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Western Romanian Carpathians
The Western Romanian Carpathians (, ), along with the Eastern Romanian Carpathians and the Southern Carpathians is one of the three main mountain ranges of Romania. Their name is given based on their geographical position, west, to the Transylvanian Plateau, which is simultaneously their eastern limits, respectively to the Timiș-Cerna Gap of the Banat Mountains, the southern group of the Western Carpathians. The Western Carpathians are positioned between the rivers Danube, Barcău and Someș. They have a maximum elevation of 1849 m in the Bihor Mountains, '' Cucurbăta Mare'' Peak ( Hungarian: Nagy-Bihar) - 1849 metres, also called Bihor Peak. Discontinuity is one of their basic characteristics. Geographical composition is varied, with a real "petrographic mosaic". (flysch, crystalline schists, limestones, igneous rocks, metamorphic rocks) Mountain ranges From north to south, three major mountain groups can be identified, separated by different river valleys. * Apuseni Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Apuseni Mountains
The Apuseni Mountains (, "Western Mountains"; , "Transylvanian Mountains") are a mountain range in Transylvania, Romania, which belongs to the Western Romanian Carpathians. The highest peak is the Bihor Peak at . The Apuseni Mountains have about 400 caves. Geography The Apuseni Mountains do not present an uninterrupted chain of mountains, but possess many low and easy passes towards the Crișana and the Pannonian Plain. Going from south to north the principal groups are: the Munții Metaliferi ("Ore Mountains") with the basaltic masses of the Detunata () near Abrud; the Bihor Mountains, with numerous caverns, with the highest peak the Bihorul (); to the east of this group are the Muntele Mare (highest peak ), to the southwest of Cluj-Napoca; the northernmost chain is the Seș and Meseș Mountains. Boundaries *To the north: the Barcău River. *To the south: the Mureș River. *To the east: the Transylvanian Plateau. *To the west: the Crișana plains. Subdivisions ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bihor Mountains
Bihor Mountains (, ) is a mountain range in western Romania. It is part of the Apuseni Mountains, which are part of the Carpathian Mountains. The massif has a length of from the northwest to the southeast and a width of . It is located east of the town Ștei, Bihor County and north of the town of Brad, Hunedoara, Brad, Hunedoara County. The highest peak is Cucurbăta Mare, with an elevation of ; this also the highest peak of the Apuseni Mountains. Other high peaks are Buteasa (1,790 m), Cârligatele (1,694 m), Piatra Grăitoare (1,658 m), and Bohodei (1,654 m). The is a volcanic range extension of the Bihor Mountains to the north, reaching a maximum height of . 
Mountain ranges of Romania
Mountain ranges of the Western Romanian Carpathians
Western Romanian Car ...
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Mountain Ranges Of The Carpathians
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains te ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Romanian Carpathians
The Western Romanian Carpathians (, ), along with the Eastern Romanian Carpathians and the Southern Carpathians is one of the three main mountain ranges of Romania. Their name is given based on their geographical position, west, to the Transylvanian Plateau, which is simultaneously their eastern limits, respectively to the Timiș-Cerna Gap of the Banat Mountains, the southern group of the Western Carpathians. The Western Carpathians are positioned between the rivers Danube, Barcău and Someș. They have a maximum elevation of 1849 m in the Bihor Mountains, '' Cucurbăta Mare'' Peak ( Hungarian: Nagy-Bihar) - 1849 metres, also called Bihor Peak. Discontinuity is one of their basic characteristics. Geographical composition is varied, with a real "petrographic mosaic". (flysch, crystalline schists, limestones, igneous rocks, metamorphic rocks) Mountain ranges From north to south, three major mountain groups can be identified, separated by different river valleys. * Apuseni Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Romanian Carpathians
The Romanian Carpathians () are a section of the Carpathian Mountains, within the borders of modern Romania. The Carpathians are a "subsystem" of the Alps-Himalaya System and are further divided into "provinces" and "subprovinces". This is an overview of the geological subdivisions of the Romanian section of the Carpathian Mountains. The broadest divisions are shown in the map on the right. The last level of the division, i.e. the actual mountain ranges and basins, is usually called "units". The lowest-level detail for those units is maintained on separate pages. Naming conventions Traditional Romanian naming conventions differ from this list. In Romania, it is usual to divide the Eastern Carpathians in Romanian territory into three geographical groups (North, Centre, South), instead in Outer and Inner Eastern Carpathians. The Transylvanian Plateau is encircled by, and geologically a part of, the Carpathians, but it is not a mountainous region and its inclusion is disputed i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Timiș River
The Timiș or Tamiš (, , , ) is a river that flows through the Banat region of Romania and Serbia and joins the Danube near Pančevo, in northern Serbia. Due to its position in the region, it has been labeled as the "spine of the Banat". Name In antiquity, the river was known as ''Tibiscus'' (in Latin) and ''Tibisis'' (Θίβισις in ancient Greek), and as ''Timisis'' in De Administrando Imperio; in addition, Edward Gibbon referred to it as the ''Teyss''. ''The Romans, who traversed the plains of Hungary, suppose that they passed several navigable rivers, either in canoes or portable boats; but there is reason to suspect that the winding stream of the Teyss, or Tibiscus, might present itself in different places under different names.'' Geography The drainage area covers , of which in Romania. With the Danube, the Timis belongs to the Black Sea drainage basin. The river flows through Romania for , and through Serbia. Its average discharge at the mouth is . The sour ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mureș River
Mureș may refer to: * Mureș County, Romania * Mureș (river) in Romania and Hungary (''Maros'') * Mureș culture, a Bronze Age culture from Romania See also * Târgu Mureș, the capital of Mureș County * Ocna Mureș, a town in Alba County, Romania {{Disambig, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hungarian Language
Hungarian, or Magyar (, ), is an Ugric language of the Uralic language family spoken in Hungary and parts of several neighboring countries. It is the official language of Hungary and one of the 24 official languages of the European Union. Outside Hungary, it is also spoken by Hungarians, Hungarian communities in southern Slovakia, western Ukraine (Zakarpattia Oblast, Transcarpathia), central and western Romania (Transylvania), northern Serbia (Vojvodina), northern Croatia, northeastern Slovenia (Prekmurje), and eastern Austria (Burgenland). It is also spoken by Hungarian diaspora communities worldwide, especially in North America (particularly the Hungarian Americans, United States and Canada) and Israel. With 14 million speakers, it is the Uralic family's most widely spoken language. Classification Hungarian is a member of the Uralic language family. Linguistic connections between Hungarian and other Uralic languages were noticed in the 1670s, and the family's existenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cucurbăta Mare
Cucurbăta Mare (), also known as Bihor Peak, is a mountain in the Bihor Mountains. It is located in the southeastern part of Bihor County, near the border with Alba County, in Romania Romania is a country located at the crossroads of Central Europe, Central, Eastern Europe, Eastern and Southeast Europe. It borders Ukraine to the north and east, Hungary to the west, Serbia to the southwest, Bulgaria to the south, Moldova to .... It is high and the tallest mountain in the Western Romanian Carpathians.2017 Romanian Statistical Yearbook p. 12 References External links Video of mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Someș
The Someș () or Szamos ( or ''Samosch'') is a left tributary of the Tisza in Hungary and Romania. It has a length of (including its source river Someșul Mare), of which 50 km are in Hungary.Analysis of the Tisza River Basin 2007 International Commission for the Protection of the Danube River, IPCDR The Someș is the fifth largest river by length and volume in Romania. The hydrographic basin forms by the confluence at Mica, Cluj, Mica, a commune about 4 km upstream of Dej, of Someșul Mare and Someșul Mic rivers. Someșul Mic (formed by the confluence of Someșul Rece with Someșul Cald) originates in the Apuseni Mountains, and Someșul Mare springs from the Rodna Mountains. Someșul Mare has a length of 130 km and an area of 5,033 km2 and a slight asym ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Orogeny
The Alpine orogeny, sometimes referred to as the Alpide orogeny, is an orogenic phase in the Late Mesozoic and the current Cenozoic which has formed the mountain ranges of the Alpide belt. Cause The Alpine orogeny was caused by the African continent, the Arabian Peninsula, the Indian subcontinent, and the Cimmerian plate colliding with Eurasia in the north. Convergent movements between the African, Arabian and Indian plates from the south, and the Eurasian plate and the Anatolian sub-plate from the north – as well as many smaller (micro)plates – had already begun during the early Cretaceous, but the major phases of mountain building began during the Paleocene to the Eocene. The process continues currently in some of the Alpide mountain ranges. The Alpine orogeny is considered one of the three major phases of orogeny in Europe that define the geology of that continent, along with the Caledonian orogeny that formed the Old Red Sandstone Continent when the continents ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
