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Bochnia
Bochnia is a town on the river Raba in southern Poland, administrative seat of Bochnia County in Lesser Poland Voivodeship. The town lies approximately halfway between Tarnów (east) and the regional capital Kraków (west). Bochnia is most noted for its Bochnia Salt Mine, salt mine, the oldest functioning in Europe, built in the 13th century, a World Heritage Site and a List of Historic Monuments (Poland), Historic Monument of Poland. As of December 2021, Bochnia has a population of 29,317 and an area of . History Bochnia is one of the oldest cities of Lesser Poland. The first known source mentioning the city is a letter of 1198, in which Aymar the Monk, Latin Patriarch of Jerusalem, confirmed a donation by the local magnate Mikora Gryfit to the monastery of the Order of the Holy Sepulchre (Catholic), Order of the Holy Sepulchre in Miechów. The discovery of major deposits of halite, rock salt at the site of the present mine in 1248 led to the grant of city privileges (Magdeb ...
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Bochnia County
__NOTOC__ Bochnia County () is a unit of territorial administration and local government (powiat) in Lesser Poland Voivodeship, southern Poland. 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 Bochnia, which lies east of the regional capital Kraków. The only other town in the county is Nowy Wiśnicz, lying south of Bochnia. The county covers an area of . As of 2019 its total population is 106,626, out of which the population of Bochnia is 29,814, that of Nowy Wiśnicz is 2,757, and the rural population is 74,055. Neighbouring counties Bochnia County is bordered by Proszowice County to the north, Brzesko County to the east, Limanowa County to the south, and Myślenice County, Wieliczka County and Kraków County to the west. Administrative division The county is subdivided into nine gminas (one urban, one urban-rural and seven rural). These are listed in the following table, in d ...
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Bochnia Salt Mine
The Bochnia Salt Mine () in Bochnia, Poland, is one of the oldest salt mines in the world and is the oldest commercial company in Poland. The Bochnia salt mine was established in 1248 after salt had been discovered there in the 12th and 13th centuries and became part of the royal mining company, ''Żupy krakowskie'' (Kraków Salt Works). In 1990, the mine ceased producing salt but remained a tourist attraction. The mine is on the UNESCO list. In 1981 the Bochnia salt mine was declared a heritage monument. It is one of Poland's official national List of Historical Monuments (Poland), Historic Monuments (''Pomnik historii''), as designated on 6 October 2000 and is overseen by the Narodowy Instytut Dziedzictwa, National Heritage Board of Poland. The chapel in the mine has train tracks running through it. History The mine shafts measure in length at about in depth below the surface, at 16 levels. In 2013, the mine was added to the World Heritage Site, UNESCO World Heritage List ...
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Lesser Poland Voivodeship
Lesser Poland Voivodeship ( ) is a voivodeships of Poland, voivodeship in southern Poland. It has an area of , and a population of 3,404,863 (2019). Its capital and largest city is Kraków. The province's name recalls the traditional name of a historic Polish region, Lesser Poland, or in Polish: . The current Lesser Poland Voivodeship, however, covers only a small part of the broader ancient Małopolska region, which stretched far north, to Radom and Siedlce, also including such cities as Lublin, Kielce, Częstochowa, and Sosnowiec. The province is bounded on the north by the Świętokrzyskie Mountains (), on the west by ''Jura Krakowsko-Częstochowska'' (a broad range of hills stretching from Kraków to Częstochowa), and on the south by the Tatra mountains, Tatra, Pieniny Mountains, Pieniny and Beskidy Mountains. Politically, it is bordered by Silesian Voivodeship to the west, Świętokrzyskie Voivodeship to the north, Subcarpathian Voivodeship to the east, and Slovakia (Prešo ...
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Lesser Poland
Lesser Poland, often known by its Polish name ''Małopolska'' (; ), is a historical region situated in southern and south-eastern Poland. Its capital and largest city is Kraków. Throughout centuries, Lesser Poland developed a separate culture featuring diverse architecture, folk costumes, dances, cuisine, traditions and a rare Lesser Polish dialect. The region is rich in historical landmarks, monuments, castles, natural scenery and UNESCO World Heritage Sites. The region should not be confused with the modern Lesser Poland Voivodeship, which covers only the southwestern part of Lesser Poland. Historical Lesser Poland was much larger than the current voivodeship that bears its name. It reached from Bielsko-Biała in the southwest as far as to Siedlce in the northeast. It consisted of the three voivodeships of Kraków, Sandomierz and Lublin. It comprised almost 60,000 km2 in area; today's population in this area is about 9,000,000 inhabitants. Its landscape is mai ...
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Voivodeship Road
According to classes and categories of public roads in Poland, a voivodeship A voivodeship ( ) or voivodate is the area administered by a voivode (governor) in several countries of central and eastern Europe. Voivodeships have existed since medieval times and the area of extent of voivodeship resembles that of a duchy in ... road () is a category of roads one step below national roads in importance. The roads are numbered from 100 to 993. Total length of voivodeship roads in Poland is of which are unpaved (2008).Transport – activity results in 2008
, Główny Urząd Statystyczny


List of voivodeship roads

Current list of voivodeship road ...
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List Of Historic Monuments (Poland)
Historic Monument (, ) is one of several categories of objects of cultural heritage (in the singular, '' zabytek'') in Poland. To be recognized as a Polish historic monument, an object must be declared such by the President of Poland. The term "historic monument" was introduced into Polish law in 1990, and the first Historic Monuments were declared by President Lech Wałęsa Lech Wałęsa (; ; born 29 September 1943) is a Polish statesman, dissident, and Nobel Peace Prize laureate who served as the president of Poland between 1990 and 1995. After winning the 1990 Polish presidential election, 1990 election, Wałę ... in 1994. List The National Heritage Board of Poland maintains the official list. References {{reflist Objects of cultural heritage in Poland Law of Poland ...
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Magdeburg Rights
Magdeburg rights (, , ; also called Magdeburg Law) were a set of town privileges first developed by Otto I, Holy Roman Emperor (936–973) and based on the Flemish Law, which regulated the degree of internal autonomy within cities and villages granted by the local ruler. Named after the city of Magdeburg, these town charters were perhaps the most important set of Middle Ages, medieval laws in Central Europe. They became the basis for the German town laws developed during many centuries in the Holy Roman Empire. The Magdeburg rights were adopted and adapted by numerous monarchs, including the rulers of Crown of Bohemia, Bohemia, Kingdom of Hungary, Hungary, Crown of Poland, Poland, and Grand Duchy of Lithuania, Lithuania, a milestone in the urbanization of the region which prompted the development of thousands of villages and cities. Provisions Being a member of the Hanseatic League, Magdeburg was one of the most important trade cities, maintaining commerce with the Low Countries ...
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Vehicle Registration Plates Of Poland
Vehicle registration plates of Poland indicate the region of Vehicle registration, registration of the vehicle given the number plate. Law According to Polish law, the registration plate is tied to the vehicle, not the owner. There is no possibility for the owner to keep the licence number for use on a different car, even if it's a cherished registration. The licence plates are issued by the powiat (county) of the vehicle owner's registered address of residence, in the case of a natural person. If it is owned by a legal person, the place of registration is determined by the person's address. Vehicles leased under operating leases and many de facto finance leases will be registered at the address of the lessor. When a vehicle changes hands, the new owner must apply for new vehicle registration document bearing their name and registered address. The new owner may obtain a new licence plate although it is not necessary. In such a situation the licence plates are usually carried o ...
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Raba (Vistula)
The Raba is a river in the south of Poland (Lesser Poland Voivodeship), and a right-bank tributary of Vistula, Vistula River. Its source is in the Beskids, between the towns of Rabka-Zdrój and Nowy Targ. It flows to the north and then to the northeast. Towns along the river Raba include Rabka-Zdrój, Mszana Dolna, Myślenice, Dobczyce and Bochnia. For centuries, the Raba was an important artery, along which several towns and villages were established. Its name probably comes from Celtic languages, and the Raba is divided into three parts: the Upper Raba ( long located in the Beskids), the Middle Raba (in the Carpathian Foothills), and the Lower Raba (in the Sandomierz Basin). The Raba has its source at the Sieniawa, LesIser Poland Voivodeship, Sieniawa mountain pass, at the height of above sea level. It flows into the Vistula near Uscie Solne, after , while the area of its drainage basin is . From its source downstream to the town of Myślenice, the Raba is a typical mountain r ...
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Central European Summer Time
Central European Summer Time (CEST, UTC+02:00), sometimes referred to as Central European Daylight Time (CEDT), is the standard clock time observed during the period of summer daylight-saving in those European countries which observe Central European Time (CET; UTC+01:00) during the other part of the year. It corresponds to UTC+02:00, which makes it the same as Eastern European Time, Central Africa Time, South African Standard Time, Egypt Standard Time and Kaliningrad Time in Russia. Names Other names which have been applied to Central European Summer Time are Middle European Summer Time (MEST), Central European Daylight Saving Time (CEDT), and Bravo Time (after the second letter of the NATO phonetic alphabet). Period of observation Since 1996, European Summer Time has been observed between 01:00 UTC (02:00 CET and 03:00 CEST) on the last Sunday of March, and 01:00 UTC on the last Sunday of October; previously the rules were not uniform across the European Union. The ...
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Europe
Europe is a continent located entirely in the Northern Hemisphere and mostly in the Eastern Hemisphere. It is bordered by the Arctic Ocean to the north, the Atlantic Ocean to the west, the Mediterranean Sea to the south, and Asia to the east. Europe shares the landmass of Eurasia with Asia, and of Afro-Eurasia with both Africa and Asia. Europe is commonly considered to be Boundaries between the continents#Asia and Europe, separated from Asia by the Drainage divide, watershed of the Ural Mountains, the Ural (river), Ural River, the Caspian Sea, the Greater Caucasus, the Black Sea, and the waterway of the Bosporus, Bosporus Strait. "Europe" (pp. 68–69); "Asia" (pp. 90–91): "A commonly accepted division between Asia and Europe ... is formed by the Ural Mountains, Ural River, Caspian Sea, Caucasus Mountains, and the Black Sea with its outlets, the Bosporus and Dardanelles." Europe covers approx. , or 2% of Earth#Surface, Earth's surface (6.8% of Earth's land area), making it ...
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Halite
Halite ( ), commonly known as rock salt, is a type of salt, the mineral (natural) form of sodium chloride ( Na Cl). Halite forms isometric crystals. The mineral is typically colorless or white, but may also be light blue, dark blue, purple, pink, red, orange, yellow or gray depending on inclusion of other materials, impurities, and structural or isotopic abnormalities in the crystals. It commonly occurs with other evaporite deposit minerals such as several of the sulfates, halides, and borates. The name ''halite'' is derived from the Ancient Greek word for "salt", ἅλς (''háls''). Occurrence Halite dominantly occurs within sedimentary rocks where it has formed from the evaporation of seawater or salty lake water. Vast beds of sedimentary evaporite minerals, including halite, can result from the drying up of enclosed lakes and restricted seas. Such salt beds may be hundreds of meters thick and underlie broad areas. Halite occurs at the surface today in playas in reg ...
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