The Ober Gabelhorn is a mountain in the Pennine Alps in Switzerland, located between Zermatt and Zinal. The Ober Gabelhorn lies in the Swiss canton of Valais at the end of the Zinal valley. It rises, together with the Dent Blanche and the Zinalrothorn, on the south side lies the Zmutt Glacier in the valley of Zmutt, which extends west of Zermatt. The Ober Gabelhorn has a shape, similar to the nearby Matterhorn. Only the smooth face is completely glaciated, the other faces being mostly rocky. The south-west ridge is called the Arbengrat while the north-north-west ridge is the Arête du Coeur, the south-east ridge looking over the Ober Gabeljoch is the Gabelhorngrat. The Wellenkuppe is a prominence on the north-east ridge, it is usually climbed as part of the normal route. Huts serving the peak are the Rothorn Hut, the Grand Mountet Hut, the first ascent was by A. W. Moore, Horace Walker and Jakob Anderegg on 6 July 1865, via the east face. The second ascent of the peak, and the first by the north-north-west ridge, was one day by Lord Francis Douglas, Peter Taugwalder.
At the time of their ascent they were not aware of Moore and Taugwalder made several attempts before they reached the summit. P. Inäbnit accompanied them on the first attempt from the south-east ridge and they didnt have enough time to go higher than the base of the mountain. On the second attempt they reached the Wellenkuppe on the north-east ridge and they finally reached the summit on their third attempt. They were disconcerted to see some footprints on the east face, not aware of the dangers that might have made the previous expedition turn back, they sat down on the summit to have lunch. Suddenly an avalanche started and everything on the summit began to fall away from them and Taugwalder were swept away, but they were roped to Viennin who was a little distance below the summit. Viennin was able to belay Taugwalder and Douglas with the rope, Francis Douglas returned to Zermatt, and was killed a week on 14 July on the first ascent of the Matterhorn. The Arbengrat was first climbed in 1874 by H. S.
Hoare and E. Hulton with guides J. von Bergen, P. Rubi and J. Moser. The route on the Gabelhorngrat was opened three years by J. Walker Hartley, W. E. Davidson, P. Rubi and J. Juan. The north face, similar to but rather steeper than the north-east face of the Lenzspitze, was first climbed on 30 July 1930 by H. Kiener and they started from Zermatt at midnight and made a direct 2, 000-metre ascent to the Triftjoch
The Weisshorn is a major peak of the Alps and Switzerland, culminating at 4,506 metres above sea level. It is part of the Pennine Alps and is located between the valleys of Anniviers and Zermatt in the canton of Valais, in the latter valley, the Weisshorn is one of the many 4000ers surrounding Zermatt, with Monte Rosa and the Matterhorn. The Weisshorn was first climbed in 1861 from Randa by the Irish physicist John Tyndall, the Weisshorn Hut is used on the normal route. The Weisshorn is considered by mountaineers to be the most beautiful mountain in the Alps and Switzerland for its pyramidal shape. In April and May 1991, two consecutive rockslides took place from a cliff above the town of Randa on the east side of the massif, the Weisshorn is situated in the southern canton of Valais, about 25 km southwards from the Rhone between Sierre and Visp. The Weisshorn faces the slightly higher Dom across the Mattertal, with the village of Randa 3100 metres below these two summits, after the Dom, the Weisshorn is the second-highest Alpine summit situated completely out the main chain and fully within Switzerland.
On both sides of the Weisshorn range, the end up in the Rhone, through the Navissence. The Weisshorn has a shape and its faces are separated by three ridges descending steeply from the summit. Two of these are nearly in a line, one running approximately north. The third ridge is nearly at right angles to two, running almost due east. In the compartment between the northern and eastern spurs lies the Bis Glacier and it is connected with the summit by long and extremely steep slopes of snow. In the compartment between the eastern and southern spurs lies the Schali Glacier, ranges of steep rocks rise round the whole basin of this glacier, except in one or two places where they are interrupted by couloirs of snow. Finally, on the side the mountain presents one gigantic face of rocky precipice. This face rises above the Weisshorn Glacier and the Moming Glacier, the northern spur forks out at a considerable distance below the summit into two branches enclosing the Turtmann Glacier. The eastern branch connects the mountain with the Bishorn, across the Weisshornjoch, the Weisshorn is the culminating point of the Dent Blanche nappe, a klippe belonging to the Austroalpine nappes.
The mountain is composed of gneisses, the west face is composed of sedimentary rocks from the cretaceous period. The mountain was first climbed on 19 August 1861 by the 29-year-old physicist John Tyndall, with guides J. J. Bennen and their itinerary corresponds to the normal route for climbing the mountain today, the east ridge, starting from the Weisshorn Hut. In 1860 an attempt was made by C. E. Mathews by the southern face and he came to Zermatt with Melchior Anderegg, and engaged Johann Kronig as second guide
The Matterhorn is a mountain of the Alps, straddling the main watershed and border between Switzerland and Italy. It is a huge and near-symmetrical pyramidal peak in the extended Monte Rosa area of the Pennine Alps, whose summit is 4,478 metres high, making it one of the highest summits in the Alps and Europe. The four steep faces, rising above the glaciers, face the four compass points and are split by the Hörnli, Leone. The mountain overlooks the Swiss town of Zermatt in the canton of Valais to the north-east, just east of the Matterhorn is Theodul Pass, the main passage between the two valleys on its north and south sides and a trade route since the Roman Era. The Matterhorn was studied by Horace-Bénédict de Saussure in the eighteenth century. It remained unclimbed after most of the other great Alpine peaks had been attained, the first ascent of the Matterhorn was finally made in 1865 from Zermatt by a party led by Edward Whymper but ended disastrously when four of its members fell to their deaths on the descent.
That climb and disaster, portrayed in films, marked the end of the golden age of alpinism. The north face was not climbed until 1931, and is amongst the three biggest north faces of the Alps, known as the ‘The Trilogy’, the west face, which is the highest of the four, was completely climbed only in 1962. It is estimated that over 500 alpinists have died on the Matterhorn since the first climb in 1865, making it one of the deadliest peaks in the world. The current shape of the mountain is the result of erosion due to multiple glaciers diverging from the peak, such as the Matterhorn Glacier at the base of the north face. Sometimes referred to as the Mountain of Mountains, the Matterhorn has become an emblem of the Swiss Alps. Since the end of the 19th century, when railways were built in the area, each year a large number of mountaineers try to climb the Matterhorn from the Hörnli Hut via the northeast Hörnli ridge, the most popular route to the summit. Many trekkers undertake the 10-day-long circuit around the mountain, the Matterhorn is part of the Swiss Federal Inventory of Natural Monuments since 1983.
Decomposing Matterhorn yields Matter and Horn, here Matter is Matte in the case. Commonly, prepositions related to Zermatt are dropped as in Matterhorn, Mattertal, in Sebastian Münsters Cosmography, published in 1543, the name Matter is given to the Theodul Pass, which seems to be the origin of the present German name of the mountain. On Münsters topographical map this group is marked under the names of Augstalberg, the French name Cervin, from which the Italian term Cervino derives, stems from the Latin Mons Silvanus where silva, means forest which was corrupted to Selvin and Servin. The change of the first letter s to c is attributed to Horace Bénédict de Saussure, servius Galba, in order to carry out Caesars orders, came with his legions from Allobroges to Octodurum in the Valais, and pitched his camp there. It is unknown when the new name of Servin, or Cervin, replaced the old, the Matterhorn is named Gran Becca by the Valdôtains and Horu by the local Walliser German speaking people
The Swiss Alps extend over both the Western Alps and the Eastern Alps, encompassing an area sometimes called Central Alps. The Swiss Alps comprise almost all the highest mountains of the Alps, such as Dufourspitze, the Dom, the Liskamm, the Weisshorn, the other following major summits can be found in this list of mountains of Switzerland. Since the Middle Ages, transit across the Alps played an important role in history, the region north of St Gotthard Pass became the nucleus of the Swiss Confederacy in the early 14th century. The Alps cover 65% of Switzerlands total 41,285 square kilometres surface area, making it one of the most alpine countries. The glaciers of the Swiss Alps cover an area of 1,220 square kilometres — 3% of the Swiss territory, the Swiss Alps are situated south of the Swiss Plateau and north of the national border. The limit between the Alps and the runs from Vevey on the shores of Lake Geneva to Rorschach on the shores of Lake Constance, passing close to the cities of Thun.
The not well defined regions in Switzerland that lie on the margin of the Alps, the Swiss Prealps are mainly made of limestone and they generally do not exceed 2,500 metres. The Alpine cantons are Valais, Graubünden, Glarus, Ticino, St. Gallen, Obwalden, Schwyz, Appenzell Innerrhoden, Appenzell Ausserrhoden, Fribourg and Zug. The countries with which Switzerland shares mountain ranges of the Alps are, Italy, the Alps are usually divided into two main parts, the Western Alps and Eastern Alps, whose division is along the Rhine from Lake Constance to the Splügen Pass. The western ranges occupy the greatest part of Switzerland while the more numerous eastern ranges are smaller and are all situated in the canton of Graubünden. The latter are part of the Central Eastern Alps, except the Ortler Alps which belong to the Southern Limestone Alps, the Pennine and Bernina Range are the highest ranges of the country, they contain respectively 38,9 and 1 summit over 4000 metres. The lowest range is the Appenzell Alps culminating at 2,500 metres, Western Alps Eastern Alps The north side of the Swiss Alps is drained by the Rhône, Rhine and Inn while the south side is mainly drained by the Ticino.
The rivers on the empty into the Mediterranean and Black Sea. The major triple watersheds in the Alps are located within the country, they are, Piz Lunghin, Witenwasserenstock, between the Witenwasserenstock and Piz Lunghin runs the European Watershed separating the basin of the Atlantic and the Mediterranean Sea. The European watershed lies in fact only partially on the main chain, Switzerland possesses 6% of Europes fresh water, and is sometimes referred to as the water tower of Europe. Since the highest dams are located in Alpine regions, many mountain lakes are artificial and are used as hydroelectric reservoirs. Some large artificial lakes can be found above 2,300 m, the melting of low-altitude glaciers can generate new lakes, such as the 0.25 km² large Triftsee which formed between 2002–2003. The following table gives the area above 2000 m and 3000 m
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
Sir Leslie Stephen KCB was an English author, historian and mountaineer, and father of Virginia Woolf and Vanessa Bell. Stephen was born at Kensington Gore in London, and son of Sir James Stephen and his father was Colonial Undersecretary of State and a noted abolitionist. He was the fourth of five children, his siblings including James Fitzjames Stephen and his family had belonged to the Clapham Sect, the early 19th century group of mainly evangelical Christian social reformers. At his fathers house he saw a deal of the Macaulays, James Spedding, Sir Henry Taylor. He recounted some of his experiences in a chapter in his Life of Fawcett as well as in less formal Sketches from Cambridge. These sketches were reprinted from the Pall Mall Gazette, to the proprietor of which, George Murray Smith, the family connections included that of William Makepeace Thackeray. His brother, Fitzjames had been a friend of Thackerays and assisted in the disposition of his estate when he died in 1863 and his sister Caroline met Thackerays daughters and Minny when they were mutual guests of Julia Margaret Cameron.
This led to an invitation to visit from Leslie Stephens mother, Lady Stephen and they met at George Murray Smiths house at Hampstead. Minny and Leslie became engaged on December 4,1866 and married on June 19,1867. After the wedding they travelled to the Swiss Alps and northern Italy, and on return to England lived at the Thackeray sisters home at 16 Onslow Gardens with Anny, in the spring of 1868 Minny miscarried but recovered sufficiently for the couple to tour the eastern United States. Minny miscarried again in 1869, but became pregnant again in 1870 and on December 7 gave birth to their daughter, Laura was premature, weighing three pounds. In March 1873 Thackeray and the Stephens moved to 8 Southwell Gardens, the couple travelled extensively, and by 1875 Minny was pregnant again, but this time was in poor health. On November 27 she developed convulsions, and died the day of eclampsia. After Minnys death, Leslie Stephen continued to live with Anny, Leslie Stephen and his daughter were cared for by his sister, the writer Caroline Emelia Stephen, although Leslie described her as Silly Milly and her books as little works.
Meanwhile, Anny was falling in love with her younger cousin Richmond Ritchie, Ritchie became a constant visitor and they became engaged in May 1877, and were married on August 2. At the same time Leslie Stephen was seeing more and more of Julia Duckworth and his second marriage was to Julia Prinsep Duckworth. Julia had been born in India and after returning to England she became a model for Pre-Raphaelite painters such as Edward Burne-Jones, in 1867 she had married Herbert Duckworth by whom she had three children prior to his death in 1870. Leslie Stephen and Julia Duckworth were married on March 26,1878 and they had four children, Vanessa married Clive Bell Thoby Virginia married Leonard Woolf Adrian In May 1895, Julia died of influenza, leaving her husband with four young children aged 11 to 15
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
Zmutt is a small village in the municipality of Zermatt, Switzerland, situated at 1936 m in the Zmutt Valley west of Zermatt. The village chapel is dedicated to Saint Catherine of Alexandria, patroness of the Valais, the valley passes the northern slope of the Matterhorn and terminates in the Zmutt Glacier on the border to Italys Aosta Valley. The Zmutt dam at 46°0′28″N 7°42′34″E, constructed in 1964, has a height of 74 m and this dam is fed by waters from the Bis and Gorner Glacier
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 Dom is a mountain of the Pennine Alps, located between Randa and Saas-Fee in the canton of Valais. With its 4,545 m summit it is the third highest mountain in the Alps, the Dom is the main summit of the Mischabel group, which is the highest massif lying entirely in Switzerland. Although Dom is a German cognate for dome, it can mean cathedral and the mountain is named after Canon Berchtold of Sitten cathedral, the first person to survey the vicinity. The former name Mischabel comes from an ancient German dialect term for pitchfork, the chain lies entirely in the district of Visp. The two valleys separated by the range are the Mattertal on the west and the Saastal on the east, the towns of Randa and Saas-Fee lie both six kilometres from the summit. The elevation difference between the summit and the floor is 3,150 metres on the west side and 3,000 metres on the east side. On the Mattertal side, the Dom faces the almost equally high Weisshorn and, on the Saastal side, the Dom is the highest point of the Saastal and the second highest mountain of the Mattertal after Monte Rosa.
Since the Dom is not on the main Alpine chain, the rivers flowing on both the west and east side of the end up in the same major river, the Rhone, through the Mattervispa. The Dom is the highest mountain in the Alps with this peculiarity, the Mischabel group includes many subsidiary summits above 4,000 metres. To the north lies the Nadelgrat, composed of the Lenzspitze, the Nadelhorn, the Stecknadelhorn, the Hohberghorn, the Nadelgrat is easily visible from the north and gives the massif its characteristic pitchfork appearance. The second highest peak of the massif, the Täschhorn to the south, culminates at 4,491 metres, in total, eight summits above 4,000 metres make up the Mischabel massif. Other important peaks of the massif are the Ulrichshorn and the Balfrin, the Dom has a western shoulder and an eastern shoulder. The massif is almost entirely composed of gneiss from the Siviez-Mischabel nappe, the latter is part of the Briançonnais microcontinent and is located in the Penninic nappes.
The Dom is a depositional mountain, the first ascent was made from the Festigrat by the Reverend John Llewelyn-Davies with guides Johann Zumtaugwald, Johann Krönig and Hieronymous Brantschen on 11 September 1858. They traversed the west face to reach the Festigrat before arriving to the summit, the first complete ascent on the western ridge was made in 1882 by Paul Güssfeldt and guides Alexander Burgener and B. The direct route on the west face was first ascended in 1962, the 1000-metre-high east face above Saas-Fee was climbed in 1875 by J. Petrus, A. and W. Puckle and L. Noti. A route on the face was first made in August 1906 by Geoffrey Winthrop Young and R. G. Major. According to Young it was more dangerous than the south-west face of the nearby Täschhorn, which they had climbed two weeks earlier