Napasorsuaq
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Napasorsuaq
The Napasorsuaq ( da, Kirkespiret) is a 1,590m–high mountain in southern Greenland, in the Kujalleq municipality. Geography The mountain rises in the mountainous peninsula of the mainland which forms the eastern side of the Southern Sermilik fjord. It is the highest peak of a moderately glaciated mountain chain stretching in a SW/NE direction with summits reaching 1,400 m. The ''Kirkespirdalen Dal'' valley, named after the mountain, stretches westwards onto the Saqqa Fjord. The Napasorsuaq is a popular mountain among climbers because of its firm granite walls, similar to other peaks in the region such as Ketil and Ulamertorsuaq. See also *Big wall climbing *List of mountains in Greenland This is a list of mountains in Greenland. List For each mountain, the municipality in which it is located is given, along with coordinates indicating the approximate centre of the mountain (follow the link to see satellite images of the location ... References External linksKarsten Sech ...
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List Of Mountains In Greenland
This is a list of mountains in Greenland. List For each mountain, the municipality in which it is located is given, along with coordinates indicating the approximate centre of the mountain (follow the link to see satellite images of the location). Above 3000 m Above 2000 m Above 1000 m Other relevant mountains See also *List of mountain peaks of Greenland *List of mountain ranges of Greenland This is a list of mountain ranges of Greenland. List by alphabetical order *Alángup Qáqai, located in SW Disko Island *Albert Heim Range ''(Albert Heim Bjerge)'', located in northern Hudson Land, north of Promenadedal. *Alexandrine Range ' ... * List of nunataks of Greenland * List of Ultras of Greenland References Bibliography''Gazetteer of Greenland''Compiled by Per Ivar Haug. UBiT, Universitetsbiblioteket i Trondheim, August 2005, {{ISBN, 82-7113-114-1.Exploration and place names in Northeastern Greenland ...
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Southern Sermilik
Southern Sermilik ( da, Søndre Sermilik) is a fjord in southwestern Greenland. Administratively it is part of the Kujalleq municipality. Geography The fjord is oriented in a roughly NE/SW direction, to the southwest the Southern Sermilik Fjord opens into the Labrador Sea of the North Atlantic Ocean. It separates two long mountainous peninsulas, the mountains on the northwestern side of the fjord rising steeply from the shore to heights of over , and the 1,590 m high Napasorsuaq peak rising in the peninsula to the east of the fjord. The islands of Amitsok and Angmalortoq —the latter rising to a height of 1,253 m— lie at the mouth of the fjord. There are further islands beyond them, Sermersooq Island being the largest. The Sermeq Glacier at the inland end of this fjord has been undergoing a well documented recession in recent history. A similar retreat of the glacier at the fjord's head has been documented in neighbouring Tasermiut Fjord as well. Bibliography *Ivar Ha ...
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Ulamertorsuaq
The Ulamertorsuaq is a 1,858 m–high mountain in southern Greenland, in the Kujalleq municipality. Geography Together with Nalumasortoq and Ketil, this mountain rises in the mountainous peninsula of the mainland which forms the eastern side of the Tasermiut Fjord. The Ulamertorsuaq has four peaks with heights of 1858 m, 1843 m, 1829 m and 1825 m. The 1843 m high peak is a popular mountain among climbers because of its challenging West Side, a mighty perpendicular cliff. It is also favoured for its firm granite structure, similar to other summits in the region such as Ketil and Napasorsuaq, the latter located on the other side of the Tasermiut Fjord. See also *Big wall climbing *List of mountains in Greenland This is a list of mountains in Greenland. List For each mountain, the municipality in which it is located is given, along with coordinates indicating the approximate centre of the mountain (follow the link to see satellite images of the location ... Bibliography *Greenl ...
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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 ...
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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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Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Saqqa Fjord
Saqqa (also known as Limmu Saqqa) is a town in south-western Ethiopia, and capital of the former Kingdom of Limmu-Ennarea. Located in the Jimma Zone of the Oromia Region, this town has a latitude and longitude of . Based on figures from the Central Statistical Agency in 2005, this town has an estimated total population of 2,679 of whom 1,379 were men and 1,300 were women. The 1994 census reported this town had a total population of 1,497 of whom 748 were males and 749 were females. It is one of two towns in Limmu Sakka woreda. History Saqqa became a town of importance when king Abba Bagido made it his capital of Limmu-Ennarea in 1825, eclipsing his father's capital, Sappa. It thrived as the major marketplace of the Gibe region, where the different kinds of Muslim traders (known as Jabarti and Afkala) bought gold, coffee, and ivory. In the mid-to-late 1830s, Abba Bagibo forbade foreign merchants to travel beyond Saqqa, so merchants from Gondar, Adwa, Derita and Dawe we ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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Ketil (mountain)
The Ketil ( kl, Uiluit Qaqqaa, meaning "Shell Mountain") is a 2,010 m–high mountain in southern Greenland, in the Kujalleq municipality. Ketil's granite walls are similar to Tiningnertok's (Apostelen Tommelfinger), another massive peak in the east coast. Geography Together with Nalumasortoq and Ulamertorsuaq, Ketil is part of the group of three massive largely unglaciated rocky mountains rising in the peninsula of the mainland which forms the eastern side of the Tasermiut Fjord. In the same manner as its slightly lower neighbour Ulamertorsuaq, Ketil has become popular among mountain climbers owing to its higher than 1000 m sheer western granite wall. It is considered one of the most challenging Big Walls on Earth. This mountain is marked as a peak in some sources.Greenland Tourism: ''Hiking Map South Greenland/Tasermiut fjorden'' – Nanortalik. 1996 See also * Big wall climbing *List of mountains in Greenland This is a list of mountains in Greenland. List For each moun ...
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Big Wall Climbing
Big wall climbing is a type of rock climbing where a climber ascends a long multi-pitch route, normally requiring more than a single day to complete the climb. Big wall routes require the climbing team to live on the route often using portaledges and hauling equipment. It is practiced on tall or more vertical faces with few ledges and small cracks. History In the early 20th century, climbers were scaling big rock faces in the Dolomites and the European Alps employing free- and aid-climbing tactics to create bold ascents. Yet, the sheer walls were waiting to be climbed by future generations with better tools and methods. In addition, many nations in the early 1900s had specialized army units that had developed wall climbing skills for gaining surprise entry into enemy fortifications by wall climbing. In the early 1900s the Filipino Scouts, a US Army unit composed of Filipino enlisted and American officers, demonstrated their specialized skills by climbing the steep walls of ...
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