Visit Cracow

t to one of Krakow's museums or galleries. In addition to visiting art museums, you can also visit the military museum or martyrdom and technical. It is also worth noting that in Krakow filmed several Polish TV series, and from ti

Visit Cracow

Krakow theaters

Krakow is an important cultural center of Polish, so while visiting this city, we can not miss a visit to one of Krakow's theaters. Even more attractive it may be a visit to one of Krakow's museums or galleries. In addition to visiting art museums, you can also visit the military museum or martyrdom and technical. It is also worth noting that in Krakow filmed several Polish TV series, and from time to time are shot in this city some movies, so with a little luck you can get also agreed to explore one of the film sets. Being in Krakow you can not forget to participate in one of the cultural events organized in the city.


Crakow uprising

The Kraków Uprising of February 1846 was an attempt, led by Polish insurgents such as Jan Tyssowski and Edward Dembowski, to incite a fight for national independence. The uprising was centered on the city of Kraków, the capital of a small state of Free City of Kraków. It was directed at the powers that partitioned Poland, in particular, the nearby Austrian Empire. The uprising lasted about nine days, and ended with Austrian victory.

Źródło: https://en.wikipedia.org/wiki/Krak%C3%B3w_Uprising


Worth to know

The Kraków-Częstochowa Upland, also known as the Polish Jurassic Highland or Polish Jura (Polish: Jura Krakowsko-Częstochowska), is part of the Jurassic System of south?central Poland, stretching between the cities of Kraków, Częstochowa and Wieluń. The Polish Jura borders the Lesser Polish Upland to the north and east, the foothills of the Western Carpathians to the south and the Silesian Upland to the west.

The Polish Jura consists of a hilly landscape with Jurassic limestone rocks, cliffs, valleys and vast limestone formations, featuring some 220 caves. The relief of the upland developed since the Paleogene, under climatic conditions changing considerably. Its main component is a peneplain, crowned by monadnocks, rocky masses that resisted erosion, generated as hard rock on Late Jurassic buildup surrounded by less resistant bedded limestone of the same age.1 The Polish Jura is visited by roughly 400,000 visitors a year. Part of it belongs to the Ojców National Park, the smallest of Poland's twenty national parks, ranking among the most attractive recreational areas of the country.2

Źródło: https://en.wikipedia.org/wiki/Krak%C3%B3w-Cz%C4%99stochowa_Upland



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