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Veľká Fatra
Veľká Fatra (; also Great Fatra or Greater Fatra; ) is a mountain range in the Western Carpathians in Slovakia. The Veľká Fatra lie to the southeast of the better known Malá Fatra, Malá (Lesser) Fatra mountains and are less developed, as well as being lower. Geology In the geomorphological system, it is a part of the Fatra-Tatra Area. It is situated approximately among the towns of Ružomberok, Harmanec, Turčianske Teplice and Martin, Slovakia, Martin. The Turiec Basin and the Lesser Fatra mountains are situated to the north west of the range and the Low Tatras mountains are in the east. It can be divided into seven parts: ''Šípska Fatra, Šiprúň, Lysec, Hôľna Fatra, Revúcke podolie, Zvolen and Bralná Fatra''. The highest mountain is Ostredok at . Other notable summits of the largest ''Hôľna Fatra'' part are Krížna at and Ploská at , where the main ridge divides into two. The western Turiec Ridge () includes, for example, Borišov at , and the eastern Liptov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Borišov
Borišov is a mountain in the Greater Fatra Range in Slovakia measuring 1,508.5 m (4,949.1 ft). Its summit is deforested, covered in grass. On the southern side there is one of the largest avalanche slopes in Slovakia. The Borišov National Nature Reserve protects a well-preserved primeval mountain forest on the northern side of the mountain. In the saddle between Borišov and Ploská is the Chata pod Borišovom (), open year-round. References * * {{DEFAULTSORT:Borisov Veľká Fatra Mountains of Slovakia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Žilina Region
The Žilina Region (; ; ) is one of the eight Regions of Slovakia, Slovak administrative regions and consists of 11 districts (okresy) and 315 municipalities, from which 18 have a town status. The region was established in 1923, however, in its present borders exists from 1996. It is a more industrial region with several large towns. Žilina is the region administrative center and there is a strong cultural environment in Martin, Slovakia, Martin. Geography It is located in northern Slovakia and has an area of 6,804 km2 and a population of 688,851 (2011). The whole area is mountainous, belonging to the Western Carpathians. Some of the mountain ranges in the region include Javorníky, the Lesser Fatra and the Greater Fatra in the west, Oravská Magura, Chočské vrchy, Low Tatras and Western Tatras in the east. Whole area belongs to the Váh river basin. Some of its left tributaries are Turiec River (Váh), Turiec and Rajčanka rivers and its right tributaries Belá River, Bel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ploská
Ploská is a mountain in the Hôlna Fatra part of the Greater Fatra Range in Slovakia Slovakia, officially the Slovak Republic, is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the west, and the Czech Republic to the northwest. Slovakia's m ... measuring . It lies on the main ridge, to South it continues to Ostredok and Krížna mountains, to the North it divides into the lower western Turiec Ridge () and higher eastern Liptov Ridge (). It is unique by its large flat grass covered summit, the slopes are dangerous in winter because of frequent avalanches which have claimed many lives. References * * {{DEFAULTSORT:Ploska Veľká Fatra Mountains of Slovakia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blatnická Valley
The Blatnica Valley () is a karst valley in the Greater Fatra Range in Slovakia. It is accessible from the village of Blatnica along a dirt road. Most of the valley is densely forested, in places with views at the surrounding limestone and dolomite strata In geology and related fields, a stratum (: strata) is a layer of Rock (geology), rock or sediment characterized by certain Lithology, lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by v .... The best known part of the valley is the rock window at its lower part. Ostrá and Drieňok mountains can be climbed from the valley bottom. References Valleys of Slovakia Veľká Fatra Geography of Žilina Region Karst {{Žilina-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaderská Valley
Gader Valley () is a long valley in the Greater Fatra Range in Central Slovakia. It is accessible from the village of Blatnica. The valley is the gateway to the peaks PEAKS is a proteomics software program for tandem mass spectrometry designed for peptide sequencing, protein identification and quantification. Description PEAKS is commonly used for peptide identification (Protein ID) through de novo peptide ... of Tlstá and Ostrá. Its upper part, from the merger with the ''Selenec'' Valley, is named ''Dedošová''. In Gader Valley, there are almost all of the protected species of animals and plants that occur throughout the Great Fatra: 3,000 species of invertebrates, 110 species of birds, and 60 mammalian species. The Tlstá mountain complex was declared a National Nature Reserve in 1972. About 2 km from the village of Blatnica are the ruins of Blatnica Castle, which dates back to the 13th century. It is located on the low limestone ridge of Plešovice (658 m a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary rock, sedimentary carbonate rock that contains a high percentage of the mineral Dolomite (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). One of the first geologists to distinguish dolomite from limestone was Déodat Gratet de Dolomieu, a French mineralogist and geologist after whom it is named. He recognized and described the distinct characteristics of dolomite in the late 18th century, differentiating it from limestone. Most dolomite was formed as a magnesium replacement of limestone or of Lime (mineral), 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 v ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous, metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade, regional metamorphism. It is the finest-grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate, called " slaty cleavage", is caused by strong compression in which fine-grained clay forms flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation with a specialized tool in the quarry, many slates display a property called fissility, forming smooth, flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen ''en masse'' covering roofs. However, slate occurs in a variety of colors even from a single locality; for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesozoic
The Mesozoic Era is the Era (geology), era of Earth's Geologic time scale, geological history, lasting from about , comprising the Triassic, Jurassic and Cretaceous Period (geology), Periods. It is characterized by the dominance of archosaurian reptiles such as the dinosaurs, and of Gymnosperm, gymnosperms such as cycads, ginkgoaceae and Araucariaceae, araucarian conifers; a hot Greenhouse and icehouse earth, greenhouse climate; and the tectonic break-up of Pangaea. The Mesozoic is the middle of the three eras since Cambrian explosion, complex life evolved: the Paleozoic, the Mesozoic, and the Cenozoic. The era began in the wake of the Permian–Triassic extinction event, the largest mass extinction in Earth's history, and ended with the Cretaceous–Paleogene extinction event, another mass extinction whose victims included the non-avian dinosaurs, Pterosaur, pterosaurs, Mosasaur, mosasaurs, and Plesiosaur, plesiosaurs. The Mesozoic was a time of significant tectonic, climatic, an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Donovaly
Donovaly () is a village in the Banská Bystrica Region of central Slovakia. Being situated in an important pass between the mountains of Veľká Fatra and Starohorské vrchy, on the route connecting Banská Bystrica with Ružomberok, it became a prominent centre of winter and summer sports. History Donovaly was founded in the early 17th century. During World War II, it became an important center of the anti-German Resistance. Tourism Donovaly is a part of Low Tatras National Park, and it hosts one of the biggest and most popular ski resorts in Slovakia. Elevation is between 910 – 1,402 m, and there are more than 11 km of ski slopes, 17 lifts and elevators. In 2006, the Telemix lift by POMA, France – the 3rd of this kind in the world – was installed. It consists of 6 seated lift chairs, and 8 seated cabins, so the skiers can choose how they will go up to the top. Winter season starts from end of November and lasts until late March, beginning of April. It is also r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low Tatra
The Low Tatras or Low Tatra (; ) is a mountain range of the Inner Western Carpathians in central Slovakia. It is located south of the Tatras proper, from which it is separated by the valleys of the Váh and Poprad rivers (the Liptov-Spiš abasement). The valley formed by the Hron River is situated south of the Low Tatras range. The ridge runs west-eastwards and is about 80 km long. The Čertovica pass divides the range into two parts. The highest peaks of the Low Tatras are located in its western part. Ďumbier is the highest mountain at 2,042 m AMSL. Its neighbour Chopok (2,024 m) is accessible by a chairlift, and it is the most visited place in the Low Tatras. Other peaks in the western part include Dereše (2,004 m) and Chabenec (1,955 m). The highest peak in the eastern part is Kráľova hoľa (1,946 m). The best viewpoints in western part are Veľká Chochuľa, Salatín, Chabenec, Skalka, Chopok, Ďumbier, Siná, Poludnica and Baba. Several karst areas are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
