Access to Krakow by train
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.
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.
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