Geologia
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ISSN 0138-0974
e-ISSN: 2353-0782
Issue Date
2005
Volume
T. 31
Number
Nr 2
Description
Journal Volume
Geologia
T. 31 (2005)
Projects
Pages
Articles
Problemy zagospodarowania wyrobisk po eksploatacji kruszywa naturalnego na przykładzie złóż w dolinie Soły między Kętami a Bielanami
(Wydawnictwa AGH, 2005) Bobrek, Kamila; Paulo, Andrzej
Deposits of the natural aggregates along the Soła valley were formed within Quaternary rendzina terrace. They are exploited from under the groundwater level. As a result, many hectares of valuable agricultural land are converted into post-mining pits, which change the natural environment of the Soła valley and preclude future crops. Being forced to declare post-mining redevelopment mode, users of the natural aggregate deposits declared construction of water reservoirs, which they call fishing ponds. However, in reality the ponds are used for recreation fishing but not for productive fish farming, which appears impossible, which cannot be drained in deep basins. A panorama of possible ways of reclamation of post-mining pits based on natural environment and social conditions is discussed, forming main body of the paper.
Różowa sól kamienna do produkcji galanteryjnych wyrobów solnych - geologiczne warunki występowania, własności i metody pozyskiwania w Kopalni Soli »Kłodawa«
(Wydawnictwa AGH, 2005) Czapowski, Grzegorz; Misiek, Grzegorz; Poborska-Młynarska, Katarzyna; Tomassi-Morawiec, Hanna
Colored rock salt types, especially pink, orange and red ones, become a more demand material for production of fancy salt goods such as salt lamps, chandelier, sculptures etc. Colored rock salts occur in many salt formations and deposits in Europe and in the world as it was illustrated by a short review of selected rock salt deposits. In Poland the discussed colored rock salts are exploited only in one salt deposit, located in the Kłodawa salt diaper (by the »Kłodawa« Salt Mine), mainly for alimentary and chemical industry and for road treatment. Last years the mine has excavated a small amount of pink salt for production of mentioned above salt fancy goods and the increased demand for this raw material initiated studies on characteristics and geological position of pink salt within the salt deposit, enabling future prediction and calculation of its resources. Preliminary characteristics of features and the geological situation as well as a classification and exploitation methods of pink rock salt were presented in the paper.
Efektywność automatycznego przetwarzania regionalnego modelu pola hydrodynamicznego na przykładzie fragmentu obszaru pasma przedkarpackiego
(Wydawnictwa AGH, 2005) Dzięgiel, Maciej
Making a regional hydrodynamic simulating model much more detailed on the given example proves that this operation should be careful. The research was done on the small part of the regional model of the Major Groundwater Basin No. 425 whose discretization grid was made five times denser. This operation was made to obtain a more exact image of, for example, the landuse of the area, for example. The means to obtain appropriate results was the interpolation of the majority of the hydrogeological parameters of the regional hydrodynamic simulating model. The Processing Modflow 5.0 code makes the above possible. The more detailed model was verified on the basis of the author's measuring of the groundwater table on the Right Bank of the Wisłok river valley. Satisfactory compatibility of hydrodynamic fields has been stated.
Debryty kohezyjne warstw istebniańskich (senon górny - paleocen) na zachód od Skawy
(Wydawnictwa AGH, 2005) Strzeboński, Piotr Andrzej
Cohesive debrites of the Istebna Beds occur within the western part of the Silesian Unit of the Outer Flysch Carpathians. The lithofacies described represents siliciclastic deposits consisting of mud-sandy matrix and scattered, psephite-size clasts. The cohesive debrites originated from sediment gravity flows that were generated on the slope of sedimentary basin by mass-movements and were deposed as aprons by submarine, cohesive debris flows. The highest content of the cohesive debrites (12% of the succession thickness) has been recorded within the Istebna Beds of the Silesian Beskid Mts, the medium in the Beskid Mały Mts (7%) and the lowest within the Moravian Beskid Mts (2%). Most frequently the lithofacies presented occurs within the Lower Istebna Sandstones, while the cohesive debrites with the biggest lithoclasts occur within the top part of the Lower Istebna Shales. The exotic material with dominating crystalline rocks, mostly gneisses, schists and granitoids, makes up 25% of the described deposits (exotic cohesive debrites). Various types of limestones prevail among much rarer clasts of sedimentary rocks and the amount of the limestones distinctly increases going to the east.
Morfotektonika przełomów Solinki i Wetlinki w świetle badań terenowych i interpretacji zdjęć lotniczych (Bieszczady Wysokie)
(Wydawnictwa AGH, 2005) Kuśmierek, Jan
Gorge-type valleys of the Solinka and Wetlinka rivers within the Upper San drainage basin represent an interesting geotouristic object in respect of distinct relationship between relief, and evolution and tectonics of complex geological structures in the foreland of the Dukla Unit in the Bieszczady Mts. They also distinguish themselves by picturesque landscapes and vast exposures of the Otryt Sandstone outcrops, this Late Oligocene member is typical of the Bieszczady facies subregion of the Silesian Nappe. Detailed cartographic and structural investigations made by the author have proved that synclines, composed of thick complexes of the Otryt Sandstones, are backward overthrust onto subsurface structural elements, a feature which has not been reflected in previous cartographic elaborations. With formation of the disharmonic tectonic structures, the inversional character and origin of the Solinka and Wetlinka water gaps are connected. Hypsometric measurements of relics of the foothill and riverside planation surfaces, carried out on stereoscopic aerial photographs, have documented significant deformation of the surfaces and oscillatory character of the Pliocene-Quaternary neotectonic uplift. The greatest denivelations of the planation surfaces correlate with the intersection of the backward overthrusts which had crucial effects on tectonic reshaping of the structures, as well as on the relief development, this resulted in the origin of the antecedent water gaps and incised meanders.