Perșani Mountains
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Perșani Mountains
The Perșani Mountains ( ro, Munții Perșani; hu, Persányi-hegység) is a mountain range in central Romania. The highest peak is , with an elevation of . Geologically, the Perșani Mountains are part of the Căliman-Harghita Mountains of the Inner Eastern Carpathians. Within Romania, however, it is traditional to divide the Eastern Carpathians in Romanian territory into three geographical groups (north, center, south), instead. The Romanian categorization includes the Perșani Mountains within the central Carpathians of Moldavia and Transylvania (''Munții Carpați Moldo-Transilvani''), which also comprise the Baraolt Mountains, the Bârgău Mountains, the Călimani Mountains, the Ciuc Mountains, the Gurghiu Mountains, and the Harghita Mountains. The main ridge runs in a north-south direction and has a length of . The Perșani Mountains consists mainly of basalt, shale, and flysch Flysch () is a sequence of sedimentary rock layers that progress from deep-water and turb ...
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Călimani Mountains
The Călimani Mountains ( ro, Munții Călimani, hu, Kelemen-havasok) are the largest volcanic complex of the Carpathian Mountains in Transylvania, Romania. Geologically they belong to the Căliman-Harghita Mountains group of the Inner Eastern Carpathians. Maximum height is reached in Pietrosul Călimanilor Peak, at 2,102 m. Other significant peaks include: Bistriciorul (1,990 m), Stuniorul (1,885 m), Gruiului (1,913 m), Negoiul Unguresc (2,084 m), Rețițiș (2,021 m), Bradul Ciont (1,899 m), Iezerul Călimanilor (2,023 m). The volcanic crater with a diameter of 10 km is bordered by the highest peaks, and to north is split by Valea Neagră, a tributary of Dorna River. Inside the crater there are several secondary volcanic funnels (Pietricelui, Vârful Haitei, Negoiul Românesc), the last one being a exploitation of sulfur until 1997. Among the major tourist attractions include odd shapes of volcanic rocks on Tihul, Rusca and Rețițiș Mountains, but especially on Tămă ...
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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 t ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable bedding ...
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Basalt
Basalt (; ) is an aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the surface of a rocky planet or moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of Venus, which cover ~80% of the surface, are basaltic; the lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flows that can spread over great areas before cooling and solidifying. Flood basalts are t ...
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Harghita Mountains
The Harghita Mountains (in Hungarian Hargita, in Romanian ''Munții Harghita'') is a volcanic mountain range of the Căliman-Harghita Mountains in Harghita County of Romania, part of the Inner Eastern Carpathians. The range is about long and wide, and is the "largest andesite mass" and the "largest volcanic body in the whole of Europe Europe is a large peninsula conventionally considered a continent in its own right because of its great physical size and the weight of its history and traditions. Europe is also considered a subcontinent of Eurasia and it is located entirel ...". Its tallest peak is Harghita Mădăraș (''Madarasi Hargita''), at . References {{Authority control Mountain ranges of Romania Mountain ranges of the Eastern Carpathians ...
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Gurghiu Mountains
300px, Carpathian Mountains in Romania. The Gurghiu Mountains are to the north of the center of this image. The Gurghiu Mountains (Romanian: Munții Gurghiu, Hungarian: Görgény) are a range in the Căliman-Harghita Mountains of the Eastern Carpathians, Romania, in the Transylvania region. They cover an area of . The mountains are relatively low, but well-wooded and naturally beautiful. They are known for an abundance of wildlife, including deer, wild boar, wolves and bears. The highest peak, Vârful Saca Mare, is . Notable peaks include Amza Peak at , Saca Mică Peak at , and Fâncelu at . Average rainfall is about and average temperature . The Gurghiu Mountains are part of the volcanic mountain chain in the western side of the Eastern Carpathians. In the north the Mureș River separates them from the Călimani Mountains. To the south are the Harghita Mountains and the Târnava River The Târnava (full name in ro, Râul Târnava; hu, Küküllő; german: Kokel; tr, ...
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Ciuc Mountains
Ciuc Mountains (Romanian ''Munții Ciucului'', Hungarian ''Csíki-havasok'') are a mid-high range of mountains of Harghita County in Transylvania, Romania. Geologically they belong to the Căliman-Harghita Mountains group of the Inner Eastern Carpathians. Within Romania, however, it is traditional to divide the Eastern Carpathians (''Carpații Orientali'') into three geographical groups (north, center and south) instead. The Romanian categorization includes the Ciuc Mountains within the central Carpathians of Moldavia and Transylvania (''Grupa Centrală'', ''Carpaţii Moldo-Transilvani''). The Trotuș River emerges from these mountains. The highest peak is Noșcolat, at 1,553 m. See also *Divisions of the Carpathians Divisions of the Carpathians are a categorization of the Carpathian mountains system. Below is a detailed overview of the major subdivisions and ranges of the Carpathian Mountains. The Carpathians are a "subsystem" of a bigger Alps-Himalaya Sy ... External l ...
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Bârgău Mountains
The Bârgău Mountains ( hu, Borgói-hegység) are a mountain range in the Carpathian Mountains, part of the Căliman-Harghita Mountains in the Bistrița-Năsăud County, in the north of Romania Romania ( ; ro, România ) is a country located at the crossroads of Central, Eastern, and Southeastern Europe. It borders Bulgaria to the south, Ukraine to the north, Hungary to the west, Serbia to the southwest, Moldova to the east, and .... The highest point is Heniu Mare at 1,610.5 meters. Mountain ranges of Romania Mountain ranges of the Eastern Carpathians {{Romania-geo-stub ...
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Baraolt Mountains
The Baraolt Mountains () is a mountain range, entirely in Covasna County of Romania. Geologically the Baraolts are part of the Căliman-Harghita Mountains, of the Inner Eastern Carpathians. By traditional Romanian categorization it's included in the Curvature Carpathians. The largest city in the area is Sfântu Gheorghe, along with the towns of Baraolt Baraolt (; hu, Barót, ) is a town and administrative district in Covasna County, Romania. It lies in the Székely Land, an ethno-cultural region in eastern Transylvania. The town was mentioned for the first time as a settlement in 1224. It adm ... and Malnaș. The highest peak is ''Vârful Havad'' at . The Baraolt Mountains is a popular hiking area. References {{coord, 46, 00, N, 25, 45, E, region:RO_type:mountain_source:kolossus-dewiki, display=title Mountain ranges of Romania Mountain ranges of the Eastern Carpathians ...
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Transylvania
Transylvania ( ro, Ardeal or ; hu, Erdély; german: Siebenbürgen) is a historical and cultural region in Central Europe, encompassing central Romania. To the east and south its natural border is the Carpathian Mountains, and to the west the Apuseni Mountains. Broader definitions of Transylvania also include the western and northwestern Romanian regions of Crișana and Maramureș, and occasionally Banat. Transylvania is known for the scenery of its Carpathian landscape and its rich history. It also contains Romania's second-largest city, Cluj-Napoca, and other iconic cities and towns such as Brașov, Sibiu, Târgu Mureș, Alba Iulia and Sighișoara. It is also the home of some of Romania's UNESCO World Heritage Sites such as the Villages with fortified churches, the Historic Centre of Sighișoara, the Dacian Fortresses of the Orăștie Mountains and the Roșia Montană Mining Cultural Landscape. It was under the rule of the Agathyrsi, part of the Dacian Kingdom (168 BC–106 ...
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