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Rhône Glacier
The Rhône Glacier (german: Rhonegletscher, Walliser German: ''Rottengletscher'', french: glacier du Rhône, it, ghiacciaio del Rodano) is a glacier in the Swiss Alps and the source of the river Rhône and one of the primary contributors to Lake Geneva in the far eastern end of the Swiss canton of Valais. Because the glacier is located close to the Furka Pass road it is easily accessible. Geography The Rhône Glacier is the largest glacier in the Urner Alps. It lies on the south side of the range at the source of the Rhône. The ''Undri Triftlimi'' (3,081 m) connects it to the Trift Glacier. The glacier is located on the northernmost part of the canton of Valais, between the Grimsel Pass and the Furka Pass and is part of the Oberwald municipality. The Dammastock (3,630 m) is the highest summit above the glacier. Evolution File:Rhone Glacier 2021.JPG, 2021 File:Rhonegletscher Sept-2018a.jpg, 2018 File:2010-10-10 Furka 035-by bohdan urbanowicz.jpg, 2010 File:Glacier du R ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tieralplistock
The Tieralplistock (3,383 m) is a mountain of the Urner Alps, located on the border between the Swiss cantons of Bern and Valais. It lies between the Trift Glacier The Trift Glacier (german: Triftgletscher) is a long glacier (2005) in the Urner Alps near Gadmen, in the extreme east of the canton Berne in Switzerland. Morphology In 1973 glacier was 5.75 km long, 3 km wide at the top and around 500 m w ... and the Rhone Glacier, just east of the lake of Gelmer. Between the Diechterhorn and the Tieralplistock is a slightly higher unnamed summit (3,388 m). References External links Tieralplistock on Hikr Mountains of the Alps Alpine three-thousanders Mountains of Switzerland Mountains of the canton of Bern Mountains of Valais Bern–Valais border {{Valais-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trift Glacier
The Trift Glacier (german: Triftgletscher) is a long glacier (2005) in the Urner Alps near Gadmen, in the extreme east of the canton Berne in Switzerland. Morphology In 1973 glacier was 5.75 km long, 3 km wide at the top and around 500 m wide at it tongue. Overall it covered an area of including glacier sides. Triftgletscher Gadmen, Schweizerisches Gletschermessnetz Since the end of the Little Ice Age, the Trift Glacier is shrinking. The valley in which lake '' Triftsee'' is today used to be filled by a large mass of ice well into the 20th century. In the 1990s small puddles of melt water began to form at the glacier tongue and gradually became larger. In the hot summer of 2003, the lake quickly grew and the glacier tongue sank into the melt water and dissolved in it, which led to a shrinkage of the glacier of more than 136 m within a year. Since 1861, the glacier has shrunk a total of 2771 meters. Tourist attractions At an altitude of 2520 meters above sea level i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of Valais
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] |
NASA Earth Observatory
NASA Earth Observatory is an online publishing outlet for NASA which was created in 1999. It is the principal source of satellite imagery and other scientific information pertaining to the climate and the environment which are being provided by NASA for consumption by the general public. It is funded with public money, as authorized by the United States Congress, and is part of the EOS Project Science Office located at Goddard Space Flight Center. , NASA Earth Observatory has won the Webby People's Voice Award in Education three times. There were a series of publicized images issued by the website in 2008, including imagery of clouds streaming over the Caspian Sea, dust storms curling off the coast of Morocco, the crumbling of the Wilkins Ice Shelf, Hurricane Bertha, and others. See also * Earth observation ** Earth observation satellite * Space exploration Space exploration is the use of astronomy and space technology to explore outer space. While the exploration ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Retreat Of Glaciers Since 1850
The retreat of glaciers since 1850 affects the availability of fresh water for irrigation and domestic use, mountain recreation, animals and plants that depend on glacier-melt, and, in the longer term, the level of the oceans. Deglaciation occurs naturally at the end of ice ages, but glaciologists find the current glacier retreat is accelerated by the measured increase of atmospheric greenhouse gases—an effect of climate change. Mid-latitude mountain ranges such as the Himalayas, Rockies, Alps, Cascades, Southern Alps, and the southern Andes, as well as isolated tropical summits such as Mount Kilimanjaro in Africa, are showing some of the largest proportionate glacial losses. Excluding peripheral glaciers of ice sheets, the total cumulated global glacial losses over the 26 year period from 1993–2018 were likely 5500 gigatons, or 210 gigatons per yr.Fox-Kemper, B., H.T. Hewitt, C. Xiao, G. Aðalgeirsdóttir, S.S. Drijfhout, T.L. Edwards, N.R. Golledge, M. Hemer, R.E. Kopp, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers
A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Glaciers by continent Africa Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Current ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers In Switzerland
A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union club Other uses * Angle of list, the leaning to either port or starboard of a ship * List (information), an ordered collection of pieces of information ** List (abstract data type), a method to organize data in computer science * List on Sylt, previously called List, the northernmost village in Germany, on the island of Sylt * ''List'', an alternative term for ''roll'' in flight dynamics * To ''list'' a building, etc., in the UK it means to designate it a listed building that may not be altered without permission * Lists (jousting), the barriers used to designate the tournament area where medieval knights jousted * ''The Book of Lists'', an American series of books with unusual lists See also * The List (other) * Listing ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dammastock
The Dammastock (3,630 m) is the highest mountain in the Urner Alps in Switzerland and is part of the Winterberg massif. Its summit ridge forms the border between the cantons of Uri and the Valais. It is the highest summit in the canton of Uri. The tripoint between the cantons of Berne, Valais and Uri lies near the Eggstock, north of the Dammastock. Politically, the Dammastock is split between the municipalities of Göschenen (Uri) and Obergoms (Valais). The massif is almost completely covered by ice, the large Rhone Glacier on the west side, the smaller Damma Glacier on the east side and the Trift Glacier further on the north side. It was first climbed by Albert Hoffmann-Burkhardt with guides Johann Fischer and Andreas von Weissenfluh on 28 July 1864. Huts *Dammastock Hut (2,445 m) *Hotel Tiefenbach (2,109 m) See also *List of mountains of Uri This is a list of mountains of the Swiss canton of Uri. Uri is a very mountainous canton and lies entirely within the Alps ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oberwald VS .
Oberwald is a village in the municipality of Obergoms in Goms District in the canton of Valais in Switzerland. It is situated at an elevation of 1,377 m and had a population of 277 in December 2007. It is located at the end of the Goms, directly before the Furka and Grimsel passes, underneath the Rhône River source at the Rhône Glacier. It is also the startpoint of the Furka Tunnel. Most inhabitants live off tourism or sheep farming. Oberwald was an independent municipality until January 1, 2009, when it merged with Ulrichen and Obergesteln to form the municipality of Obergoms Obergoms is the upper part of the Goms and a municipality in the district of Goms in the canton of Valais in Switzerland. It was formed on 1 January 2009 when the three municipalities Ulrichen, Obergesteln and Oberwald merged. References External links * http://www.oberwald.ch {{Authority control[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grimsel Pass
The Grimsel Pass (german: Grimselpass; french: Col du Grimsel; it, Passo del Grimsel) is a mountain pass in Switzerland, crossing the Bernese Alps at an elevation of . The pass connects the Haslital, the upper valley of the river Aare, with the upper valley of the Rhône. In so doing, and as the Aare is a tributary of the Rhine, the pass crosses the continental divide between the North Sea and the Mediterranean Sea. A paved road follows the pass, running from Gletsch to Meiringen. The road is normally closed between October and May, due to the high snowfall on the pass. As it is the only direct road pass between the cantons of Bern and Valais across the Bernese Alps, attempts are made to keep the road open as long as possible with snow ploughs. A PostBus Switzerland service uses the pass several times a day, connecting Meiringen and Oberwald. The Grimsel Pass road is part of the Aare Route, which is national cycle route 8 of Switzerland. It has been used on sever ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Urner Alps
The Uri Alps (also known as ''Urner Alps'', german: Urner Alpen) are a mountain range in Central Switzerland and part of the Western Alps. They extend into the cantons of Obwalden, Valais, Bern, Uri and Nidwalden and are bordered by the Bernese Alps (Grimsel Pass) and the Emmental Alps to the west (the four lakes: Lungerersee, Sarnersee, Wichelsee, and Alpnachersee), the Schwyzer Alps to the north (Lake Lucerne), the Lepontine Alps to the south (the valley of Urseren with Andermatt) and the Glarus Alps to the east ( Reuss). The Uri Alps are composed of two distinct groups separated by the Susten Pass. The Dammastock massif on the south is the most glaciated part while the northern part, which culminates on Titlis, has lower summits but greater extent. Geography The group south of the Susten Pass forms the dividing range between the head waters of the Aare (west) from those of the Reuss. In addition a small portion of the range (south-west) is located in the basin of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
