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Engadine Line
The Engadine Line is an over long strike-slip fault in the Swiss canton of Graubünden, which extends into Italy and Austria. It runs along the Engadine Valley (which formed on the fault) and the Bregaglia Valley and offsets Austroalpine and Penninic units in a sinistral direction. The western end of the fault appears to peter out into ductile deformation in the Bregaglia Valley or continues as the Gruf Line to the southwest; the eastern end is buried by the Ötztal tectonic block and may continue as the " Inntal fault", "Isar fault" or "Loisach fault". Total offset along the Engadine Line is about , decreasing southwest. It began in the Oligocene, but there is evidence of recent neotectonic activity, which resulted in the collapse of the Maloja Pass area at the beginning of the Holocene. Seismic activity occurs along the Engadine Line, and springs and carbon dioxide exhalations in the Engadine are linked to the fault. Geology The Engadine Line is an over long northeast ...
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Strike-slip Fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ...
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Samedan
Samedan (, ) is a town and municipality in the Maloja Region in the Swiss canton of Grisons. It is served by Samedan railway station on the Rhaetian Railway network and by the Samedan Airport. History Samedan is first mentioned in 1139 as ''Samaden''. In 1334 it was mentioned as ''Semeden'', in 1367 as ''Semaden'', in 1498 as ''Sumada'' and in 1527 as ''Sameden''. Johann Heinrich Müller, 1825-1894 J08 Samaden.JPG, Samedan c. 1870 with the Bernina hotel (opened in 1865), one of the oldest hotels in the Engadin. Etching by Heinrich Müller Samedan circa 1870.jpg, A photograph of Samedan in the circa 1870s Samedan circa 1870 B.jpg, Another photographic view of Samedan in the circa 1870s ETH-BIB-Samedan-LBS H1-017880.tif, Aerial view (1954) Geography Samedan has an area, (as of the 2004/09 survey) of . Of this area, about 15.5% is used for agricultural purposes, while 9.7% is forested. Of the rest of the land, 1.9% is settled (buildings or roads) and 72.9% is unproductive la ...
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S-chanf
S-chanf (; german: Scanfs; it, Scanevo) is a municipality in the Maloja Region in the Swiss canton of Graubünden. Localities in the municipality of include Susauna, Chapella and Cinuos-chel. Name is first mentioned around 1137–1139 as ''Scaneves''. In 1356 it was mentioned as ''Scanevo''. The Romansh name ' is pronounced . The German ''Scanfs'' was official until 1943.Amtliches Gemeindeverzeichnis der Schweiz
published by the Swiss Federal Statistical Office accessed 23 September 2009
Chapella is the site of a chapel mentioned in 1209. Susauna is mentioned as ''Sauzana'' in 1285.


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Nauders
Nauders ( rm, Danuder) is a municipality in the district of Landeck in the Austrian state of Tyrol. Geography The municipal area is situated in a high valley of the Ötztal Alps north of the Alpine crest, at an altitude of . It is located about south of the district capital Landeck, on the road that leads from Pfunds in the Inntal valley via the narrow Finstermünz Gorge up to Reschen Pass and the border with the Vinschgau region in South Tyrol, Italy. Nearby is the tripoint with the Swiss border; in the west, a road leads into the Sesvenna Alps and to Martina in the Lower Engadin valley. Climate History In ancient times, the trade route across Reschen Pass was part of the Roman Via Claudia Augusta, leading from Italy across the Eastern Alps to the Raetian capital Augusta Vindelicorum (Augsburg). Nauders is probably located at the site of a mansio called ''Inutrium'' in contemporary sources. From 200 AD onwards, however, the significance of the road connection faded, when it ...
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Bever, Switzerland
Bever ( Romansh: ; German and official until 1943 ''Bevers'') is a municipality in the Maloja Region in the Swiss canton of Graubünden. History Bever is first mentioned in 1139 as ''ad Bevero''. Geography Bever has an area, (as of the 2004/09 survey) of . Of this area, about 15.3% is used for agricultural purposes, while 15.1% is forested. Of the rest of the land, 1.2% is settled (buildings or roads) and 68.4% is unproductive land. Over the past two decades (1979/85-2004/09) the amount of land that is settled has increased by and the agricultural land has decreased by .Swiss Federal Statistical Office - Regional portraits
accessed 2 May 2016
Until 2017 the municipality was located in the Oberengadin sub-district of the Maloja district, after 2017 it was part of the ...
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Maloja Region
Maloja Region is one of the eleven administrative districts in the canton of Graubünden in Switzerland ). Swiss law does not designate a ''capital'' as such, but the federal parliament and government are installed in Bern, while other federal institutions, such as the federal courts, are in other cities (Bellinzona, Lausanne, Luzern, Neuchâtel .... It has an area of and a population of (as of ). It was created on 1 January 2017 as part of a reorganization of the Canton.Swiss Federal Statistical Office - Amtliches Gemeindeverzeichnis der Schweiz - Mutationsmeldungen 2016
accessed 16 February 2017


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Sils Im Engadin/Segl
Sils im Engadin/Segl (german: Sils im Engadin; Romansh ), often also as ''Sils i.E./Segl'', is a municipality and village in the Maloja Region, Upper Engadine in the Swiss canton of the Grisons. It consists of two villages, Segl Maria (Romansh, german: Sils Maria; ''Seglias'' is part of Segl Maria) and Segl Baselgia (German: ''Sils Baselgia''; ''Baselgia'' is Romansh for church); the Val Fex (German: ''Fextal''); and three ''Maiensäss''e (Alpine pastures traditionally used for spring grazing): Grevasalvas, Blaunca and Buaira, above ''Plaun da Lej'' on the left side of the valley. Name and coat of arms The municipality's official label uses both the German and the Romansh versions of its name: ''Segl'' is the Romansh version while ''Sils im Engadin'' is the German. Engadin is Romansh for "Valley of the Inn ( rm, En)", the river, which flows northeast from Maloja through Sils Baselgia and eventually into the Danube at Passau, Germany at the German-Austrian border. Sils i. ...
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Upper Engadine
The Engadin or Engadine ( rm, ;This is the name in the two Romansh idioms that are spoken in the Engadin, Vallader and Puter, as well as in Sursilvan and Rumantsch Grischun. In Surmiran, the name is ''Nagiadegna'', and in Sutsilvan, it is ''Gidegna''. german: ; it, Engadina; french: Engadine) is a long high Alpine valley region in the eastern Swiss Alps in the canton of Graubünden in southeasternmost Switzerland with about 25,000 inhabitants. It follows the route of the Inn ( rm, En, links=no) from its headwaters at Maloja Pass in the southwest running roughly northeast until the Inn flows into Austria, little less than one hundred kilometers downstream. The En/Inn subsequently flows at Passau into the Danube, making it the only Swiss river to drain into the Black Sea. The Engadine is protected by high mountain ranges on all sides and is famous for its sunny climate, beautiful landscapes and outdoor activities. Name In English, the valley is either known as ''Engadin'' ...
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Lower Engadine
The Engadin or Engadine ( rm, ;This is the name in the two Romansh idioms that are spoken in the Engadin, Vallader and Puter, as well as in Sursilvan and Rumantsch Grischun. In Surmiran, the name is ''Nagiadegna'', and in Sutsilvan, it is ''Gidegna''. german: ; it, Engadina; french: Engadine) is a long high Alpine valley region in the eastern Swiss Alps in the canton of Graubünden in southeasternmost Switzerland with about 25,000 inhabitants. It follows the route of the Inn ( rm, En, links=no) from its headwaters at Maloja Pass in the southwest running roughly northeast until the Inn flows into Austria, little less than one hundred kilometers downstream. The En/Inn subsequently flows at Passau into the Danube, making it the only Swiss river to drain into the Black Sea. The Engadine is protected by high mountain ranges on all sides and is famous for its sunny climate, beautiful landscapes and outdoor activities. Name In English, the valley is either known as ''Engadin'' () ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Schema Tettonico Delle Alpi
The word schema comes from the Greek word ('), which means ''shape'', or more generally, ''plan''. The plural is ('). In English, both ''schemas'' and ''schemata'' are used as plural forms. Schema may refer to: Science and technology * SCHEMA (bioinformatics), an algorithm used in protein engineering * Schema (genetic algorithms), a set of programs or bit strings that have some genotypic similarity * Schema.org, a web markup vocabulary * Schema (logic) ** Axiom schema, in formal logic * Image schema, a recurring pattern of spatial sensory experience * Database schema * XML schema Other * Body schema, a neural representation of one's own bodily posture * Galant Schemata, stock phrases in Galant music * Schema (Kant), in philosophy * Schema (psychology), a mental set or representation * Schema Records, a jazz record label in Milan, Italy *, a solemn vow of asceticism of a monk in Orthodox monasticism ** Great Schema, the highest degree of Orthodox monasticism * ''Schema'' (fly) ...
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