Sub-Tatra Trench
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Sub-Tatra Trench
Sub-Tatra Trench (Polish language, Polish: Rów Podtatrzański; Slovakian language, Slovakian: Podtatranská brázda) (Regions of Poland, 514.14) is 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 Spiš–Gubałówka Highlands. The region has an elevation of between 700 and 1000 m.a.s.l. It is 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 valleys 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 ...
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Polish Language
Polish (, , or simply , ) is a West Slavic languages, West Slavic language of the Lechitic languages, Lechitic subgroup, within the Indo-European languages, Indo-European language family, and is written in the Latin script. It is primarily spoken in Poland and serves as the official language of the country, as well as the language of the Polish diaspora around the world. In 2024, there were over 39.7 million Polish native speakers. It ranks as the sixth-most-spoken among languages of the European Union. Polish is subdivided into regional Dialects of Polish, dialects. It maintains strict T–V distinction pronouns, Honorifics (linguistics), honorifics, and various forms of formalities when addressing individuals. The traditional 32-letter Polish alphabet has nine additions (, , , , , , , , ) 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. The traditional set compri ...
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Alluvial Fan
An alluvial fan is an accumulation of sediments that fans outwards from a concentrated source of sediments, such as a narrow canyon emerging from an escarpment. They are characteristic of mountainous terrain in arid to Semi-arid climate, semiarid climates, but are also found in more humid environments subject to intense rainfall and in areas of modern glaciation. They range in area from less than to almost . Alluvial fans typically form where a flow of sediment or rocks emerge from a confined channel and are suddenly free to spread out in many directions. For example, many alluvial fans form when steep mountain valleys meet a flat plain. The transition from a narrow channel to a wide open area reduces the carrying capacity of flow and results in Deposition (geology), deposition of sediments. The flow can take the form of infrequent debris flows like in a landslide, or can be carried by an intermittent stream or creek. The reduction of flow is key to the formation of alluvial ...
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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 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 (; Goral ethnolect: ''Górole''; ; Cieszyn Silesian dialect, Cieszyn Silesian: ''Gorole''), also anglicized as the Highlanders, are an ethnographic group with historical ties to the Vlachs. The Goral people are primarily found in thei .... References Villages in Tatra County {{Tatra-geo-stub ...
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Małe Ciche
Małe Ciche , () 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 (; ), sometimes referred to as the Polish Highlands, is Poland's southernmost region. The Podhale is located in the foothills of the Tatra range of the Carpathian Mountains. It is the most famous region of the Goral Lands which are a ... 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 Karpie ...
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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 confluence of rivers and . The Biały Dunajec then 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. The river flows by the Bór na Czerwonem nature reserve. The Biały Dunajec 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 meters. Below Szaflary, the river is regulated and separated by high concrete sills. Main tributaries * left: Suchy Potok, Potok Bustrycki, Syposi Potok, Florynów Potok, Krajowy Potok * right: Świdrów ...
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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 ...
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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. The main towns that the Czarny Dunajec flows through include Witów, Chochołów, Koniówka, Podczerwone, Czarny Dunajec, Wróblówka, Długopole, Krauszów and Ludźmierz. In Nowy Targ it j ...
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Forest
A forest is an ecosystem characterized by a dense ecological community, community of 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 (biology), 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 (FRA), Global Forest Resources Assessment 2020'' found that forests covered , or approximately 31 percent of the world's land area in 2020. Forests are the largest Terrestrial ecosystem, terrestrial ecosystems of Earth by area, and are found around the globe. 45 percent of forest land is in the Tropical forest, trop ...
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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. Changes in atmospheric and associated radiative forcing were among the primary drivers of globally cold glacial and warm interglacial climates, with changes in ocean physical circulation, biological productivity and seawater acid-base chemistry likely causing most of the recorded changes Penultimate Glacial Period The Pe ...
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Gravel
Gravel () is a loose aggregation of rock fragments. Gravel occurs naturally on Earth as a result of sedimentation, sedimentary and erosion, erosive geological processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by grain size, particle size range and includes size classes from granule (geology), granule- to boulder-sized fragments. In the grain size, Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges for fine and for coarse. One cubic metre of gravel typically weighs about , or one cubic yard weighs about . Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as construction aggregate, 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 bitumen, asphalt or other binders.) Natu ...
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