|
Western Carpathians
The Western Carpathians () are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains. The mountain belt stretches from the Low Beskids range of the Eastern Carpathians along the border of Poland with Slovakia toward the Moravian region of the Czech Republic and the Austrian Weinviertel. In the south the North Hungarian Mountains cover northern Hungary. The area of the Western Carpathians comprises about 70,000 km2. The highest elevation is the Gerlachovský štít (2,655m) situated in the High Tatra Mountains. Geographical definition Most of the perimeter of the Western Carpathians is quite sharply defined by valleys. To the northwest and north they are separated from the Bohemian Massif by the Outer Subcarpathia and the Lesser Poland Upland; to the west the Moravian Gate leads over to the Sudetes. To the south the mountain chain falls away towards the Pannonian Plain, a large plain situated between the Alps, the Dinari ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kościelec (High Tatras)
Kościelec (2,155 m above sea level) is a mountain in the High Tatras in the Gąsienicowa Valley of Poland. In popular culture On February 8, 1909, the composer Mieczysław Karłowicz Mieczysław Karłowicz (, 11 December 18768 February 1909) was a Polish composer and conductor. Life Mieczysław Karłowicz was born in Vishneva, in the Vilna Governorate of the Russian Empire (now in Belarus) into a noble family belonging to ... was killed at the age of 32 by an avalanche while skiing in the Little Kościelec. This incident was commemorated by Wojciech Kilar in his tone poem ''Kościelec 1909'', composed in 1976. File:Kościelec a9.jpg, General view of Kościelec File:Czarny Staw Gąsienicowy, widok na Kościelec.jpg, Kościelec seen from Czarny Staw Gąsienicowy File:Koscielec-widok-z-hali-gasienicowej.JPG, View from Królowe Rówienki References High Tatras Mountains of the Western Carpathians Two-thousanders of Poland {{LesserPoland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bohemian Massif
The Bohemian Massif ( or ''Český masiv'', or ''Böhmisches Massiv'') is a geomorphological province in Central Europe. It is a large massif stretching over most of the Czech Republic, eastern Germany, southern Poland and northern Austria. The massif encompasses a number of mittelgebirges and consists of crystalline rocks, which are older than the Permian (more than 300 million years old) and therefore deformed during the Variscan Orogeny. Parts of the Sudetes within the Bohemian Massif, Giant Mountains in particular, stand out from the ordinary mittelgebirge pattern by having up to four distinct levels of altitudinal zonation, glacial cirques, small periglacial landforms and an elevation significantly above the timber line. Geomorphological divisions The Bohemian Massif is a province within the Hercynian Forest subsystem. It borders with four provinces: Western Carpathians on the east, Eastern Alps on the south, North European Plain on the north, and Central Upla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
High Tatra Mountains
The High Tatras or High Tatra Mountains (; ; ,'' Vysoki Tatry''; ; ), are a mountain range along the border of northern Slovakia in the Prešov Region, and southern Poland in the Lesser Poland Voivodeship. They are a range of the Tatra Mountains chain. Description The mountain range borders the Belianske Tatras to the east, the Podtatranská kotlina to the south, and the Western Tatras to the west. Most of the range, and all the highest peaks, are in Slovakia. The highest peak is Gerlachovský štít, at . Biogeography The High Tatras, having 29 peaks over AMSL are, with the Southern Carpathians, the only mountain ranges with an alpine character and habitats in the entire length of the Carpathian Mountains system. The first European cross-border national park, Tatra National Park, was founded here with Tatra National Park (''Tatranský národný park'') in Slovakia in 1948, and Tatra National Park (''Tatrzański Park Narodowy'') in Poland in 1954. The contiguous parks p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hungary
Hungary is a landlocked country in Central Europe. Spanning much of the Pannonian Basin, Carpathian Basin, it is bordered by Slovakia to the north, Ukraine to the northeast, Romania to the east and southeast, Serbia to the south, Croatia and Slovenia to the southwest, and Austria to the west. Hungary lies within the drainage basin of the Danube, Danube River and is dominated by great lowland plains. It has a population of 9.6 million, consisting mostly of ethnic Hungarians, Hungarians (Magyars) and a significant Romani people in Hungary, Romani minority. Hungarian language, Hungarian is the Languages of Hungary, official language, and among Languages of Europe, the few in Europe outside the Indo-European languages, Indo-European family. Budapest is the country's capital and List of cities and towns of Hungary, largest city, and the dominant cultural and economic centre. Prior to the foundation of the Hungarian state, various peoples settled in the territory of present-day Hun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Hungarian Mountains
The North Hungarian Mountains (), sometimes also referred to as the Northeast Hungarian Mountains, Northeast Mountains, North Hungarian Highlands, North Hungarian Mid-Mountains or North Hungarian Range, is the northern, mountainous part of Hungary. It forms a geographical unity with the Mátra-Slanec Area, the adjacent parts of Slovakia. It is a separate geomorphological area within the Western Carpathians. The mountains run along the northeastern border of Hungary as well as eastern parts of the Hungarian–Slovak border in broadband from the Danube Bend to the town of Prešov. Subdivisions The area consists of the following geomorphological units: * Börzsöny Regional Map Series of Hungary ( + Burda (SK) * [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Austria
Austria, formally the Republic of Austria, is a landlocked country in Central Europe, lying in the Eastern Alps. It is a federation of nine Federal states of Austria, states, of which the capital Vienna is the List of largest cities in Austria, most populous city and state. Austria is bordered by Germany to the northwest, the Czech Republic to the north, Slovakia to the northeast, Hungary to the east, Slovenia and Italy to the south, and Switzerland and Liechtenstein to the west. The country occupies an area of and has Austrians, a population of around 9 million. The area of today's Austria has been inhabited since at least the Paleolithic, Paleolithic period. Around 400 BC, it was inhabited by the Celts and then annexed by the Roman Empire, Romans in the late 1st century BC. Christianization in the region began in the 4th and 5th centuries, during the late Western Roman Empire, Roman period, followed by the arrival of numerous Germanic tribes during the Migration Period. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovakia
Slovakia, officially the Slovak Republic, 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 west, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , hosting a population exceeding 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of the present-day Slovakia in the 5th and 6th centuries. From the late 6th century, parts of modern Slovakia were incorporated into the Pannonian Avars, Avar Khaghanate. In the 7th century, the Slavs played a significant role in the creation of Samo's Empire. When the Avar Khaghanate dissolved in the 9th century, the Slavs established the Principality of Nitra before it was annexed by the Great Moravia, Principality of Moravia, which later became Great Moravia. When Great Moravia fell in the 10th century, the territory was integrated i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low Beskids
The Low Beskids () or Central Beskids (; ; ) are a mountain range in southeastern Poland and northeastern Slovakia. They constitute a middle (central) section of the Beskids, within the Outer Eastern Carpathians. Since there are several traditional divisions of the '' Beskid Mountains'' in general, this particular region has also been classified by different designations. In Slovak terminology, the region is called ''Low Beskids'' (). In Polish terminology, the same region is not classified under the term ''Low Beskids'' (), since that term is used to designate only one part of the region, while the Polish equivalent term for the entire region is ''Central Beskids'' (). It is a hilly region, encompassing the Prešov Region, Sanok County and Jasło County, and covering the area between Busov, Ondavská vrchovina, Laborecká vrchovina, Beskydské predhorie in Slovakia, and Beskid Sądecki, Pogórze Bukowskie and Bieszczady near the river Wisłoka, Wisłok and Osława in Po ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology () is the scientific study of the origin and evolution of topographic and bathymetric features generated by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes comprise the action of water, wind, ice, wildfire, and lif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Range
A mountain range or hill range is a series of mountains or hills arranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets. Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types. Major ranges Most geolo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inner Western 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 System that stretches from western Europe all the way to southern Asia, and are further divided into "provinces" and "subprovinces". The last level of the division, i.e. the actual mountain ranges and basins, is usually classified as "units". The main divisions are shown in the map on the right. To generalize, there are three major provinces (regions): Western Carpathians, Eastern Carpathians, and the Southern Carpathians. Naming conventions The division is largely (with many exceptions) undisputed at the lowest level (except for the Ukrainian part), but various divisions are given for the higher levels, especially for the penultimate level. A geomorphological division has been used as much as the data was available; other new physioge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
