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Drance
The Drance (, ) is a river in Valais, Switzerland with a length of to the confluence with the Rhône, a maximum length of . It has a drainage basin of . The river is formed from the confluence of the ''Dranse d'Entremont'' and the ''Dranse de Bagnes'' at the village of Sembrancher. Further upriver the ''Dranse d'Entremont'' splits into the ''Dranse d'Entremont'' and the ''Dranse de Ferret''. History In 57/56 BC Julius Caesar sent Servius Galba with the Twelfth Legion and some cavalry to open the Great St Bernard Pass. The legion fought the Veragri at the village of Octodurus along the Drance river and drove them across the river before establishing a camp near the river. The Seduni and Veragri attacked the legion camp a few days later in the Battle of Octodurus. In 1349 a wooden toll bridge and dam are mentioned near La Bâtiaz village (now part of Martigny). In 1595 the river flooded and destroyed a chapel in La Bâtiaz and damage in Bagnes. In 1818 a glacial dam gave w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rhône
The Rhône ( , ; Occitan language, Occitan: ''Ròse''; Franco-Provençal, Arpitan: ''Rôno'') is a major river in France and Switzerland, rising in the Alps and flowing west and south through Lake Geneva and Southeastern France before discharging into the Mediterranean Sea (Gulf of Lion). At Arles, near its mouth, the river divides into the Great Rhône () and the Little Rhône (). The resulting River delta, delta forms the Camargue region. The river's source is the Rhône Glacier, at the east edge of the Cantons of Switzerland, Swiss canton of Valais. The glacier is part of the Saint-Gotthard Massif, which gives rise to three other major rivers: the Reuss (river), Reuss, Rhine and Ticino (river), Ticino. The Rhône is, with the Po (river), Po and the Nile, one of the three Mediterranean rivers with the largest Discharge (hydrology), water discharge. Etymology The name ''Rhône'' continues the Latin name (Ancient Greek, Greek ) in Greco-Roman geography. The Gaulish name of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great St Bernard Pass
The Great St Bernard Pass (, , ; ) is the third highest road pass in Switzerland, at an elevation of . It connects Martigny in the canton of Valais in Switzerland with Aosta in the region Aosta Valley in Italy. It is the lowest pass lying on the ridge between the two highest mountains of the Alps, Mont Blanc and Monte Rosa. It is located on the main watershed that separates the basin of the Rhône from that of the Po. Great St Bernard is one of the most ancient passes through the Western Alps, with evidence of use as far back as the Bronze Age and surviving traces of a Roman road. In 1800, Napoleon's army used the pass to enter Italy, an event depicted in Jacques-Louis David's '' Napoleon at the Saint-Bernard Pass'' and Paul Delaroche's '' Bonaparte Crossing the Alps'', both notable oil paintings. Having been bypassed by easier and more practical routes, particularly the Great St Bernard Tunnel, a road tunnel which opened in 1964, its value today is mainly historical and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Martigny
Martigny (; , ; ) is the capital city of the district of Martigny (district), Martigny, cantons of Switzerland, canton of Canton of Valais, Valais, Switzerland. It lies at an elevation of , and its population is approximately 20,000 inhabitants (''Martignerains'' or "Octoduriens"). It is a junction of roads joining Italy, France and Switzerland. One road links it over the Great St. Bernard Pass to Aosta (Italy), and the other over the col de la Forclaz to Chamonix (France). In winter, Martigny is known for its numerous nearby Alp ski resorts such as Verbier. Geography Martigny lies at an elevation of , about south-southeast of Montreux. It is on the left foothills of the steep hillsides of the Rhone Valley, at the foot of the Swiss Alps, and is located at the point where the southwestern-flowing Rhone turns ninety degrees northward and heads toward Lake Geneva. The river La Drance flows from the southern Valais Alps (Wallis) through Martigny and joins the Rhone from the left just ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bovernier
Bovernier is a Municipalities of Switzerland, municipality in the district of Martigny (district), Martigny in the Cantons of Switzerland, canton of Valais in Switzerland. History Bovernier is first mentioned in 1228 as ''Burgus Warnierus''. Geography Bovernier has an area, , of . Of this area, 5.0% is used for agricultural purposes, while 72.1% is forested. Of the rest of the land, 4.3% is settled (buildings or roads) and 18.5% is unproductive land. The municipality is located in the Martigny district, at the entrance to the Entremont region. It consists of the village of Bovernier and the hamlet (place), hamlet of Les Valettes. Coat of arms The blazon of the municipal coat of arms is ''Azure, issuant from a Castle Argent an Alder-tree Branch palewise Or.'' Demographics Bovernier has a population () of . , 6.1% of the population are resident foreign nationals. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seduni
The Seduni were a Gallic tribe dwelling in the upper Rhône valley, around present-day Sion, during the Iron Age and the Roman period. Along with the Nantuates, Veragri and Uberi, they were part of the Vallenses, a group of tribes living between Lake Geneva and the Pennine Alps, in the modern Canton of Valais (Switzerland). Name They are mentioned as ''Sedunos,'' ''Sedunorum'' and ''Sedunis'' by Caesar (mid-1st c. BC),Caesar. ''Commentarii de Bello Gallico''3:1: and as ''Seduni'' by (late 1st c. BC) and [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluvial Processes
In geography and geology, fluvial sediment processes or fluvial sediment transport are associated with rivers and streams and the Deposition (geology), deposits and landforms created by sediments. It can result in the formation of ripple marks, ripples and dunes, in fractal-shaped patterns of erosion, in complex patterns of natural river systems, and in the development of floodplains and the occurrence of flash floods. Sediment moved by water can be larger than sediment moved by air because water has both a higher density and viscosity. In typical rivers the largest carried sediment is of sand and gravel size, but larger floods can carry Cobble (geology), cobbles and even boulders. When the stream or rivers are associated with glaciers, ice sheets, or ice caps, the term ''glaciofluvial'' or Fluvioglacial landform, ''fluvioglacial'' is used, as in periglacial flows and glacial lake outburst floods. Fluvial sediment processes include the sediment transport, motion of sediment and ero ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography, Switzerland's national mapping agency. The current name was made official in 2002. It had been used as the domain name for the homepage of the instituteswisstopo.admin.ch since 1997. Maps The main class of products produced by Swisstopo are topographical maps on seven different Scale (map), scales. Swiss maps have been praised for their accuracy and quality. Regular maps * 1:25.000. This is the most detailed map, useful for many purposes. Those are popular with tourists, especially for famous areas like Zermatt and St. Moritz. These maps cost CHF 13.50 each (2004). 208 maps on this scale are published at regular intervals. The first map published on this scale was ''1125 Chasseral'', in 1952. The last map published on this scale was ''1292 Maggia'', in 1972. Since 1956, composites have been published, starting with ''2501 St. Gallen''. They have the same information, but consist of several parts of re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lac De Mauvoisin
__NOTOC__ Lac de Mauvoisin is a reservoir in the canton of Valais, Switzerland. The reservoir is formed by the Mauvoisin Dam, which is high. The dam is the 11th highest in the world, and the 6th highest arch dam. It was built in 1951–1957, and raised by in 1991. The reservoir lies in the upper Val de Bagnes, between the massif of the Grand Combin, one of the highest mountains of the Alps, and La Ruinette. The highest peak visible from the lake is the Combin de la Tsessette (). Gallery Mauvoisin.jpg, Mauvoisin Dam, with Mont Blanc de Cheilon in the background Dranse de Bagnes.jpg, Dranse de Bagnes, a stream flowing from the Mauvoisin lake See also *List of lakes of Switzerland *List of mountain lakes of Switzerland This is a list of high-altitude lakes of Switzerland. It includes all significant lakes located either entirely or partly in Switzerland, both natural and artificial, with an area of at least 4 ha (9.9 acres) and a location at over above sea l ... Exte ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pointe De Drône
The Pointe de Drône is a mountain of the Pennine Alps, located on the border between Italy and Switzerland Switzerland, officially the Swiss Confederation, is a landlocked country located in west-central Europe. It is bordered by Italy to the south, France to the west, Germany to the north, and Austria and Liechtenstein to the east. Switzerland .... It lies west of the Great St. Bernard Pass. References External links Pointe de Drône on Hikr Mountains of the Alps Mountains of Switzerland Mountains of Italy Italy–Switzerland border International mountains of Europe Mountains of Valais Two-thousanders of Switzerland {{Aosta-mountain-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lac Des Toules
__NOTOC__ Lac des Toules is a reservoir in Valais, Switzerland, at Bourg-Saint-Pierre. Its surface area is . It has a €2.2 million floating solar plant that was flown in by helicopter in 2019, and delivers 800 MWh/year. The dam Les Toules was completed in 1963. See also *List of lakes of Switzerland *List of mountain lakes of Switzerland This is a list of high-altitude lakes of Switzerland. It includes all significant lakes located either entirely or partly in Switzerland, both natural and artificial, with an area of at least 4 ha (9.9 acres) and a location at over above sea l ... References Lakes of Valais Reservoirs in Switzerland {{valais-lake-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orsières
Orsières is a Municipalities of Switzerland, municipality in the district of Entremont (district), Entremont in the Cantons of Switzerland, canton of Valais in Switzerland. History Orsières is first mentioned in 972 as ''Pons Ursarii''. In medieval times, it was a stage on the ''Via Francigena''. Geography Orsières has an area, , of . Of this area, 16.8% is used for agricultural purposes, while 25.2% is forested. Of the rest of the land, 1.5% is settled (buildings or roads) and 56.5% is unproductive land. The municipality is located at the foot of the Mont Blanc Massif on the road over the Great St Bernard Pass. It is located on the border with both Italy and France and covers two valleys, the Val Ferret and the Vallée de Champex. It consists of the village of Orsières and twelve hamlet (place), hamlets including Champex, Ferret, Issert, La Fouly and Praz-de-Fort. La Fouly La Fouly () is a tourist destination for families and a starting point for many hikes into the su ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giétro Glacier
The Giétro Glacier or Giétroz Glacier () is a 4 km long valley glacier located in south-western Switzerland. The 1818 Giétro Glacier catastrophe, which led to a lake outburst flood, is one of the most famous and most disastrous historical cases in the Swiss Alps. Description The Giétro Glacier lies on the northern side of the Pennine Alps in the Swiss canton of Valais. It is located in the upper Bagnes Valley, south of Martigny and Verbier. The length of the glacier is 4.45 km (2017) and its area is 5.3 km2 (2017). The glacier is fed by the snows of Mont Blanc de Cheilon (3,870 m) and La Ruinette (3,875 m). On the upper part, the glacier is relatively flat. It descends to the north on the side of Mont Rouge du Giétro and then curves to the west between Le Pleureur and Mont Rouge. On the lower part, the glacier reaches a steepness of 40% forming a large number of crevasses. The terminus is located at about 2,750 metres. Part of the glacier is linked to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
