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Gleirsch-Halltal Chain
The Gleirsch-Halltal Chain (german: Gleirsch-Halltal-Kette) or Gleirsch-Halltal Range is a mountain chain in the Karwendel in the Northern Limestone Alps. It follows to the south of the Hinterautal-Vomper Chain, the longest mountain chain in the Karwendel, and is almost as big as it. South of the Stempeljochspitze on the other side of the ''Stempeljoch'' saddle () it is joined to the Nordkette. The name of the range is derived from the two valleys: the ''Gleirschtal'' to the west and southwest and the Halltal to the southeast. Its highest summit is the Großer Bettelwurf (), which towers 2,200 metres over the Inn valley. Other well known peaks are its two "cornerstones". First, the ''Lafatscher Joch'' (), which forms the only crossing from the Hinterau valley to the Halltal: the Speckkarspitze, the Kleiner Lafatscher with the famous Verschneidung and the Großer Lafatscher. From Scharnitz the western cornerstone of the chain, the Hoher Gleirsch, may easily be climbed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordkette
The Nordkette, also variously called the North Chain, Northern Range, rarely the Inn Valley Range or Inn Valley Chain (''Inntalkette''), is a range of mountains just north of the city of Innsbruck in Austria. It is the southernmost of the four great mountain chains in the Karwendel. To the west it is linked by the Erl Saddle to the Erlspitze Group, to the east via the ''Stempeljoch'' saddle () to the Gleirsch-Halltal Range. To the south it is bounded by the Inn valley. Its highest summit is the Kleiner Solstein () in the west of the range. The Nordkette is served by the Nordkette Cable Car, which offers easy access to the ski area and the Innsbruck Klettersteig. The latter starts in the east, near ''Hafelekar'' station () on the Nordkette Cable Car, and runs via the Seegrubenspitze, the Kemacher and the ''Langen Sattel'' to Frau Hitt and the Frau Hitt Saddle in the west. In addition, the Goethe Way (''Goetheweg'') runs from Hafelekar Station along the arête eastwards to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Scharnitz
Scharnitz is a municipality in the district of Innsbruck-Land in the Austrian state of Tyrol located north of Innsbruck and from Seefeld in Tirol on the German border. It is one of the largest municipalities and has 10 parts: Au, Eisack, Gießenbach, Inrain, Jägerviertel, Oberdorf, Schanz, Schießstand, Siedlung, Unterdorf. The village was founded in the early Middle Ages and was once an important commercial route between Germany and Italy. The main source of income is tourism, both in summer and winter. Scharnitz is the western entry point to the Hinterau valley, where the source of river Isar The Isar is a river in Tyrol, Austria, and Bavaria, Germany, which is not navigable for watercraft above raft size. Its source is in the Karwendel range of the Alps in Tyrol; it enters Germany near Mittenwald and flows through Bad Tölz, Mu ... is located. Population References External links Cities and towns in Innsbruck-Land District {{Tyrol-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Main Dolomite
Main Dolomite (german: Hauptdolomit, hu, Fődolomit, it, Dolomia Principale) is a lithostratigraphic unit in the Alps of Europe. Formation was defined by K.W. Gümbel in 1857. Middle to Late Triassic sedimentary record in the Alpine realm is characterized by presence of various masses of dolomitic rock formations. In the Northern Calcareous Alps the dolomitic mass of Ladinian - Norian age is divided by the Carnian sandstones and shales of Lunz Formation to the Ladinian - Carnian Wetterstein Dolomite and Norian Main Dolomite.Tollmann, A., 1976: Analyse des klassischen nordalpinen Mesozoikums, Wien, Franz Deuticke, 580 pp. The Main Dolomite reaches higher thickness than underlying dolomites in Alps, therefore it is considered as more important "Main". Extent The formation is found in: * the Northern Limestone Alps and Southern Limestone Alps of the Limestone Alps, a mountain system of the western and Central Eastern Alps. * the Apennines in Italy * the Western Carpathians (Ta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lagoon
A lagoon is a shallow body of water separated from a larger body of water by a narrow landform, such as reefs, barrier islands, barrier peninsulas, or isthmuses. Lagoons are commonly divided into ''coastal lagoons'' (or ''barrier lagoons'') and ''atoll lagoons''. They have also been identified as occurring on mixed-sand and gravel coastlines. There is an overlap between bodies of water classified as coastal lagoons and bodies of water classified as estuaries. Lagoons are common coastal features around many parts of the world. Definition and terminology Lagoons are shallow, often elongated bodies of water separated from a larger body of water by a shallow or exposed shoal, coral reef, or similar feature. Some authorities include fresh water bodies in the definition of "lagoon", while others explicitly restrict "lagoon" to bodies of water with some degree of salinity. The distinction between "lagoon" and "estuary" also varies between authorities. Richard A. Davis Jr. restrict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wetterstein Limestone
The Wetterstein Formation is a regional geologic formation of the Northern Limestone Alps and Western Carpathians extending from southern Bavaria, Germany in the west, through northern Austria to northern Hungary and western Slovakia in the east. The formation dates back to the Ladinian to Carnian stages of the Late Triassic. The formation is named after the Wetterstein Mountains in southern Germany and northwestern Austria. The center of its distribution, however, is in the Karwendel Mountains. It occurs in the Northern and Southern Limestone Alps and in the Western Carpathians. The formation is composed of mostly reefal limestones and dolomites, the latter the result of widespread diagenesis. In many areas there is a frequent alternation of limestone and dolomite facies. Local variants to indicate the Wetterstein Formation include german: Wettersteinkalk (Wetterstein Limestone), Wettersteindolomit ("Wetterstein Dolomite") and combinations thereof. The Wetterstein Formation rea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
