A visit to the main research units located in Cracow
Cracow is one of the student Polish cities, because very often organizes trips to this city student, whose aim is to explore the city, exploring the history of our country also in terms of scientific and visiting universities. Some foreign students staying in Poland on an exchange or on any internship program, they also try to get to know the city, to which they came. Often they visit the nationwide research centers located in city, such as the National Center for Science and the Branch of the Polish Academy of Sciences. In addition, they can learn the rules of research by Cracow's research units. Clearly, part of their visit is a tour of Cracow's universities.
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.
The KrakÃ³w-CzÄ™stochowa Upland
The KrakÃ³w-CzÄ™stochowa Upland, also known as the Polish Jurassic Highland or Polish Jura (Polish: Jura Krakowsko-CzÄ™stochowska), is part of the Jurassic System of south?central Poland, stretching between the cities of KrakÃ³w, CzÄ™stochowa and WieluÅ„. 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 OjcÃ³w National Park, the smallest of Poland's twenty national parks, ranking among the most attractive recreational areas of the country.2