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Považský Inovec
Považský Inovec is a mountain range in western Slovakia, named after the Váh river. It is 48 km (30 mi) long and 15–25 km (9-16 mi) wide mountain range. It is situated from the city of Hlohovec, raising from the Danubian Hills, and slowly raising further north until nearly to the city of Trenčín where it borders the Strážov Mountains, where is also the highest hill of the entire mountain range, ''Inovec'' (1042 m). The mountain range separates basins of the Váh and Nitra rivers. There are many monuments in or near the mountain range, including Great Moravian hill fort ''Kostolec'' near Ducové, Hlohovec Castle near Hlohovec, Beckov Castle near Beckov, Topoľčany Castle and Tematín Castle. The famous spa city of Piešťany lies under Považský Inovec. Geology Považský Inovec Mts. is considered as asymmetric horst emerging from the Neogene sedimentary fill of the Pannonian Basin between the Váh and Nitra rivers. The horst is bordered b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Piešťany
Piešťany (; german: Pistyan, hu, Pöstyén, pl, Pieszczany , cs, Píšťany ) is a town in Slovakia. It is located in the western part of the country within the Trnava Region and is the seat of its own district. It is the biggest and best known spa town in Slovakia and has around 28,000 inhabitants. Etymology The name Piešťany comes from Slovak ''Piesok'' (sand), referring to local sandbanks. The etymology is straightforward – ''Piešťanci'' – people who live on the sandy site and ''Piešťany'' – their settlement. History The first human settlement in the area is dated to the prehistoric times, about 80,000 years ago. People were attracted to the site by abundance of game in the vicinity of the thermal springs that did not freeze in winter. A small female statue called Venus of Moravany was found in the nearby village Moravany nad Váhom. It is made of mammoth ivory and is dated to 22,800 BC. It currently resides in the Bratislava Castle museum. In another nearb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hrádok
Hrádok ( hu, Temetvény) is a village and municipality in Nové Mesto nad Váhom District in the Trenčín Region of western Slovakia. History In historical records the village was first mentioned in 1246. Geography The municipality lies at an altitude of 200 metres and covers an area of 24.135 km². It has a population of about 596 people. Genealogical resources The records for genealogical research are available at the state archive "Statny Archiv in Bratislava, Slovakia" * Roman Catholic church records (births/marriages/deaths): 1719-1907 (parish A) * Lutheran church records (births/marriages/deaths): 1660-1895 (parish B) See also * List of municipalities and towns in Slovakia This is an alphabetical list of the 2,891 Obec, obcí (singular ''obec'', "municipality") in Slovakia. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Selec
Selec ( hu, Szelec) is a village and municipality in Trenčín District in the Trenčín Region of north-western Slovakia. History The village was first mentioned in historical records of 1439. During World War II, on the December 3, 1944, German troops invaded the village and arrested 56 men from the village for help to partisans. 50 from them have been later taken to the concentration camps where 45 of them died. Geography The municipality lies at an altitude of 319 metres and covers an area of 24.802 km². It has a population of about 957 people. From a geomorphological point of view of the village lies in Fatra-Tatra Area in the northern part of the Považský Inovec Mts. External links *http://www.statistics.sk/mosmis/eng/run.html Villages and municipalities in Trenčín District {{Trenčín-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kálnica Group
Kálnica ( hu, Kalános) is a village and municipality in Nové Mesto nad Váhom District Nové Mesto nad Váhom District ( sk, okres Nové Mesto nad Váhom, hu, Vágújhelyi járás) is a district in the Trenčín Region of western Slovakia. Before 1920, the territory of the district was mostly part of the county of Kingdom of Hun ... in the Trenčín Region of western Slovakia. History In historical records the village was first mentioned in 1396. Geography The municipality lies at an elevation of 215 metres (705 ft) and covers an area of 26.404 km² (10.195 mi²). It has a population of about 1,047. Genealogical resources The records for genealogical research are available at the state archive "Statny Archiv in Bratislava, Slovakia" * Roman Catholic church records (births/marriages/deaths): 1676-1934 (parish B) Notable residents * Gyula Kertész (1888–1982), Hungarian footballer See also * List of municipalities and towns in Slovakia Re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Late Paleozoic
Late may refer to: * LATE, an acronym which could stand for: ** Limbic-predominant age-related TDP-43 encephalopathy, a proposed form of dementia ** Local-authority trading enterprise, a New Zealand business law ** Local average treatment effect, a concept in econometrics Music * ''Late'' (album), a 2000 album by The 77s * Late!, a pseudonym used by Dave Grohl on his '' Pocketwatch'' album * Late (rapper), an underground rapper from Wolverhampton * "Late" (song), a song by Blue Angel * "Late", a song by Kanye West from '' Late Registration'' Other * Late (Tonga), an uninhabited volcanic island southwest of Vavau in the kingdom of Tonga * "Late" (''The Handmaid's Tale''), a television episode * LaTe, Oy Laivateollisuus Ab, a defunct shipbuilding company * Late may refer to a person who is Dead See also * * * '' Lates'', a genus of fish in the lates perch family * Later (other) * Tardiness * Tardiness (scheduling) {{disambig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Migmatite
Migmatite is a composite rock found in medium and high-grade metamorphic environments, commonly within Precambrian cratonic blocks. It consists of two or more constituents often layered repetitively: one layer is an older metamorphic rock that was reconstituted subsequently by partial melting ("paleosome"), while the alternate layer has a pegmatitic, aplitic, granitic or generally plutonic appearance ("neosome"). Commonly, migmatites occur below deformed metamorphic rocks that represent the base of eroded mountain chains. Migmatites form under extreme temperature and pressure conditions during prograde metamorphism, when partial melting occurs in metamorphic paleosome. Components exsolved by partial melting are called neosome (meaning ‘new body’), which may or may not be heterogeneous at the microscopic to macroscopic scale. Migmatites often appear as tightly, incoherently folded veins ( ptygmatic folds).Recommendations by the IUGS Subcommission on the Systematics of M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibolite
Amphibolite () is a metamorphic rock that contains amphibole, especially hornblende and actinolite, as well as plagioclase feldspar, but with little or no quartz. It is typically dark-colored and dense, with a weakly foliated or schistose (flaky) structure. The small flakes of black and white in the rock often give it a salt-and-pepper appearance. Amphibolite frequently forms by metamorphism of mafic igneous rocks, such as basalt. However, because metamorphism creates minerals entirely based upon the chemistry of the protolith, certain 'dirty marls' and volcanic sediments may also metamorphose to an amphibolite assemblage. Deposits containing dolomite and siderite also readily yield amphibolite (tremolite-schist, grunerite-schist, and others) especially where there has been a certain amount of contact metamorphism by adjacent granitic masses. Metamorphosed basalt (metabasalt) creates ''ortho-amphibolite'' and other chemically appropriate lithologies create ''para-amphibolite''. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Normal Fault
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
