest, it has its mouth in the Skovfjord which empties in Labrador Sea at approximately .Ivittuut/Narsarsuaq/Qaqortoq, Saga Map, Tage Schjøtt, 1992 The Narsaq Sound, between the peninsula forming the northern shore of Tunulliarfik Fjord and Tuttutooq and Illutaliq islands, connects with neighbouring Bredef ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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