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Devín Gate
Devín Gate, Hainburger Gate or Hungarian Gates ( sk, Devínska brána, ; german: Hainburger Pforte) is a natural gate in the Danube valley at the border of Slovakia and Austria. It is one out of four geomorphological areas of the Devín Carpathians, part of the Little Carpathians mountain range. Passau, Devín Gate, and the Iron Gates divide the Danube river into four distinct sections. Devín Gate has been inhabited since prehistoric times, with continuous settlement since 5000 BC. It was a strategic part of the ancient Amber Road connecting Northern Europe with the Mediterranean and during the Middle Ages, five castles have been built here, Heimenburg Castle, Rothelstein Castle, Pottenburg Castle, Devín Castle, and Bratislava Castle. It was continually guarded since Roman times and it has served as a border of the Roman Empire, Austrian Empire, the Iron Curtain during the Cold War and finally a border between Austria and Czechoslovakia, today Slovakia. On 1 May 2004 Slo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devin Gate
Devin may refer to: Places *Devin, Bulgaria, a town *Devin, Minab, a village in Hormozgan Province, Iran *Devin, North Khorasan, a village in North Khorasan Province, Iran *Devin, Razavi Khorasan, a village in Razavi Khorasan Province, Iran *Devin, the Slovene name of Duino in Italy *Devín, a borough of Bratislava, Slovakia **Devín Castle *Děvín, a mountain in the Czech Republic *Devín Gate, a natural gate in the Danube valley at the border of Slovakia and Austria *Camp Devin, Montana, a temporary United States Army camp established in 1878 People *Devin (name), a list of people with the given name or surname *Devin the Dude (born 1970), American hip hop artist Devin Copeland Other uses *Devin Enterprises Devin Enterprises was an American automotive manufacturer that operated from 1955 to 1964. Devin was mainly known for producing high quality fiberglass car bodies that were sold as kits, but they also produced automotive accessories as well as co ..., an American manufac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austrian Empire
The Austrian Empire (german: link=no, Kaiserthum Oesterreich, modern spelling , ) was a Central- Eastern European multinational great power from 1804 to 1867, created by proclamation out of the realms of the Habsburgs. During its existence, it was the third most populous monarchy in Europe after the Russian Empire and the United Kingdom. Along with Prussia, it was one of the two major powers of the German Confederation. Geographically, it was the third-largest empire in Europe after the Russian Empire and the First French Empire (). The empire was proclaimed by Francis II in 1804 in response to Napoleon's declaration of the First French Empire, unifying all Habsburg possessions under one central government. It remained part of the Holy Roman Empire until the latter's dissolution in 1806. It continued fighting against Napoleon throughout the Napoleonic Wars, except for a period between 1809 and 1813, when Austria was first allied with Napoleon during the invasion o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the 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). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of 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 vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite whic ... [...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 lime ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago (Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' (" coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian lin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained ( phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or '' granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lamač Gate
Lamač Gate ( sk, Lamačská brána) is a tectonic erosion subsidence in Bratislava, the capital of Slovakia. It is one out of four geomorphological areas of the Devín Carpathians, part of the Little Carpathians mountain range, separating Devín Carpathians from the central massif of Little Carpathians. The city borough of Lamač and parts of Dúbravka lie geographically within the Lamač Gate. Location and description Lamač Gate is located in the north-western part of Bratislava to the east of the Devín Gate. Both gates are predisposed tectonic erosion subsidences where parts of the city of Bratislava are located. Lamač Gate forms the continuation of the Záhorie Lowland but it does not connect all the way to the Danubian Lowland. It consists of the mouth of the gate close to the Záhorie Lowland, central part (called the Lamač-Dúbravka part) is the largest and highest part of the gate, it then significantly narrows down between the massifs of Kamzík and Staré Grunty ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
AMSL
Height above mean sea level is a measure of the vertical distance (height, elevation or altitude) of a location in reference to a historic mean sea level taken as a vertical datum. In geodesy, it is formalized as '' orthometric heights''. The combination of unit of measurement and the physical quantity (height) is called "metres above mean sea level" in the metric system, while in United States customary and imperial units it would be called " feet above mean sea level". Mean sea levels are affected by climate change and other factors and change over time. For this and other reasons, recorded measurements of elevation above sea level at a reference time in history might differ from the actual elevation of a given location over sea level at a given moment. Uses Metres above sea level is the standard measurement of the elevation or altitude of: * Geographic locations such as towns, mountains and other landmarks. * The top of buildings and other structures. * Flying objects s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hundsheimer Berge
The Hundsheimer Berge (also Hainburger Berge) is a hill range located in Lower Austria and Burgenland, Austria next to the Devín Gate. It is the most southern part of the Devín Carpathians. The mountain range covers approximately 36 km2 and is bordered by the river Danube to the north and east, and the Vienna plate to the south and west. Its highest peak is Hundsheimer Berg (481 meters AMSL). While fairly low, the Hundsheimer Berge rise from only 140 meters above sea level by the Danube. The mountains are densely forested, mostly with beech trees. The southern slopes are traditionally used by humans for agriculture and particularly wine-making. There are many vineyards in the area. South of Edelstal are wine cellars offering wine-tasting. The mountains feature the ruins of the Pottenburg Castle. Major peaks: * Hundsheimer Berg (481 meters AMSL) * Weisses Kreuz (363 meters AMSL) * Braunsberg (346 meters AMSL) * Königswarte (344 meters AMSL) * Pfaffenberg (331 meters AMSL) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hundsheimer Berg
Hundsheimer Berg is a hill located in the Hundsheimer Berge hill range in Lower Austria, Austria close to the border with Slovakia Slovakia (; sk, Slovensko ), officially the Slovak Republic ( sk, Slovenská republika, links=no ), 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 .... Its peak is above sea level which makes it the highest hill in the Hundsheimer Berge. The north slopes of the Hundsheimer Berg are covered with forests while the southern slopes have a steppe vegetation. Since 1965, a nature reserve with the same name, '' Hundsheimer Berg'', is located on these southern slopes. References {{Reflist Geography of Lower Austria ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schengen Zone
The Schengen Area ( , ) is an area comprising 27 European countries that have officially abolished all passport and all other types of border control at their mutual borders. Being an element within the wider area of freedom, security and justice policy of the EU, it mostly functions as a single jurisdiction under a common visa policy for international travel purposes. The area is named after the 1985 Schengen Agreement and the 1990 Schengen Convention, both signed in Schengen, Luxembourg. Of the 27 EU member states, 23 participate in the Schengen Area. Of the five EU members that are not part of the Schengen Area, three—Bulgaria, Cyprus and Romania—are legally obligated to join the area in the future; Croatia has been approved to join on January 1, 2023; Ireland maintains an opt-out, and instead operates its own visa policy. The four European Free Trade Association (EFTA) member states, Iceland, Liechtenstein, Norway, and Switzerland, are not members of the EU, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
