Pieniny Gorals
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Pieniny Gorals
The Pieniny (sometimes also the PieninsSzafer, Władysław. 2013. ''The Vegetation of Poland: International Series of Monographs in Pure and Applied Biology''. Warsaw: Pergamon Press, pp. 156, 388. or the Pienin Mountains,Griffiths, Graham C. D. 1976. Studies on Boreal Agromyzidae (Diptera). XII. ''Phytomyza'' and ''Chromatomyia'' miners on Astereae (Compositae).''Quaestiones Entomologicae'' 12: 239–275, p. 255. ) is a mountain range in the south of Poland and the north of Slovakia. It is classified within the eastern section of the Western Beskids. The Pieniny mountain range is divided into three parts – ''Pieniny Spiskie'' () and ''Pieniny Właściwe'' (Slovak: ''Centrálne Pieniny'') in Poland; and, ''Małe Pieniny'' (; ) in Poland and Slovakia. The Pieniny mountains consist mainly of beds of limestone and dolomite. The most famous peak, ''Trzy Korony'' (Three Crowns), is 982 metres high. It is also the summit of the Three Crowns Massif. Pieniny's highest peak &ndash ...
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Poland
Poland, officially the Republic of Poland, is a country in Central Europe. It extends from the Baltic Sea in the north to the Sudetes and Carpathian Mountains in the south, bordered by Lithuania and Russia to the northeast, Belarus and Ukraine to the east, Slovakia and the Czech Republic to the south, and Germany to the west. The territory has a varied landscape, diverse ecosystems, and a temperate climate. Poland is composed of Voivodeships of Poland, sixteen voivodeships and is the fifth most populous member state of the European Union (EU), with over 38 million people, and the List of European countries by area, fifth largest EU country by area, covering . The capital and List of cities and towns in Poland, largest city is Warsaw; other major cities include Kraków, Wrocław, Łódź, Poznań, and Gdańsk. Prehistory and protohistory of Poland, Prehistoric human activity on Polish soil dates to the Lower Paleolithic, with continuous settlement since the end of the Last Gla ...
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Above Sea Level
Height above mean sea level is a measure of a location's vertical distance (height, elevation or altitude) in reference to a vertical datum based on a historic mean sea level. In geodesy, it is formalized as orthometric height. The zero level varies in different countries due to different reference points and historic measurement periods. Climate change and other forces can cause sea levels and elevations to vary over time. Uses Elevation or altitude above sea level is a standard measurement for: * Geographic locations such as towns, mountains and other landmarks. * The top of buildings and other structures. * Mining infrastructure, particularly underground. * Flying objects such as airplanes or helicopters below a Transition Altitude defined by local regulations. Units and abbreviations Elevation or altitude is generally expressed as "metres above mean sea level" in the metric system, or " feet above mean sea level" in United States customary and imperial units. Com ...
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Mikołaj Zyblikiewicz
Mikołaj Zyblikiewicz (; ; 28 November 1823 – 16 May 1887) was a Polish politician and lawyer of Ruthenians, Ruthenian origin. He was the Mayor of Kraków – in the then Austrian partition, Austrian sector of Partitioned Poland. A street in Kraków's Kraków Old Town, Old Town is named in his memory, while his monument stands in front of the City Hall. Some of his achievements included the restoration of Sukiennice, the creation of a "national Panthéon" at Skałka, and his campaign towards the renovation of Wawel Castle. Career Mikołaj Zyblikiewicz was the son of Szymon Zyblikiewicz, a furrier of Ruthenians, Ruthenian (Ukrainian) background in the town of Stare Miasto near Sambir, Sambor (now Stary Sambir in western Ukraine); he would later self-identify as "Polish-Lithuanian identity#16th-18th centuries, gente Ruthenus, natione Polonus". After graduating from high-school in Lviv, he enrolled at the Lviv University while working as a home tutor for szlachta, local ...
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Pieniny National Park (Slovakia)
Pieniny National Park (; abbr. PIENAP) is a national park in northern Slovakia. The park is located in the eastern Pieniny Mountains on the border with Poland. It is the smallest national park in Slovakia with an area of 37.49 km2 (14.48 mi2) and a buffer zone of 224.44 km2 (86.66 mi2). The park is located in the Slovak districts of Kežmarok and Stará Ľubovňa in the Prešov Region. History The Zamagurie region was already declared as a protected territory in 1932, making it the first protected international nature park in Europe. On the Polish side it was called Pieniński Park Narodowy, while the Slovak part of the Pieniny Mountains was a national nature reserve. The National Park itself was founded on 16 January 1967, which makes it the second oldest national park in Slovakia after the Tatra National Park. By the 1994 act of the Slovak parliament regarding nature and landscape protection, the name of the park was changed to the Pieniny National Park. ...
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Czorsztyn
Czorsztyn (German: ''Schorstin'') is a village in Poland, in Lesser Poland Voivodeship, Nowy Targ County. The village lies in Pieniny, the mountain range on the current Polish- Slovak border. It is famous for the ruins of a 14th-17th-century castle, which was the scene of the Kostka-Napierski Uprising in 1651. Highlights Czorsztyn gave its name to the man-made reservoir also known as Lake Czorsztyn, completed in 1994. The village along with its mountainous surroundings is a recreational destination with well developed tourist infrastructure: accommodations, pleasure-boats dock, and numerous marked hiking trails.The attractions of Lake Czorsztyn
from The Department of Hotel & Tourist Services ''Niedzica.com''.


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File:061. Czorsztyn.JPG, Czorsztyn Castle and lake panorama File:Poland Czorszty ...
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Niedzica Castle
Niedzica Castle, also known as Dunajec Castle (, , , ), is located in the southernmost part of Poland in Niedzica (Nowy Targ County in Lesser Poland). It was erected between the years 1320 and 1326 by Kokos of Brezovica on the site of an ancient stronghold surrounded by earthen walls in the Pieniny mountains. The Niedzica Castle stands at an altitude of 566 m, on a hill upstream from the Dunajec River mouth, measured from the center of the dam on Lake Czorsztyn. The outline of Niedzica Castle can best be viewed from the ruins of Czorsztyn Castle on the other side of the lake. It is known as one of the most picturesque castles in the country and adorns the covers of many books. History The castle was an important centre of Polish-Hungarian relations since the 14th century. It was a place where the money lent by the Polish king to the Hungarian king Sigismund, Holy Roman Emperor, Sigismund had to be returned following an agreement signed in 1412. Once the loan was paid ba ...
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Dunajec
The Dunajec (; Goral dialects: ''Dónajec''; ) is a river running through northeastern Slovakia and southern Poland. It is also regarded as the main river of the Goral Lands. It is a right tributary of the Vistula River. It begins in Nowy Targ at the junction of two short mountain rivers, Czarny Dunajec and Biały Dunajec (Black and White Dunajec). Dunajec forms the border between Poland and Slovakia for in the Pieniny Środkowe (Slovak: Centrálne Pieniny) range, east of the Czorsztyn reservoir. Geography The Dunajec is long, including its source river Czarny Dunajec,Statistical Yearbook of the Republic of Poland 2017

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Volcanic
A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and because most of Earth's plate boundaries are underwater, most volcanoes are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes resulting from divergent tectonic activity are usually non-explosive whereas those resulting from convergent tectonic activity cause violent eruptions."Mid-ocean ridge tectonics, volcanism and geomorphology." Geology 26, no. 455 (2001): 458. https://macdonald.faculty.geol.ucsb.edu/papers/Macdonald%20Mid-Ocean%20Ridge%20Tectonics.pdf Volcanoes can also form where there is stretching a ...
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Pieniny National Park (Poland)
Pieniny National Park () is a protected area located in the heart of the Pieniny mountains in the southernmost part of Poland. It is the oldest national park in Poland. Administratively, the park lies in the Lesser Poland Voivodeship on the border with Slovakia. Its head office is in Krościenko nad Dunajcem. The Pieniny mountain chain is divided into three ranges: ''Pieniny Spiskie'', ''Małe Pieniny'', and the ''Pieniny Właściwe'' range where the Park is located. The park's area is , of which 13.11 km2 is forested. One-third (7.5 km2) is strictly protected. On the Slovak side of the mountains there is a parallel park called the Pieninský národný park. History The idea for the creation of the National Park in Pieniny came from Prof. Władysław Szafer, a member of the National Commission for the Preservation of Nature () in 1921. The same year, a private preserve on the area of 75,000 m2 was opened by Stanisław Drohojowski around the ruins of the Czorsztyn c ...
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Dunajec River Gorge
The Dunajec River Gorge (; ; ) runs through the Pieniny Mountains in the south of Poland and the north of Slovakia (as Dunajec is the border river between the two countries in the area). The gorge is characterized by some of the most interesting geological and geomorphological structures and area-specific natural ecosystems with little anthropogenic influence. It is featured on UNESCO's Tentative List of World Heritage Sites in Poland.UNESCO World Heritage List, Poland.
Accessed 7 September 2011.
Dunajec Gorge is also one of the best-known tourist attractions in the Pieniny Mountains. Wooden raft trips have been organized daily by ...
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Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ...
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Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by Solvation, dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ...
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