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Weißeck
The Weißeck () is the highest mountain in the Radstadt Tauern range in Austria and is popular, both as a ski touring destination in winter and a climbing peak in summer. It gets its name (which means "white corner") from the mighty block of light-coloured Wetterstein dolomite of which the mountain is made. The summit of the Weißeck is located on the municipal boundary between Muhr, in the national park, and Zederhaus, in the nature park. Bases for tours to the Weißeck are, on one side, the Riedingtal valley in Zederhaus, and, on the other, the Stickler Hut (1,752 m) in the upper Mur valley. The normal route from the Rieding gap along the western ridge to the top is signed and only requires a little sure-footedness, but is generally an easy climbing grade. There are several legends about the Weißeck. The best-known is about the Weißeck dog. The Weißeck is also popular with mineral collectors; since time immemorial it has been a well-known site for finds of fluorite ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Radstadt Tauern
The Radstadt Tauern (german: Radstädter Tauern) are a subrange of the Central Eastern Alps in Austria. Together with the Schladming Tauern, the Rottenmann and Wölz Tauern and the Seckau Tauern the Radstadt Tauern form the major range of mountains known as the Low Tauern. The mountains are found in the southeast of the Austrian state of Salzburg, between the upper reaches of the Enns and Mur rivers. Geography Location The Radstadt Tauern form the westernmost part of the Low Tauern range. They are bounded to the southwest by the High Tauern, to the northwest by the Salzburg Pongau region, and to the east by the Schladming Tauern. Their name is derived from the historic town of Radstadt in the Enns valley. Neighbouring ranges The Radstadt Tauern border on the following other mountain ranges of the Alps: * Schladming Tauern (to the east) * Nock Mountains (Gurktal Alps; to the southeast) * Ankogel Group (High Tauern; to the west) * Salzburg Slate Alps (to the north) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zederhaus
Zederhaus is a municipality of the Tamsweg District in the Austrian state of Salzburg. Geography The Zederhaus Valley is located in the northwestern part of the Salzburg ''Lungau'' region, on the southern slopes of the Lower Tauern mountain range, reaching up to Mt Weißeck at . The crest of the Radstadt Tauern in the north separates it from the ''Pongau'' region. From the Rieding high valley, today a protected area, the Zederhaus creek flows southeastwards, reaching the upper Mur River at neighbouring Sankt Michael. The smaller village stream passes several historic watermills. The sparsely settled municipal area, the largest in the Tamsweg District, comprises the cadastral communities of Lamm, Rothenwand, Wald, and Zederhaus proper. The valley today is characterised by the construction of the Tauern Autobahn in the 1970s, a major north-south road connection which is part of the European route E55. The south portal of the Tauern Road Tunnel, one of the longest in Austria, i ... [...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] |
Wetterstein Dolomite
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 Limestone Alps, Northern and Southern Limestone Alps and in the Western Carpathians. The formation is composed of mostly coral reef, reefal limestones and dolomite (rock), 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ladinian
The Ladinian is a stage and age in the Middle Triassic series or epoch. It spans the time between Ma and ~237 Ma (million years ago). The Ladinian was preceded by the Anisian and succeeded by the Carnian (part of the Upper or Late Triassic). The Ladinian is coeval with the Falangian regional stage used in China. Stratigraphic definitions The Ladinian was established by Austrian geologist Alexander Bittner in 1892. Its name comes from the Ladin people that live in the Italian Alps (in the Dolomites, then part of Austria-Hungary). The base of the Ladinian Stage is defined as the place in the stratigraphic record where the ammonite species '' Eoprotrachyceras curionii'' first appears or the first appearance of the conodont ''Budurovignathus praehungaricus''. The global reference profile for the base (the GSSP) is at an outcrop in the river bed of the Caffaro river at Bagolino, in the province of Brescia, northern Italy.The GSSP was established by Brack ''et al.'' (2005) The t ... [...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] |
Muhr (Salzburg)
Muhr is a municipality of the Tamsweg District in the Austrian state of Salzburg. Geography It is located in a southwestern valley of the Salzburg Lungau region at the source of the river Mur River, between the Hohe Tauern and the Niedere Tauern ranges of the Central Eastern Alps. The mountains of the Ankogel Group in the south separate it from the state of Carinthia. The municipal area comprises the Katastralgemeinden of Vordermuhr, Hintermuhr, and Schellgaden. In the west it adjoins the Hohe Tauern national park. History Like the eponymous river, its name may derive from Proto-Celtic ''mori'', 'water' (compare Welsh ''môr'' or English mere). The Lungau region belonged to the Prince-Archbishopric of Salzburg until its secularisation in 1803. The settlement was first mentioned about 1470, the St. Rupert Church in a 1523 deed. Muhr once was a mining area for gold and arsenic. A local custom is the annual procession with ''Prangstangen'', up to 8 m (26 ft) high woode ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normal Route
A normal route or normal way (french: voie normale; german: Normalweg) is the most frequently used route for ascending and descending a mountain peak. It is usually the simplest route. Overview In the Alps, routes are classed in the following ways, based on their waymarking, construction and upkeep: * Footpaths (''Fußwege'') *Hiking trails (''Wanderwege'') * Mountain trails (''Bergwege'') * Alpine routes (''Alpine Routen'') *Climbing routes (''Kletterrouten'') and High Alpine routes (''Hochalpine Routen'') in combined rock and ice terrain, (UIAA) graded by difficulty Sometimes the normal route is not the easiest ascent to the summit, but just the one that is most used. There may be technically easier variations. This is especially the case on the Watzmannfrau, the Hochkalter and also Mount Everest. There may be many reasons these easier options are less well-used: * the simplest route is less well known than the normal route (Watzmannfrau). * the technically easiest route is mor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sure-footedness
Sure-footedness is the ability, especially when hiking or mountain climbing, to negotiate difficult or rough terrain safely. Such situations place demands on a person's coordination and reserves of strength as well as requiring sufficient appreciation of the terrain. A person who is sure-footed is thus unlikely to slip or stumble, and will have a good head for heights when required. On many hiking trails and mountain tours, sure-footedness is assumed to be a prerequisite without ever being defined. The term is frequently used in the literature presumably to ensure that the reader is made sufficiently aware that, under certain circumstances, one false step may lead to serious consequences. Required attributes Although there is no standard definition of sure-footedness, [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluorite
Fluorite (also called fluorspar) is the mineral form of calcium fluoride, CaF2. It belongs to the halide minerals. It crystallizes in isometric cubic habit, although octahedral and more complex isometric forms are not uncommon. The Mohs scale of mineral hardness, based on scratch hardness comparison, defines value 4 as fluorite. Pure fluorite is colourless and transparent, both in visible and ultraviolet light, but impurities usually make it a colorful mineral and the stone has ornamental and lapidary uses. Industrially, fluorite is used as a flux for smelting, and in the production of certain glasses and enamels. The purest grades of fluorite are a source of fluoride for hydrofluoric acid manufacture, which is the intermediate source of most fluorine-containing fine chemicals. Optically clear transparent fluorite lenses have low dispersion, so lenses made from it exhibit less chromatic aberration, making them valuable in microscopes and telescopes. Fluorite optics are also ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
