Písečník Hill near Javorník ? drumlin with preserved subglacial and supraglacial succession of sediments

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F13%3A00000196" target="_blank" >RIV/00025798:_____/13:00000196 - isvavai.cz</a>

Result on the web

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DOI - Digital Object Identifier

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Result language

čeština

Original language name

Písečník u Javorníku ? drumlin se zachovalou sukcesí subglaciálních a supraglaciálních sedimentů

Original language description

Písečník Hill is an isolated elevation located near the Javorník town close to the NE foothill of the main ridge of the Rychleby Mts. (Eastern Sudetes). It has a shape of a ridge elongated in the SE?NW direction, made of compacted Miocene sands covered by Pleistocene glacial sediments. Glacial sediments have been deposited during the Elsterian glaciation. The presented study is aimed at the interpretation of the evolution of the Písečník Hill linked to continental glaciation. Facies description has beensupplemented by petrological analyses. The glacial sequence is composed of five members. The first one is a lodgement till (Jk1), which followed the erosional phase producing elongated scours. Glacitectonic features, such as plucking of underlying Miocene sands and formation of rip-up clasts could be seen in the lodgement till unit. Boulder lag with boulders up to 2 m long originated by blocking of large clasts in compact, plastic, unlithified basement. The second member (Jk2) is a mass

Czech name

Písečník u Javorníku ? drumlin se zachovalou sukcesí subglaciálních a supraglaciálních sedimentů

Czech description

Písečník Hill is an isolated elevation located near the Javorník town close to the NE foothill of the main ridge of the Rychleby Mts. (Eastern Sudetes). It has a shape of a ridge elongated in the SE?NW direction, made of compacted Miocene sands covered by Pleistocene glacial sediments. Glacial sediments have been deposited during the Elsterian glaciation. The presented study is aimed at the interpretation of the evolution of the Písečník Hill linked to continental glaciation. Facies description has beensupplemented by petrological analyses. The glacial sequence is composed of five members. The first one is a lodgement till (Jk1), which followed the erosional phase producing elongated scours. Glacitectonic features, such as plucking of underlying Miocene sands and formation of rip-up clasts could be seen in the lodgement till unit. Boulder lag with boulders up to 2 m long originated by blocking of large clasts in compact, plastic, unlithified basement. The second member (Jk2) is a mass

Type

J_x - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

CEP classification

DB - Geology and mineralogy

OECD FORD branch

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Project

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Continuities

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Publication year

2013

Confidentiality

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Name of the periodical

Geologické výzkumy na Moravě a ve Slezsku

ISSN

1212-6209

e-ISSN

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Volume of the periodical

20

Issue of the periodical within the volume

podzim

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

8

Pages from-to

18-25

UT code for WoS article

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EID of the result in the Scopus database

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