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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Language: | English |
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Sciendo
2019-08-01
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Series: | Geologos |
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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. |
first_indexed | 2024-12-18T01:10:34Z |
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id | doaj.art-b209a0e8b10d4cd9b8fca32d1e29bff2 |
institution | Directory Open Access Journal |
issn | 2080-6574 |
language | English |
last_indexed | 2024-12-18T01:10:34Z |
publishDate | 2019-08-01 |
publisher | Sciendo |
record_format | Article |
series | Geologos |
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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