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Nördlicher 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 |
Bavaria Top
Bavaria ( ; ), officially the Free State of Bavaria (german: Freistaat Bayern, link=no ), is a state in the south-east of Germany. With an area of , Bavaria is the largest German state by land area, comprising roughly a fifth of the total land area of Germany. With over 13 million inhabitants, it is second in population only to North Rhine-Westphalia, but due to its large size its population density is below the German average. Bavaria's main cities are Munich (its capital and largest city and also the third largest city in Germany), Nuremberg, and Augsburg. The history of Bavaria includes its earliest settlement by Iron Age Celtic tribes, followed by the conquests of the Roman Empire in the 1st century BC, when the territory was incorporated into the provinces of Raetia and Noricum. It became the Duchy of Bavaria (a stem duchy) in the 6th century AD following the collapse of the Western Roman Empire. It was later incorporated into the Holy Roman Empire, became an ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firn
__NOTOC__ Firn (; from Swiss German "last year's", cognate with ''before'') is partially compacted névé, a type of snow that has been left over from past seasons and has been recrystallized into a substance denser than névé. It is ice that is at an intermediate stage between snow and glacial ice. Firn has the appearance of wet sugar, but has a hardness that makes it extremely resistant to shovelling. Its density generally ranges from 0.35 g/cm3 to 0.9 g/cm3, and it can often be found underneath the snow that accumulates at the head of a glacier. Snowflakes are compressed under the weight of the overlying snowpack. Individual crystals near the melting point are semiliquid and slick, allowing them to glide along other crystal planes and to fill in the spaces between them, increasing the ice's density. Where the crystals touch they bond together, squeezing the air between them to the surface or into bubbles. In the summer months, the crystal metamorphosis can occur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Winter Sport
Winter sports or winter activities are competitive sports or non-competitive recreational activities which are played on snow or ice. Most are variations of skiing, ice skating and sledding. Traditionally, such games were only played in cold areas during winter, but artificial snow and artificial ice allow more flexibility. Playing areas and fields consist of either snow or ice. Artificial ice can be used to provide ice rinks for ice skating, ice hockey, para ice hockey, ringette, broomball, bandy, rink bandy, rinkball, and spongee in a milder climate. The sport of speed skating uses a frozen circular track of ice, but in some facilities the track is combined in an enclosed area used for sports requiring an ice rink or the rink itself is used. Alternatively, ice cross downhill uses a track with various levels of elevation and a combination of bends. Long distance skating ( "marathon skating") such as tour skating is only performed outdoors and uses the available ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Accumulation Zone
On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, (melting, evaporation, and sublimation). The annual equilibrium line separates the accumulation and ablation zone Ablation zone or ''ablation area'' refers to the low-altitude area of a glacier or ice sheet below firn with a net loss in ice mass due to melting, sublimation, evaporation, ice calving, aeolian processes like blowing snow, avalanche, and any o ... annually. The accumulation zone is also defined as the part of a glacier's surface, usually at higher elevations, on which there is net accumulation of snow, which subsequently turns into firn and then glacier ice. Part of the glacier where snow builds up and turns to ice moves outward from there. External links * * Glaciology {{Glaciology-stub ... [...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, Mudflow, mudslides, Landslide#Debris landslide, rock slides, and serac collapses. They are also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, Rain and snow mixed, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called shower (precipitation), showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schneefernerkopf
The Schneefernerkopf is a peak in the Zugspitze massif in the Alps. It lies at the western end of the Wetterstein chain in the Alps on the border between the German state of Bavaria and the Austrian state of Tyrol. It is the dominant mountain in the Wetterstein, especially when viewed from Ehrwald. Distinction from the Zugspitze Although the Schneefernerkopf may be viewed as the 'second highest mountain in Germany' after the Zugspitze, this depends heavily on the definition of the term 'mountain'. Due to its proximity to the Zugspitze (it has a topographic isolation of 1.7 km) it is questionable whether it can be counted as an independent mountain, or merely as a sub-peak of the Zugspitze. Either way, its prominence is 176 m. If it is not reckoned as an independent peak, then the claim to the second highest mountain in Germany goes to the Hochwanner (2,746 m), which is clearly separated from the Zugspitze massif by the Rein Valley, Gatterl and Feldernjöchl. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arête
An arête ( ) is a narrow ridge of rock which separates two valleys. It is typically formed when two glaciers erode parallel U-shaped valleys. Arêtes can also form when two glacial cirques erode headwards towards one another, although frequently this results in a saddle-shaped pass, called a col. The edge is then sharpened by freeze-thaw weathering, and the slope on either side of the arête steepened through mass wasting events and the erosion of exposed, unstable rock. The word ''arête'' () is actually French for "edge" or "ridge"; similar features in the Alps are often described with the German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver'' is a type of arête that separates a unified flow of glacial ice from its uphill side into two glaciers flanking, and flowing parallel to, the ridge. ''Cleaver'' gets its name from the way it resembles a meat cleaver slicing meat into two parts. A cleaver may be t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blaueis
The Blaueis ("blue ice") is the northernmost glacier in the Alps and lies within the municipality of Ramsau in the Bavarian part of the Berchtesgaden Alps. Geography The glacier lies on the exposed north-facing slopes in the upper Blaueis cirque, nestling between the rock faces of the Blaueisspitze (2480 m), Hochkalter (2607 m) and Kleinkalter (2513 m), which ring the glacier in a horseshoe shape. Because of its relatively low elevation, the Blaueis has been particularly affected by glacial retreat which is common amongst Alpine glaciers. Since the mid-1980s, rocks in the middle of the Blaueis have become increasingly free of snow and the upper part of the glacier is now more or less completely separated from the lower field of what is now dead ice. The thickness of the ice as determined by ground-penetrating radar was only up to 13 feet in 2007, and the average thickness of the ice was less than four metres; giving a volume of around 0.4 million m³. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Watzmann Glacier
The Watzmann Glacier is one of the five recognised glaciers in Germany.The Watzmann has been recognised as a glacier by the Commission for Glaciology of the Bavarian Academy of Science since 1959 Geography Watzmann Glacier is located below the famous east face of the Watzmann in the Watzmann cirque and is surrounded by the ''Watzmanngrat'' arête, the ''Watzmannkindern'' and the ''Kleiner Watzmann''. The size of the glacier reduced from around in 1820 until it split into a few fields of firn, but between 1965 and 1980 it advanced significantly again and now has an area of .''Watzmanngletscher - Topographie'' at www.lrz.de. Accessed on 24 Dec 2010 Its classification as a glacier is not undisputed by scientists, however, due to its size and its low flow velocity. Above and to the west of the icefield ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Höllentalferner
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 Schneeferner, 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 to 2,200 m, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nördlicher 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 |
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