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Rink Glacier
Rink Glacier ( da, Rink Isbræ; kl, Kangilliup Sermia) is a glacier in Avannaata, Greenland. This glacier is named in honor of Hinrich Johannes Rink, Danish geologist and Greenlandic researcher. Geography The Rink Glacier is the largest glacier on the west coast of Greenland. Its terminus is in the Karrat Fjord, Nordost Bay, Baffin Bay, North Atlantic Ocean. It drains an area of of the Greenland Ice Sheet with a flux (quantity of ice moved from the land to the sea) of per year, as measured for 1996. As reported by Anker Weidick and Ole Bennike in 2007, it is ranked second or third in iceberg production in western Greenland. It is also the swiftest moving and highest surface ice in the world. See also *List of glaciers in Greenland This is a list of glaciers in Greenland. Details on the size and flow of some of the major Greenlandic glaciers are listed by Eric Rignot and Pannir Kanagaratnam (2006) Ice sheets and caps *Greenland Ice Sheet * Christian Erichsen Ice Cap * Fla ...
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Avannaata
Avannaata (, da, Det Nordlige, lit=The Northern) is a municipality of Greenland created on 1 January 2018 from the bulk of the former Qaasuitsup municipality. It encompasses an area of 522,700 km2 and has 10,726 inhabitants. Geography In the south, Avannaata is flanked by the Qeqertalik municipality. In the southeast, it is bordered by the Sermersooq municipality, however this border runs north–south ( 45° West meridian) through the center of the Greenland ice sheet ( kl, Sermersuaq), and as such is free of traffic. In the east and northeast it is bordered by the Northeast Greenland National Park. At the southern end of the municipal coastline are the waters of Disko Bay, although some Disko Bay communities belong to the municipality of Qeqertalik. This bay is an inlet of the larger Baffin Bay, which to the north edges into the island of Greenland in the form of Melville Bay. The coastline of northeastern Baffin Bay is dotted with islands of the Upernavik Archipela ...
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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'', ...
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Karrat Fjord
Karrat Fjord ( da, Karrats Fjord) is a fjord in Avannaata municipality in western Greenland. Geography Karrat Fjord has its mouth in the Nordost Bay of the Baffin Bay. The head of the fjord is formed by a number of tributaries, including the Rink Glacier, Ingia Glacier and Umiamako Glacier fjords, as well as the Ukkusissat Fjord. The fjord heads to the southwest, with the islands of Qeqertarsuaq Island (Karrat Fjord), Illorsuit Island and Upernivik Island near its mouth.Google Earth See also *List of fjords of Greenland This is a list of the most important fjords of Greenland:In Northern Greenland, a large area made up entirely of fjords; therefore Peary Land above not a fjord but a fjord area.In Northeastern Greenland, a large area made up entirely of fjor ... References Fjords of Greenland {{Greenland-fjord-stub ...
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Baffin Bay
Baffin Bay ( Inuktitut: ''Saknirutiak Imanga''; kl, Avannaata Imaa; french: Baie de Baffin), located between Baffin Island and the west coast of Greenland, is defined by the International Hydrographic Organization as a marginal sea of the Arctic Ocean. It is sometimes considered a sea of the North Atlantic Ocean. It is connected to the Atlantic via Davis Strait and the Labrador Sea. The narrower Nares Strait connects Baffin Bay with the Arctic Ocean. The bay is not navigable most of the year because of the ice cover and high density of floating ice and icebergs in the open areas. However, a polynya of about , known as the North Water, opens in summer on the north near Smith Sound. Most of the aquatic life of the bay is concentrated near that region. Extent The International Hydrographic Organization defines the limits of Baffin Bay as follows: History The area of the bay has been inhabited since  BC. Around AD 1200, the initial Dorset settlers were replaced by ...
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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 ...
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Glacier
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#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, 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 lati ...
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Hinrich Johannes Rink
Dr. Hinrich Johannes Rink (first name sometimes as Henrik) (26 August 1819 – 15 December 1893) was a Danish geologist, one of the pioneers of glaciology, and the first accurate describer of the inland ice of Greenland. Rink, who first came to Greenland in 1848, spent 16 winters and 22 summers in the Arctic region, and became notable for Greenland's development. Becoming a Greenlandic scholar and administrator, he served as Royal Inspector of South Greenland and went on to become Director of the Royal Greenland Trading Department. With "Forstanderskaber", Rink introduced the first steps towards Greelandic home rule. Rink carried out and printed in four volumes the first systematic collection of Greenlandic oral tradition stories. He was the founder of '' Atuagagdliutit'', the first Kalaallisut language newspaper. Early years Rink was born in Copenhagen to Holstein parents. His father was Johannes Rink (1783–1865), a Kiel, Germany merchant, and his mother was Agnese Margare ...
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Danish People
Danes ( da, danskere, ) are a North Germanic ethnic group and nationality native to Denmark and a modern nation identified with the country of Denmark. This connection may be ancestral, legal, historical, or cultural. Danes generally regard themselves as a nationality and reserve the word "ethnic" for the description of recent immigrants, sometimes referred to as "new Danes". The contemporary Danish national identity is based on the idea of "Danishness", which is founded on principles formed through historical cultural connections and is typically not based on racial heritage. History Early history Denmark has been inhabited by various Germanic peoples since ancient times, including the Angles, Cimbri, Jutes, Herules, Teutones and others. The first mentions of " Danes" are recorded in the mid-6th century by historians Procopius ( el, δάνοι) and Jordanes (''danī''), who both refer to a tribe related to the Suetidi inhabiting the peninsula of Jutland, the province of Sc ...
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Geologist
A geologist is a scientist who studies the solid, liquid, and gaseous matter that constitutes Earth and other terrestrial planets, as well as the processes that shape them. Geologists usually study geology, earth science, or geophysics, although backgrounds in physics, chemistry, biology, and other sciences are also useful. Field research (field work) is an important component of geology, although many subdisciplines incorporate laboratory and digitalized work. Geologists can be classified in a larger group of scientists, called geoscientists. Geologists work in the energy and mining sectors searching for natural resources such as petroleum, natural gas, precious and base metals. They are also in the forefront of preventing and mitigating damage from natural hazards and disasters such as earthquakes, volcanoes, tsunamis and landslides. Their studies are used to warn the general public of the occurrence of these events. Geologists are also important contributors to climate ch ...
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Glacier Terminus
A glacier terminus, toe, or snout, is the end of a glacier at any given point in time. Although glaciers seem motionless to the observer, in reality glaciers are in endless motion and the glacier terminus is always either advancing or retreating. The location of the terminus is often directly related to glacier mass balance, which is based on the amount of snowfall which occurs in the accumulation zone of a glacier, as compared to the amount that is melted in the ablation zone. The position of a glacier terminus is also impacted by localized or regional temperature change over time. Tracking Tracking the change in location of a glacier terminus is a method of monitoring a glacier's movement. The end of the glacier terminus is measured from a fixed position in neighboring bedrock periodically over time. The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of trac ...
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Nordost Bay
Nordost Corporation is an American high-end audio company founded in 1991 by Joe Reynolds and based in Holliston, Massachusetts. Nordost manufactures and sells audio and video cables, interconnects and unique accessories to the audiophile market and is distributed in 72 countries. Overview Nordost was founded in Massachusetts in 1991. Nordost manufactures audio cables, power distribution systems, grounding systems and resonance control devices for the high-end market. Their original Flatline cable was the first flat loudspeaker cable to use FEP (Fluorinated Ethene Propylene). All Nordost cables use a flexible FEP insulation originally developed by DuPont. All Nordost products are manufactured at their facilities in the USA. Nordost produces five ranges of cable products (Lifestyle, Leif, Norse 2, Valhalla 2, Odin Supreme Reference). In addition to power cables and interconnect cable, digital cable and loudspeaker the company also manufactures the QRT line of products. pow ...
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Greenland Ice Sheet
The Greenland ice sheet ( da, Grønlands indlandsis, kl, Sermersuaq) is a vast body of ice covering , roughly near 80% of the surface of Greenland. It is sometimes referred to as an ice cap, or under the term ''inland ice'', or its Danish equivalent, ''indlandsis''. An acronym, GIS, is frequently used in the scientific literature. It is the second largest ice body in the world, after the Antarctic ice sheet. The ice sheet is almost long in a north–south direction, and its greatest width is at a latitude of 77°N, near its northern margin. The average thickness is about and over at its thickest point. In addition to the large ice sheet, smaller ice caps (such as Maniitsoq and Flade Isblink) as well as glaciers, cover between around the periphery. The Greenland ice sheet is adversely affected by climate change. It is more vulnerable to climate change than the Antarctic ice sheet because of its position in the Arctic, where it is subject to the regional amplification o ...
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