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Biskupia Kopa
Biskupia Kopa ( cs, Biskupská kupa, german: Bischofskoppe) is a mountain in the crest of the Opawskie Mountains, eastern part of the Sudetes, lying on the border between Poland and the Czech Republic. It belongs to the Crown of Polish Mountains and is the highest reaching point of the Opole Voivodeship. It's about away from the closest county town of Prudnik. The Biskupia Kopa massif is built of Devonian sedimentary rocks – sandstone and slate Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. .... Many excavations in the area have remained after their exploitation, such as Gwarkowa Perć, Piekiełko, Morskie Oczko. References Nysa County Jeseník District Mountains of Poland Mountains and hills of the Czech Republic Czech Republic–Poland border International mountains ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jarnołtówek
Jarnołtówek (german: Arnoldsdorf) is a village in the administrative district of Gmina Głuchołazy, within Nysa County, Opole Voivodeship, in south-western Poland, close to the Czech border. It lies approximately south-east of Głuchołazy, south of Nysa, and south-west of the regional capital Opole Opole (; german: Oppeln ; szl, Ôpole) ; * Silesian: ** Silesian PLS alphabet: ''Ôpole'' ** Steuer's Silesian alphabet: ''Uopole'' * Silesian German: ''Uppeln'' * Czech: ''Opolí'' * Latin: ''Oppelia'', ''Oppolia'', ''Opulia'' is a city loc .... The village has a population of 820. Places of interest * the Saint Bartholomew church * the dam * the Opawskie Mountains Landscape Park * the Biskupia Kopa mountain * the mountain caves * the restaurant "Włoski Smak" References Villages in Nysa County {{Nysa-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains And Hills Of The Czech Republic
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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Poland
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 300 metres (1,000 feet) 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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jeseník District
Jeseník District ( cs, okres Jeseník) is a district ('' okres'') in the Olomouc Region of the Czech Republic. Its seat is the town of Jeseník. With approximately 38,000 inhabitants it is the least populated district of the Czech Republic. The area called Jeseníky region is in the most northern bulge of Silesia and Moravia. It is closed by frontier with Poland that passes westward through Rychleby Hills and crosses the Nysa Lowlands to Zlaté Hory. The massif of Hrubý Jeseník in the south represents both the geomorphologic and climatic contrast to the lowlands of Javorník and Vidnava opened to Poland. The town of Jeseník, an important crossing connection, connecting Silesia, separated by the mountain ridge from Moravia is the cultural and economic centre of the region. This town is situated at rivers Bělá and Staříč confluence forming a wide and branching valley where the diversity in the composition of nationalities is very diversified. Nature Mountains The landscap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nysa County
__NOTOC__ Nysa County ( pl, powiat nyski) is a unit of territorial administration and local government (powiat) in Opole Voivodeship, south-western Poland, on the Czech border. It came into being on January 1, 1999, as a result of the Polish local government reforms passed in 1998. Its administrative seat and largest town is Nysa, which lies south-west of the regional capital Opole. The county contains four other towns: Głuchołazy, south of Nysa, Paczków, west of Nysa, Otmuchów, west of Nysa, and Korfantów, east of Nysa. The county covers an area of . As of 2019 its total population is 136,393. The most populated towns are Nysa with 43,849 inhabitants, Głuchołazy with 13,534 inhabitants, and Paczków with 7,460 inhabitants. Neighbouring counties Nysa County is bordered by Ząbkowice Śląskie County to the west, Strzelin County and Brzeg County to the north, Opole County to the north-east, and Prudnik County to the south-east. It also borders the Czech Republic to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Opawskie Mountains
The Opawskie Mountains ( pl, Góry Opawskie, german: Oppagebirge) or Zlatohorská Highlands / Zlaté Hory Highlands ( cs, Zlatohorská vrchovina, German: ''Zuckmanteler Bergland'') are a mountain range of the Eastern Sudetes in the Czech Republic and Poland. Location The Opawskie Mountains stretch from northern Czech Silesia into Polish Upper Silesia, the eastern continuation of the Golden Mountains range. It borders on the Nízký Jeseník range in the south and the Hrubý Jeseník (High Ash Mountains) in the southwest. The Polish part of the range includes the protected area known as Opawskie Mountains Landscape Park. It is named after the Opava River with its source in the neighbouring Hrubý Jeseník range. The highest peak is Příčný vrch (975 meters above sea level). Towns and villages Poland * Prudnik * Głuchołazy * Jarnołtówek * Pokrzywna * Łąka Prudnicka * Moszczanka * Trzebina * Skrzypiec * Dytmarów * Krzyżkowice * Dębowiec * Opawica * Lenarcice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prudnik
Prudnik (, szl, Prudnik, Prōmnik, german: Neustadt in Oberschlesien, Neustadt an der Prudnik, la, Prudnicium) is a town in southern Poland, located in the southern part of Opole Voivodeship near the border with the Czech Republic. It is the administrative seat of Prudnik County and Gmina Prudnik. Its population numbers 21,368 inhabitants (2016). Since 2015, Prudnik is a member of the Cittaslow International. The town was founded in the 1250s, and was historically part of the Polish-ruled Duchy of Opole, and afterwards was located within the Habsburg monarchy, Poland, Habsburg Monarchy again, Prussia, Germany, and eventually Poland again. It was once an important industrial hub known for its shoe-making traditions and more recently towel making by the ZPB "Frotex" Company, one of the largest towel manufacturers in Europe. The town also possesses numerous architectural monuments and historic buildings such as the Main Town Hall and "Wok's Tower" (''Wieża Woka'') from the 1 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Opole Voivodeship
Opole Voivodeship, or Opole Province ( pl, województwo opolskie ), is the smallest and least populated voivodeship (province) of Poland. The province's name derives from that of the region's capital and largest city, Opole. It is part of Upper Silesia. A relatively large German minority, with representatives in the Sejm, lives in the voivodeship, and the German language is co-official in 28 communes. Opole Voivodeship is bordered by Lower Silesian Voivodeship to the west, Greater Poland and Łódź Voivodeships to the north, Silesian Voivodeship to the east, and the Czech Republic (Olomouc Region and Moravian-Silesian Region) to the south. Opole Province's geographic location, economic potential, and its population's level of education make it an attractive business partner for other Polish regions (especially Lower Silesian and Silesian Voivodeships) and for foreign investors. Formed in 1997, the Praděd/Pradziad Euroregion with its headquarter in Prudnik has facilitated e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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