Disclaimer The Tentative Lists of States Parties are published by the World Heritage Centre at its website and/or in working documents in order to ensure transparency, access to information and to facilitate harmonization of Tentative Lists at regional and thematic levels. The sole responsibility for the content of each Tentative List lies with the State Party concerned. The publication of the Tentative Lists does not imply the expression of any opinion whatsoever of the World Heritage Committee or of the World Heritage Centre or of the Secretariat of UNESCO concerning the legal status of any country, territory, city or area or of its boundaries. Description Introduction When visitors from Bohemia and all of Europe call a part of this Earth 'Paradise', they must certainly have a good reason. The name 'ttesky rij' (Czech Paradise) has become a symbol for the delight felt by the intellectual and social elite in the second half of the 19th century over the beauties of nature in this country. The name was soon accepted and the professional public was required to give the name a professional framework and to increase the care devoted to preserving the quality of nature. Recognition of the values of this territory was manifested by proclaiming the Prachovskd skily Nature Reserve in 1933 and the tesky rij Protected Landscape Areas in 1955, the first large protected natural territory in the Czech Republic.
Jul 12, 2010 Unlimited DVR storage space. Live TV from 60+ channels. No cable box required. Cancel anytime. The Tentative Lists of States Parties are published by the World Heritage Centre at its website and/or in working documents in order to ensure transparency, access to information and to facilitate harmonization of Tentative Lists at regional and thematic levels. The sole responsibility for the.
The chief phenomena in the territory are sandstone rock cities of Mesozoic age with various characters and various stages of development. Together with the rich variety of other geomorphic forms, valuable biotic components in the surrounding nutritive habitats make this territory quite unique and impart to it very high aesthetic and scientific value. Climate Cesky raj is located in a temperate, mildly humid climatic area with mild winters.
Harvard marketing simulation solution. The average annual temperature lies within the limits of 7?8 °C and the average annual precipitation is 550? 650 (700) mm. Area of the Territory The rock cities, in themselves, have a discontinuous boundary and cover an area of about 17.6 km2. The actual area of the territory involved equals about 200 km', of which 93 km' constitutes the Cesky raj Protected Landscape Area and 30 km~ corresponds to the Maloskalsko Nature Park. Description of the Territory The proposed natural monument consists of several separate rock cities and rock walls formed from sediments of Cretaceous age, with a thickness of 240 m in some places.
A description and their characteristics are given below. The territory has enjoyed various levels of protection from the standpoint of nature protection. A number of small protected territories have been proclaimed here, which partly overlap the tesky raj Protected Landscape Area or the Maloskalsko proclaimed Nature Parkm.The ltesky raj Protected Landscape Area contains four zones of increased nature protection and the rock cites are mostly classified in the first category with the strictest regime. In addition, each small protected territory has a specific protective zone with a width of at least 50m around its boundary. An extended Protected Landscape Area is being prepared for the whole proposed territory as a natural monument (about 219 km2), creating unified protective zones for all the local rock phenomena. These isolated rock cities with protective zones form a unified territory of exceptional universal importance from both a scientific point of view and in connection with protection of the natural environment.
The territory consists primarily of Mesozoic Cretaceous sandstones of various ages (Cenomanian, Turonian, Coniacian). The sediments were formed primarily in the shallow beach zone of a Cretaceous sea. The macro?relief of the entire area is very varied? Consisting of a mixture of low hills, highlands and basins.
There are also numerous canyons and valleys with well?developed flood plains. The surface modelled in the Tertiary by block movements in the vicinity of or directly on the Lu2ice fault forms a dominant feature. Thus, a number of cuests were formed.
In the Tertiary, volcanic bodies and veins penetrated through the sandstones. The significantly changing river beds of water courses (especially the Jizera and Paleo?Jizera) participated greatly in modelling the terrain and creation of the mezo?relief.
The landscape contains a number of historical monuments, emphasizing the natural dominant features and accenting their aesthetic value. The tesky raj rock cities The rock cities and formations are the main natural and aesthetic phenomenon of the landscape of the tesky raj. In spite of some common features, the individual rock cities are very different in their age, manner of sedimentation, grain quality and cementing material, thickness of the individual layers, character of the exogenic formation factors or stage of development of the rock city. Hruba skala Rock City (PR, area of 2.2 km2) This is a typical pillar rock city in Coniacian sandstones.