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Lower Grindelwald Glacier
The Lower Grindelwald Glacier () is a Glacier in the Switzerland, Swiss Bernese Alps, situated to the south-east of Grindelwald. It starts below the Agassizhorn and the Strahlegghörner and is connected with the Finsteraar Glacier via the Finsteraarjoch (). The Lower Grindelwald Glacier yet has a major tributary, the Ischmeer (Swiss German for ''Ice Sea'', formerly known as ''Grindelwald-Fiescher Glacier'', ), which is the glacier overlooked by the Jungfrau Railway's Eismeer railway station. The Lower Grindelwald Glacier was about long and covered an area of in 1973. The glacier has significantly shrunk since, having a length of just in 2015, with most of the retreat () happening since 2007. In the middle of the 19th century it clearly reached into the valley of Grindelwald as far as ''Mettenberg'' at an altitude of , an eastern quarter of Grindelwald, near the conjunction of the Schwarze and Weisse LütschineNot to be mismatched with the Weisse Lütschine in the Valley of La ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fiescherhörner
Grosses Fiescherhorn is a mountain peak of the Bernese Alps, located on the border between the cantons of Bern and Valais, halfway between the Mönch and the Finsteraarhorn. At above sea level, its summit culminates over the whole Fiescherhorn massif (), which is also composed of the slightly lower Hinteres Fiescherhorn () to the south and Kleines Fiescherhorn (also called ''Ochs'' aka ox, ) to the east. From the north both are well hidden behind other mountain peaks and can only been seen from ''Isch'' in Grindelwald (1,095 m). The mountain is shared between the municipalities of Grindelwald and Fieschertal. Ascents are usually made from one of these three popular routes: one starts from the Mönchsjoch Hut, one from the Konkordia Hut, and the third from the Finsteraarhorn Hut. Climbing history The summit was first reached on 23 July 1862 by H. B. George and Adolphus Warburton Moore, with guides Christian Almer and Ulrich Kaufmann. They used what is now the normal rout ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jungfrau Railway
The Jungfrau Railway (, , JB) is a mountain rack railway in the Bernese Alps, Switzerland, connecting Kleine Scheidegg in the Bernese Oberland to the Jungfraujoch, across the Valais border. It is the highest railway in Switzerland and Europe, running from the station of Kleine Scheidegg () to the Jungfraujoch (), well above the perennial snow line. As a consequence, the railway runs essentially within the Jungfrau Tunnel, built into the neighbouring Eiger and Mönch, to protect the line from snow and extreme weather. The Jungfrau Railway got its name from the highest of the three high peaks above it: the Jungfrau (; ), which was the initial goal of the project. A lift connecting the summit of the Jungfrau with an underground railway was planned. In 1912, the project ultimately ended at the Jungfraujoch, the saddle between the Mönch and Jungfrau. It was one of the highest railways in the world at the time of its inauguration. At Kleine Scheidegg the Jungfrau Railway connects ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciers Of The Canton Of Bern
A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, 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“Glacier, N., Pronunciation.” Oxford English Dictionary, Oxford University Press, Oxford UP, June 2024, https://doi.org/10.1093/OED/7553486115. Accessed 25 Jan. 2025. 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swiss Alps
The Alps, Alpine region of Switzerland, conventionally referred to as the Swiss Alps, 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 Physical geography, 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 Range, 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 (mountain), 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 Switzerland. Since the Middle Age ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Retreat Of Glaciers Since 1850
The retreat of glaciers since 1850 is a well-documented effects of climate change, effect of climate change. The retreat of Mountain glacier, mountain glaciers provides evidence for the Instrumental temperature record, rise in global temperatures since the late 19th century. Examples include mountain glaciers in western North America, Asia, Alps, the Alps in central Europe, and tropical and subtropical regions of South America and Africa. Since glacial mass is affected by long-term climatic changes, e.g. Precipitation (meteorology), precipitation, Temperature, mean temperature, and cloud cover, glacial mass changes are one of the most sensitive indicators of climate change. The retreat of glaciers is also a major reason for sea level rise. Excluding peripheral glaciers of Ice sheet, ice sheets, the total cumulated global glacial losses over the 26 years from 1993 to 2018 were likely 5500 gigatons, or 210 gigatons per year.Fox-Kemper, B., H.T. Hewitt, C. Xiao, G. Aðalgeirsdóttir, ... [...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. Catalogs of glaciers include:World Glacier Inventory* World Glacier Monitoring ServiceGlobal Land Ice Measurements from Space (GLIMS) Glacier Database Glaciers by continent
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List Of Glaciers In Switzerland
This is a non-exhaustive list of the major glaciers in Switzerland. It contains their surface area, their lengths since the start of measurement and the most current year, their height and their outflow. Most of them are retreating and many will vanish. All of these glaciers are located within the Swiss Alps. Most of them are situated in the Pennine and Bernese Alps. The Jungfrau-Aletsch protected area includes the largest glaciers of the Alps. There are glaciers in the four major drainage basins of Switzerland. The Rhine and Rhône basins are located on the northern side of the Alps while the Po basin is located on the south side of the Alps. The Danube basin is located on the east side of the Alps. There are no glaciers in the Swiss portion of the Adige basin. There are approximately 1,800 glaciers in the Swiss Alps. List See also * List of mountains in Switzerland * Retreat of glaciers since 1850#Europe References External links List of dangerous glaciers in Switze ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caspar Wolf Oberer Und Unterer Grindelwaldgletscher 1774
Caspar is a masculine given name. It may refer to: People * Caspar (magus), a name traditionally given to one of the Three Magi in the Bible who brought the baby Jesus gifts * Caspar Austa (born 1982), Estonian cyclist *Caspar Badrutt (1848–1904), Swiss businessman and pioneer of alpine resorts * Caspar Barlaeus (1584–1648), Dutch polymath, Renaissance humanist, theologian, poet and historian *Caspar Bartholin the Elder (1585–1629), Danish theologian and medical professor *Caspar Bartholin the Younger (1655–1738), Danish anatomist *Caspar Buberl (1834–1899), American sculptor * Caspar del Bufalo (1786–1837), Italian priest and saint *Caspar Commelijn (1668–1731), Dutch botanist * Caspar de Crayer (1582–1669), Flemish painter * Caspar Cruciger the Younger (1525–1597), German theologian, son of Caspar Creuziger * Caspar Creuziger or Caspar Cruciger the Elder (1504–1548), German humanist, professor of theology and preacher *Caspar Detlef Gustav Müller (1927–2003) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fiescherhorn
Grosses Fiescherhorn is a mountain peak of the Bernese Alps, located on the border between the cantons of Bern and Valais, halfway between the Mönch and the Finsteraarhorn. At above sea level, its summit culminates over the whole Fiescherhorn massif (), which is also composed of the slightly lower Hinteres Fiescherhorn () to the south and Kleines Fiescherhorn (also called ''Ochs'' aka ox, ) to the east. From the north both are well hidden behind other mountain peaks and can only been seen from ''Isch'' in Grindelwald (1,095 m). The mountain is shared between the municipalities of Grindelwald and Fieschertal. Ascents are usually made from one of these three popular routes: one starts from the Mönchsjoch Hut, one from the Konkordia Hut, and the third from the Finsteraarhorn Hut. Climbing history The summit was first reached on 23 July 1862 by H. B. George and Adolphus Warburton Moore, with guides Christian Almer and Ulrich Kaufmann. They used what is now the normal rou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fiescher Glacier
The Fiescher Glacier (''Fieschergletscher'' in German) is a valley glacier on the south side of the Bernese Alps in the canton of Valais, Switzerland. in length, it is the second longest glacier in the Alps. The glacier covers an area of . The starting point of the Fiescher Glacier is above sea level, on the eastern slope of the Fiescherhorn, it is flanked to the west by the Grünhorn and Gross Wannenhorn and to the east by the Finsteraarhorn. In the lower section, the Fiescher Glacier flows south through a deep valley between the Gross Wannenhorn and the Wasenhorn. In summer, when the snow layer melts, it has a grey colour as it is covered with rocks coming from the steep slopes of the mountains around. The end of glacier tongue is at around above sea level. On the south western slope of the Finsteraarhorn, about above the Fieschergletscher, the Finsteraarhornhütte of the Swiss Alpine Club ( above sea level) is often used as an intermediate station on the route from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Grindelwald Glacier
The Upper Grindelwald Glacier (German: ''Oberer Grindelwaldgletscher'') is one of the two valley glaciers near Grindelwald on the northern side of the Bernese Alps, in the canton of Bern (the other being the Lower Grindelwald Glacier). It had a length of about and covered an area of in 1973. The Upper Grindelwald Glacier arises from a vast snow field north of the Schreckhorn and south of the Wetterhorn. The glacier tongue is currently at around above sea level, making it one of the lowest glaciers in the Alps. Johann Heinrich Müller, 1825-1894 H20 Oberer Grindelwaldgletscher.JPG, Upper Grindelwald Glacier c. 1870/80. Etching by Heinrich Müller See also * List of glaciers in Switzerland * List of glaciers * Retreat of glaciers since 1850 *Swiss Alps The Alps, Alpine region of Switzerland, conventionally referred to as the Swiss Alps, represents a major natural feature of the country and is, along with the Swiss Plateau and the Swiss portion of the Jura Mountains, on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mättenberg
The Mettenberg (also spelled ''Mättenberg'') is a mountain of the Bernese Alps, overlooking Grindelwald in the Bernese Oberland. It lies north of the Schreckhorn and forms a huge buttress of the Schreckhorn range. From Grindelwald, an aerial tramway goes as high as Pfingstegg (1,387 m), which is situated below the first cliffs of the mountain.Swisstopo Swisstopo is the official name for the Swiss Federal Office of Topography, Switzerland's national mapping agency. The current name was made official in 2002. It had been used as the domain name for the homepage of the instituteswisstopo.admi ... maps References External links Mettenberg on Hikr Bernese Alps Mountains of the Alps Alpine three-thousanders Mountains of Switzerland Mountains of the canton of Bern {{Bern-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
