|
Glarus Thrust
The Glarus thrust (german: Glarner Überschiebung) is a major thrust fault in the Alps of eastern Switzerland. Along the thrust the Helvetic nappes were thrust more than 100 km to the north over the external Aarmassif and Infrahelvetic complex. The thrust forms the contact between older (Helvetic) Permo-Triassic rock layers of the Verrucano group and younger (external) Jurassic and Cretaceous limestones and Paleogene flysch and molasse. The Glarus thrust crops out over a relatively large area in the cantons Glarus, St. Gallen and Graubünden, due to its horizontal orientation and the high local relief. Famous outcrops include those at Lochsite near Glarus (the town) and in a mountain cliff called ''Tschingelhörner'' between Elm and Flims (in the same cliff is a natural hole called the Martinsloch). World Heritage Thrust faults of this kind are not uncommon in many mountain chains around the world, but the Glarus thrust is a well accessible example and has as such ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tschingelhörner
The Tschingelhörner (also spelled ''Tschingelhoren'') are a chain of mountain peaks in the Glarus Alps, located on the border between the Swiss cantons of Glarus and Graubünden. They are composed of several summits on a long ridge, of which the highest is named ''Grosses Tschingelhorn'' (2,849 m). The mountain is located between Elm and Flims Flims ( rm, Flem) is a municipality in the Imboden Region in the Swiss canton of Graubünden. The town of Flims is dominated by the Flimserstein which one can see from almost anywhere in the area. Flims consists of the village of Flims (called ..., west of the Segnas Pass (2,627 m). East of the main summit is the Martinsloch, a 6-by-18-metre (20-by-60 ft) triangular breakthrough, or hole, through which the sun shines at particular times of the year. The mountain is part of the Swiss Tectonic Arena Sardona and is a UNESCO World Heritage Site. References External links Tschingelhörner on Hikr Mountains of the Alps Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orogenesis
Orogeny is a mountain building process. An orogeny is an event that takes place at a convergent boundary, convergent plate margin when plate motion compresses the margin. An ''orogenic belt'' or ''orogen'' develops as the compressed plate crumples and is tectonic uplift, uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation (physics), deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere (crust (geology), crust and uppermost mantle (geology), mantle). A synorogenic process or event is one that occurs during an orogeny. The word "orogeny" () comes from Ancient Greek (, , + , , ). Although it was used before him, the term was employed by the American geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flims
Flims ( rm, Flem) is a municipality in the Imboden Region in the Swiss canton of Graubünden. The town of Flims is dominated by the Flimserstein which one can see from almost anywhere in the area. Flims consists of the village of Flims (called Flims Dorf) and the hamlets of Fidaz and Scheia as well as Flims-Waldhaus, the initial birthplace of tourism in Flims, where most of the hotels were built before and after around 1900. Geography Flims has an area of . Of this area, 33.7% is used for agricultural purposes, while 28.9% is forested. Of the rest of the land, 3.6% is settled (buildings or roads) and the remainder (33.9%) is non-productive (rivers, glaciers or mountains). Before 2017, the municipality was located in the Trin sub-district, of the Imboden district, after 2017 it was part of the Imboden Region. Flims is located on a terrace north of the Rhine valley, forming the Ruinaulta gorge here. The country-side has numerous streams and lakes north of the village, f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elm, Switzerland
Elm ( rm, ) is a village, and former municipality, in the municipality of Glarus Süd and canton of Glarus in Switzerland. Elm lies in the valley of the Sernf river, and consists of the village of Elm itself, and the hamlets of Sulzbach, Schwändi, Müsli, Untertal, Vogelsang, Töniberg, Obmoos, Steinibach and Wald. History Elm is first mentioned in 1344 as ''Elme''. The baths at Wichlen were in use since the middle ages and are first mentioned in 1547. They were very popular until they were buried by an avalanche in 1762. Many characteristic wooden structures have survived. In 1799, Russian General Alexander Suvorov and his troops stayed the night in Elm before crossing Panix Pass to Pigniu on their retreat into Austria. By 1861, slate quarrying was taking place. On September 11, 1881, an avalanche caused by excessive quarrying of slate killed 114 and buried 83 structures in the municipality. In 1892, the owner of a spring in Elm that had long been hailed as benefici ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glarus
, neighboring_municipalities= Glarus Nord, Glarus Süd, Muotathal (SZ), Innerthal (SZ) , twintowns= Wiesbaden-Biebrich (Germany) } Glarus (; gsw, Glaris; french: Glaris; it, Glarona; rm, Glaruna) is the capital of the canton of Glarus in Switzerland. Since 1 January 2011, the municipality Glarus incorporates the former municipalities of Ennenda, Netstal and Riedern.Amtliches Gemeindeverzeichnis der Schweiz published by the Swiss Federal Statistical Office accessed 18 February 2011 Glarus lies on the river between the foot of the |
Relief
Relief is a sculptural method in which the sculpted pieces are bonded to a solid background of the same material. The term '' relief'' is from the Latin verb ''relevo'', to raise. To create a sculpture in relief is to give the impression that the sculpted material has been raised above the background plane. When a relief is carved into a flat surface of stone (relief sculpture) or wood (relief carving), the field is actually lowered, leaving the unsculpted areas seeming higher. The approach requires a lot of chiselling away of the background, which takes a long time. On the other hand, a relief saves forming the rear of a subject, and is less fragile and more securely fixed than a sculpture in the round, especially one of a standing figure where the ankles are a potential weak point, particularly in stone. In other materials such as metal, clay, plaster stucco, ceramics or papier-mâché the form can be simply added to or raised up from the background. Monumental bronze relief ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canton Of St
Canton may refer to: Administrative division terminology * Canton (administrative division), territorial/administrative division in some countries, notably Switzerland * Township (Canada), known as ''canton'' in Canadian French Arts and entertainment * Canton (band), an Italian synth pop group * "Canton" (song) by Japan * Canton, a fictional town in " Jaynestown", an episode of ''Firefly'' Design * Canton (building), a corner pilaster * Canton (flag), an emblem placed in the top left quarter of a flag * Canton (heraldry), a square or other charge (symbol) occupying the upper left corner of a coat of arms * Canton porcelain, Chinese ceramic ware People * Canton (surname), and list of people with the surname * Canton Jones, American Christian music/hip-hop artist Places Canada * Canton, New Brunswick, a community in Drummond Parish, New Brunswick * Canton, Ontario China * Guangdong (Canton Province), province in southern China * Guangzhou (Canton City), capit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outcrop
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human excavations such as quarrying and build ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_01.JPG "Click for more on -> Relief")
