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Hintere Brandjochspitze
The Hintere Brandjochspitze () is a summit roughly 200 metres northwest of the Vordere Brandjochspitze in the Nordkette range above Innsbruck. It rises above its "forward" neighbour by around 40 metres. The summit may be reached in 20 minutes from the Vordere Brandjochspitze at climbing grade UIAA I through a gully left of the 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 frequen .... A more difficult route runs along the western arête (grade III-) from the Hohe Warte. Other routes along the northern ''Hippengrat'' ( UIAA IV) from the ''Hippenspitze'' (2,388 m) and from the northwest ( UIAA IV) are rarely used. Literature * (Hippengrat, northwest route) * (normal route, west arête) {{authority control Two-thousanders of Austria Karwendel Mountai ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hohe Warte (Karwendel)
The Hohe Warte is a mountain, Bundesamt für Eich- und Vermessungswesen Österreich: Austrian Map online (Österreichische Karte 1:50,000)'. Retrieved 13 February 2012. in height, in the Karwendel range in Austria. It is located between the Kleiner Solstein to the west and the Hintere Brandjochspitze to the east, in the Nordkette in the state of Tyrol, north of the Innsbruck quarter of Kranebitten and has a prominence of at least 77 metres. Access The Hohe Warte was first climbed in 1870 by Hermann von Barth. The present normal route to the top runs from the Aspach Hut () above Innsbruck and poses no great difficulties. It runs through ''schrofen'' terrain up to the Gamswart Saddle, then for a short way along the western ridge to the summit. Another ascent runs up the south ridge and has a climbing grade of UIAA IV. Crossings to the Kleiner Solstein and Hintere Brandjochspitze are possible at grade III-.Walter Klier: ''Alpenvereinsführer alpin, Karwendel, pp. 142 f, Rz 730 ... [...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] |
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] |
Two-thousanders Of Austria
Two-thousanders are mountains that have a height of at least 2,000 metres above sea level, but less than 3,000 metres. The term is used in Alpine circles, especially in Europe (e.g. German: ''Zweitausender''). The two photographs show two typical two-thousanders in the Alps that illustrate different types of mountain. The Säuling (top) is a prominent, individual peak, whereas the Schneeberg (bottom) is an elongated limestone massif. In ranges like the Allgäu Alps, the Gesäuse or the Styrian-Lower Austrian Limestone Alps the mountain tour descriptions for mountaineers or hikers commonly include the two-thousanders, especially in areas where only a few summits exceed this level. Examples from these regions of the Eastern Alps are: * the striking Nebelhorn (2,224 m) near Oberstdorf or the Säuling (2,047 m) near Neuschwanstein, * the Admonter Reichenstein (2,251 m), Eisenerzer Reichenstein (2,165 m), Großer Pyhrgas (2,244 m) or Hochtor (2,369&nbs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bergverlag Rudolf Rother
Bergverlag Rother is a German publisher with its headquarters in Oberhaching, Upper Bavaria. Since 1950 the company, that formerly went under the name of ''Bergverlag Rudolf Rother'', has published the Alpine Club Guides in cooperation with the German Alpine Club (DAV), the Austrian Alpine Club (ÖAV) and the South Tyrol Alpine Club. Rother publish a "famous series of English language guides" covering most of the popular walking destinations in the Alps and Europe. History The company was founded on 16 November 1920 in Munich Munich ( ; german: München ; bar, Minga ) is the capital and most populous city of the States of Germany, German state of Bavaria. With a population of 1,558,395 inhabitants as of 31 July 2020, it is the List of cities in Germany by popu ... by Rudolf Rother sen., a bookseller and mountaineer, and is one of the oldest and most important specialist Alpine publishers. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Club Guide
The ''Alpine Club Guides'' (german: Alpenvereinsführer, commonly shortened to ''AV Führer'' or ''AVF'') are the standard series of Alpine guides that cover all the important mountain groups in the Eastern Alps. They are produced jointly by the German (DAV), Austrian (ÖAV) and South Tyrol Alpine Clubs (AVS). They have been published since 1950 by the firm of Bergverlag Rother in Munich, Germany. The AV guides contain all the routes – hiking trails, mountain hut approaches and summit climbs as well as ice and high mountain routes and ''klettersteigs'' in each mountain range. The descriptions are factual and dry, with few illustrations - rather unlike mountain books by e.g. Walter Pause – and despite introductory sections require general Alpine knowledge and experience. Examples are the ''AVF Allgäuer Alpen'' and the ''AVF Verwallgruppe''.The AV guides are often used as the basis for other publications and complement the Alpine Club maps or other map series. Available guid ... [...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 Mass wasting, also known as mass movement, is a general term for the movement of rock or soil down slopes under the force of gravity. It differs from other processes of erosion in that the debris transported by mass wasting is not entrained in ... 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 language, German equivalent term ''Grat''. Where three or more cirques meet, a pyramidal peak is created. Cleaver A ''cleaver' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UIAA
The International Climbing and Mountaineering Federation, commonly known by its French name Union Internationale des Associations d'Alpinisme (UIAA, lit. ''International Union of Alpine Clubs''), was founded in August 1932 in Chamonix, France when 20 mountaineering associations met for an alpine congress. Count Charles Egmond d’Arcis, from Switzerland, was chosen as the first president and it was decided by the founding members that the UIAA would be an international federation which would be in charge of the "study and solution of all problems regarding mountaineering". The UIAA Safety Label was created in 1960 and was internationally approved in 1965 and currently (2015) has a global presence on five continents with 86 member associations in 62 countries representing over 3 million people. After the 2022 Russian invasion of Ukraine, the UIAA suspended all UIAA officials from Russia, and delegates from the Russian Mountaineering Federation (RMF) and Russian officials and at ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vordere Brandjochspitze
The Vordere Brandjochspitze is a peak, high, in the Nordkette in the Karwendel range and is one of its highest and most striking peaks. In its immediate vicinity to the north-northwest is its sister summit, the Hintere Brandjochspitze, which is about 40 metres higher. To the south a prominent arête runs over to the ''Brandjochkreuz'' () and the ''Achselkopf'' () and down to the Innsbruck quarter of Hötting. To the east, the main ridge of the Nordkette runs over to Frau Hitt. Ascents The easiest ascent, the Julius Pock Way, runs from the Frau Hitt Saddle (), which may be reached on various routes from Innsbruck or Scharnitz Scharnitz is a municipality in the district of Innsbruck-Land in the Austrian state of Tyrol located north of Innsbruck and from Seefeld in Tirol on the German border. It is one of the largest municipalities and has 10 parts: Au, Eisack, Gieße ... through the ''Gleirschtal'' and ''Kleinkristental'' valleys, up to the summit on a UIAA grade I, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kleiner Solstein
The Kleiner Solstein is a mountain, high, in the Nordkette in the Karwendel Alps in the Austrian state of Tyrol. Despite its name ("Small Solstein") it towers above its western neighbour, the Großer Solstein ("Great Solstein") () by almost and is thus the highest summit in the Nordkette. The southern side of the Kleiner Solstein facing the Inn valley is characterised by ''schrofen'' and steep-sided cirques. To the north it plummets in a rock face up to high towards the valley of ''Großkristental'', which runs from the Gleirsch valley in a southwesterly direction to the Erl Saddle. Ascent The normal route to the Kleiner Solstein runs from the saddle between the Großer and Kleiner Solstein, initially crossing a small ridge of rock (''Felsrippe'') then over ''schrofen'' from the south to the flat summit ridge following a waymarked route to the top. The route to the saddle between the two peaks may be reached either from the Solsteinhaus and the Großer Solstein or on two ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wetterstein Limestone
The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians. The formation is composed of mostly reefal limestones and dolomites, the latter the result of widespread diagenesis. In many areas there is a frequent alternation of limestone and dolomite facies. Local variants to indicate the Wetterstein Formation include german: Wettersteinkalk (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation rea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
