Visiting historic sites in Krakow
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.
International Airport in Krakow
Organizing tourist visits to Cracow is a relatively easy task logistically. Foreign tourists fly to the airplane and land on the international airport in Cracow. A larger number of people can be taken away from him by coach and drive to the hotel. In contrast, individuals can use taxis or public transport. From various parts of the Polish cii=ty you can commute by train. These types of trips are usually organized by a single tourists or families with children. In contrast, school trips, student or corporate commute to Cracow coach. The fact that the cracked, you can so easily get certainly more encouraged to visit this city.
The Kraków-Częstochowa Upland
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