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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 (german: Granatspitzgruppe), sometimes also the Granatspitz Group, is a sub-group of the Austrian Central Alps, 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 Hohe Tauern, High Tauern. The Granatspitze Group is located in Austria in the federal states of Salzburg (Bundesland), Salzburg and Tirol (Bundesland), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Tauern
The High Tauern ( pl.; german: Hohe Tauern, it, Alti Tauri) are a mountain range on the 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, Carinthia and East Tyrol, with a small part in the southwest belongs to the Italian province of South Tyrol. The range includes Austria's highest mountain, the Grossglockner at 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 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 Pass to the west (separating it from the Zillertal Alps). Its most important s ... [...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'' , and all of them 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 either France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these three 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 the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the 'Alpi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Tyrol
East Tyrol, occasionally East Tirol (german: Osttirol), is an exclave of the Austrian state of Tyrol, separated from the main North Tyrol part by the short common border of Salzburg and Italian South Tyrol (''Südtirol'', it, Alto Adige). It is congruent with the administrative district (''Bezirk'') of Lienz. History The area around the former Roman ''municipium'' of Aguntum was, from the 12th century, held by the Counts of Gorizia, who took their residence at Lienz and inherited the County of Tyrol in 1253. While Tyrol was lost to the Austrian House of Habsburg in 1363, the Gorizian counts retained Lienz until the extinction of the line in 1500. Emperor Maximilian I of Habsburg finally incorporated it into Austrian Tyrol. East Tyrol's present-day situation arose from the defeat of the Austro-Hungarian Empire in World War I and its subsequent dissolution. By the 1915 Treaty of London, the Kingdom of Italy, which had joined the victorious Triple Entente, was to obtain the Tyrol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Salzburg (Bundesland)
Salzburg (, ; bar, Soizbuag, label=Austro-Bavarian) (also known as ''Salzburgerland'') is a state (''Land'') of the modern Republic of Austria. It is officially named ''Land Salzburg'' to distinguish it from its eponymous capital — the city of Salzburg. For centuries, it was an independent Prince-Bishopric of the Holy Roman Empire. Geography Location The state of Salzburg covers area of . It stretches along its main river — the Salzach – which rises in the Central Eastern Alps in the south to the Alpine foothills in the north. It is located in the north-west of Austria, close to the border with the German state of Bavaria; to the northeast lies the state of Upper Austria; to the east the state of Styria; to the south the states of Carinthia and Tyrol. With 529,085 inhabitants, it is one of the country's smaller states in terms of population. Running through the south are the main ranges of the Alpine divide (incl. the Hohe Tauern mountains) with numerous three-thousander ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climbing Grade
In rock climbing, mountaineering, and other climbing disciplines, climbers give a grade to a climbing route or boulder problem, intended to describe concisely the difficulty and danger of climbing it. Different types of climbing (such as sport climbing, bouldering or ice climbing) each have their own grading systems, and many nationalities developed their own, distinctive grading systems. There are a number of factors that contribute to the difficulty of a climb, including the technical difficulty of the moves, the strength, stamina and level of commitment required, and the difficulty of protecting the climber. Different grading systems consider these factors in different ways, so no two grading systems have an exact one-to-one correspondence. Climbing grades are inherently subjective.Reynolds Sagar, Heather, 2007, ''Climbing your best: training to maximize your performance'', Stackpole Books, UK, 9. They may be the opinion of one or a few climbers, often the first ascensi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) 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 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 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) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crevasse
A crevasse is a deep crack, that forms in a glacier or ice sheet that can be a few inches across to over 40 feet. 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 45 metres and as wide as 20 metres. by |
Mountains Of Tyrol (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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Salzburg (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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
