Ghiacciaio Del Belvedere
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Ghiacciaio Del Belvedere
, photo = Monte Rosa east face.jpg , photo_caption = The east face of Monte Rosa with the glacier at the bottom , type = Valley glacier , location = Valle Anzasca, Verbano-Cusio-Ossola (VB), Piedmont, Italy , coordinates = , map = Alps#Northern Italy , label_position = right , map_width = , map_alt = , map_caption = Glacier's location in the Alps , area = , length = , thickness = , terminus = Alpe Burki , status = receding , embedded = The Belvedere Glacier ( it, Ghiacciaio del Belvedere) is a valley glacier located above Macugnaga of the Valle Anzasca in the region of Piedmont. The glacier lies at the base of the east face of Monte Rosa. It reaches approximately above sea level at its highest point and terminates near the Alpe Burki at about . The glacier is mostly covered by rocks. The glacier is fed by the snows and glaciers on the east side of Monte Rosa, including the Ghiacciaio del Monte Rosa, not to be confused with the Monte Rosagletscher on ...
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Monte Rosa
: , other_name = Monte Rosa massif , translation = Mount Rose , photo = Dufourspitze (Monte Rosa) and Monte Rosa Glacier as seen from Gornergrat, Wallis, Switzerland, 2012 August.jpg , photo_caption = Central Monte Rosa massif, with Dufourspitze to the south (right) and Nordend to the north (left), the Monte Rosa Glacier right below on its western wing, the upper Gorner Glacier on the left, and the Grenzgletscher to the right , country_type = Countries , country = , subdivision1_type = Canton, Regions , subdivision1 = , parent = Pennine Alps, Western Alps , listing = Country high point Canton high pointUltra , length_km = , length_orientation= , width_km = , width_orientation = , geology = , orogeny = , highest = Dufourspitze , elevation_m = 4634 , range_coordinates = , coordinates = , map = Switzerland , map_ ...
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Glaciers Of Italy
A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Glaciers by continent Africa Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Currently, th ...
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Toce
The Toce () is a river in Piedmont, Italy, which stretches the length of the Val d'Ossola from the Swiss border to Lake Maggiore into which it debouches near Fondotoce in the commune of Verbania. The river is long and is formed in the upper Val Formazza by the confluence of a number of torrents in the plain of Riale. Geography The source of one of these, the Gries, is situated on the Italian southern side of the Gries Pass; another forms beneath the Passo di San Giacomo, others flow from little Alpine lakes such as Lago Castel and Lago di Sabbione. South of La Frua the water of the river plummets over the Cascata del Toce into the Formazza Valley, through which it flows before transversing Valle Antigorio after another series of cascades. Near Crevola d'Ossola the river Diveria flows into the Toce. At this point, the valley gets wider and is known as Val d'Ossola. The Toce flows next to the capital of the valley, Domodossola, and then Villadossola and Ornavasso. After a ...
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Anza (river)
The Anza is a Alpine torrent of the Ossola in northern Italy. It flows from the glaciers of Monte Rosa through the Valle Anzasca and into the river Toce, of which it is a right tributary. Its own principal tributaries are the Pedriola, the Tambach, the Orlovono and the Quarazza near Macugnaga and the Olocchia at Bannio Anzino. Sources :''This original version of this article included text translated from its counterpart in the Italian Wikipedia The Italian Wikipedia ( it, Wikipedia in italiano) is the Italian-language edition of Wikipedia. This edition was created on May 11, 2001 and first edited on June 11, 2001. As of , , it has articles and more than registered accounts. It is th ....'' Rivers of Italy Rivers of the Province of Verbano-Cusio-Ossola Rivers of the Alps {{Italy-river-stub ...
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Punta Delle Loccie
Punta is an Afro-indigenous dance and cultural music originating in the Caribbean Island of Saint Vincent And The Grenadines by the Garifuna people before being exiled from the island. Which is also known as Yurumei. It has African and Arawak elements which are also the characteristics of the Garifuna language. Punta is the best-known traditional dance belonging to the Garifuna community. It is also known as banguity or bunda, before the first arrival of the Garifuna people in Punta Gorda, Roatan, Honduras on April 12, 1797. The diaspora of Garifuna people, commonly called the "Garifuna Nation", dates back to the amalgamation of West African slaves and the Arawak and Carib Amerindians. Punta is used to reaffirm and express the struggle felt by the indigenous population's common heritage through cultural art forms, such as dance and music, and to highlight their strong sense of endurance as well as reconnecting back to the ancestors of the Garifuna people. Besides Honduras, pu ...
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Monte Rosagletscher
Monte may refer to: Places Argentina * Argentine Monte, an ecoregion * Monte Desert * Monte Partido, a ''partido'' in Buenos Aires Province Italy * Monte Bregagno * Monte Cassino * Montecorvino (other) * Montefalcione Portugal * Monte (Funchal), a civil parish in the municipality of Funchal * Monte, a civil parish in the municipality of Fafe * Monte, a civil parish in the municipality of Murtosa * Monte, a civil parish in the municipality of Terras de Bouro Elsewhere * Monte, Haute-Corse, a commune in Corsica, France * Monte, Switzerland, a village in the municipality Castel San Pietro, Ticino, Switzerland * Monte, U.S. Virgin Islands, a neighborhood * Monte Lake, British Columbia, Canada Arts, entertainment, and media * ''Monte'' (film), a 2016 drama film by Amir Naderi * Three-card Monte * Monte Bank or Monte, a card game Other uses * Monte (dessert) a milk cream dessert produced by the German dairy company Zott * Monte (mascot), the mascot of the University of ...
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Alpe Burki
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation le ...
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Valley Glacier
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ...
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Macugnaga
Macugnaga ( Walser German: ''Z'Makana'') is a mountain village and a comune at elevation, in the province of Verbano-Cusio-Ossola, in the north of the Piedmont region of Italy. It is located at the base of Monte Rosa (), the second-tallest mountain in western Europe, along Valle Anzasca, one of the seven valleys around the mount. Sights in the town include the Chiesa Vecchia (old church) and its linden also of the 13th century, the ''Chiesa Nuova'' (new church) built in 1707, the 17th century ''Casa Pala''. The town also houses a museum of mountaineering, while in the hamlet of Borca is the Walser Museum, devoted to the local German population who colonised the valley during the Middle Ages coming from the Swiss canton Wallis. The area gives many opportunities for skiing in winter (a cableway brings from the central square of the town to the 3000 m (9800 ft) of the Passo del Monte Moro on the border with Switzerland), and hiking and mountaineering in summer. There ...
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Valley Glacier
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. ...
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