hearing the bugle call from the tower of St Mary's
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.
tour in the footsteps of John Paul II
For better organization of package tours dealing with sightseeing of Krakow, set in the city several tourist routes, so that tour guides certainly not skip some interesting places during the show tourists around the city. One of the important points of a visit to Krakow is a tour of Krakow's religious monuments, which after all, in this city there is no shortage, and are a very good testimony to the progressive development of the architecture. Many people will want to also travel route in the footsteps of John Paul II. The traditional route, which is not to be missed during a visit to Krakow is also a route that allows to know the history of Polish kings, who resided in this city.
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