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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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
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] |
GoogleEarth
Google Earth is a computer program that renders a 3D representation of Earth based primarily on satellite imagery. The program maps the Earth by superimposing satellite images, aerial photography, and GIS data onto a 3D globe, allowing users to see cities and landscapes from various angles. Users can explore the globe by entering addresses and coordinates, or by using a keyboard or mouse. The program can also be downloaded on a smartphone or tablet, using a touch screen or stylus to navigate. Users may use the program to add their own data using Keyhole Markup Language and upload them through various sources, such as forums or blogs. Google Earth is able to show various kinds of images overlaid on the surface of the earth and is also a Web Map Service client. In 2019, Google has revealed that Google Earth now covers more than 97 percent of the world, and has captured 10 million miles of Street View imagery. In addition to Earth navigation, Google Earth provides a series of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tiningnertok
Tiningnertok ( da, Apostelen Tommelfinger, meaning 'Thumb of the Apostles in the New Testament, Apostle') is a mountain in King Frederick VI Coast, Kujalleq municipality, southern Greenland. This mountain is popular among mountaineers, especially its Northeast Face, but it is of difficult access for it lies in an isolated area where climatic conditions are often rough. Its granite walls are similar to Ketil (mountain), Ketil's. Geography Tiningnertok is a massive ultra-prominent mountain with multiple peaks at the top. It rises steeply from the shore east of small Tininnertooq Bay on the northern side of the middle section of Lindenow Fjord (Kangerlussuatsiaq), west of the mouth of the Nørrearm branch of the fjord. Akuliarusersuaq is another massive peak rising barely 3 km to the southeast at to a height of . History The history of mountaineering in Southeast Greenland began quite recently. In 1971 members of the French ''Club Alpin'' of Paris reached the base of the Apo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nalumasortoq
The Nalumasortoq or Naluumasortoq is a 2,045 meter high mountain in southern Greenland, in the Kujalleq municipality. Geography The mountain rises not far from Nanortalik, in the mountainous peninsula of the mainland which forms the eastern side of the Tasermiut Fjord. The Nalumasortoq closes an east-facing valley that lies between the Ulamertorsuaq and Ketil mountain peaks and with its 2,045 m it is the tallest peak of the group. Glaciers only appear below 1,600 meters in the east, NW and SW. Its massive western wall is especially popular among mountain climbers. In: |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Unglaciated
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 over many years, often centuries. It acquires distinguishing features, such as crevasses and 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 latitudes 35°N and 35°S, glaciers occur only in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasermiut Fjord
Tasermiut Fjord is a 70-kilometre-long fjord in southwestern Greenland. Administratively it is part of the Kujalleq municipality. Nanortalik Island is located near the mouth of the fjord. Tasermiut Fjord has some of the very few growths of dwarf trees in Greenland, notably in Qinngua Valley and Tiningnertoq valley. Geography The fjord is oriented in a roughly NE/SW direction, to the southwest the fjord opens into the Labrador Sea of the North Atlantic Ocean. It separates two long mountainous peninsulas, the 1,590 m high Napasorsuaq peak rising in the peninsula to the west of the fjord. To the east rise the 1,858 m high Ulamertorsuaq, the 2,045 m high Nalumasortoq and the 2,010 m high Ketil. The 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 the Sermeq Glacier in neighbouring Southern Sermilik Fjord as well. Tourism This fjord attracts ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
