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Napfspitze (Ahrntal)
The Napfspitze (, also called the ''Dreiecketer'', it, Cima Cadini), is a peak on the main chain of the Zillertal Alps and on the border between the Austrian federal state of Tyrol and the Italian province of South Tyrol. Geography The Napfspitze lies north of St. Peter in the Tauferer Ahrntal valley and south of the Zillergrund bottom. The long ridge of ''Riblerkamm'' branches from the main chain of the Zillertal Alps at the Napfspitze heading in a northerly direction. Along the ridge are two more peaks that exceed 3,000 metres in height: an unnamed 3,103-metre-summit and, further south, the ''Hohe Warte'' at 3,095 metres. On the northeastern side of the Napfspitze lies a small glacier, the ''Grießbachjochkees''. First ascent The mountain was first climbed by R. Seyerlein and St. Kirchner in the year 1880; they reached the summit via the southern arête.Goedecke (2004), p.156. Ascent options The normal route runs from the Zillergrund to the north of the Napfspi ... [...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] |
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] |
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 may refer 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, Ande ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waymark
Trail blazing or way marking is the practice of marking paths in outdoor recreational areas with signs or markings that follow each other at certain, though not necessarily exactly defined, distances and mark the direction of the trail. A blaze in the beginning meant "a mark made on a tree by slashing the bark" (''The Canadian Oxford Dictionary''). Originally a waymark was "any conspicuous object which serves as a guide to travellers; a landmark" (''Oxford English Dictionary''). There are several ways of marking trails, including paint, carvings, affixed markers, posts, flagging, cairns, and crosses, with paint being the most widely used. Types of signage Paint A painted marking of a consistent shape or shapes (often rectangular), dimension and colour or combination of colours is used along the trail route. The system by which blazes are used to signify turns and endpoints in trails (see below) strongly favors the use of paint blazes. European countries usually use systems ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
UIAA Scale
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 ascensioni ... [...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] |
First Climbed
In mountaineering, a first ascent (abbreviated to FA in guide books) is the first successful, documented attainment of the top of a mountain or the first to follow a particular climbing route. First mountain ascents are notable because they entail genuine exploration, with greater risks, challenges and recognition than climbing a route pioneered by others. The person who performs the first ascent is called the first ascensionist. In free climbing, a first ascent (or first free ascent, abbreviated FFA) of a climbing route is the first successful, documented climb of a route without using equipment such as anchors or ropes for aiding progression or resting. History The details of the first ascents of even many prominent mountains are scanty or unknown; sometimes the only evidence of prior summiting is a cairn, artifacts, or inscriptions at the top. Today, first ascents are generally carefully recorded and usually mentioned in guidebooks. The term is also used when referrin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tauferer Ahrntal
The Tauferer Ahrntal denotes the valley of the Ahr ( it, Aurino) River, a tributary valley of the Puster Valley in South Tyrol, Italy. It is commonly divided into the Tauferer Tal (''Val di Tures''), stretching from the confluence with the Rienz River near Bruneck up to Sand in Taufers, and the Ahrntal (''Valle Aurina'') proper up to the source in Prettau. Geography The valley in the Central Eastern Alps forms the northeasternmost part of South Tyrol close to the Austrian border, separating the Zillertal Alps in the north and west from the Hohe Tauern range (Rieserferner Group) in the south and east. The municipalities in the valley are Gais, Sand in Taufers, Ahrntal, and Prettau, the northernmost ''comune'' of Italy. The municipality of Mühlwald is congruent with a northwestern side valley of the Tauferer Ahrntal including the Neves Reservoir. In the southeast, the Reinbach stream joins the Ahr near Sand in Taufers; the area around the village of Rein in Taufers is part ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rauhkofel
The Rauhkofel or Rauchkofel (, it, Monte Fumo) is a summit on the main crest of the Zillertal Alps, which forms the border between the Austrian state of Tyrol and the Italian province of South Tyrol. The name of the mountain ("rugged peak") comes from the rugged appearance of the granite blocks that form the summit . The Rauhkofel rises above its neighbouring peaks on the main Zillertal ridge considerably and it is considered the best lookout mountain in the eastern Zillertal Alps.Goedecke: ''3000er in den Nordalpen.'' page 155, see literature The east and south arêtes of the Rauhkofel are part of the main crest of the Zillertal Alps. Another ridge runs from the summit heading northwest; on its continuation at a distance of just under two kilometres is the Kleinspitze (3,172 m). North of the summit are the remnants of the Rauhkofelkees glacier. At the southwestern foot of the peak is the Waldner See, the largest lake in the Ahrntal valley. Ascent The summit is almost exclus ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ahrntal
Ahrntal (; it, Valle Aurina ) is a ''comune'' (municipality) in South Tyrol in northern Italy, located about northeast of the city of Bolzano (''Bozen''), on the border with Austria. Geography Ahrntal borders the following municipalities: Mühlwald, Prettau, Sand in Taufers, Brandberg (Austria), Finkenberg (Austria), and Mayrhofen (Austria). Frazioni The municipality of Ahrntal contains the ''frazioni'' (subdivisions, mainly villages and hamlets) Luttach (Lutago), Steinhaus (Cadipietra), St. Jakob (San Giacomo), St. Johann (San Giovanni), St. Peter (San Pietro) and Weißenbach (Riobianco). Weißenbach is composed of picturesque alpine farmhouses, grouped around the foaming white glacial stream from which its name is derived. With a population of around 550, it sits at an elevation of above sea level. Topography To the north, west and southwest the municipality is surrounded by the Zillertal Alps. The main chain of these Alps at the head of the valley also forms the border ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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