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Sudeten Mountains
The Sudetes ( ; pl, Sudety; german: Sudeten; cs, Krkonošsko-jesenická subprovincie), commonly known as the Sudeten Mountains, is a geomorphological subprovince in Central Europe, shared by Germany, Poland and the Czech Republic. They consist mainly of mountain ranges and are the highest part of Bohemian Massif. They stretch from the Saxony, Saxon capital of Dresden in the northwest across to the region of Lower Silesian Voivodeship, Lower Silesia in Poland and to the Moravian Gate in the Czech Republic in the east. Geographically the Sudetes are a ''Mittelgebirge'' with some characteristics typical of high mountains. Its plateaus and subtle summit relief makes the Sudetes more akin to mountains of Northern Europe than to the Alps. In the west, the Sudetes border with the Elbe Sandstone Mountains. The westernmost point of the Sudetes lies in the Dresden Heath (''Dresdner Heide''), the westernmost part of the West Lusatian Hill Country and Uplands, in Dresden. In the east of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Śnieżne Kotły
Śnieżne Kotły (, cs, Sněžné jámy, german: Schneegruben, literally ''Snowy Pits'', ''Snowy Cirque'', ''Snowy Cwm'') are two glacial cirques situated in Poland in the Sudetes in the Karkonosze National Park. They are a unique example of the alpine landscape in the area and have been a nature reserve since 1933. Description The walls of both cirques are about high and contain small tarn lakes. They were formed during the last phase of the glacial period and consist predominantly of granite. However, in two exposed places basalt was found (apparently of volcanic origin), which is quite rare in this part of Central Europe. Some rare species of arctic and alpine plants appear in the cold and dark parts of the cirques: Pulsatilla alpina, Gentiana asclepiadea, Aconitum napellus, and the only place in the Sudetes where Micranthes nivalis appears. At the top of the larger cirque, at the Łabski Szczyt, there is a radio and television tower. Hiking and climbing It is possibl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dresden Heath
The Dresden Heath (german: Dresdner Heide) is a large forest in the city of Dresden, Germany. The heath is the most important recreation area in the city and is also actively forested. Approximately 6,133 hectares of the Dresden Heath are designated as a nature preserve, making it one of the largest municipal forests in Germany by area. Though mainly agricultural areas border the forest in the east, in all other directions the Dresden Heath is bordered by districts of the city and reaches nearly to the city centre in the southwest. The forest exhibits a transition, both in its geology and in its plant and animal life, between the North German Plain and the Central Uplands. Except for small areas, the Dresden Heath is considered part of the western Lusatian Highlands and, consequently, is one of the westernmost parts of the Sudetes. Though the rocky subsoil of the forest was raised during the tectonic formation of the Dresden Basin, the mixed woodland of the heath is largely cha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Elbe Sandstone Mountains
The Elbe Sandstone Mountains, also called the Elbe Sandstone Highlands (german: Elbsandsteingebirge; cs, Děčinská vrchovina), are a mountain range straddling the border between the state of Saxony in southeastern Germany and the North Bohemian region of the Czech Republic, with about three-quarters of the area lying on the German side. In both countries, core parts of the mountain range have been declared a national park. The name derives from the sandstone which was carved by erosion. The river Elbe breaks through the mountain range in a steep and narrow valley. The Saxon Switzerland and Bohemian Switzerland national parks, known also as Saxon-Bohemian Switzerland, are located within the territory of Elbe Sandstone Mountains. Geography Extent The Elbe Sandstone Mountains extend on both sides of the Elbe from the Saxon town of Pirna in the northwest toward Bohemian Děčín in the southeast. Their highest peak with is the Děčínský Sněžník in Bohemian Switzerland o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alps
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northern Europe
The northern region of Europe has several definitions. A restrictive definition may describe Northern Europe as being roughly north of the southern coast of the Baltic Sea, which is about 54th parallel north, 54°N, or may be based on other geographical factors such as climate and ecology. Climate The climate is mainly Oceanic climate (Cfb), Humid continental climate (Dfb), Subarctic climate (Dfc and Dsc) and Tundra (ET). Geography Northern Europe might be defined roughly to include some or all of the following areas: British Isles, Fennoscandia, the peninsula of Jutland, the Baltic region, Baltic plain that lies to the east and the many islands that lie offshore from mainland Northern Europe and the main European continent. In some cases, Greenland is also included, although it is only politically European, comprising part of the Kingdom of Denmark, and not considered to be geographically in Europe. The area is partly mountainous, including the northern volcanic islands ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographia Polonica
''Geographia Polonica'' is a peer-reviewed scientific journal published by the Institute of Geography and Spatial Organisation of the Polish Academy of Sciences. The journal is subsidized by the Ministry of Science and Higher Education of Poland. See also *Fennia (journal), ''Fennia'' *''Geografiska Annaler'' *''Danish Journal of Geography'' *''Norwegian Journal of Geography'' References External links * Geography journals Multilingual journals Polish-language journals English-language journals 1964 establishments in Poland Publications established in 1964 Academic journals associated with learned and professional societies Quarterly journals {{Poland-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mittelgebirge
A ''Mittelgebirge'' (German: ''Mittel'', "middle/medium"; ''Gebirge'', "mountain range") is a type of relatively low mountain range or highland area typical of the geography of central Europe, especially central and southern Germany; it refers to something between rolling low hill country or ''Hügelland'' and a proper mountain range (german: link=no, Gebirge or ''Hochgebirge'') like the High Alps. Characteristics The term is not precise, but typically refers to topography where the peaks rise at least to ''above the surrounding terrain'' (as opposed to above sea level). The summits usually do not reach the tree line and were not glaciated after the last glacial period. In contrast, ''Hochgebirge'' is used to refer to mountain ranges rising above approximately to . The delineation corresponds with the differentation between Montane and Alpine level according to altitudinal zonation. ''Mittelgebirge'' ranges In the plural, ''die Mittelgebirge'' (as opposed to the singular, ''d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moravian Gate
The Moravian Gate ( cs, Moravská brána, pl, Brama Morawska, german: Mährische Pforte, sk, Moravská brána) is a geomorphological feature in the Moravian region of the Czech Republic and the Upper Silesia region in Poland. It is formed by the depression between the Carpathian Mountains in the east and the Sudetes in the west. The drainage divide between the upper Oder river and the Baltic Sea in the north and the Bečva River of the Danube basin runs through it. Geography It stretches from Moravia towards Czech Silesia north-eastward in the length of about and is bordered by the confluence of the Olza and the Odra (Oder) rivers in the north. Its crest is located between the villages of Olšovec and Bělotín at . Because of its low altitude, the Moravian Gate has since ancient times been a natural pass between the Sudetes (Oderské vrchy range) in the northwest and the Western Carpathians (Moravian-Silesian Beskids) in the southeast. Here ran the most important trade route ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dresden
Dresden (, ; Upper Saxon: ''Dräsdn''; wen, label=Upper Sorbian, Drježdźany) is the capital city of the German state of Saxony and its second most populous city, after Leipzig. It is the 12th most populous city of Germany, the fourth largest by area (after Berlin, Hamburg and Cologne), and the third most populous city in the area of former East Germany, after Berlin and Leipzig. Dresden's urban area comprises the towns of Freital, Pirna, Radebeul, Meissen, Coswig, Radeberg and Heidenau and has around 790,000 inhabitants. The Dresden metropolitan area has approximately 1.34 million inhabitants. Dresden is the second largest city on the River Elbe after Hamburg. Most of the city's population lives in the Elbe Valley, but a large, albeit very sparsely populated area of the city east of the Elbe lies in the West Lusatian Hill Country and Uplands (the westernmost part of the Sudetes) and thus in Lusatia. Many boroughs west of the Elbe lie in the foreland of the Ore Mounta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, North Europe ... [...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] |
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