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West 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). 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 Forecarpathian Lowland 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 Dinaric Alps, and the main mass of the Eas ...
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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 was killed at the age of 32 by an avalanche while skiing in the Kościelec mountain. This incident was commemorated by Wojciech Kilar Wojciech Kilar (; 17 July 1932 – 29 December 2013) was a Polish classical and film music composer. One of his greatest successes came with his score to Francis Ford Coppola's '' Bram Stoker's Dracula'' in 1992, which received the ASCAP Award a ... in his tone poem ''Kościelec 1909'', composed in 1976. File:Kościelec path 1.jpg, Path to Kościelec File:Kościelec view 9.jpg, View from the top of the mountain File:Czarny Staw Gąsienicowy, widok na Kościelec.jpg, The mountain seen from Czarny Staw Gąsienicowy lake References High Tatras Mountains of the Western Carpathians Two-thousanders of Poland {{LesserPoland-geo-stub ...
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Andesite
Andesite () is a volcanic rock of intermediate composition. In a general sense, it is the intermediate type between silica-poor basalt and silica-rich rhyolite. It is fine-grained (aphanitic) to porphyritic in texture, and is composed predominantly of sodium-rich plagioclase plus pyroxene or hornblende. Andesite is the extrusive equivalent of plutonic diorite. Characteristic of subduction zones, andesite represents the dominant rock type in island arcs. The average composition of the continental crust is andesitic. Along with basalts, andesites are a component of the Martian crust. The name ''andesite'' is derived from the Andes mountain range, where this rock type is found in abundance. It was first applied by Christian Leopold von Buch in 1826. Description Andesite is an aphanitic (fine-grained) igneous rock that is intermediate in its content of silica and low in alkali metals. It has less than 20% quartz and 10% feldspathoid by volume, with at least 65% of ...
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Lesser Poland Upland
Lesser, from Eliezer (, "Help/Court of my God"), is a surname. Notable people with the surname include: * Adolf Lesser (1851–1926), German physician * Aleksander Lesser (1814–1884), Polish painter and art critic * Anton Lesser (born 1952), British actor * Axel Lesser (born 1946), East German cross country skier * Edmund Lesser (1852–1918), German dermatologist * Erik Lesser (born 1988), German biathlete * Gabriele Lesser (born 1960), German historian and journalist * George Lesser, American musician * Gerald S. Lesser (1926–2010), American psychologist * Henry Lesser (born 1963), German footballer * J Lesser (born 1970), American musician * Len Lesser (1922–2011), American actor * Louis Lesser (born 1916), American real estate developer * Matt Lesser, Connecticut politician * Mike Lesser (born 1943), British mathematical philosopher and political activist * Milton Lesser or Stephen Marlowe (1928–2008), American author * Norman Lesser (1902–1985), Anglican bis ...
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Bohemian Massif
The Bohemian Massif ( cs, Česká vysočina or ''Český masiv'', german: Böhmische Masse 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, N ...
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Hungary
Hungary ( hu, Magyarország ) is a landlocked country in Central Europe. Spanning 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 has a population of nearly 9 million, mostly ethnic Hungarians and a significant Romani people in Hungary, Romani minority. Hungarian language, Hungarian, the Languages of Hungary, official language, is the world's most widely spoken Uralic languages, Uralic language and among the few non-Indo-European languages widely spoken in Europe. Budapest is the country's capital and List of cities and towns of Hungary, largest city; other major urban areas include Debrecen, Szeged, Miskolc, Pécs, and Győr. The territory of present-day Hungary has for centuries been a crossroads for various peoples, including Celts, Ancient Rome, Romans, Germanic peoples, Germanic trib ...
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North Hungarian Mountains
The North Hungarian Mountains ( hu, Északi-középhegység), 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
( hu, Börzsöny +
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Austria
Austria, , bar, Östareich officially the Republic of Austria, is a country in the southern part of Central Europe, lying in the Eastern Alps. It is a federation of nine states, one of which is the capital, Vienna, the most populous city and state. A landlocked country, 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 a population of 9 million. Austria emerged from the remnants of the Eastern and Hungarian March at the end of the first millennium. Originally a margraviate of Bavaria, it developed into a duchy of the Holy Roman Empire in 1156 and was later made an archduchy in 1453. In the 16th century, Vienna began serving as the empire's administrative capital and Austria thus became the heartland of the Habsburg monarchy. After the dissolution of the H ...
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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 southwest, and the Czech Republic to the northwest. Slovakia's mostly mountainous territory spans about , with a population of over 5.4 million. The capital and largest city is Bratislava, while the second largest city is Košice. The Slavs arrived in the territory of present-day Slovakia in the fifth and sixth centuries. In the seventh century, they played a significant role in the creation of Samo's Empire. In the ninth century, they established the Principality of Nitra, which was later conquered by the Principality of Moravia to establish Great Moravia. In the 10th century, after the dissolution of Great Moravia, the territory was integrated into the Principality of Hungary, which then became the Kingdom of Hungary in 1000. In 1241 ...
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Low Beskids
The Low Beskids ( sk, Nízke Beskydy) or Central Beskids ( pl, Beskidy Środkowe; cs, Centrální Beskydy; uk, Центральні Бескиди) 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'' ( sk, Nízke Beskydy). In Polish terminology, the same region is not classified under the term ''Low Beskids'' ( pl, Beskid Niski), 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'' ( pl, Beskidy Środkowe). It is a hilly region, encompassing the Prešov Region, Sanok County and Jasło County, and covering the area between Busov, Ondavská vrchovina, Lab ...
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Geomorphology
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created 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 processe ...
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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 ...
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