| Watzmann Glacier | |
|---|---|
 The Watzmann Glacier is seen in the center of the photograph. | |
  Watzmann Glacier  Watzmann Glacier  Watzmann Glacier | |
| Coordinates | 47°33′19.8″N12°55′48.7″E / 47.555500°N 12.930194°E |
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The Watzmann Glacier is one of the five recognised glaciers in Germany. [1]
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 30 hectares (74 acres) in 1820 until it split into a few fields of firn, but between 1965 and 1980 it advanced significantly again [2] and now has an area of 10.1 hectares (25 acres). [3] 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 lie the remains of a Ju 52 transport aircraft which crashed in October 1940.
Amongst the other permanent snow and icefields nearby are the Eiskapelle ("Ice Chapel"), which is well known due to its easy accessibility from St. Bartholomä and may be the lowest-lying, permanent snowfield in the Alps, and the Schöllhorneis on the east face itself.
The Bavarian Alps is a collective name for several mountain ranges of the Northern Limestone Alps within the German state of Bavaria.
The Watzmann is a mountain in the Berchtesgaden Alps south of the village of Berchtesgaden. It is the third highest in Germany, and the highest located entirely on German territory.
Kenai Fjords National Park is an American national park that comprises the Harding Icefield, its outflowing glaciers, and coastal fjords and islands. The park covers an area of 669,984 acres on the Kenai Peninsula in south-central Alaska, west of the town of Seward.
The Columbia Icefield is the largest ice field in North America's Rocky Mountains. Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park. It is about 325 square kilometres (125 sq mi) in area, 100 to 365 metres in depth and receives up to 7 metres (280 in) of snowfall per year.
Mendenhall Glacier is a glacier about 13.6 miles (21.9 km) long located in Mendenhall Valley, about 12 miles (19 km) from downtown Juneau in the southeast area of the U.S. state of Alaska. The glacier and surrounding landscape is protected as part of the 5,815 acres (2,353 ha) Mendenhall Glacier Recreation Area, a federally designated unit of the Tongass National Forest.
The Trinity Alps are a mountain range in Trinity County and Siskiyou County in Northern California. They are a subrange of the Klamath Mountains located to the north of Weaverville.
An ice field is a mass of interconnected valley glaciers on a mountain mass with protruding rock ridges or summits. They are often found in the colder climates and higher altitudes of the world where there is sufficient precipitation for them to form. The higher peaks of the underlying mountain rock that protrude through the icefields are known as nunataks. Ice fields are larger than alpine glaciers, but smaller than ice caps and ice sheets. The topography of ice fields is determined by the shape of the surrounding landforms, while ice caps have their own forms overriding underlying shapes.
Mount Crillon is a high peak of the Fairweather Range, the southernmost part of the Saint Elias Mountains. It lies southeast of Mount Fairweather, in the promontory between the Gulf of Alaska and Glacier Bay. It is included in Glacier Bay National Park. The peak was named after Felix-Francois-Dorothee de Bretton, Comte de Crillon, by his friend, the French explorer Jean Francois de Galaup de la Perouse.
Mount Miller is an isolated peak of the Saint Elias Mountains in Alaska, United States. It is notable for its position among spectacular icefields, its distance from any inhabited place, and its large rise above local terrain. It is over 65 miles (105 km) from McCarthy, the nearest habitation, and over 105 miles (169 km) away from Yakutat, the nearest significant town. Exemplifying the size of the mountain, the south flank rises 9,000 feet (2,700 m) above the Duktoth River valley to the south in approximately 9 horizontal miles (14 km).
The Wapta Icefield is a series of glaciers located on the Continental Divide in the Waputik Mountains of the Canadian Rockies, in the provinces of British Columbia and Alberta, in Yoho National Park in the Canadian Rockies. The icefield is shared by Banff and Yoho National Parks and numerous outlet glaciers extend from the icefield, including the Vulture, Bow and Peyto Glaciers. Runoff from the icefields and outlet glaciers supply water to both the Kicking Horse and Bow Rivers, as well as numerous streams and lakes.
The Stikine Icecap is a large icefield straddled on the Alaska–British Columbia boundary in the Alaska Panhandle region. It lies in the Boundary Ranges of the Coast Mountains. Within the United States, most of it is under the administration of the Tongass National Forest and is part of MENthe Stikine-LeConte Wilderness within the national forest.
Glacier morphology, or the form a glacier takes, is influenced by temperature, precipitation, topography, and other factors. The goal of glacial morphology is to gain a better understanding of glaciated landscapes and the way they are shaped. Types of glaciers can range from massive ice sheets, such as the Greenland ice sheet, to small cirque glaciers found perched on mountain tops. Glaciers can be grouped into two main categories:
The Homathko Icefield is an icefield in British Columbia, Canada. Officially named the Homathko Snowfield from 1950 until the current name was adopted in 1976, it is one of the largest icefields in the southern half of the Coast Mountains, with an area of over 2,000 km2 (770 sq mi). It is located between Chilko Lake and the Homathko River, and lies across the Great Canyon of that river to the east of the Waddington Range. Although adjacent to Mount Queen Bess, the Homathko Icefield is largely an expanse of ice, about 30 km (19 mi) across, ringed by relatively minor peaks and distinguished, relative to the other Coast Mountains icefields, by lack of any major ones. The Lillooet Icecap and the Compton Névé, both similar in size to the Homathko Icefield but much more peak-studded, lie to the Homathko Icefield's southeast across the Southgate River which bends around the icefield-massif's southern flank to reach the head of Bute Inlet adjacent to the mouth of the Homathko River. The icefield is essentially one large ice-girt montane plateau between these two rivers.
The Pemberton Icefield or Pemberton Icecap, is the southernmost of the series of very large icefields studding the Pacific Ranges of the southern Coast Mountains in British Columbia, Canada.
The Blaueis is the northernmost glacier in the Alps and lies within the municipality of Ramsau in the Bavarian part of the Berchtesgaden Alps.
The Schneeferner in the Bavarian Alps is Germany's highest and largest glacier.
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.
A randkluft or rimaye is the headwall gap between a glacier or snowfield and the adjacent rock face at the back of the cirque or, more loosely, between the rock face and the side of the glacier.
Berchtesgaden National Park is in the south of Germany, on its border with Austria, in the municipalities of Ramsau bei Berchtesgaden and Schönau am Königsee, Berchtesgadener Land in Bavaria. The national park was established in 1978 to protect the landscapes of the Berchtesgaden Alps. Headquartered in the town of Berchtesgaden, the park was designated a UNESCO Biosphere Reserve in 1990.
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