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Oberaletsch Glacier
The Oberaletsch Glacier (German: ''Oberaletschgletscher'', meaning ''Upper Aletsch Glacier'') is a valley glacier on the south side of the Bernese Alps, in the canton of Valais. It had a length of with an average width of just under and an area of about in 1973. The Oberaletsch Glacier system consists of two approximately equal arms. The eastern one takes its starting point on the south western flank of the Aletschhorn at around , and joins the western arm (Beichgletscher) in the valley at the foot of the Nesthorn. Then the glacier flows to the south-east towards the Aletsch Glacier without reaching it. The glacier tongue ends at around . During the Little Ice Age in the middle of the 19th century the glacier was part of the Aletsch Glacier. The Swiss Alpine Club Oberaletschhütte () is above the junction of the two glacier arms and has been accessible to hikers since 2005 with a new trail from Belalp. The area of the Oberaletsch Glacier, along with the Aletsch Glacier, was dec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nesthorn
The Nesthorn is a mountain in the Bernese Alps. It is located in the Swiss canton of Valais north of Brig. The mountain lies between the Oberaletsch Glacier on the north and east side and the Gredetschtal on the south side. It is part of the subrange of the Bernese Alps that culminates at the Aletschhorn. The Nesthorn was first ascended from Belalp in 1865 by B. George and H. Mortimer, with Christian Almer and his son. Passing the base of the peak nearly to the head of the west branch of the Beich Firn (tributary of the Oberaletsch Glacier), they had on their left a steep iceslope, broken in five places by protruding masses of rock. Ascending the steep channel between the two masses nearest the Nesthorn they reached the ridge overlooking the Gredetschtal, turned to the left, and crossing a minor peak, and attained the summit in 6 hours, exclusive of halts. John Ball, ''The Alpine Guide: Central Alps'', 1869, p. 94 See also *List of mountains of Switzerland This article conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oberaletschhütte
The Oberaletsch Glacier (German: ''Oberaletschgletscher'', meaning ''Upper Aletsch Glacier'') is a valley glacier on the south side of the Bernese Alps, in the canton of Valais. It had a length of with an average width of just under and an area of about in 1973. The Oberaletsch Glacier system consists of two approximately equal arms. The eastern one takes its starting point on the south western flank of the Aletschhorn at around , and joins the western arm (Beichgletscher) in the valley at the foot of the Nesthorn. Then the glacier flows to the south-east towards the Aletsch Glacier without reaching it. The glacier tongue ends at around . During the Little Ice Age in the middle of the 19th century the glacier was part of the Aletsch Glacier. The Swiss Alpine Club Oberaletschhütte () is above the junction of the two glacier arms and has been accessible to hikers since 2005 with a new trail from Belalp. The area of the Oberaletsch Glacier, along with the Aletsch Glacier, was dec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swiss Alps
The Alpine region of Switzerland, conventionally referred to as the Swiss Alps (german: Schweizer Alpen, french: Alpes suisses, it, Alpi svizzere, rm, Alps svizras), represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, one of its three main physiographic regions. The Swiss Alps extend over both the Western Alps and the Eastern Alps, encompassing an area sometimes called Central Alps. While the northern ranges from the Bernese Alps to the Appenzell Alps are entirely in Switzerland, the southern ranges from the Mont Blanc massif to the Bernina massif are shared with other countries such as France, Italy, Austria and Liechtenstein. The Swiss Alps comprise almost all the highest mountains of the Alps, such as Dufourspitze (4,634 m), the Dom (4,545 m), the Liskamm (4,527 m), the Weisshorn (4,506 m) and the Matterhorn (4,478 m). The other following major summits can be found in this list of mountains of S ... [...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, G ... [...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. Currently, ... [...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 (di ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UNESCO World Heritage Site
A World Heritage Site is a landmark or area with legal protection by an international convention administered by the United Nations Educational, Scientific and Cultural Organization (UNESCO). World Heritage Sites are designated by UNESCO for having cultural, historical, scientific or other form of significance. The sites are judged to contain " cultural and natural heritage around the world considered to be of outstanding value to humanity". To be selected, a World Heritage Site must be a somehow unique landmark which is geographically and historically identifiable and has special cultural or physical significance. For example, World Heritage Sites might be ancient ruins or historical structures, buildings, cities, deserts, forests, islands, lakes, monuments, mountains, or wilderness areas. A World Heritage Site may signify a remarkable accomplishment of humanity, and serve as evidence of our intellectual history on the planet, or it might be a place of great natural beauty. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belalp
Belalp is a village and ski resort in the Swiss canton of Valais, situated at approximately above sea level in the municipality of Naters. Because of its altitude, Belalp is a vantage point offering views of the Dom and Fletschhorn mountains and other peaks of the Pennine and Lepontine Alps. Close to the village are the summits of Nesthorn, Hohstock and Sparrhorn mountains. Belalp is a car free village. It can be reached from Blatten bei Naters by cable car. With a length of , this rises and can carry a maximum of 740 passengers per hour. Notable residents The British and Irish physicist John Tyndall maintained a holiday home in the village from 1877. After his death in 1893, a memorial (the ''Tyndalldenkmal'') was erected at an elevation of on the mountain slopes above the village, and in sight of the Aletsch Glacier The Aletsch Glacier (german: Aletschgletscher, ) or Great Aletsch Glacier () is the largest glacier in the Alps. It has a length of about (2014), has about ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swiss Alpine Club
The Swiss Alpine Club (german: Schweizer Alpen-Club, french: Club Alpin Suisse, it, Club Alpino Svizzero, rm, Club Alpin Svizzer) is the largest mountaineering club in Switzerland. It was founded in 1863 in Olten and it is now composed of 111 sections with 160,000 members (2020). These include the Association of British Members of the Swiss Alpine Club. History The Swiss Alpine Club was the first Alpine club founded in continental Europe after the foundation of the Alpine Club (1857) in London. One of the founders and the first president of the Club was Dr. Melchior Ulrich; other members were Gottlieb Samuel Studer and Dr. Simler. The inaugural meeting was held in Olten. With the increasing number of climbers, steps had to be taken to make the approach to the mountains a little less complicated and exhausting. Until mountain huts were built, there had been no choice for the climbers other than sleeping in the highest chalets or in a Bivouac shelter under some overhanging ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valais
Valais ( , , ; frp, Valês; german: Wallis ), more formally the Canton of Valais,; german: Kanton Wallis; in other official Swiss languages outside Valais: it, (Canton) Vallese ; rm, (Chantun) Vallais. is one of the cantons of Switzerland, 26 cantons forming the Switzerland, Swiss Confederation. It is composed of thirteen districts and its capital and largest city is Sion, Switzerland, Sion. The flag of the canton is made of thirteen stars representing the districts, on a white-red background. Valais is situated in the southwestern part of Switzerland, the country. It borders the cantons of Canton of Vaud, Vaud and Canton of Bern, Bern to the north, the cantons of Canton of Uri, Uri and Ticino to the east, as well as Italy to the south and France to the west. It is one of the three large southern Alps, Alpine cantons, along with Ticino and the Grisons, which encompass a vast diversity of ecosystems. It is a bilingual canton, French language, French and German language, German ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Ice Age
The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Matthes described glaciers in the Sierra Nevada of California that he believed could not have survived the hypsithermal; his usage of "Little Ice Age" has been superseded by "Neoglaciation". The period has been conventionally defined as extending from the 16th to the 19th centuries, (noted in Grove 2004:4). but some experts prefer an alternative timespan from about 1300 to about 1850. The NASA Earth Observatory notes three particularly cold intervals. One began about 1650, another about 1770, and the last in 1850, all of which were separated by intervals of slight warming. The Intergovernmental Panel on Climate Change Third Assessment Report considered that the timing and the areas affected by the Little Ice Age suggested largely independent ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aletsch Glacier
The Aletsch Glacier (german: Aletschgletscher, ) or Great Aletsch Glacier () is the largest glacier in the Alps. It has a length of about (2014), has about a volume of (2011), and covers about (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near . It then continues towards the valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost of its length, since 1870 , and lost also more than of its thickness. The whole area, including other glaciers is part of the Protected Area, which was declared a UNESCO World Heritage Site in 2001. Geography The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is consider ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
