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
Zermatt is a municipality in the district of Visp in the German-speaking section of the canton of Valais in Switzerland. It has a population of about 5,800 inhabitants, the town lies at the upper end of Mattertal at an elevation of 1,620 m, at the foot of Switzerlands highest peaks. It lies about 10 km from the over 10,800 ft high Theodul Pass bordering Italy, Zermatt is famed as a mountaineering and ski resort of the Swiss Alps. The year round population is 5,759, though there may be several times as many tourists in Zermatt at any one time. Much of the economy is based on tourism, with about half of the jobs in town in hotels or restaurants. Just over one-third of the permanent population was born in the town, the name of Zermatt, as well as that of the Matterhorn itself, derives from the alpine meadows, or matten, in the valley. The name appeared first as Zur Matte and became Zermatt and it does not appear until 1495 on a map or 1546 in a text, but may have been employed long before. Praborno or Prato Borno are the names of Zermatt, they appear in the ancient maps as early as the thirteenth century.
The Romand-speaking people from the Aosta Valley and from the Romand-speaking part of canton Wallis used this name until about 1860 in the form of Praborne, the reason of this change from Praborno to Zermatt is attributed to the gradual replacement of the Romance-speaking people by German-speaking colony. The town of Zermatt lies at the end of the Matter Valley. Zermatt is almost completely surrounded by the mountains of the Pennine Alps among which Monte Rosa. It is followed by the Dom, Lyskamm and the Matterhorn, most of the Alpine four-thousanders are located around Zermatt or in the neighbouring valleys. The town of Zermatt, while dense, is geographically small, there are three main streets which run along the banks of the river Matter Vispa, and numerous cross-streets, especially around the station and the church which forms the centre of Zermatt. In general anything is at most a thirty-minute walk away, there are several suburbs within Zermatt. Winkelmatten, which was once a hamlet, lies on a hill on the southern side.
Steinmatten is located on the bank of the main river. Many hamlets are located in the valleys above Zermatt, however they are not usually inhabited all year round, zum See lies south of Zermatt on the west bank of the Gorner gorge, near Furi where a cable car station is located. On the side of Zmutt valley lies the hamlet of Zmutt, findeln is located in the eastern valley above the Findelbach river
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
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 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
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
Europe is a continent that comprises the westernmost part of Eurasia. Europe is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, yet the non-oceanic borders of Europe—a concept dating back to classical antiquity—are arbitrary. Europe covers about 10,180,000 square kilometres, or 2% of the Earths surface, Europe is divided into about fifty sovereign states of which the Russian Federation is the largest and most populous, spanning 39% of the continent and comprising 15% of its population. Europe had a population of about 740 million as of 2015. Further from the sea, seasonal differences are more noticeable than close to the coast, Europe, in particular ancient Greece, was the birthplace of Western civilization. The fall of the Western Roman Empire, during the period, marked the end of ancient history. Renaissance humanism, exploration and science led to the modern era, from the Age of Discovery onwards, Europe played a predominant role in global affairs. Between the 16th and 20th centuries, European powers controlled at times the Americas, most of Africa, Oceania.
The Industrial Revolution, which began in Great Britain at the end of the 18th century, gave rise to economic and social change in Western Europe. During the Cold War, Europe was divided along the Iron Curtain between NATO in the west and the Warsaw Pact in the east, until the revolutions of 1989 and fall of the Berlin Wall. In 1955, the Council of Europe was formed following a speech by Sir Winston Churchill and it includes all states except for Belarus and Vatican City. Further European integration by some states led to the formation of the European Union, the EU originated in Western Europe but has been expanding eastward since the fall of the Soviet Union in 1991. The European Anthem is Ode to Joy and states celebrate peace, in classical Greek mythology, Europa is the name of either a Phoenician princess or of a queen of Crete. The name contains the elements εὐρύς, broad and ὤψ eye, broad has been an epithet of Earth herself in the reconstructed Proto-Indo-European religion and the poetry devoted to it.
For the second part the divine attributes of grey-eyed Athena or ox-eyed Hera. The same naming motive according to cartographic convention appears in Greek Ανατολή, Martin Litchfield West stated that phonologically, the match between Europas name and any form of the Semitic word is very poor. Next to these there is a Proto-Indo-European root *h1regʷos, meaning darkness. Most major world languages use words derived from Eurṓpē or Europa to refer to the continent, in some Turkic languages the originally Persian name Frangistan is used casually in referring to much of Europe, besides official names such as Avrupa or Evropa