Pizzo Tambò
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Pizzo Tambò
Tambohorn or Pizzo Tambo (Swiss names) or Pizzo Tambò (used in Italy) is a mountain located at the eastern extremity of the Lepontine Alps on the Swiss-Italian border. The mountain lies on the German-Italian language border, west of the Splügen Pass which divides the Western Alps from the Eastern Alps. Reaching a height of 3,279 metres, it is the highest peak in the Mesolcina sub-chain which, starting from the Lugano Prealps northwards, ends near the Splügen Pass on the boundary between Lombardy (northern Italy) and the Graubünden canton of Switzerland. The Tambo is composed mostly of metamorphic rock such as gneiss, mica-schist and phyllite, with a small layer of dolomite just under the peak. It includes three small glaciers, the severally shrunk Tambogletscher on the northeast flank and the Ghiacciaio del Tambo on the west flank, both on the Swiss side, and the by now larger Vedretta della Spianata (3,000-2,740 m) on the southeast side in Italy. Southwards the mas ...
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Swisstopo
Swisstopo is the official name for the Swiss Federal Office of Topography (in German language, German: ''Bundesamt für Landestopografie''; French language, French: ''Office fédéral de topographie''; Italian language, Italian: ''Ufficio federale di topografia''; Romansh language, Romansh: ''Uffizi federal da topografia''), Switzerland's national mapping agency. The current name was made official in 2002. It had been in use as the domain name for the institute's homepage, swisstopo.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 ...
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Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ...
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Mountains Of Lombardy
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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Mountains Of Graubünden
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 an ...
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Mesocco
Mesocco ( Lombard: ''Mesòch'') is a municipality in the Moesa Region in the Swiss canton of Graubünden. History The first human settlement in the area dates back to the Mesolithic era. Stone tools dating to about 6000 BC have been found in the Silex section of the municipality. At the same site, Neolithic fire pits and ceramics (5000 BC) were also discovered. The first permanent settlements in the area date to the Bronze Age (about 1400-1200 BC) and the pre-Roman Iron Age. A notable necropolis from the early Iron Age (600-500 BC) and traces of a Roman settlement were discovered on Gorda hill near the village. Additionally, an Early Middle Ages grave (6th century AD) was also discovered on the same hill. The castle was built in the 12th century and is first mentioned in 1219. The village of Mesocco is first mentioned in 1203 as ''Mesoco''. In 1383 it was mentioned as ''Misogg''. In 1480 Mesocco and Soazza willingly joined the Gray League. Between 1907 and 1978, Mesocco was l ...
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Rheinwald
The Rheinwald (from Latin ''Rheni vallis'' meaning "Rhine Valley"; Romansh: ''Valrain'') is a valley in the Canton of Grisons in Switzerland, the first section of the Hinterrhein valley. The river Hinterrhein flows through three valleys in the Grisons, the Rheinwald, the Schams and the Domleschg. Geography The Rheinwald is about 26 km long and mainly runs from East to West. It is lined on both sides with peaks of over 3000 m high. The highest peaks are the Rheinwaldhorn (3402 m) to the West and the Pizzo Tambo (3279 m) in the South. The Hinterrhein leaves the valley at the entrance to the Rofla Gorge, which separates the Rheinwald from the Schams valley. Two mountain passes lead South from the Rheinwald: the San Bernardino Pass into Misox valley and the Splügen Pass into Val San Giacomo in Italy. The San Bernardino Tunnel (Swiss Highway A13) was opened in 1967 and stays open all winter. Mule tracks on Mount Safierberg and Mount Valserberg connect ...
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Italy–Switzerland Border
The border between the modern states of Switzerland and Italy extends for , from the French-Swiss-Italian tripoint at Mont Dolent in the west to the Austrian-Swiss-Italian tripoint near Piz Lad in the east. Much of the border runs across the High Alps, rising above as it passes east of Dufourspitze, but it also descends to the lowest point in Switzerland as it passes Lago Maggiore at below . It is the longest border of both Italy and of Switzerland. History The border is a product of the Napoleonic period, established with the provisional constitution of the Helvetic Republic of 15 January 1798, restored in 1815. While this border existed as a border of Switzerland from 1815, there was only a unified Italian state to allow the existence of a "Swiss-Italian border" with the formation of the Kingdom of Italy in 1861, it previously comprised the borders between Switzerland and the Kingdom of Sardinia, the Kingdom of Lombardy–Venetia and the province of Cisleithania of Austria- ...
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International Mountains Of Europe
International is an adjective (also used as a noun) meaning "between nations". International may also refer to: Music Albums * ''International'' (Kevin Michael album), 2011 * ''International'' (New Order album), 2002 * ''International'' (The Three Degrees album), 1975 *''International'', 2018 album by L'Algérino Songs * The Internationale, the left-wing anthem * "International" (Chase & Status song), 2014 * "International", by Adventures in Stereo from ''Monomania'', 2000 * "International", by Brass Construction from ''Renegades'', 1984 * "International", by Thomas Leer from ''The Scale of Ten'', 1985 * "International", by Kevin Michael from ''International'' (Kevin Michael album), 2011 * "International", by McGuinness Flint from ''McGuinness Flint'', 1970 * "International", by Orchestral Manoeuvres in the Dark from '' Dazzle Ships'', 1983 * "International (Serious)", by Estelle from '' All of Me'', 2012 Politics * Political international, any transnational organization of ...
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Alpine Three-thousanders
Three-thousanders are mountains with a height of between , but less than above sea level. Similar terms are commonly used for mountains of other height brackets e. g. four-thousanders or eight-thousanders. In Britain, the term may refer to mountains above . Climatological significance In temperate latitudes three-thousanders play an important role, because even in summer they lie below the zero degree line for weeks. Thus the chains of three-thousanders always form important climatic divides and support glaciation - in the Alps the contour is roughly the general limit of the "nival step"; only a few glaciated mountains are under (the Dachstein, the easternmost glaciated mountain in the Alps, is, at , not a three-thousander). In the Mediterranean, however, the three-thousanders remain free of ice and, in the tropics, they are almost insignificant from a climatic perspective; here the snow line lies at around to , and in the dry continental areas (Trans-Himalayas, Ande ...
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List Of Most Isolated Mountains Of Switzerland
A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union club Other uses * Angle of list, the leaning to either port or starboard of a ship * List (information), an ordered collection of pieces of information ** List (abstract data type), a method to organize data in computer science * List on Sylt, previously called List, the northernmost village in Germany, on the island of Sylt * ''List'', an alternative term for ''roll'' in flight dynamics * To ''list'' a building, etc., in the UK it means to designate it a listed building that may not be altered without permission * Lists (jousting), the barriers used to designate the tournament area where medieval knights jousted * ''The Book of Lists'', an American series of books with unusual lists See also * The List (other) * Listing (di ...
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Pizzo Ferré
Pizzo Ferré (; 3,103 m) is a mountain of the Lepontine Alps, located west of Isola in the Italian region of Lombardy. The Swiss Swiss may refer to: * the adjectival form of Switzerland * Swiss people Places * Swiss, Missouri * Swiss, North Carolina *Swiss, West Virginia * Swiss, Wisconsin Other uses *Swiss-system tournament, in various games and sports *Swiss Internation ... border runs 140 metres west of the summit at approximately 3,040 m. On the north side lies a glacier named ''Ghiacciaio del Pizzo Ferré''. References External linksMontespluga-Pizzo Ferré {{DEFAULTSORT:Ferre Alpine three-thousanders Lepontine Alps Mountains of Lombardy Mountains of the Alps Mountains partially in Switzerland ...
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Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ...
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