Walk on the Main Market
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.
Tramways of Cracow
Tourists can move around Cracow in several different ways. At small distances can simply walk, and larger sections are driven around by coach. After , you can also navigate using the trams, which have several lines and thus allow you to reach many places of city. Currently there are also light rail tunnel and a water tram ride which may be for many tourists an added attraction. A good complement to Cracow tram lines is extensive bus service, running on the system day and night, and faster and supportive. An additional motivation for the authorities cracked for expanding the public transport network is also a presence in this city of many students, including foreign.
Some facts about 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