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Wyszukujesz frazę "moraine" wg kryterium: Temat


Wyświetlanie 1-3 z 3
Tytuł:
Geomorphology, sedimentology and origin of the glacigenic Złota Góra hills near Konin (Central Poland)
Autorzy:
Widera, M.
Powiązania:
https://bibliotekanauki.pl/articles/2059142.pdf
Data publikacji:
2011
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Central Poland
sandur
end moraine
interlobate landform
Opis:
The Złota Góra hills (Central Poland) have been variously interpreted as a kame, a sandur and as different types of moraine. Due to their morphology and internal structure, the Złota Góra hills differ, however, from typical depositional glacigenic landforms in the European lowlands. Morphologically, the Złota Góra hills consist of numerous asymmetrical and oval hills of various sizes. The deposits show a wide variety of lithofacies, which are diagnostic for debris flows, hyperconcentrated flows, sheetfloods, braided rivers, deltas and ephemeral lakes. The combination of such deposits is characteristic of an environmental setting including both an end moraine fan (debris flows, hyperconcentrated flows, sheetfloods and ephemeral lake deposits) and a sandur (braided river, sheetfloods, and delta or ephemeral lake deposits). Therefore, these hills must be interpreted as representing an end moraine/sandur massif. The hills were probably formed subaerially by meltwater in an interlobate area of the retreating Scandinavian ice sheet.
Źródło:
Geological Quarterly; 2011, 55, 3; 253-268
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrogeochemistry and vulnerability of ground water in the moraine upland aquifers of the Gdańsk region (Northern Poland)
Autorzy:
Pruszkowska, M.
Malina, G.
Powiązania:
https://bibliotekanauki.pl/articles/2060217.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Gdańsk region
hydrogeochemistry
groundwater protection
moraine upland aquifers
Opis:
The focus of this study was on determination and comparison of natural and current hydrogeochemical features of the groundwater, in order to evaluate changes of water quality and to identify the origin of these changes. Both natural processes and anthropogenic stress affect the chemical composition of groundwater were recognised. In both aquifer groups groundwater chemical composition dem on strates some similarities and is formed by the same kinds of natural processes, which are taking place already in the upper zones of the shallow aquifers, where groundwater is saturated with respect to most of carbon ate and clay minerals, as well as minerals containing Fe exp. 2+ ions. During seepage into deeper aquifers, water is being enriched with Fe exp. 2+ and Mn exp. 2+ ions and in some places with SO4exp.2 - and Mg exp.2+ as well. The types and intensity of human activities, as well as the vulnera ility of aquifers to contamination, were concluded to play an important role in generating the observed changes in the chemical character is tics of the groundwater. They effect on changes of hydrogeochemical back ground values (e.g. TDS, N-com pounds), the current in crease of maximum concentrations of N-com pounds, chlorides, sulphates, magnesium and TDS (total dissolved solids).
Źródło:
Geological Quarterly; 2008, 52, 3; 291-291
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Morena szaflarska w świetle nowych danych z odsłonięć i wierceń w 100-lecie jej odkrycia
Szaflary moraine in the light of new data from exposures and drilling on the 100th anniversary of its discovery
Autorzy:
Wójcik, Antoni
Powiązania:
https://bibliotekanauki.pl/articles/2087064.pdf
Data publikacji:
2022
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Czwartorzęd
Podhale
tatrzańskie lodowce
morena
kamieniołom w Szaflarach
Quaternary
Podhale Region
Tatra glaciers
moraine
quarry in Szaflary
Opis:
In the northern part of the Podhale Region, nearly 100 years ago, Matkowski (1924, 1928) described gravels exposed in a quarry in Szaflary and considered them to be moraine sediments - Szaflar moraine. Romer (1929) confirmed this interpretation of the sediments. Later studies of Halicki (1930), Klimaszewski (1948, 1988), Birkenmajer (1976) and Birkenmajer and Stuchlik (1975) completely excluded the possibility of moraines in this area and showed that these sediments have are of fluvioglacial origin. Comparing the quarry's ranges due to exploitation, it was found that the authors could observe various deposits exposed during the progress of exploitation towards the west. In the profiles of trenches for new buildings to the NW from the quarry, clays containing sands and gravels and individual boulders and blocks of quartzite and granite with a diameterof0.8 to 1.2m were found. The exposed erratics exactly correspond to the description of the moraine by Matkowski (1924, 1928) from the quarry in Szaflary. In addition, in the recently drilled Nowy Targ PIG-2 borehole, similarly developed pieces were found at a depth of19.7-69.5 m. Combining archival data and new facts from drilling and exposures, a view can be proposed that, during the Southern Polish Glaciations, the Tatra glaciers reached the Nowy Targ Basin and perhaps the foothills of the Gorce Mts, which was already suggested by Rehman (1895), Zapatowicz (1913) and Matkowski (1928).
Źródło:
Przegląd Geologiczny; 2022, 70, 6; 458--467
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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