"region is related to the stresses associated with post-glacial rebound. Greenland Plate The Greenland Plate is a supposed tectonic plate bounded to the west by Nares Strait, a probable transform fault, on the southwest by the Ungava transform underlying Davis Strait, on the southeast by the Mid-Atlantic Ridge, and the northeast by the Gakkel Ridge, with its northwest border is still being explored.). The Greenland craton is made up of some of the oldest rocks on Earth. The Isua greenstone belt in southwestern Greenland contains the oldest known rocks on Earth dated at 3.7–3.8 billion years old. The Precambrian basement"
"Denmark Strait The Denmark Strait () or Greenland Strait (, 'Greenland Sound') is an oceanic strait between Greenland (to its northwest) and Iceland (to its southeast). The Norwegian island of Jan Mayen lies northeast of the strait. The strait connects the Greenland Sea, an extension of the Arctic Ocean, to the Irminger Sea, a part of the Atlantic Ocean. It stretches long and wide at its narrowest, between Straumnes, the northwestern headland of the Westfjords peninsula of Hornstrandir, and Cape Tupinier on ""Blosseville Coast"" in East Greenland). The official International Hydrographic Organization (IHO) delineation between the Arctic and the North"
", which exploded with the loss of all but three of its 1,418 crew; was seriously damaged in the engagement. ""Bismarck"" entered the Atlantic through the Strait, but damage sustained in the battle—combined with British aircraft search-and-destroy missions—led to its sinking three days later. Denmark Strait The Denmark Strait () or Greenland Strait (, 'Greenland Sound') is an oceanic strait between Greenland (to its northwest) and Iceland (to its southeast). The Norwegian island of Jan Mayen lies northeast of the strait. The strait connects the Greenland Sea, an extension of the Arctic Ocean, to the Irminger Sea, a part of"
"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. Fram Strait is the northernmost ocean area having"
"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"
"meters closer to Greenland's coast. The channel also contains two more islands, Franklin Island and Crozier Island which are located much closer to the Greenland coast and therefore belong to Greenland. Kennedy Channel Kennedy Channel (; ; ) is an Arctic sea passage between Greenland and Canada's most northerly island, Ellesmere Island. It was named by Elisha Kane around 1854 during his second Arctic voyage in search of the lost Franklin expedition. It is not entirely clear, however, for which Kennedy he named the channel. Kane may have had his fellow explorer William Kennedy in mind, whom he had met"
"Greenland Greenland (, ; , ) is an autonomous constituent country of the Kingdom of Denmark between the Arctic and Atlantic Oceans, east of the Canadian Arctic Archipelago. Though physiographically a part of the continent of North America, Greenland has been politically and culturally associated with Europe (specifically Norway and Denmark, the colonial powers, as well as the nearby island of Iceland) for more than a millennium. The majority of its residents are Inuit, whose ancestors began migrating from the Canadian mainland in the 13th century, gradually settling across the island. Greenland is the world's largest island. Australia and Antarctica"
"Fiann Paul. The Greenland Sea is bounded to the west by the island of Greenland, and to the south by the Denmark Strait and Iceland. To the southeast, behind the Jan Mayen island (Norway) lies the vast expanse of the Norwegian Sea, of which Greenland Sea may be considered an extension. Across the Fram Strait to the northeast, the sea is delimited by the Svalbard archipelago (Norway). The bottom of the Greenland Sea is a depression bounded to the south by the underwater and to the east by the Mohns Ridge and Knipovich Ridge (parts of the Mid-Atlantic Ridge). To"
"Geography of Greenland Greenland is located between the Arctic Ocean and the North Atlantic Ocean, northeast of Canada and northwest of Iceland. The territory comprises the island of Greenland–the largest island in the world–and more than a hundred other smaller islands (see ). As an island, Greenland has no land boundaries and 44,087 km of coastline. A sparse population is confined to small settlements along certain sectors of the coast. Greenland possesses the world's second largest ice sheet. Greenland sits atop the Greenland plate, a subplate of the North American plate. The Greenland craton is made up of some of"
"of the Humboldt Glacier. Kane Basin Kane Basin (; ) 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 Elisha Kane, whose expedition in search of the lost Franklin 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,"
"Ammarqua Strait Ammarqua Strait (old spelling: ""Angmarqua"") is a strait in the southern part of the Upernavik Archipelago in the Qaasuitsup municipality in northwestern Greenland. The strait separates Nutaarmiut Island from four large islands in the east, Uilortussoq Island and Saninngassoq Island in the north; Nako Island and Akuliaruseq Island in the south. The Eqalugaarsuit Suulluat Fjord opens into Ammarqua Strait immediately to the east of the southern cape, to the north of Kangeq Peninsula off the mainland of Greenland. At the southern mouth of the strait at the confluence with Baffin Bay are two islands: the Ineraq Island and"
"Øresund Øresund or Öresund (, ; , ), commonly known in English as the Sound, is a strait which forms the Danish–Swedish border, separating Zealand (Denmark) from Scania (Sweden). The strait has a length of and the width varies from to . It is wide at its narrowest point between Helsingør in Denmark and Helsingborg in Sweden. Øresund is along with the Great Belt, Little Belt and Kiel Canal one of four waterways that connects the Baltic Sea to the Atlantic Ocean via Kattegat, Skagerrak, and the North Sea, and is one of the busiest waterways in the world. The"
"Greenland Sea and Labrador Sea. Countries bordering the Arctic Ocean are: Russia, Norway, Iceland, Greenland, Canada and the United States. There are several ports and harbors around the Arctic Ocean In Alaska, the main ports are Barrow () and Prudhoe Bay (). In Canada, ships may anchor at Churchill (Port of Churchill) () in Manitoba, Nanisivik (Nanisivik Naval Facility) () in Nunavut, Tuktoyaktuk () or Inuvik () in the Northwest Territories. In Greenland, the main port is at Nuuk (Nuuk Port and Harbour) (). In Norway, Kirkenes () and Vardø () are ports on the mainland. Also, there is Longyearbyen"
"the double Singarnaq-Annertussoq Island, as well as smaller skerries. Ammarqua Strait Ammarqua Strait (old spelling: ""Angmarqua"") is a strait in the southern part of the Upernavik Archipelago in the Qaasuitsup municipality in northwestern Greenland. The strait separates Nutaarmiut Island from four large islands in the east, Uilortussoq Island and Saninngassoq Island in the north; Nako Island and Akuliaruseq Island in the south. The Eqalugaarsuit Suulluat Fjord opens into Ammarqua Strait immediately to the east of the southern cape, to the north of Kangeq Peninsula off the mainland of Greenland. At the southern mouth of the strait at the confluence with"
"of its natural resources, the grant will gradually be diminished. This is generally considered to be a step toward eventual full independence from Denmark. Greenlandic was declared the sole official language of Greenland at the historic ceremony. Greenland is the world's largest non-continental island and the third largest country in North America. It is between latitudes 59° and 83°N, and longitudes 11° and 74°W. The Atlantic Ocean borders Greenland's southeast; the Greenland Sea is to the east; the Arctic Ocean is to the north; and Baffin Bay is to the west. The nearest countries are Canada, to the west and"
"that is at the core of the North American continent. Greenland was formed in two rifting stages from the main body of North America. The first, during the Cretaceous period formed Baffin Bay. Baffin Bay is the northwestern extension and terminus of the North Atlantic-Labrador Sea rift system that started forming 140 million years ago in the Early Cretaceous epoch. The Labrador Sea started opening 69 million years ago during the Maastrichtian age but seafloor spreading appears to have ceased by the Oligocene epoch, 30–35 million years ago. Correlations between tectonic units in Canada and Greenland have been proposed, however,"
"Great Belt The Great Belt () is a strait between the major islands of Zealand (""Sjælland"") and Funen (""Fyn"") in Denmark. It is one of the three Danish Straits. Effectively dividing Denmark in two, the Belt was served by the Great Belt ferries from the late 19th century until the islands were connected by the Great Belt Fixed Link in 1997–98. The Great Belt is the largest and most important of the three Danish Straits that connect the Baltic Sea to the Kattegat strait and Atlantic Ocean. The others are the Øresund and the Little Belt straits. The Great Belt"
"East Greenland Current The East Greenland Current (EGC) is a cold, low salinity current that extends from Fram Strait (~80N) to Cape Farewell (~60N). The current is located off the eastern coast of Greenland along the Greenland continental margin. The current cuts through the Nordic Seas (the Greenland and Norwegian Seas) and through the Denmark Strait. The current is of major importance because it directly connects the Arctic to the Northern Atlantic, it is a major contributor to sea ice export out of the Arctic, and it is a major freshwater sink for the Arctic. The EGC is composed of"
"Disagreement over the passages' status has raised Canadian concerns about environmental enforcement, national security, and general sovereignty. Hans Island, in the Nares Strait east of Ellesmere Island, is a territory currently contested between Canada and Denmark. The archipelago extends some longitudinally and from the mainland to Cape Columbia, the northernmost point on Ellesmere Island. It is bounded on the west by the Beaufort Sea; on the northwest by the Arctic Ocean; on the east by Greenland, Baffin Bay and Davis Strait; and on the south by Hudson Bay and the Canadian mainland. The various islands are separated from each other"
"width of the Fram Strait is what allows for both inflow and outflow on the Atlantic side of the Arctic Ocean. Because of this, it is influenced by the Coriolis force, which concentrates outflow to the East Greenland Current on the western side and inflow to the Norwegian Current on the eastern side. Pacific water also exits along the west coast of Greenland and the Hudson Strait (1–2 Sv), providing nutrients to the Canadian Archipelago. As noted, the process of ice formation and movement is a key driver in Arctic Ocean circulation and the formation of water masses. With this"
"is number three with ca. 5,000 inhabitants. See Cartographic expeditions to Greenland Geography of Greenland Greenland is located between the Arctic Ocean and the North Atlantic Ocean, northeast of Canada and northwest of Iceland. The territory comprises the island of Greenland–the largest island in the world–and more than a hundred other smaller islands (see ). As an island, Greenland has no land boundaries and 44,087 km of coastline. A sparse population is confined to small settlements along certain sectors of the coast. Greenland possesses the world's second largest ice sheet. Greenland sits atop the Greenland plate, a subplate of the"
"in the Arctic and are opposed by the European Union and the U.S. This is especially important with the Northwest Passage. Canada asserts control of this passage as part of the Canadian Internal Waters because it is within of Canadian islands; the U.S. claims that it is in international waters. Today ice and freezing temperatures make this a minor issue, but climate change may make the passage more accessible to shipping, something that concerns the Canadian government and inhabitants of the environmentally sensitive region. Similarly, the disputed Hans Island (with Denmark), in the Nares Strait, which is west of Greenland,"
"melt and precipitation in the central Greenland Sea. East Greenland Current The East Greenland Current (EGC) is a cold, low salinity current that extends from Fram Strait (~80N) to Cape Farewell (~60N). The current is located off the eastern coast of Greenland along the Greenland continental margin. The current cuts through the Nordic Seas (the Greenland and Norwegian Seas) and through the Denmark Strait. The current is of major importance because it directly connects the Arctic to the Northern Atlantic, it is a major contributor to sea ice export out of the Arctic, and it is a major freshwater sink"
"Grønsund Grønsund is a strait in Denmark separating the island Falster from the islands Møn and Bogø. Grønsund's maximum depth is at approx. 20 metres and the width is between 1 - 4 km. Storstrømmen channel is situated to the west and Stege Bugt lies to the north between Zealand and Møn. A ferry crosses the channel in the summertime from Stubbekøbing to Bogø island. Grønsund has several shallow areas, i.e. near Bogø, and has a strong and alternating current. Both submersed and riparian vegetation is rich, and the sound is an important breeding area for wildlife and fish. Many"
"Øresund, Sweden carried out two great projects, the foundation of Göteborg (Gothenborg) in 1621 and the construction of the Göta Canal from 1810 to 1832. The Copenhagen Convention of 1857 abolished the Dues and made the Danish straits an international waterway. A fixed connection was opened across the strait in 2000, the Øresund Bridge. Øresund Øresund or Öresund (, ; , ), commonly known in English as the Sound, is a strait which forms the Danish–Swedish border, separating Zealand (Denmark) from Scania (Sweden). The strait has a length of and the width varies from to . It is wide at"
"Nares Strait in the early 13th century, where they hunted with and traded with Vikings. Archeological remains of Thule Culture and Viking presence are found on Ruin Island. Missing 'Ice Arches' Contributed to 2007 Arctic Ice Loss Nares Strait Nares Strait (; ) is a waterway between Ellesmere Island and Greenland that is the northern part of Baffin Bay where it meets the Lincoln Sea. From south to north, the strait includes Smith Sound, Kane Basin, Kennedy Channel, Hall Basin and Robeson Channel. During 1962–64 a 20 km by 10 km ice island drifted southward from the Lincoln Sea through"
"in winter carrying mail and passengers before the era of ice breaking ferries. Northumberland Strait The Northumberland Strait (French: ""détroit de Northumberland"") is a strait in the southern part of the Gulf of Saint Lawrence in eastern Canada. The strait is formed by Prince Edward Island and the gulf's eastern, southern and western shores. The western boundary of the strait is delineated by a line running between North Cape, Prince Edward Island and Point Escuminac, New Brunswick while the eastern boundary is delineated by a line running between East Point, Prince Edward Island and Inverness, Nova Scotia. The Northumberland Strait"
"Greenland. On April 27, 2010, Norway and Russia announced an end to their 40-year arctic demarcation dispute in the Barents Sea. Future joint energy development is expected. Maritime boundaries between Canada and the United States in the Beaufort Sea and between Canada and Denmark in Baffin Bay remain under dispute. Denmark (Greenland), Russia and Canada may have competing extended continental shelf claims over the Lomonosov Ridge, an underwater mountain chain crossing the central Arctic basin. Global warming has had a greater impact on summer sea ice in the Arctic than previously estimated. Based on the recent studies, the Arctic will"
"an extensive fjord system. Although the eastern shore is more regular, it includes the Petermann Fjord of the Petermann Glacier at its southern end. Hall Basin Hall Basin is an Arctic waterway between Hall Land in Greenland to the west and Canada's northernmost island to the east, Ellesmere Island. Hall Basin is named after American polar explorer Charles Francis Hall. Hall Basin is located in Nares Strait with its entrance between Cape Baird on the eastern coast of Ellesmere Island and Cape Morton on the northwestern coast of Greenland. Robeson Channel is to the north of the basin, and Kennedy"
"financial losses. An alternative between Greenland and the United States/Canada is Air Iceland/Icelandair with a plane change in Iceland. Sea passenger and freight transport is served by the coastal ferries operated by Arctic Umiaq Line. It makes a single round trip per week, taking 80 hours each direction. Greenland has a population of 56,370 (January 2013 estimate), of whom 88% are Greenlandic Inuit (including mixed persons). The remaining 12% are of European descent, mainly Greenland Danes. Several thousand Greenlandic Inuit reside in the Danish Peninsula. The majority of the population is Lutheran. Nearly all Greenlanders live along the fjords in"
"Ikerasaa Strait Ikerasaa Strait (old spelling: ""Ikerasâ"") is a strait in the Upernavik Archipelago in the Qaasuitsup municipality in northwestern Greenland. The strait separates Kiatassuaq Island in the north from the mainland Sanningassorsuaq Peninsula in the south. The name of the strait is the local dialect version of ""ikerasak"", a generic word for 'strait' in the Greenlandic language. The strait is long and at most wide. Located in the northern part of Upernavik Archipelago, it is an inner waterway of Inussulik Bay, linking it with Alison Bay in the northeast. In the northwest, the strait is bounded by the mountainous"
"Hans Island Hans Island (; ; ; ) is a small, uninhabited barren knoll measuring , long and wide, in the centre of the Kennedy Channel of Nares Strait—the strait that separates Ellesmere Island from northern Greenland and connects Baffin Bay with the Lincoln Sea. Hans Island is the smallest of three islands in Kennedy Channel; the others are Franklin Island and Crozier Island. The strait at this point is wide, placing the island within the territorial waters of both Canada and Greenland. A theoretical line in the middle of the strait goes through the island. The island has likely"
"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 shelves to the southwest, northwest, and northeast. It connects to the north with Baffin Bay through the Davis Strait. It has been described as 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"