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EN
Kielce is a city situated in the centre of the Holy Cross Mountains, one of the most interesting geological areas in Europe. For this reason, institutions related to mining and geology have been operating here for over 200years. After the establishment of the Polish Geological Institute in 1919 in Warsaw, one of its founders, Jan Czarnocki, took steps to establish a regional branch of the Institute in Kielce, whose aim was to conduct scientific and exploratory research in the Holy Cross Mountains area. These activities were successfully completed in 1937, and since then, with a short break due to the Second World War, a branch of the Polish Geological Institute has been operating in Kielce. Since 1961, its headquarters have been located in a modern building, designed entirely for its needs, which has recently been modernized and expanded. Several dozen people employed in the Holy Cross Branch of the PGI-NRI carry out tasks in the field of applied geology and scientific research, focused on the study of an almost complete succession of Phanerozoic rocks in this region - from the Cambrian the history of the Holy Cross Branch of the PGI-NRI, and to present the most important to the Quaternary. The aim of this article is to provide a brief introduction to data related to the research and accomplishments of the geologists working in Kielce.
EN
Established a few months after regaining independence in 1918, the Polish Geological Institute was carrying out research aimed at ensuring the supply of necessary mineral raw resources to the domestic industry. The director of the Institute, Prof. J. Morozewicz as well as the state authorities were aware of the fact that for the proper functioning of the Institute suitable headquarter was needed. Therefore, already in the mid-1919, the appropriate area and financial resources were allocated for the construction of large buildings, the designer of which S W0łk0wicZ T M Pervt was Prof. M. Lalewicz. The laboratory pavilion was opened in 1926. The main building, which was put into use in 1936 and rebuilt after the destruction during World War II, has been the pride of the Institute until today. The extension of the state and a wide range of research issues meant that already in 1921, it was necessary to establish the Upper Silesian Station in Dąbrowa Górnicza, whose activity was focused on the coal geology. The Geological Station in Borysław, operating in the structure of the PGI since 1920, was transformed three years later into the Oil and Salt Department of the PGI, which closely co-operated with the Carpathian oil industry. The Holy Cross Mountain research group was located during 1937-1955 in the family home of Jan Czarnocki. After World War II, due to the significant intensification of geological research and exploration in Poland, new regional divisions of the Institute were established that currently have their headquarters in Kraków, Sosnowiec, Wrocław, Kielce, Gdańsk and Szczecin; all have the rank of branches. The organizational structure of the PGI is of an extremely regional nature, and the research issues of individual branches are mostly related to the recognition of the geological structure and mineral resources occurring in a given region. In addition, the Polish Geological Institute possesses 8 core repositories.
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