Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)

The Suchedniów water reservoir is located in the central section of the River Kamionka in the northern part of the Holy Cross Mountains of central Poland. This area once belonged to the Old Polish Industrial District that, during the Middle Ages, was very intensively developed by iron metallurgy. Ma...

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Main Authors: Przepióra Paweł, Kalicki Tomasz, Aksamit Michał, Biesaga Piotr, Frączek Marcin, Grzeszczyk Paulina, Malęga Emanuela, Chrabąszcz Mariusz, Kłusakiewicz Edyta, Kusztal Piotr
Format: Article
Language:English
Published: Sciendo 2019-08-01
Series:Geologos
Subjects:
Online Access:https://doi.org/10.2478/logos-2019-0013
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author Przepióra Paweł
Kalicki Tomasz
Aksamit Michał
Biesaga Piotr
Frączek Marcin
Grzeszczyk Paulina
Malęga Emanuela
Chrabąszcz Mariusz
Kłusakiewicz Edyta
Kusztal Piotr
author_facet Przepióra Paweł
Kalicki Tomasz
Aksamit Michał
Biesaga Piotr
Frączek Marcin
Grzeszczyk Paulina
Malęga Emanuela
Chrabąszcz Mariusz
Kłusakiewicz Edyta
Kusztal Piotr
author_sort Przepióra Paweł
collection DOAJ
description The Suchedniów water reservoir is located in the central section of the River Kamionka in the northern part of the Holy Cross Mountains of central Poland. This area once belonged to the Old Polish Industrial District that, during the Middle Ages, was very intensively developed by iron metallurgy. Many forges and mills along the rivers used water power, which led to the construction of an anthropogenic, small-scale water retention system. At the beginning of the twentieth century many of these reservoirs were drained after the collapse of metallurgical activities. The present-day reservoir was built in 1974 and drained in 2017. Research into the drained basin has documented various forms and sediments, some of which record present-day depositional processes (fire proof clay layer, inland fan delta), while others represent the historical period (lacustrine sediments of older reservoirs). Traces of catastrophic events have been preserved as well; an assemblage of megaripples marks the sudden drainage caused by a dam break in 1974.
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spelling doaj.art-b209a0e8b10d4cd9b8fca32d1e29bff22022-12-21T21:26:06ZengSciendoGeologos2080-65742019-08-0125213915210.2478/logos-2019-0013logos-2019-0013Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)Przepióra Paweł0Kalicki Tomasz1Aksamit Michał2Biesaga Piotr3Frączek Marcin4Grzeszczyk Paulina5Malęga Emanuela6Chrabąszcz Mariusz7Kłusakiewicz Edyta8Kusztal Piotr9Institute of Geography, Jan Kochanowski University in Kielce, PolandInstitute of Geography, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandInstitute of Geography, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandStudent Science Club of Geomorphologists „Złoty Bażant”, Jan Kochanowski University in Kielce, PolandThe Suchedniów water reservoir is located in the central section of the River Kamionka in the northern part of the Holy Cross Mountains of central Poland. This area once belonged to the Old Polish Industrial District that, during the Middle Ages, was very intensively developed by iron metallurgy. Many forges and mills along the rivers used water power, which led to the construction of an anthropogenic, small-scale water retention system. At the beginning of the twentieth century many of these reservoirs were drained after the collapse of metallurgical activities. The present-day reservoir was built in 1974 and drained in 2017. Research into the drained basin has documented various forms and sediments, some of which record present-day depositional processes (fire proof clay layer, inland fan delta), while others represent the historical period (lacustrine sediments of older reservoirs). Traces of catastrophic events have been preserved as well; an assemblage of megaripples marks the sudden drainage caused by a dam break in 1974.https://doi.org/10.2478/logos-2019-0013sedimentologylacustrine sedimentsfan deltamegaripplesanthropogenic pond
spellingShingle Przepióra Paweł
Kalicki Tomasz
Aksamit Michał
Biesaga Piotr
Frączek Marcin
Grzeszczyk Paulina
Malęga Emanuela
Chrabąszcz Mariusz
Kłusakiewicz Edyta
Kusztal Piotr
Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
Geologos
sedimentology
lacustrine sediments
fan delta
megaripples
anthropogenic pond
title Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
title_full Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
title_fullStr Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
title_full_unstemmed Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
title_short Secular and catastrophic processes reflected in sediments of the Suchedniów water reservoir, Holy Cross Mountains (Poland)
title_sort secular and catastrophic processes reflected in sediments of the suchedniow water reservoir holy cross mountains poland
topic sedimentology
lacustrine sediments
fan delta
megaripples
anthropogenic pond
url https://doi.org/10.2478/logos-2019-0013
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