2014
DOI: 10.7306/gq.1200
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Depositional environment of the glacigenic deposits from the Holy Cross Mountains (Poland) – interpretation based on macro- and microstructure analyses

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Cited by 2 publications
(6 citation statements)
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“…The highest elevations feature mostly Devonian sandstone and claystone outcrops as well as some weathered debris. Pleistocene sediments are found on slopes at lower elevations (Klatka, 1962;Filonowicz, 1969;Ludwikowska-Kędzia and Olszak, 2009) and include glaciofluvial sand, loess, slope deposits and polygenic sands with a complex fluvial, slope and aeolian origin. Fluvial sand, forming a terrace, can be found at the foot of the slope on the sides of the Belnianka River valley.…”
Section: Study Areamentioning
confidence: 99%
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“…The highest elevations feature mostly Devonian sandstone and claystone outcrops as well as some weathered debris. Pleistocene sediments are found on slopes at lower elevations (Klatka, 1962;Filonowicz, 1969;Ludwikowska-Kędzia and Olszak, 2009) and include glaciofluvial sand, loess, slope deposits and polygenic sands with a complex fluvial, slope and aeolian origin. Fluvial sand, forming a terrace, can be found at the foot of the slope on the sides of the Belnianka River valley.…”
Section: Study Areamentioning
confidence: 99%
“…The diamicton deposits are formed of displaced material derived from weathered basement rocks, loess and sand. The diamictons vary in age and represent two stages of slope process evolution (Filonowicz, 1969) dated by thermoluminescence (TL) to the beginning of the Odranian glaciation (Drenthe) and the Upper Vistulian (Weichselian) (Ludwikowska-Kędzia and Olszak, 2009). At both study sites, diamicton occurs with sand interpreted as a glaciofluvial deposit (Klatka, 1962) and sand redeposited by fluvial, slope and aeolian processes (Filonowicz, 1969;Ludwikowska-Kędzia, 2007) (Figure 1b).…”
Section: Study Areamentioning
confidence: 99%
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