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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&nbs ... [...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 Another ascent runs from the col of ''Grießkarscharte'' (2,460 m), which is reached either from the Höllentalanger Hut in the Höllental valley via the cirque of ''Mathaisenkar'' (involving a ''klettersteig'') or from the lake of Stuibensee via the ''Grießkar'' cirque. The popular route from the Alpspitze via t ... [...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 '' Zugspitzplatt'', 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 (; 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 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 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 be found in mountain ranges on every contine ... [...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&nbs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klettersteig
A via ferrata (Italian for "iron path", plural ''vie ferrate'' or in English ''via ferratas'') is a protected climbing route found in the Alps and certain other Alpine locations. The protection includes steel fixtures such as cables and railings to arrest the effect of any fall, which the climber can either hold onto or clip into using climbing protection. Some via ferratas can also include steel fixtures that provide aid in overcoming the obstacles encountered, including steel ladders and steel steps. Description A via ferrata is a climbing route in the mountains that employs steel cables, rungs, or ladders, fixed to the rock to which the climbers affix 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 ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Global Warming
Present-day climate change includes both global warming—the ongoing increase in global average temperature—and its wider 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 temperatures is driven by human activities, especially fossil fuel burning since the Industrial Revolution. Fossil fuel use, deforestation, and some agricultural and industrial practices release greenhouse gases. These gases absorb some of the heat that the Earth radiates after it warms from sunlight, warming the lower atmosphere. Carbon dioxide, the primary gas driving global warming, has increased in concentration by about 50% since the pre-industrial era to levels not seen for millions of years. Climate change has an increasingly large impact on the environment. Deserts are expanding, while heat waves and wildfires are becoming more common. Amplified warming in the Arctic has c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avalanche
An avalanche is a rapid flow of snow down a Grade (slope), slope, such as a hill or mountain. Avalanches can be triggered spontaneously, by factors such as increased precipitation or snowpack weakening, or by external means such as humans, other 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, Mudflow, mudslides, Landslide#Debris landslide, rock slides, and serac collap ... [...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&nbs ... [...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 Normalhöhennull, sea level, is the highest peak of the Wetterstein Mountains and the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen in Bavaria, and the Austria–Germany border ... * Höllental on the German Wikipedia External links ZUGSPITZE 360° atop the Zugspitze via the Höllental 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 and the highest mountain in Germany. It lies south of the town of Garmisch-Partenkirchen in Bavaria, and the Austria–Germany border is on its western summit. South of the mountain is the ''Zugspitzplatt'', a high karst plateau with numerous caves. On the flanks of the Zugspitze are two glaciers, the largest in Germany: the Schneeferner#Northern Schneeferner, Northern Schneeferner with an area of 30.7 hectares and Höllentalferner with an area of 24.7 hectares. Shrinking of the Schneeferner#Southern Schneeferner, Southern Schneeferner led to the loss of glacier status in 2022. 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 (Wetterst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
