visit in the city's spas
Cracow may seem very attractive place for nature lovers. In this city there are over forty parks, where you can walk and spend time in nature. One of the most interesting places of city in terms of nature are also river valleys and reservoirs located within a specific corridor of the Vistula River. In addition, in Cracow there are several nature reserves and more than two hundred natural monuments, most of which are trees. Visiting all of these sites can definitely be a highlight of a visit to Cracow. Satisfied with your stay in city may also be people who have decided to visit one of the spas. They can benefit from the healing baths and wellness treatments.
Organization of tourist visits to the Cracow
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.
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