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Děvín
Děvín (german: Mayden Berg) is a double peak mountain in the Pavlov municipality in the South Moravian Region of the Czech Republic. With an elevation of , it is the highest mountain of the Pavlov Hills within the Mikulov Highlands, and of the Pálava Protected Landscape Area. It is located right on trace where runs line of drainage divide of Upper Thaya drainage and Thaya/Morava mesodrainage. History The summit of Děvín has the remains of a huge Iron Age hill fort, while the ancient Amber Route runs neighbors of the mountains base, and all archaic roads in landscape, originally created by animals and later overtaken by humans. The area around base of the mountain is permanently settled longer than last 30,000 years. Since Cromagnos hunters, ower Celtic tribes settlement, Roman fortress, Great Moravia hillforts ( Strachotín and Děvín). Geology The entire Děvín massif consists mainly by Jurassic limestone, i.e. series of rocks generated during sedimentation. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Děvín A Kotel, Pohled Ze Stolové Hory
Děvín (german: Mayden Berg) is a double peak mountain in the Pavlov municipality in the South Moravian Region of the Czech Republic. With an elevation of , it is the highest mountain of the Pavlov Hills within the Mikulov Highlands, and of the Pálava Protected Landscape Area. It is located right on trace where runs line of drainage divide of Upper Thaya drainage and Thaya/Morava mesodrainage. History The summit of Děvín has the remains of a huge Iron Age hill fort, while the ancient Amber Route runs neighbors of the mountains base, and all archaic roads in landscape, originally created by animals and later overtaken by humans. The area around base of the mountain is permanently settled longer than last 30,000 years. Since Cromagnos hunters, ower Celtic tribes settlement, Roman fortress, Great Moravia hillforts ( Strachotín and Děvín). Geology The entire Děvín massif consists mainly by Jurassic limestone, i.e. series of rocks generated during sedimentation. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mikulov Highlands
The Mikulov Highlands ( cs, Mikulovská vrchovina) is a mountain range in the South Moravian Region of the Czech Republic. The Highlands, together with the Waschberg Zone and Lower Austria Inselberg threshold, form the South-Moravian Carpathians. Geography The Mikulov Highlands rise to the south of the Thaya between Nový Přerov, the Nové Mlýny reservoirs, Bulhary, Mikulov, and the Austrian border. The Highlands have an area of and an average height of . The highest peak is Děvín at ; other peaks are ''Obora'' (), ''Stolova hora'' (), ''Pálava'' (), ''Stará hora'' (), and ''Turold '' (). To the north is the Thaya River valley, the natural border with Lower Morava Valley. To the east is the mountainous region between the Thaya and Včelínek, also from the Lower Morava Valley. To the southeast is the March Field, and to the southwest a ridge in Austria in the Waschberg Zone which forms the western border of the Thaya valley. Geomorphological subunits form Pálava ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pálava Protected Landscape Area
The Pálava Protected Landscape Area (abbreviated Pálava PLA; cs, Chráněná krajinná oblast Pálava, abbreviated ''CHKO Pálava'') is a protected landscape area and a UNESCO biosphere reserve located in the South Moravian Region in the Czech Republic, on the border with Austria. The highest point is Děvín with its a.s.l. Description This unique area was originally recognized by UNESCO in 1986 and expanded in 2003 to include another UNESCO site, the Lednice–Valtice Cultural Landscape. Pálava PLA is dominated by the limestone Pálava Hills (part of the outer Western Carpathians), and contains a significant proportion of natural or little affected steppe ecosystems that include meadow steppe, forest steppe, and thermophilic oak forest. In the floodplain of the river Thaya, forests alternate with meadows and wetland habitat that also include halophytic vegetation. The remaining part of Pálava PLA is used agriculturally, with many sustainably farmed vineyards that are a p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pavlov (Břeclav District)
Pavlov (german: Pollau) is a municipality and village in Břeclav District in the South Moravian Region of the Czech Republic. It has about 600 inhabitants. Geography Pavlov lies approximately northwest of Břeclav and south of Brno. It lies in the Pavlov Hills within the Mikulov Highlands. The village lies under the Děvín mountain, which is the highest mountain of the municipality and of the entire region with an elevation of . Pavlov is located in the Pálava Protected Landscape Area. See also *Pavlovian culture The Pavlovian is an Upper Paleolithic culture, a variant of the Gravettian, that existed in the region of Moravia, northern Austria and southern Poland around 29,000–25,000 years BP. The culture used sophisticated stone age technology to survive ... References Villages in Břeclav District {{SouthMoravia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Moravian Region
The South Moravian Region ( cs, Jihomoravský kraj; , ; sk, Juhomoravský kraj) is an administrative unit () of the Czech Republic, located in the south-western part of its historical region of Moravia (an exception is Jobova Lhota which traditionally belongs to Bohemia). The region's capital is Brno, the nation's 2nd largest city. South Moravia is bordered by the South Bohemian Region (west), Vysočina Region (north-west), Pardubice Region (north), Olomouc Region (north east), Zlín Region (east), Trenčín and Trnava Regions, Slovakia (south east) and Lower Austria, Austria (south). Administrative divisions The South Moravian Region is divided into 7 districts (Czech: ''okres''): There are in total 673 municipalities in the region, of which 49 have the status of towns. There are 21 municipalities with extended powers and 34 municipalities with a delegated municipal office. The region is famous for its wine production. The area around the towns of Mikulov, Znojmo, Velké ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Klentnice
Klentnice (german: Klentnitz) is a municipality and village in Břeclav District in the South Moravian Region of the Czech Republic. It has about 500 inhabitants. Geography Klentnice lies about northwest of Břeclav. It lies in the Pavlov Hills within the Mikulov Highlands. The village is situated on the eastern slope of the hill Stolová hora ( above sea level). The highest point of the municipality is the slope of the hill Obora with an elevation of about . Klentnice is located in the Pálava Protected Landscape Area. History Grave findings of the La Tène culture are documents of an early settlement. In the times of Great Moravia, the area was inhabited by Slavs. After the empire fell, the inhabitants were replaced by German colonists. The first written mention of Klentnice is from 1322, when it was part of the Mikulov estate. As a part of the Mikulov estate, it was owned by the House of Liechtenstein. They contributed to cultural and ethnic enrichment when they invited Jews ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flysch
Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turbidity flow deposits to shallow-water shales and sandstones. It is deposited when a deep basin forms rapidly on the continental side of a mountain building episode. Examples are found near the North American Cordillera, the Alps, the Pyrenees and the Carpathians. Sedimentological properties Flysch consists of repeated sedimentary cycles with upwards fining of the sediments. There are sometimes coarse conglomerates or breccias at the bottom of each cycle, which gradually evolve upwards into sandstone and shale/mudstone. Flysch typically consists of a sequence of shales rhythmically interbedded with thin, hard, graywacke-like sandstones. Typically the shales do not contain many fossils, while the coarser sandstones often have fractions of micas and glauconite. Tectonics In a continental collision, a subducting tectonic plate pushes on the plate above it, making the rock fold, often to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Limestone Alps
The Northern Limestone Alps (german: Nördliche Kalkalpen), also called the Northern Calcareous Alps, are the ranges of the Eastern Alps north of the Central Eastern Alps located in Austria and the adjacent Bavarian lands of southeastern Germany. The distinction from the latter group, where the higher peaks are located, is based on differences in geological composition. Geography If viewed on a west–east axis, the Northern Limestone Alps extend from the Rhine valley and the Bregenz Forest in Vorarlberg, Austria in the west extending along the border between the German federal-state of Bavaria and Austrian Tyrol, through Salzburg, Upper Austria, Styria and Lower Austria and finally ending at the Wienerwald at the city-limits of Vienna in the east. The highest peaks in the Northern Limestone Alps are the Parseierspitze () in the Lechtal Alps,Reynolds, Kev (2010). ''Walking in the Alps'', Cicerone, . and the Hoher Dachstein (). Other notable peaks in this range include the Zugs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strachotín
Strachotín is a municipality and village in Břeclav District in the South Moravian Region of the Czech Republic. It has about 800 inhabitants. Geography Strachotín is located about northwest of Břeclav and south of Brno. It lies in the northwestern tip of the Lower Morava Valley. It it situated on the shores of the Nové Mlýny Reservoir and Strachotínský Pond. History The first written mention of Strachotín is from 1046. In 1334, it was promoted to a market town. During the Thirty Years' War, Strachotín was completely burned down. After the World War II World War II or the Second World War, often abbreviated as WWII or WW2, was a world war that lasted from 1939 to 1945. It involved the vast majority of the world's countries—including all of the great powers—forming two opposin ..., the municipality lost its market town title. References Villages in Břeclav District {{SouthMoravia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Claystone
Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too small to study readily in the field. At first sight, the rock types appear quite similar; however, there are important differences in composition and nomenclature. There has been a great deal of disagreement involving the classification of mudrocks. A few important hurdles to their classification include the following: # Mudrocks are the least understood and among the most understudied sedimentary rocks to date. # Studying mudrock constituents is difficult due to their diminutive size and susceptibility to weathering on outcrops. # And most importantly, scientists accept more than one classification scheme. Mudrocks make up 50% of the sedimentary rocks in the geologic record and are easily the most widespread deposits on Earth. Fine sedimen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calcareous
Calcareous () is an adjective meaning "mostly or partly composed of calcium carbonate", in other words, containing lime or being chalky. The term is used in a wide variety of scientific disciplines. In zoology ''Calcareous'' is used as an adjectival term applied to anatomical structures which are made primarily of calcium carbonate, in animals such as gastropods, i.e., snails, specifically about such structures as the operculum, the clausilium, and the love dart. The term also applies to the calcium carbonate tests of often more or less microscopic Foraminifera. Not all tests are calcareous; diatoms and radiolaria have siliceous tests. The molluscs are calcareous, as are calcareous sponges ( Porifera), that have spicules which are made of calcium carbonate. In botany ''Calcareous grassland'' is a form of grassland characteristic of soils containing much calcium carbonate from underlying chalk or limestone rock. In medicine The term is used in pathology, for example i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ernstbrunn Formation
The Ernstbrunn Formation is a geologic formation in Austria and the Czech Republic. It preserves fossils dated to the 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 J ... period. See also * List of fossiliferous stratigraphic units in Austria References * Geologic formations of Austria Geologic formations of the Czech Republic Jurassic Austria Jurassic System of Europe Tithonian Stage {{Jurassic-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
