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Granatspitze
The Granatspitze () is the mountain giving its name to the Granatspitze Group in the High Tauern, the Alpine backbone of Austria. This, despite the fact that several peaks in this group are actually higher, for example the Stubacher Sonnblick which is less than a kilometre to the north and two metres higher. But, unlike, its oft-climbed neighbour, the Granatspitze is more rarely frequented due to the level of difficulty of the ascent. The steep summit block of this striking peak is made of granite. Ascent The easiest ascent runs from initially westwards towards the notch of the ''Granatscharte'', turning south in front of it to continue along the East Ridge (''Ostgrat'') to the summit. This route takes about 3 hours and has a climbing grade of II-. Another option is offered by the North Ridge (''Nordgrat'') with its several pinnacles or rock towers (''Grattürme''), but this is more difficult, albeit still II-. The South Ridge is also an option, especially from the East Tyrolea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granatspitze Group
The Granatspitze Group (), sometimes also the Granatspitz Group, is a sub-group of the Central Alps within the Eastern Alps. Together with the Ankogel Group, the Goldberg Group, the Glockner Group, the Schober Group, the Kreuzeck Group, the Venediger Group, the Villgraten Mountains and the Rieserferner Group, the Granatspitze Group forms the main range known as the High Tauern. The Granatspitze Group is located in Austria in the federal states of Salzburg and Tyrol. Its highest summit is the Großer Muntanitz, The Granatspitze Group is located in the central part of the High Tauern. The Felbertauernstraße road is the boundary of the group in the west. The group is rather overshadowed by its more famous neighbours which include the Großglockner and the Großvenediger. The range takes its name from the Granatspitze, Neighbouring ranges The Granatspitze Group is bordered by the following other mountain ranges of the Alps: * Kitzbühel Alps (to the north) * Glockner G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Tauern
The High Tauern (plural, pl.; , ) are a mountain range on the Main chain of the Alps, main chain of the Central Eastern Alps, comprising the highest peaks east of the Brenner Pass. The crest forms the southern border of the Austrian states of Salzburg (state), Salzburg, Carinthia (state), Carinthia and East Tyrol, with a small part in the southwest belongs to the Italy, Italian province of South Tyrol. The range includes Austria's highest mountain, the Grossglockner at metres above the Adriatic, above the Adriatic. In the east, the range is adjoined by the Lower Tauern. For the etymology of the name, see Tauern. Geography According to the Alpine Club classification of the Eastern Alps, the range is bounded by the Salzach valley to the north (separating it from the Kitzbühel Alps), the Mur (river), Mur valley and the Murtörl Pass to the east (separating it from the Lower Tauern), the Drava valley to the south (separating it from the Southern Limestone Alps), and the Birnlücke P ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of The Alps
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , all exceeding in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion. The list of these most prominent mountains is continued down to 2500 m elevation at List of prominent mountains of the Alps (2500–2999 m) and down to 2000 m elevation on List of prominent mountains of the Alps (2000–2499 m). All such mountains are located in France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these lists include all 44 ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 of the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpine four-thousanders' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term refers to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Andes) it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Salzburg (federal State)
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Institute For Meteorology And Geodynamics
The Central Institution for Meteorology and Geodynamics (, ZAMG) is the national meteorological and geophysical service of Austria. It is a subordinate agency of the Federal Ministry of Education, Science and Research. The ZAMG headquarters are located in Vienna, with regional offices in Salzburg, Innsbruck, Graz and Klagenfurt. ZAMG was founded in 1851 and is the oldest weather service in the world. Its task is not only to operate monitoring networks and to conduct research in various fields, but also to make the results available to the public. Organization The Hohe Warte in the Döbling district of Vienna is the headquarters of the Institution and is the regional office for Vienna, Lower Austria and Burgenland. Other regional ZAMG offices are: * Regional office for Salzburg and Upper Austria (city of Salzburg) * Regional office for Vorarlberg and Tyrol (Innsbruck) * Regional office for Carinthia ( Klagenfurt) * Regional office for Styria (Graz) Other ZAMG facilities a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crevasse
A crevasse is a deep crack that forms in a glacier or ice sheet. Crevasses form as a result of the movement and resulting stress associated with the shear stress generated when two semi-rigid pieces above a plastic substrate have different rates of movement. The resulting intensity of the shear stress causes a breakage along the faces. Description Crevasses often have vertical or near-vertical walls, which can then melt and create seracs, arches, and other ice formations. These walls sometimes expose layers that represent the glacier's stratigraphy. Crevasse size often depends upon the amount of liquid water present in the glacier. A crevasse may be as deep as and as wide as The presence of water in a crevasse can significantly increase its penetration. Water-filled crevasses may reach the bottom of glaciers or ice sheets and provide a direct hydrologic connection between the surface, where significant summer melting occurs, and the bed of the glacier, where additional wa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tundra Climate
The tundra climate is a polar climate sub-type located in high latitudes and high mountains. It is classified as ET according to the Köppen climate classification. It is a climate which at least one month has an average temperature high enough to melt snow (), but no month with an average temperature in excess of . If the climate occurs at high elevations, it is known as alpine climate. Despite the potential diversity of climates in the ''ET'' category involving precipitation, extreme temperatures, and relative wet and dry seasons, this category is rarely subdivided. Rainfall and snowfall are generally slight due to the low vapor pressure of water in the chilly atmosphere, but as a rule potential evapotranspiration is extremely low, allowing soggy terrain of swamps and bogs even in places that get precipitation typical of deserts of lower and middle latitudes. The amount of native tundra biomass depends more on the local temperature than the amount of precipitation. Tundra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
