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Höllentalferner Von NO
The Höllentalferner is a glacier in the western Wetterstein Mountains. It is a cirque glacier that covers the upper part of the Höllental valley and its location in a rocky bowl between the Riffelwandspitzen and Germany's highest mountain, the Zugspitze, means that it is well-protected from direct sunshine. Geography With an area of (as of 2006)''Höllentalferner - Topographie'' at www.lrz.de. Accessed on 24 December 2010 it is almost as big as the nearby Northern , the largest glacier in Germany. It is about long and up to wide. It is the only German glacier with a proper glacial tongue. In spite of its relatively low elevation of just 2,570 m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpspitze
The Alpspitze is a mountain, 2628 m, in Bavaria, Germany. Its pyramidal peak is the symbol of Garmisch-Partenkirchen and is one of the best known and most attractive mountains of the Northern Limestone Alps. It is made predominantly of Wetterstein limestone from the Upper Triassic. Ascent Several ''klettersteigs'' run up the Alpspitze. The shortest ascent starts at the valley station of ''Osterfelderkopf'' (2,033 m) on the Alpspitze Cable Car from Garmisch-Partenkirchen. From the Osterfelderkopf the Alpspitze may be climbed either directly along the Alpspitz-Ferrata, an easy, mostly protected and much frequented ''klettersteig'' (ca. 2 hours from the Osterfelderkopf) or the summit may be reached on the North Face Climb (''Nordwandsteig''), which runs in a curve to the east into the Oberkar cirque and from there along the left-hand edge of the cirque to the top. Another ascent runs from the col of ''Grießkarscharte'' (2,460 m), which is reached either from th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneeferner
} The Schneeferner in the Bavarian Alps is Germany's highest and largest glacier.''Kaltgestellter Gletscher'' at www.sueddeutsche.de. Accessed on 23 Dec 2010 Geography Schneeferner glacier is located on the '''', a plateau south of the country's highest peak, the , that descends from west to east and forms the head of the Reintal valley. The |
Glaciers Of The Alps
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] |
Glaciers Of Bavaria
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] |
Höllentalferner Von NO
The Höllentalferner is a glacier in the western Wetterstein Mountains. It is a cirque glacier that covers the upper part of the Höllental valley and its location in a rocky bowl between the Riffelwandspitzen and Germany's highest mountain, the Zugspitze, means that it is well-protected from direct sunshine. Geography With an area of (as of 2006)''Höllentalferner - Topographie'' at www.lrz.de. Accessed on 24 December 2010 it is almost as big as the nearby Northern , the largest glacier in Germany. It is about long and up to wide. It is the only German glacier with a proper glacial tongue. In spite of its relatively low elevation of just 2,570 m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klettersteig
A via ferrata (Italian language, Italian for "iron path", plural ''vie ferrate'' or in English ''via ferratas'') is a protected climbing route found in the Alps and certain other locations. The term "via ferrata" is used in most countries and languages except notably in German-speaking regions, which use ''Klettersteig''—"climbing path" (plural ''Klettersteige''). Infrastructure A via ferrata is a climbing route that employs steel cables, rungs or ladders, fixed to the rock to which the climbers affix #Safety and equipment, a harness with two leashes, which allows the climbers to secure themselves to the metal fixture and limit any fall. The cable and other fixtures, such as iron rungs (stemples), pegs, carved steps, and ladders and bridges, provide both footings and handholds, as well. This allows climbing on otherwise dangerous routes without the risks of unprotected scrambling and climbing or the need for technical climbing equipment. They expand the opportunities for acce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Randkluft
A randkluft (from the German for ''marginal cleft/crevasse'') or rimaye (from the same French ) is the headwall gap between a glacier or snowfield and the adjacent rock face at the back of the cirqueWhittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 438. . or, more loosely, between the rock face and the side of the glacier. In French, the word ''rimaye'' covers both notions of randkluft and bergschrund. Formation It is formed by the melting of ice against warmer rock and may be very deep. During summer therefore, a randkluft will become wider and thus more difficult for climbers to negotiate. Randklufts are often found in relatively low-lying glaciers such as the Blaueis in the Berchtesgaden Alps or the Höllentalferner in the Wetterstein. A randkluft is similar to, but not identical with, a bergschrund, which is the place on a high-altitude glacier where the moving ice stream breaks away from the static ice frozen to the rock creating a la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Global Warming
In common usage, climate change describes global warming—the ongoing increase in global average temperature—and its effects on Earth's climate system. Climate change in a broader sense also includes previous long-term changes to Earth's climate. The current rise in global average temperature is more rapid than previous changes, and is primarily caused by humans burning fossil fuels. Fossil fuel use, deforestation, and some agricultural and industrial practices increase greenhouse gases, notably carbon dioxide and methane. Greenhouse gases absorb some of the heat that the Earth radiates after it warms from sunlight. Larger amounts of these gases trap more heat in Earth's lower atmosphere, causing global warming. Due to climate change, deserts are expanding, while heat waves and wildfires are becoming more common. Increased warming in the Arctic has contributed to melting permafrost, glacial retreat and sea ice loss. Higher temperatures are also causing m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avalanche
An avalanche is a rapid flow of snow down a slope, such as a hill or mountain. Avalanches can be set off spontaneously, by such factors as increased precipitation or snowpack weakening, or by external means such as humans, animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, mudslides, rock slides, and serac collapses. They are also different from large scale movement ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Höllentalferner HQ
The Höllentalferner is a glacier in the western Wetterstein Mountains. It is a cirque glacier that covers the upper part of the Höllental valley and its location in a rocky bowl between the Riffelwandspitzen and Germany's highest mountain, the Zugspitze, means that it is well-protected from direct sunshine. Geography With an area of (as of 2006)''Höllentalferner - Topographie'' at www.lrz.de. Accessed on 24 December 2010 it is almost as big as the nearby Northern , the largest glacier in Germany. It is about long and up to wide. It is the only German glacier with a proper glacial tongue. In spite of its relatively low elevation of just 2,570 m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Höllental (Wetterstein)
The ''Höllental'', English translation "Hell Valley" or "Valley of Hell" is one of the routes on the German side leading up the Zugspitze on the German-Austrian border in the northern Alps. It is located in the district of Garmisch-Partenkirchen. See also *Zugspitze The Zugspitze (), at above sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western su ... * Höllental on the German Wikipedia ZUGSPITZE 360° atop the Zugspitze via the Höllental External links Valleys of the Alps Valleys of Bavaria Canyons and gorges of Germany {{GarmischPartenkirchendistrict-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zugspitze
The Zugspitze (), at above Normalhöhennull, sea level, is the highest peak of the Wetterstein Mountains as well as the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen, and the Austria–Germany border runs over its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are three glaciers, including the two largest in Germany: the Schneeferner#Northern Schneeferner, Northern Schneeferner with an area of 30.7 hectares and the Höllentalferner with an area of 24.7 hectares. The third is the Schneeferner#Southern Schneeferner, Southern Schneeferner which covers 8.4 hectares. The Zugspitze was first climbed on 27 August 1820 by Josef Naus, his survey assistant, Maier, and mountain guide, Johann Georg Tauschl. Today there are three normal routes to the summit: one from the Höllental (Wetterstein), Höllental valley to the northeast; another out of the Reintal (Wetterste ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
