Refuge Aoste
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Refuge Aoste
Refuge Aoste is a mountain hut in the Valpelline, in the Pennine Alps, owned by the Club Alpino Italiano. It is in the commune of Bionaz, Aosta Valley , Valdostan or Valdotainian it, Valdostano (man) it, Valdostana (woman)french: Valdôtain (man)french: Valdôtaine (woman) , population_note = , population_blank1_title = Official languages , population_blank1 = Italian French ..., Italy. History The first refuge was built in 1908, but destroyed by an avalanche in 1951. It was rebuilt and inaugurated in 1956, but in 1990 lost its roof. The current hut opened in 1995. External links Mountain huts in the Alps Mountain huts in Aosta Valley Mountain huts of Club Alpino Italiano Official website
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Mountain Hut
A mountain hut is a building located high in the mountains, generally accessible only by foot, intended to provide food and shelter to mountaineers, climbers and hikers. Mountain huts are usually operated by an Alpine Club or some organization dedicated to hiking or mountain recreation. They are known by many names, including alpine hut, mountain shelter, mountain refuge, mountain lodge, and mountain hostel. It may also be called a refuge hut, although these occur in lowland areas (e.g. lowland forests) too. Mountain huts can provide a range of services, starting with shelter and simple sleeping berths. Some, particularly in remote areas, are not staffed, but others have staff which prepare meals and drinks and can provide other services, including providing lectures and selling clothing and small items. Mountain huts usually allow anybody to access their facilities, although some require reservations. While shelters have long existed in mountains, modern hut systems date bac ...
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Valpelline (valley)
---- Valpelline is one of the side valleys of the Aosta Valley in north-west Italy. It shares its name with one of the communes within its territory ( Valpelline). The stream running through the Valpelline is the River Buthier. Geography The Valpelline branches from the Great St Bernard Valley near Gignod and rises to Collon Pass, which it shares with Valais, and which is located at the foot of the Grand Combin, whose peak is across the border in Switzerland. Principal mountains * Dent d'Hérens (4,171 m) * Punta Margherita (''Pointe Marguerite'') (3,905 m) * Dents des Bouquetins (3,838 m) * Tête de Valpelline (3,802 m) * Tête Blanche (3,724 m) * Mont Vélan (3,708 m) * Gran Becca Blanchen (3,680 m) * Grande Tête de By (3,587 m) * Aouille Tseuque (3,554 m) * Mont Brulé (3,538 m) * Becca Rayette (3,529 m) * Mont Gelé (3,519 m) * Becca di Luseney (''Pic de Luseney'') (3,504 m) * Punta Kurz (3,496 m) * Château des Dames (3,488 m) * Punta di Fontanella (3,384 m) ...
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Pennine 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 ...
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Club Alpino Italiano
The Club Alpino Italiano is the senior Italian alpine club which stages climbing competitions, operates alpine huts, marks and maintains paths, and is active in protecting the Alpine environment. It was founded in Turin in 1863 by the then finance minister, and mountaineer, Quintino Sella; together with the Swiss Alpine Club, founded in the same year, it is the second oldest Alpine Club in the world, only preceded by the British Alpine Club. After First World War and the annexation of Trento and Trieste to Italy, it absorbed the "Società degli Alpinisti Tridentini" and the "Società Alpina delle Giulie". As of December 2018, it had 322,022 members, 507 sections and 309 sub-sections; the greatest numbers of members came from Lombardy (88,057), Veneto (54,948), and Piedmont (51,396). Its most famous achievement is the 1954 Italian Karakoram expedition to K2 that made the first successful ascent of K2. The CAI operates 433 mountain hut A mountain hut is a building located ...
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Bionaz
Bionaz ( Valdôtain: ; from 1939 to 1946) is a '' comune sparso'' which extends over of the North-Eastern Valpelline area of the Aosta Valley region of northwest Italy. The commune lies on the left side of the river Dora Baltea. The population of about 240 is dispersed among 20 or more small alpine villages and hamlets including ''Plan-de-Veyne'', which is the main centre and the ''capoluogo'' (locally and officially also ''chef-lieu'', in French). The commune belongs to the ''Unité des communes valdôtaines du Grand-Combin''. Villages, hamlets and other centres The commune's statute designates the following ''frazioni'' (locally officially called ''hameaux'', in French): *Les Balmes *Chentre *Chez-Chenoux *Chez-Noyer *Chez-les-Merloz *Les Crêtes *Les Dzovennoz *Lexert *Les Ley *Le Moulin *Plan-de-Veyne *Perquis *Les Places *Pouillayes *La Quelod *Les Rey *Les Rus (Ru)Les Rus is named in the statute as Rû. *Les Vagère *Le Vianoz The following localities, villages and ...
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Aosta Valley
, Valdostan or Valdotainian it, Valdostano (man) it, Valdostana (woman)french: Valdôtain (man)french: Valdôtaine (woman) , population_note = , population_blank1_title = Official languages , population_blank1 = Italian French , demographics_type1 = Citizenship , demographics1_footnotes = , demographics1_title1 = Italian , demographics1_info1 = 95% , demographics1_title2 = , demographics1_info2 = , demographics1_title3 = , demographics1_info3 = , timezone1 = CET , utc_offset1 = +1 , timezone1_DST = CEST , utc_offset1_DST = +2 , postal_code_type = , postal_code = , area_code_type = ISO 3166 code , area_code = IT-23 , blank_name_sec1 = GDP (nominal) , blank_info_sec1 = €4.9 billion (2018) , blank1_name_sec1 = GDP per capita , blank1_info_sec1 = €38,900 (2018) , blank2_name_sec1 = H ...
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Mountain Huts In The Alps
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 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 isolated summits, but most occur in mountain ranges. Mountains are formed through 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 slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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Mountain Huts In Aosta Valley
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 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, ecosystems of mountains: ...
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