Podtatrzański Trench
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Podtatrzański Trench
Sub-Tatra Trench (Polish language, Polish: Rów Podtatrzański; Slovakian language, Slovakian: Podtatranská brázda) (Regions of Poland, 514.14) - a Mesoregion (geomorphology), mesoregion located below the Tatra Mountains, part of the Podhale-Magura Area, Orava-Podhale Depression. The trench divides the Choč Mountains, Choč and Tatra Mountains from the Spisko-Gubałowski Plateau. The region is located between 700 and 1000 m.a.s.l., formed from Eocene marlstone slates (Podhalański Flysch). In Poland, the area has a total length of 20 km and a total surface area of 130 km². The regional valleyss incline in the north, covered with alluvial fans, formed via upper course river flow. The Zakopane Valley has three gravel top soil coverings from three separate glacial periods. The western part and eastern borderlands of the Podtatrzański Trench are forested. The main brooks that drain through the valley are the Czarny Dunajec (river), Czarny Dunajec, as well as the Zakopianka an ...
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Polish Language
Polish (Polish: ''język polski'', , ''polszczyzna'' or simply ''polski'', ) is a West Slavic language of the Lechitic group written in the Latin script. It is spoken primarily in Poland and serves as the native language of the Poles. In addition to being the official language of Poland, it is also used by the Polish diaspora. There are over 50 million Polish speakers around the world. It ranks as the sixth most-spoken among languages of the European Union. Polish is subdivided into regional dialects and maintains strict T–V distinction pronouns, honorifics, and various forms of formalities when addressing individuals. The traditional 32-letter Polish alphabet has nine additions (''ą'', ''ć'', ''ę'', ''ł'', ''ń'', ''ó'', ''ś'', ''ź'', ''ż'') to the letters of the basic 26-letter Latin alphabet, while removing three (x, q, v). Those three letters are at times included in an extended 35-letter alphabet, although they are not used in native words. The traditional ...
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Zakopane
Zakopane ( Podhale Goral: ''Zokopane'') is a town in the extreme south of Poland, in the southern part of the Podhale region at the foot of the Tatra Mountains. From 1975 to 1998, it was part of Nowy Sącz Voivodeship; since 1999, it has been part of Lesser Poland Voivodeship. its population was 27,266. Zakopane is a centre of Goral culture and is often referred to as "the winter capital of Poland". It is a popular destination for mountaineering, skiing, and tourism. Zakopane lies near Poland's border with Slovakia, in a valley between the Tatra Mountains and Gubałówka Hill. It can be reached by train or bus from the provincial capital, Kraków, about two hours away. Zakopane lies 800–1,000 metres above sea level and centres on the intersection of its Krupówki and Kościuszko Streets. History The earliest documents mentioning Zakopane date to the 17th century, describing a glade called ''Zakopisko''. In 1676, it was a village of 43 inhabitants. In 1818, Zakopane was a ...
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Murzasichle
Murzasichle is a village in the administrative district of Gmina Poronin, within Tatra County, Lesser Poland Voivodeship, in southern Poland. It lies approximately south-east of Poronin, east of Zakopane, and south of the regional capital Kraków. The village has a population of 1,100. Its name came from the merging of the names of two settlements: ''Mur'' and ''Zasichle''. The village is a part of the Podhale region and is inhabited by Gorals The Gorals ( pl, Górale; Goral dialect: ''Górole''; sk, Gorali; Cieszyn Silesia dialect, Cieszyn Silesian: ''Gorole''), also known as the Highlanders (in Poland as the Polish Highlanders) are an indigenous ethnographic or ethnic group primar .... References {{coord, 49, 18, 42, N, 20, 2, 37, E, region:PL_type:city, display=title Villages in Tatra County ...
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Małe Ciche
Małe Ciche , ( sk, Malé Tiché) is a village and a ski resort, in the administrative district of Gmina Poronin, within Tatra County, Lesser Poland Voivodeship, in southern Poland. It lies approximately south-east of Poronin, east of Zakopane, and south of the regional capital Kraków. The village has a population of 400. See also * Podhale Podhale (literally "below the mountain pastures") is Poland's southernmost region, sometimes referred to as the "Polish Highlands". The Podhale is located in the foothills of the Tatra range of the Carpathian mountains. It is the most famous ... References Villages in Tatra County Ski areas and resorts in Poland {{Tatra-geo-stub ...
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Kościelisko
Kościelisko is a village in Tatra County, Lesser Poland Voivodeship, in southern Poland, close to the border with Slovakia. (It was previously in Nowy Sącz Voivodeship from 1975 to 1998.) It is the seat of the gmina (administrative district) called Gmina Kościelisko. It lies approximately west of Zakopane and south of the regional capital Kraków. In 2006 the village had a population of 3,900. Notable people * Sabała (1809 in Kościelisko - 1894 in Zakopane) a Goral amateur musician, storyteller and folk singer active in or around the Tatra Mountains. * Klemens Bachleda (1851 in Kościelisko - The Tatraa 1910), Polish mountain guide and mountain rescuer, born in Kościelisko * Wacław Krzeptowski (1897 in Kościelisko – 1945 in Zakopane) was one of the leaders of the Goralenvolk action in Podhale during WWII. * Andrzej Krzeptowski (1902 in Kościelisko – 1981 in Zakopane) was a Polish cross-country skier who competed in the 1928 Winter Olympics. * Stanisław Karpiel (1 ...
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Biały Dunajec (river)
The Biały Dunajec is a river in Poland, the right tributary of the Dunajec. The river arises at an altitude of approx. 730 m in Poronin from the junction of the Zakopianka with the Poroniec. Then, the Biały Dunajec river flows through the eponymous Biały Dunajec village, Szaflary and Nowy Targ, where at an altitude of about 577 m it joins the Czarny Dunajec, giving rise to the Dunajec. Before its mouth, the river flows by the Bór na Czerwonem nature reserve. The Biały Dunajec River is formed in the Podtatrzański Trench, while its lower course and mouth are located in the Orava-Nowy Targ Basin. In the upper part of the course, down to Szaflary, the river has a more mountain character. There are large boulders, plunge pools and riffles in its bed, and the width of the river ranges from several meters to several dozen. Below Szaflary, the river is regulated and separated by high concrete sills. Main tributaries * left: Suchy Potok, Potok Bustrycki, Syposi Potok, Flo ...
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Poroniec (river)
A (; plural ) is a hostile and malicious demon from Slavic mythology. They were believed to come into existence from stillborn fetuses, but also from improperly buried remains of children who had died during infancy. Folklore A is somewhat similar to a being from Scandinavian folklore, the . were considered to be extremely powerful demons, due to their potential of unrealized life. were associated with many taboos regarding pregnant women, such as drawing water from a well, leaving home with an infant, or engaging in sexual intercourse. A stillborn fetus did not turn into a if it was buried under the threshold of the house. Instead, it turned into a – a protective house spirit. In popular culture *In the 2015 video game '' The Witcher 3: Wild Hunt'', one of the main quests revolves around the search for a botchling ( in the original version) that can be killed or turned into a lubberkin (). See also * Drekavac (the South Slavic equivalent) * Myling * Pontianak * Ko ...
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Czarny Dunajec (river)
The Czarny Dunajec is a river in southern Poland (Lesser Poland Voivodeship), in the Vistula basin. Course The Wyżni Chochołowski Potok is considered the source of the Czarny Dunajec river. It flows out at an altitude of about under Volovec in the Western Tatras. After the merger with the Jarząbcze Potok, the Chochołowski Potok is formed, called Siwa Woda in the lower part. It is the middle course of Czarny Dunajec. In Roztoki (part of the village of Witów), Siwa Woda connects with Kirowa Woda and the lower course of the Czarny Dunajec begins here. The Czarny Dunajec flows through Podhale, initially to the north-west, between Pogórze Gubałowskie and Orawicko-Witowskie Wierchy, then north through the Orava-Nowy Targ Basin. It makes a wide arc and flows to the east. It flows through the following towns: Witów, Chochołów, Koniówka, Podczerwone, Czarny Dunajec, Wróblówka, Długopole, Krauszów and Ludźmierz. In Nowy Targ it joins the Biały Dunajec riv ...
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Forest
A forest is an area of land dominated by trees. Hundreds of definitions of forest are used throughout the world, incorporating factors such as tree density, tree height, land use, legal standing, and ecological function. The United Nations' Food and Agriculture Organization (FAO) defines a forest as, "Land spanning more than 0.5 hectares with trees higher than 5 meters and a canopy cover of more than 10 percent, or trees able to reach these thresholds ''in situ''. It does not include land that is predominantly under agricultural or urban use." Using this definition, '' Global Forest Resources Assessment 2020'' (FRA 2020) found that forests covered , or approximately 31 percent of the world's land area in 2020. Forests are the predominant terrestrial ecosystem of Earth, and are found around the globe. More than half of the world's forests are found in only five countries (Brazil, Canada, China, Russia, and the United States). The largest share of forests (45 percent) are in th ...
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Glacial Periods
A glacial period (alternatively glacial or glaciation) is an interval of time (thousands of years) within an ice age that is marked by colder temperatures and glacier advances. Interglacials, on the other hand, are periods of warmer climate between glacial periods. The Last Glacial Period ended about 15,000 years ago. The Holocene is the current interglacial. A time with no glaciers on Earth is considered a greenhouse climate state. Quaternary Period Within the Quaternary, which started about 2.6 million years before present, there have been a number of glacials and interglacials. At least eight glacial cycles have occurred in the last 740,000 years alone. Penultimate Glacial Period The Penultimate Glacial Period (PGP) is the glacial period that occurred before the Last Glacial Period. It began about 194,000 years ago and ended 135,000 years ago, with the beginning of the Eemian interglacial. Last Glacial Period The last glacial period was the most recent glacial period wi ...
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Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ...
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