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Akuliaruseq Island
Akuliaruseq Island is an uninhabited island in the Avannaata municipality in northwestern Greenland. Geography Location within the archipelago Akuliaruseq Island is located in the southern part of the Upernavik Archipelago, in the group between Nunavik Peninsula in the south, and Upernavik Icefjord in the north.''Upernavik'', Saga Map, Tage Schjøtt, 1992 In the west, Ammarqua Strait separates Akuliaruseq Island from Nutaarmiut Island, the largest island in the archipelago. A small, unnamed channel branching to the east off Ammarqua separates the island from Nako Island in the north. In the east, the narrow Torsukattak Strait separates Akuliaruseq from Amarortalik Island. The long Eqalugaarsuit Sulluat Fjord separates the island from the large Kangeq Peninsula in the south. The southern coastline is indented by a small ''Puugutaata Ilua'' bay branching off the fjord. It is the only indentation in the otherwise undeveloped coastline of the island. Topography Like all ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upernavik Archipelago
Upernavik Archipelago is a vast coastal archipelago in the Avannaata municipality in northwestern Greenland, off the shores of northeastern Baffin Bay. The archipelago extends from the northwestern coast of Sigguup Nunaa peninsula in the south at approximately Nunavik, Saga Map, 1:250.000, Tage Schjøtt, 1992 to the southern end of Melville Bay ( kl, Qimusseriarsuaq) in the north at approximately .Upernavik Avannarleq, Saga Map, 1:250.000, Tage Schjøtt, 1992 History The archipelago belongs to the earliest-settled areas of Greenland, the first migrants arriving approximately 2,000 BCE. All southbound migrations of the Inuit passed through the area, leaving behind a trail of archeological sites. The early Saqqaq culture diminished in importance around 1,000 BCE, followed by the migrants of Dorset culture, who spread alongside the coast of Baffin Bay, being in turn displaced by the Thule people in the 13th and 14th centuries. The area has been continuously inhabited since then. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eqalugaarsuit Sulluat Fjord
Eqalugaarsuit (old spelling: ''Eqalugârssuit'') is a settlement in the Kujalleq municipality in southern Greenland, located southeast of Qaqortoq and northwest of Alluitsup Paa. Its population was 49 in 2020. Until January, 2009, the settlement—along Qassimiut and Saarloq, as well as 13 sheep farms—belonged to the Qaqortoq municipality. On January 1, 2009, the settlement became part of the Kujalleq municipality, when the Narsaq, Qaqortoq, and Nanortalik municipalities ceased to exist. The settlements are presently governed by a joint settlement council. Economy The main occupations are hunting and fishing. There are currently plans of introducing muskox to the surrounding area, as a source of food and traditional hide, called ''qiviut'', and as a tourist attraction. Infrastructure The settlement has two general stores, operated by KNI. There is also a church, a service house, and a home for the elderly. The settlement has its own school--''Daanialiup atuarfia''—prese ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Islands Of The Upernavik Archipelago
An island or isle is a piece of subcontinental land completely surrounded by water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges Delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental islands and oceanic islands. There are also artificial islands (man-made islands). There are about 900,000 official islands in the world. This number consists of all the officially-reported islands of each country. The total number of islands in the world is unknown. There may be hundreds of thousands of tiny islands that are unknown and uncounted. The number of sea islands in the world is estimated to be more than 200,000. The t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Uninhabited Islands Of Greenland
The list of uninhabited regions includes a number of places around the globe. The list changes year over year as human beings migrate into formerly uninhabited regions, or migrate out of formerly inhabited regions. List As a group, the list of uninhabited places are called the "nonecumene". This is a special geography term which means the uninhabited area of the world. * Virtually all of the Ocean *Virtually all of Antarctica *Most of The Arctic *Most of Greenland *Most of The Sahara * Antipodes Islands * Ashmore and Cartier Islands * Bajo Nuevo Bank * Baker Island * Ball's Pyramid * Balleny Islands * Big Major Cay * Bouvet Island * Much of the interior of Brazil * Caroline Island * Clipperton Island * The semi-arid regions and deserts of Australia * Devon Island * Much of Eastern Oregon * Elephant Island * Elobey Chico * Ernst Thälmann Island * Much of Fiordland, New Zealand * Goa Island * Gough Island * Hans Island * Harmil * Hashima Island * Hatutu * Heard Island and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediments
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Campanian
The Campanian is the fifth of six ages of the Late Cretaceous Epoch on the geologic timescale of the International Commission on Stratigraphy (ICS). In chronostratigraphy, it is the fifth of six stages in the Upper Cretaceous Series. Campanian spans the time from 83.6 (± 0.2) to 72.1 (± 0.2) million years ago. It is preceded by the Santonian and it is followed by the Maastrichtian. The Campanian was an age when a worldwide sea level rise covered many coastal areas. The morphology of some of these areas has been preserved: it is an unconformity beneath a cover of marine sedimentary rocks. Etymology The Campanian was introduced in scientific literature by Henri Coquand in 1857. It is named after the French village of Champagne in the department of Charente-Maritime. The original type locality was a series of outcrop near the village of Aubeterre-sur-Dronne in the same region. Definition The base of the Campanian Stage is defined as a place in the stratigraphic column wher ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albian
The Albian is both an age of the geologic timescale and a stage in the stratigraphic column. It is the youngest or uppermost subdivision of the Early/Lower Cretaceous Epoch/Series. Its approximate time range is 113.0 ± 1.0 Ma to 100.5 ± 0.9 Ma (million years ago). The Albian is preceded by the Aptian and followed by the Cenomanian. Stratigraphic definitions The Albian Stage was first proposed in 1842 by Alcide d'Orbigny. It was named after Alba, the Latin name for River Aube in France. A Global Boundary Stratotype Section and Point (GSSP), ratified by the IUGS in 2016, defines the base of the Albian as the first occurrence of the planktonic foraminiferan '' Microhedbergella renilaevis'' at the Col de Pré-Guittard section, Arnayon, Drôme, France. The top of the Albian Stage (the base of the Cenomanian Stage and Upper Cretaceous Series) is defined as the place where the foram species '' Rotalipora globotruncanoides'' first appears in the stratigraphic column. The Albia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precambrian
The Precambrian (or Pre-Cambrian, sometimes abbreviated pꞒ, or Cryptozoic) is the earliest part of Earth's history, set before the current Phanerozoic Eon. The Precambrian is so named because it preceded the Cambrian, the first period of the Phanerozoic Eon, which is named after Cambria, the Latinised name for Wales, where rocks from this age were first studied. The Precambrian accounts for 88% of the Earth's geologic time. The Precambrian is an informal unit of geologic time, subdivided into three eons ( Hadean, Archean, Proterozoic) of the geologic time scale. It spans from the formation of Earth about 4.6 billion years ago ( Ga) to the beginning of the Cambrian Period, about million years ago ( Ma), when hard-shelled creatures first appeared in abundance. Overview Relatively little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth's history, and what is known has largely been discovered from the 1960s onwards. The Precambrian fossil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isthmus
An isthmus (; ; ) is a narrow piece of land connecting two larger areas across an expanse of water by which they are otherwise separated. A tombolo is an isthmus that consists of a spit or bar, and a strait is the sea counterpart of an isthmus. Isthmus vs land bridge vs peninsula ''Isthmus'' and ''land bridge'' are related terms, with isthmus having a broader meaning. A land bridge is an isthmus connecting Earth's major landmasses. The term ''land bridge'' is usually used in biogeology to describe land connections that used to exist between continents at various times and were important for migration of people and various species of animals and plants, e.g. Beringia and Doggerland. An isthmus is a land connection between two bigger landmasses, while a peninsula is rather a land protrusion which is connected to a bigger landmass on one side only and surrounded by water on all other sides. Technically, an isthmus can have canals running from coast to coast (e.g. the Panama ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kangeq Peninsula
Kangeq Peninsula is a peninsula of Greenland. It is located in the Upernavik Archipelago Upernavik Archipelago is a vast coastal archipelago in the Avannaata municipality in northwestern Greenland, off the shores of northeastern Baffin Bay. The archipelago extends from the northwestern coast of Sigguup Nunaa peninsula in the south at .... The Kangerlussuaq Fjord (Kangeq Peninsula) cuts across the peninsula in a north–south direction. References Peninsulas of the Upernavik Archipelago {{Greenland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amarortalik Island
Amarortalik Island is an uninhabited island in Avannaata municipality in northwestern Greenland. The name of the island means "''the place of wolves''" in the Greenlandic language. Geography Location within the archipelago Amarortalik Island is located in the southern part of the Upernavik Archipelago, in the group between Nunavik Peninsula in the south, and Upernavik Icefjord in the north.''Upernavik'', Saga Map, Tage Schjøtt, 1992 In the west, the narrow Torsukattak Strait separates Amarortalik from Akuliaruseq Island. In the north, the small ''Kangerluarsuk Fjord'' separates it from Kangerluarsup Nunaa Peninsula, a peninsula branching off to the west from Koch's Land on the mainland of Greenland. Koch's land in turn is separated from Amarortalik by a small, unnamed strait. The long Eqalugaarsuit Sulluat Fjord separates the island from the large Kangeq Peninsula in the south. Topography Like all larger islands in the neighborhood, Amarortalik Island is very mountain ... [...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] |
