The Breithorn is a mountain range of the Pennine Alps with its highest peak of the same name, located on the border between Switzerland and Italy. It lies on the chain of the Alps, approximately halfway between the Matterhorn and Monte Rosa and east of the Theodul Pass. Most of the massif is glaciated and includes several peaks, all located east of the main summit, the Central Breithorn, the western Breithorn Twin, the Gendarm. The main summit is distinguished by the name Western Breithorn. The nearest settlements are Zermatt and St-Jacques, the Breithorn is considered the most easily climbed 4,000 m Alpine peak. This is due to the Klein Matterhorn cable car which takes climbers to over 3,820 m from Zermatt for a starting point. The standard route is from the Italian side of the mountain, inexperienced mountaineers may run into severe difficulty if caution is not taken near cornices or in bad weather. For experienced climbers wanting more of a challenge, the traverse of the Breithorn crest is another option.
The Breithorn was first climbed in 1813 by Henry Maynard, Joseph-Marie Couttet, Jean Gras, Jean-Baptiste Erin, media related to Breithorn at Wikimedia Commons Breithorn on SummitPost Breithorn on Peakware - photos Breithorn on 4000er. de Breithorn on WinterClimb. com - photos, practical info
Castor is a mountain in the Pennine Alps on the border between Valais and the Aosta Valley in Italy. It is the higher of a pair of peaks, the other being Pollux. Castors peak is at an elevation of 4,223 m and it is separated from Pollux by a pass at 3,847 m, named Passo di Verra in Italian and Zwillingsjoch in German. Ascents are usually made from the alpine hut Capanna Quintino Sella on the Italian side, by means of the Felikjoch, from the Swiss side, ascents start from Klein Matterhorn and go by way of the Italian glacier Grand Glacier of Verra and the mountains west flank. The first ascent was made on August 23,1861, Castor and Pollux are a pair of summits in Yellowstone National Park in Wyoming, USA. Located in the Absaroka Range, Castor is 3,308 m,65 m lower than its twin
The Dent Blanche is a mountain in the Pennine Alps, lying in the canton of Valais in Switzerland. With its 4,357 metres -high summit, it is one of the highest peaks in the Alps, the original name was probably Dent dHérens, the actual name of the nearby Dent dHérens which does not overlook the Val dHérens. The nearby north face of the Dent dHérens is glaciated while the Dent Blanche holds much less snow, in fact on older maps, in the area where lie both summits, only the name Weisszahnhorn was indicated, the French name appearing in 1820 only. The actual names are official since the completion of the Dufour map in 1862, the summit of Dent Blanche is an important geographic place as it is the converging point of three ridges. The three valleys separated by them are the Val dHérens, Val dAnniviers and Mattertal, the respective villages of Evolène, Zinal and Zermatt lie approximatively at the same distance of the mountain. The four ridges encompass almost exactly the four cardinal directions, the west ridge is named Arête de Ferpècle and the east ridge is named Arête des Quatre Ânes.
The Col de la Dent Blanche lies at the foot of the northern ridge, the Dent Blanche Hut lies at the foot of the southern ridge which is used as the normal route. The region around Dent Blanche consists of many 4000 metres peaks, the Ober Gabelhorn, Dent dHérens and Matterhorn are the closest high summits. The first ascent was made via the ridge, which is the less difficult route to the summit. On 12 July 1862, T. S. Kennedy, after an attempt on the east face of the unconquered Matterhorn, almost reached the summit with the guides Peter Taugwalder, but after a minor accident, Peter Taugwalder refused to go any higher. Kennedy would finally reach the only a few days later, on July 18,1862 with W. Wigram, J. Croz and J. Konig. A route on the west ridge was opened on 11 August 1882 by John Stafford Anderson and G. P. Baker, with guides Alois Pollinger of St. Niklaus in the canton Valais and Ulrich Almer. They started from the Mountet Hut and arrived at the summit after a difficult 12 hours climbing on a ridge overlooking the north face.
As Almer said on the summit, We are four asses, the north ridge was explored in 1899. On 28 August O. G. Jones, F. W. Hill with guides E. Furrer, zurbriggen and J. Vuignier headed to the summit but they fell and only Hill survived. He reached alone the summit and a storm forced him to make a bivouac and he could report the news of the fatal accident in Zermatt only two days later. The first ascent of the face is attributed to K. Schneider. They climbed from the part at the base of the face to the summit
The Alphubel is a mountain of the Swiss Pennine Alps, located between the valleys of Zermatt and Saas in the canton of Valais. It is part of the Mischabel range, which culminates at the Dom, the summit of the Alphubel consists of a large ice-covered plateau, part of the Fee Glacier on its east side. The west side of the mountain is rocky and much steeper. The nearest settlements are Täsch and Saas-Fee, media related to Alphubel at Wikimedia Commons The Alphubel on SummitPost The Alphubel on Mount Wiki
The Bishorn is a mountain in the Pennine Alps in Switzerland, just north of the Weisshorn. The mountain has two summits, separated by a 600-metre easy-angled snow ridge. The west and higher summit, first ascent by G. S. Barnes and R. Chessyre-Walker with guides Joseph Imboden, the east summit, first ascent by Elizabeth Burnaby with guides Joseph Imboden and Peter Sarbach on 6 May 1884. Huts serving the peak are the Cabane de Tracuit and the Turtmann hut, access to both huts is snow-free in summertime. The Tracuit hut is accessed from the Zinal valley, a long and demanding walk of around five hours from the village to the hut. The Turtmann hut is used for climbing the Barrhorn and the Brunegghorn. Note that climbing the Bishorn from the Turtmann hut requires a far longer glacier walk through sections with numerous crevasses, the access roads to the huts are from the Rhone valley in the north. The road to Zinal starts at Sierre, and the road starts from Turtmann village. In both cases these are good and attractive mountain roads typical of the area, dumler and Willi P.
Burkhardt, The High Mountains of the Alps, Diadem,1994 The Bishorn on SummitPost
The Pennine Alps, known as the Valais Alps, and formerly called Alpes Poeninae, are a mountain range in the western part of the Alps. They are located in Switzerland and Italy, the Italian side is drained by the rivers Dora Baltea 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. The main chain runs from west to east on the border between Italy and Switzerland, 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 Matterhorn or Monte Rosa. Unlike many other ranges, the higher peaks are often located outside the main chain
Lyskamm, known as Silberbast, is a mountain in the Pennine Alps lying on the border between Switzerland and Italy. It consists of a ridge with two distinct peaks. The mountain has gained a reputation for seriousness because of the many cornices lying on the ridge, because of its modest prominence, Liskamm is sometimes considered to be part of the extended Monte Rosa group. The northern side of the mountain is an impressive 1,100 metres ice-covered wall, the gentler southern side rises only a few hundred metres above the glacier of the same name, Lysgletscher. The eastern and higher of the two peaks is 4,527 m, and was first ascended in 1861 from the Lisjoch up the east ridge by a 14-man team led by J. F. Hardy, others in the party included A. C. Ramsey, F. Sibson, T. Rennison, J. A. Hudson, C. H. Pilkington, the guides were Franz Josef Lochmatter of St. Niklaus in the canton Valais, J. -P. Cachet, K. Kerr, S. Zumtaugwald, P. and J. -M, the ridge as a whole was first traversed three years by Leslie Stephen, Edward N.
Buxton, Jakob Anderegg and Franz Biener. The first attempt to climb the imposing north-east face was made in 1880 by the brothers Kalbermatten and they were carried down to the glacier by an avalanche but they survived the accident. On 9 August 1890, L. Norman-Neruda with guides Christian Klucker and J. Reinstadler were the first to reach the summit by the north face, the first winter ascent of this route was made on 11 March 1956 by C. In 1907, Geoffrey Winthrop Young and his guide traversed the whole ridge two times, Young wanted to traverse the ridge from the Nordend to the Breithorn. They started from Riffelalp at midnight and finished the traverse of the Monte Rosa massif at midday, but after the traverse of the Liskamm and Castor the guide was too tired. Young, who was disappointed, convinced him to go back by the Lisjoch before descending to Zermatt. Young even wanted to back to the Nordend but his guide refused to prolong the journey. The normal route starts from the Lisjoch, which can be accessed from the Gnifetti Hut or from the Monte Rosa Hut, the route follows the route taken by the first ascensionist.
The mountain is climbed as a traverse from the Feliksjoch. The traverse consists mostly of a narrow, snow-covered ridge, with some scrambling over rocks. W. E. Hall The fatal accident on the Lyskamm, Alpine Journal,5, 23–32 Liskamm on Peakbagger. com Liskamm on SummitPost Italian route account from south - Czech and English
A mountain range is a geographic area containing numerous geologically related mountains. A mountain system or system of ranges, sometimes is used to combine several geological features that are geographically related. Mountain ranges are usually segmented by highlands or mountain passes and valleys, individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, most geologically young mountain ranges on the Earths land surface are associated with either the Pacific Ring of Fire or the Alpide Belt. The Andes is 7,000 kilometres long and is considered the worlds longest mountain system. The Alpide belt includes Indonesia and southeast Asia, through the Himalaya, the belt includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, mountain ranges outside of these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Altai Mountains and the Hijaz Mountains.
If the definition of a range is stretched to include underwater mountains. The mountain systems of the earth are characterized by a tree structure, the sub-range relationship is often expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, and the White Mountains and the Blue Ridge Mountains are children of the Appalachians. The position of mountains influences climate, such as rain or snow, when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the side, it warms again and is drier. Often, a shadow will affect the leeward side of a range. Mountain ranges are constantly subjected to forces which work to tear them down. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills, rivers are traditionally believed to be the principle erosive factor on mountain ranges, with their ability of bedrock incision and sediment transport.
The rugged topography of a range is the product of erosion. The basins adjacent to a mountain range are filled with sediments which are buried and turned into sedimentary rock. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example and this mass of rock was removed as the range was actively undergoing uplift
The Strahlhorn is a mountain of the Swiss Pennine Alps, located south of Saas-Fee and east of Zermatt in the canton of Valais. It lies on the range separates the Mattertal from the Saastal and is located approximately halfway between the Rimpfischhorn and the Schwarzberghorn. Dumler and Willi P. Burkhardt, The High Mountains of the Alps, Diadem,1994 Strahlhorn