Visit Cracow

Dodane: 30-05-2016 10:23
Visit Cracow climbing travels poland

Polish uprisings - cracow

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


School trips to Cracow

Cracow is typically Polish, a beautiful city, which reflects the history of Polish. Therefore, all schools are trying to organize their students a trip to Cracow. Besides the fact that such a trip can be one of the opportunities for fun and integration with each other the whole class, it can also be an opportunity to explore the history of our country through visiting historical sights. It seems that such places in Cracow is so much that each teacher must choose from among them those that may long remain in the memory of his disciples. A must-visit Cracow after a walk through the market in city and listen to the bugle call from the tower of St Mary's. Hearing such a bugle call live can become for many people an unforgettable experience.


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