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Record of Late Holocene palaeoenvironmental changes in a Carpathian Lanslide: a case study of the Siekierczyna landslide (Beskid Wyspowy Mts., Outer Carpathians, South Poland)

Bryndal T., Cabaj W., Margielewski W., Pelc S.

Folia Quaternaria

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2003

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nr 74

75-96

EN

Successive phases of the Siekierczyna landslide evolution (the Beskid Wyspowy Mts., Outer West Carpathians) are related to Holocene climatic changes. Three phases of the landslide rejuvenation have been radiocarbon dated at: 3.8 ka, 2.9 ka and 2.2 ka. During these phases the valley of the Lasówka stream was dammed with colluvium and formed a natural dam lake. Mobilisation of the landslide occurred in response to strong climatic changes (cooling and wetting), recorded for the Subboreal Phase (ca. 4.2-3.8 ka and 3.3-2.9 ka), as well as (especially strong) at the start of the Subatlantic Phase (ca. 2.4-1.8 ka BP). Results of dendrochronological analysis indicate that the youngest phases of ground mobilisation were triggered by heavy rainfalls which caused floods in the Carpathians in years: 1940-41, 1958 and 1960, as well as in 1970-1974.

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Late Glacial - Holocene peat bog on Kotoń Mt. and its significance for reconstruction of palaeoenvironment in the Western Outer Carpathians (Beskid Makowski Range, South Poland)

Margielewski W., Obidowicz A., Pelc S.

Folia Quaternaria

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2003

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nr 74

35-56

EN

On the south slope of the pass between Kotoń Mt. and Pękalówka Mt. (Western Carpathians, Beskid Makowski Range), there occur big landslide with longitudinal deppressions, felt up of minerotrophic mire, with particularly long sequence of the Late Glacial deposits. The sediments were analysed by palynologic, macrofossils and sedimentological methods. Climatic changes of the Late Glacial and the Holocene were registered as changes in regional and local vegetation, as well as changes in the sediments. The maximal depth of the deposits amounts to about 4.7 m. On the bottom there occurs silt with gravel and a thin layer of decomposed peat, dated by 14C at 12, 140-70 years BP. Above, peat of the moss fen and sedge-moss fen type occurs, covered by a thick layer (thickness about 0.9 m) of minerogenic deposits (clay and silty clay). The beginning of the minerogenic cover sedimentation was dated at ca. 8, 230-80 years BP. The results of pollen analysis, confirmed by radiocarbon datings, show that the landslide depression was created in the Bolling Interstadial. The peat accumulation was started in the Older Dryas. The sedimentation of minerogenic deposits covering the mire, began during the strong wet phases registered in the Early Atlantic, and being continued in the wet periods of the Subboreal and Subatlantic.

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Systemy radiowego powiadamania o awariach przepompowni ścieków oraz urządzenia i obiekty z tworzyw sztucznych w gospodarce wodno-ściekowej

Szepielak E., Pelc S.

Zeszyty Naukowe Politechniki Świętokrzyskiej. Budownictwo

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2001

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Z. 40

231-245

PL

Referat przedstawia działalność Z.U.H INSTALBUD-SZEPIELAK w Koszycach Wielkich koło Tarnowa jako producenta materiałów budowlanych w zakresie urządzeń i obiektów gospodarki wodno-ściekowej. Produkcja obejmuje między innymi zbiorniki przepompowni ścieków i kompletne przepompownie, studzienki kanalizacyjne, wpusty uliczne syfonowe, separatorów ropopochodnych itp. wykonywane z tworzyw sztucznych, głównie z polietylenu. Podejmowanie tych działań ma za zadanie z jednej strony zabezpieczenie wzrastających potrzeb na tego typu materiały, a także ewentualne ograniczenie importu, a co za tym idzie obniżenie kosztów realizacji inwestycji sieci wodociągowych i kanalizacyjnych.

EN

In the paper the activity of Z.U.H. INSTALBUD-SZEPIELAK in Koszyce Wielkie near Tarnów as a producer of the building materials required for water and waste water disposal is presented. The range of production comprises: the tanks for sewage pump station, the pump stations, manholes, crude oil separators and so on - all made of plastic (mostly polyethylene).