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Lake Rożnów
Lake Rożnow ( pl, Jezioro Rożnowskie) is an artificial lake, built in 1935–1941. It is located in southernmost part of Poland ( Lesser Poland Voivodeship). The lake was built in the interwar period to regulate the Dunajec river flowing through the foothills of Beskid Mountains; and also, to provide electricity for the Rożnow Power Plant (''Elektrownia Rożnow'') built into the dam. The lake took two years to fill which took place during World War II, from mid 1941 until 1943. It was named after the village of Rożnow. History Lake Rożnow was created not long before the invasion of Poland, after a dam had been built on the 80th kilometre distance of the Dunajec river. It lies among the hills of the Island Beskids, in Nowy Sącz County, some 12 kilometers north of Nowy Sącz. The valley of the Dunajec narrows here, turning into a canyon. The lake has the shape of an irregular letter S, with length ranging from 18 to 20 kilometres, and width of 1 app. kilometre (in fe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Island Beskids
The Island Beskids (in Polish, ''Beskid Wyspowy'') is a mountain range in southern Poland, part of the Western Beskids of the Outer Western Carpathians, with significant natural resources, folk culture, medieval history, and developing resources for tourism. The distinctive feature of this region is its isolated, individual peaks, from which derives its name. The highest peak is Mogielica (1170 meters). Other major peaks include '' Ćwilin'' (1072 meters), ''Jasien'' (1052 meters), '' Modyń'' (1029 meters), ''Luboń Wielki'' (1022 meters), and '' Krzystonów'' (1012 meters). The Outline of Island Beskids Natural reserves in the range include: * Białowodzka Mountain Nature Reserve * Kamionna Nature Reserve * Kostrza Nature Reserve * Luboń Wielki Nature Reserve Luboń (german: Luban) is a town in Poland, situated on the Warta River, in the Poznań metropolitan area, in the Poznań County in the Greater Poland Voivodeship. It has 29,301 inhabitants (2010). The town was c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nowy Sącz County
__NOTOC__ Nowy Sącz County ( pl, powiat nowosądecki) is a unit of territorial administration and local government (powiat) in Lesser Poland Voivodeship, southern Poland, on the Slovak border. It came into being on January 1, 1999, as a result of the Polish local government reforms passed in 1998. Its administrative seat is the city of Nowy Sącz, although the city is not part of the county (it constitutes a separate city county). The county contains five towns: Krynica-Zdrój, south-east of Nowy Sącz, Stary Sącz, south-west of Nowy Sącz, Grybów, east of Nowy Sącz, Piwniczna-Zdrój, south of Nowy Sącz, and Muszyna, south-east of Nowy Sącz. The county covers an area of . As of 2006 its total population is 197,718, out of which the population of Krynica-Zdrój is 11,243, that of Stary Sącz is 8,987, that of Grybów is 6,025, that of Piwniczna-Zdrój is 5,717, that of Muszyna is 4,980, and the rural population is 160,766. Neighbouring counties Apart from the city of No ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
General Government
The General Government (german: Generalgouvernement, pl, Generalne Gubernatorstwo, uk, Генеральна губернія), also referred to as the General Governorate for the Occupied Polish Region (german: Generalgouvernement für die besetzten polnischen Gebiete), was a German zone of occupation established after the invasion of Poland by Nazi Germany, Slovakia and the Soviet Union in 1939 at the onset of World War II. The newly occupied Second Polish Republic was split into three zones: the General Government in its centre, Polish areas annexed by Nazi Germany in the west, and Polish areas annexed by the Soviet Union in the east. The territory was expanded substantially in 1941, after the German Invasion of the Soviet Union, to include the new District of Galicia. The area of the ''Generalgouvernement'' roughly corresponded with the Austrian part of the Polish–Lithuanian Commonwealth after the Third Partition of Poland in 1795. The basis for the formation of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Invasion Of Poland
The invasion of Poland (1 September – 6 October 1939) was a joint attack on the Republic of Poland by Nazi Germany and the Soviet Union which marked the beginning of World War II. The German invasion began on 1 September 1939, one week after the signing of the Molotov–Ribbentrop Pact between Germany and the Soviet Union, and one day after the Supreme Soviet of the Soviet Union had approved the pact. The Soviets invaded Poland on 17 September. The campaign ended on 6 October with Germany and the Soviet Union dividing and annexing the whole of Poland under the terms of the German–Soviet Frontier Treaty. The invasion is also known in Poland as the September campaign ( pl, kampania wrześniowa) or 1939 defensive war ( pl, wojna obronna 1939 roku, links=no) and known in Germany as the Poland campaign (german: Überfall auf Polen, Polenfeldzug). German forces invaded Poland from the north, south, and west the morning after the Gleiwitz incident. Slovak military forces ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
1934 Flood In Poland
1934 flood in Poland ( pl, Powódź w Polsce, 1934) was the biggest flood in the Second Polish Republic. It began with heavy rains in the Dunajec river basin, which took place between 13 and 17 July 1934. In the following days, the flood spread to the basins of the Raba, Wisłoka, and Skawa, all of which are tributaries to the Vistula. The disaster took the lives of 55 people and caused damages estimated at 60 million interbellum zlotys. The flood The first heavy rains took place on 13 July 1934, and it continued during the coming days, with more than of rain noted on 14 and 15 July. Peak of the rainfall was marked on 16 July, with heaviest rains ever recorded in the Dunajec basin. On that day, of rain fell in the village of Witów, and in Kuźnice—. On the same day, Polish record of rainfall was broken in Tatras valley of Hala Gąsienicowa, where were recorded. Even though the Dunajec basin was the most affected, heavy rain was also recorded in the basins of the Skawa, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gord (archaeology)
A gord is a medieval Slavonic fortified settlement, usually built on strategic sites such as hilltops, riverbanks, lake islets or peninsulas between the 6th and 12th centuries CE in Central and Eastern Europe. The typical gord usually consisted of a group of wooden houses surrounded by a wall made of earth and wood, and a palisade running along the top of the bulwark. Etymology The term ultimately descends from the reconstructed Proto-Indo-European root '' ǵʰortós'', enclosure. The Proto-Slavic word ''*gordъ'' later differentiated into grad ( Cyrillic: град), gorod (Cyrillic: город), gród in Polish, gard in Kashubian, etc. It is the root of various words in modern Slavic languages pertaining to fences and fenced-in areas (Belarusian гарадзіць, Ukrainian horodyty, Czech ohradit, Russian ogradit, Serbo-Croatian ograditi, and Polish ogradzać, grodzić, to fence off). It also has evolved into words for a garden in certain languages. Additionally, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shoreline
A shore or a shoreline is the fringe of land at the edge of a large body of water, such as an ocean, sea, or lake. In physical oceanography, a shore is the wider fringe that is geologically modified by the action of the body of water past and present, while the beach is at the edge of the shore, representing the intertidal zone where there is one. In contrast to a coast, a shore can border any body of water, while the coast must border an ocean or a sea. Therefore, in that sense, a coast is a type of shore. However, the word "coast" often refers to an area far wider than the shore, often stretching miles into the interior. Shores are influenced by the topography of the surrounding landscape, as well as by water induced erosion, such as waves. The geological composition of rock and soil dictates the type of shore which is created. Rivieras ''Riviera'' is an Italian word for "shoreline", ultimately derived from Latin ''ripa'' ("riverbank"). It came to be applied as a proper ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nowy Sącz
Nowy Sącz (; hu, Újszandec; yi, Tzanz, צאַנז; sk, Nový Sonč; german: Neu-Sandez) is a city in the Lesser Poland Voivodeship of southern Poland. It is the district capital of Nowy Sącz County as a separate administrative unit. It has a population of around 83,116 as of 2021. Names Nowy Sącz has been known in German as ''Neu Sandez'' and in Hungarian as ''Újszandec''. The Rusyn name was Novyj Sanc. Its Yiddish names include צאַנז (''Tsanz'') and נײַ-סאַנץ (''Nay-Sants''). Geography Nowy Sącz is located at the confluence of the Kamienica River and Dunajec, about north of the Slovak border, in the Sądecka Valley (''Kotlina Sądecka'') at an altitude of . It is surrounded by ranges of the eastern Outer Western Carpathian Mountains: Beskid Sądecki to the south, Beskid Wyspowy to the west, Beskid Niski to the southeast, and the foothills of Pogórze Rożnowskie to the north. The geological basis is Carpathian flysch – an undifferentiated gre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Invasion Of Poland
The invasion of Poland (1 September – 6 October 1939) was a joint attack on the Republic of Poland by Nazi Germany and the Soviet Union which marked the beginning of World War II. The German invasion began on 1 September 1939, one week after the signing of the Molotov–Ribbentrop Pact between Germany and the Soviet Union, and one day after the Supreme Soviet of the Soviet Union had approved the pact. The Soviets invaded Poland on 17 September. The campaign ended on 6 October with Germany and the Soviet Union dividing and annexing the whole of Poland under the terms of the German–Soviet Frontier Treaty. The invasion is also known in Poland as the September campaign ( pl, kampania wrześniowa) or 1939 defensive war ( pl, wojna obronna 1939 roku, links=no) and known in Germany as the Poland campaign (german: Überfall auf Polen, Polenfeldzug). German forces invaded Poland from the north, south, and west the morning after the Gleiwitz incident. Slovak military forces ad ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Artificial Lake
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
