Formation and role of Neogene sediments from Tatra Mountains in the shaping of Czarna Orawa River alluvial plain

2012
journal article
article
dc.abstract.enThe paper presents researches that were conducted in Czarna Orawa River catchment, situated within the Tatra and Beskidy Mountains. Czarna Orawa River channel is segmental meandering system with the index of tortuosity up to 1.6. The aim of the article is to characterize gravels which were transported from the Tatra Mountains and their role in valley bottom formation. The gravels; originating from Beskidy and Tatra mountains, supply the alluvial cone of Czarny Dunajec. In Czarna Orawa Valley we meet coarser gravel (the Tatra Mountains gravel) and more angular than grains from the Beskidy Mountains. On the Holocene terraces in the valley gravel layer is 1-2 m thick. The grains are 1-6 cm in diameter and the biggest are found on the south bank (up to 20 cm). Between Jabłonka and Orawa Reservoir the change of petrographic composition is observed. Beneath Jabłonka village flysh gravels are common, and in the lower part, in the neighbourhoods of Orawa Reservoir, more than 55% are granites and gneisses. Gravel sediments are basic material building Holocene plain, showing fast erosional incision into the higher terrace levelpl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Geografii i Gospodarki Przestrzennejpl
dc.contributor.authorKrzaklewski, Paweł - 143486 pl
dc.date.accession2016-04-21pl
dc.date.accessioned2016-04-28T10:39:25Z
dc.date.available2016-04-28T10:39:25Z
dc.date.issued2012pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.number3pl
dc.description.physical41-46pl
dc.description.points9pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume31pl
dc.identifier.doi10.2478/v10117-012-0003-ypl
dc.identifier.eissn2081-6383pl
dc.identifier.issn2082-2103pl
dc.identifier.projectROD UJ / Ppl
dc.identifier.urihttp://ruj.uj.edu.pl/xmlui/handle/item/24756
dc.identifier.weblinkhttps://content.sciendo.com/view/journals/quageo/31/3/article-p41.xmlpl
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska*
dc.rights.licenceCC-BY-NC-ND
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/legalcode*
dc.share.typeotwarte czasopismo
dc.subtypeArticlepl
dc.titleFormation and role of Neogene sediments from Tatra Mountains in the shaping of Czarna Orawa River alluvial plainpl
dc.title.journalQuaestiones Geographicaepl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
The paper presents researches that were conducted in Czarna Orawa River catchment, situated within the Tatra and Beskidy Mountains. Czarna Orawa River channel is segmental meandering system with the index of tortuosity up to 1.6. The aim of the article is to characterize gravels which were transported from the Tatra Mountains and their role in valley bottom formation. The gravels; originating from Beskidy and Tatra mountains, supply the alluvial cone of Czarny Dunajec. In Czarna Orawa Valley we meet coarser gravel (the Tatra Mountains gravel) and more angular than grains from the Beskidy Mountains. On the Holocene terraces in the valley gravel layer is 1-2 m thick. The grains are 1-6 cm in diameter and the biggest are found on the south bank (up to 20 cm). Between Jabłonka and Orawa Reservoir the change of petrographic composition is observed. Beneath Jabłonka village flysh gravels are common, and in the lower part, in the neighbourhoods of Orawa Reservoir, more than 55% are granites and gneisses. Gravel sediments are basic material building Holocene plain, showing fast erosional incision into the higher terrace level
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Geografii i Gospodarki Przestrzennej
dc.contributor.authorpl
Krzaklewski, Paweł - 143486
dc.date.accessionpl
2016-04-21
dc.date.accessioned
2016-04-28T10:39:25Z
dc.date.available
2016-04-28T10:39:25Z
dc.date.issuedpl
2012
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.numberpl
3
dc.description.physicalpl
41-46
dc.description.pointspl
9
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
31
dc.identifier.doipl
10.2478/v10117-012-0003-y
dc.identifier.eissnpl
2081-6383
dc.identifier.issnpl
2082-2103
dc.identifier.projectpl
ROD UJ / P
dc.identifier.uri
http://ruj.uj.edu.pl/xmlui/handle/item/24756
dc.identifier.weblinkpl
https://content.sciendo.com/view/journals/quageo/31/3/article-p41.xml
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 3.0 Polska
dc.rights.licence
CC-BY-NC-ND
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-nd/3.0/legalcode
dc.share.type
otwarte czasopismo
dc.subtypepl
Article
dc.titlepl
Formation and role of Neogene sediments from Tatra Mountains in the shaping of Czarna Orawa River alluvial plain
dc.title.journalpl
Quaestiones Geographicae
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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