Three-thousanders Of Antarctica
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Three-thousanders Of Antarctica
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, Andes) i ...
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Mountain
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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Piz Boe
Piz may refer to: * Piz Gloria, a mountain-top restaurant in Switzerland * Piz Buin, a mountain * Piz Dolf, a mountain * Piz Segnas, a mountain * Piz Buin (brand), a suncream brand * Piz (river), a river in Russia * Stosh "Piz" Piznarski ''Veronica Mars'' is an American television series created by Rob Thomas (writer), Rob Thomas. The series premiered on September 22, 2004, during UPN's last two years, and ended on May 22, 2007, after a season on UPN's successor, The CW Televisi ..., a character from Veronica Mars * PIZ (Compression Method), a compression method built into OpenEXR {{disambiguation ...
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Großer Hafner
Großer Hafner is a high partly-glaciated mountain of the Ankogel Group in the High Tauern range, located at the border between the Austrian states of Carinthia and Salzburg. It is the easternmost three-thousander peak (with at least prominence) of the range, and also in the entire Alps. Geography The Hafner massif rises between the Radstadt Tauern and the Mur valley of the Salzburg Lungau region in the north and the Carinthian Malta valley in the south. It comprises Kleiner Hafner () and Großer Sonnblick () subpeaks, lying just to the southeast. In the south, the Malta valley leads to the Reißeck Group, while in the east, Katschberg Pass separates it from the neighbouring Gurktal Alps. The Hafner summit marks the eastern rim of the geological Hohe Tauern window. It has three glaciers, with the largest on its north face, and also comprises numerous Alpine lakes. The high mountain region, formerly a mining area, recently has become a centre of hydropower economy, most nota ...
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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 ...
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Silvretta Panorama Wiki Mg-k
The Silvretta Alps are a mountain range of the Central Eastern Alps shared by Tirol, Vorarlberg (both in Austria) and Graubünden (Switzerland). The Austrian states of Tirol and Vorarlberg are connected by a pass road (Silvretta Hochalpenstraße at 2032 m). The majority of the peaks are elevated above three thousand metres and are surrounded by glaciers. Thus, the area is also known as the "Blue Silvretta". Borders According to the Alpine Clubs, the Silvretta Alps are outlined from other groups by the following borders: St. Gallenkirch - Ill river as far as Partenen - Zeinisjoch - Zeinisbach - Paznauntal as far as Ischgl - Fimbertal - Fimber Pass - Val Chöglias - Val Sinestra - Inn River from the mouth of the Branclabach to the mouth of the Susasca - Val Susasca - Flüela Pass - Davos - Wolfgang, Switzerland, Wolfgang - Laretbach - Klosters - Schlappinbach - Schlappiner Joch - Valzifensbach - Gargellental - St. Gallenkirch. The Silvretta Alps are surrounded by the Rä ...
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Aiguille Du Midi
The Aiguille du Midi () is a mountain in the Mont Blanc massif within the French Alps. It is a popular tourist destination and can be directly accessed by cable car from Chamonix that takes visitors close to Mont Blanc. Cable car The idea for a cable car to the summit, the ''Téléphérique de l'Aiguille du Midi'', was originally proposed around 1909, but did not come into operation until 1955 when it held the title of the world's highest cable car for about two decades. It still holds the record as the highest vertical ascent cable car in the world, from . There are two sections: from Chamonix to ''Plan de l'Aiguille'' at and then directly, without any support pillar, to the upper station at 3,777 m (the building contains an elevator to the summit). The span of the second section is measured directly, but only measured horizontally. Thus it remains the second longest span width, measured directly. The cable car travels from Chamonix to the top of the Aiguille du Midi – ...
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Klein Matterhorn
The Klein Matterhorn (sometimes translated as ''Little Matterhorn'') is a peak of the Pennine Alps, overlooking Zermatt in the Swiss canton of Valais. At above sea level, it is the highest place in Europe that can be reached by aerial tramway or gondola lift, as well as by any other means of transport. The Klein Matterhorn is part of the Breithorn massif and overlooks on its south side the almost equally high flat glacier named ''Breithorn Plateau'', just north of the international border with Italy. The name "Klein Matterhorn" is a reference to its much larger neighbour, the Matterhorn, which lies away across the Theodul Pass. The Klein Matterhorn, with the adjacent ski-lifts to the slightly higher Gobba di Rollin, is also a year-round ski area, marketed as "Matterhorn Glacier Paradise", and part of the international ski area between Zermatt and Breuil-Cervinia. Fast ascents to a height above will frequently lead to headaches or other symptoms of altitude sickness with sens ...
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Acclimatisation
Acclimatization or acclimatisation ( also called acclimation or acclimatation) is the process in which an individual organism adjusts to a change in its environment (such as a change in altitude, temperature, humidity, photoperiod, or pH), allowing it to maintain fitness across a range of environmental conditions. Acclimatization occurs in a short period of time (hours to weeks), and within the organism's lifetime (compared to adaptation, which is evolution, taking place over many generations). This may be a discrete occurrence (for example, when mountaineers acclimate to high altitude over hours or days) or may instead represent part of a periodic cycle, such as a mammal shedding heavy winter fur in favor of a lighter summer coat. Organisms can adjust their morphological, behavioral, physical, and/or biochemical traits in response to changes in their environment. While the capacity to acclimate to novel environments has been well documented in thousands of species, researche ...
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Ortler Alps
The Ortler Alps ( it, Ortles-Cevedale ; german: Ortler-Alpen; rm, Alps da l'Ortler) are a mountain range of the Southern Limestone Alps mountain group in the Central Eastern Alps, in Italy and Switzerland. Geography The Ortler Alps are separated from: # the Sesvenna Alps in the north by the Ofen Pass and the Val Müstair # the Livigno Alps in the southwest by the Passo di Fraéle and the Adda valley (Valtellina) # the Adamello-Presanella Alps in the south by the Tonale Pass # the Ötztal Alps in the north-east by the upper Adige valley (Vinschgau). The part west of the Gavia Pass is also called Sobretta-Gavia Group. The Ortler Alps are drained by the rivers Adda, Oglio, Adige and its tributary Noce. Peaks The main peaks of the Ortler Alps are: Mountain passes The main mountain pass A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key ...
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Monte Vioz
Monte Vioz is a mountain in Northern Italy, on the border between Lombardy and Trentino Trentino ( lld, Trentin), officially the Autonomous Province of Trento, is an autonomous province of Italy, in the country's far north. The Trentino and South Tyrol constitute the region of Trentino-Alto Adige/Südtirol, an autonomous region .... It is located in the Ortler Alps. The Forni glacier (Ghiacciaio dei Forni) lies on the west side of Monte Vioz, flowing into the Valle dei Forni. On the east side of the mountain lies the glacier Vedretta Rossa, and the smaller glacier Vedretta di Vioz is on the south side of the mountain. The most popular climbing route is from the trailhead at Pèio Fonti, a cable car to the refuge Doss dei Cembri, and a 1,350 metre climb from there. below the summit is the Mantova del Vioz refuge. The best season to climb is from June to September.
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Wallis Alps
The Pennine Alps (german: Walliser Alpen, french: Alpes valaisannes, it, Alpi Pennine, la, Alpes Poeninae), also known as the Valais Alps, are a mountain range in the western part of the Alps. They are located in Switzerland (Valais) and Italy (Piedmont and the Aosta Valley). The Pennine Alps are amongst the three highest major subranges of the Alps, together with the Bernese Alps and the Mont Blanc massif. Geography The Italian side is drained by the rivers Dora Baltea, Sesia and Toce, tributaries of the Po. The Swiss side is drained by the Rhône. The Great St Bernard Tunnel, under the Great St Bernard Pass, leads from Martigny, Switzerland to Aosta. Morphology The main chain ( watershed between the Mediterranean Sea and the Adriatic Sea) runs from west to east on the border between Italy (south) and Switzerland (north). From Mont Vélan, the first high summit east of St Bernard Pass, the chain rarely goes below 3000 metres and contains many four-thousanders such as Matt ...
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