All

What are you looking for?

All
Projects
Results
Organizations

Quick search

  • Projects supported by TA ČR
  • Excellent projects
  • Projects with the highest public support
  • Current projects

Smart search

  • That is how I find a specific +word
  • That is how I leave the -word out of the results
  • “That is how I can find the whole phrase”

Geomorphological and sedimentary evidence of probable glaciation in the Jizerské hory Mountains, Central Europe

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F17%3A10332394" target="_blank" >RIV/00216208:11310/17:10332394 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.geomorph.2016.12.008" target="_blank" >http://dx.doi.org/10.1016/j.geomorph.2016.12.008</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.geomorph.2016.12.008" target="_blank" >10.1016/j.geomorph.2016.12.008</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Geomorphological and sedimentary evidence of probable glaciation in the Jizerské hory Mountains, Central Europe

  • Original language description

    The Jizerské hory Mountains in the Czech Republic have traditionally been considered to be a highland that lay beyond the limits of Quaternary glaciations. Recent work on cirque-like valley heads in the central part of the range has shown that niche glaciers could form during the Quaternary. Here we report geomorphological and sedimentary evidence for a small glacier in the Pytlácká jáma Hollow that represents one of the most-enclosed valley heads within the range. Shape and size characteristics of this landform indicate that the hollow is a glacial cirque at a degraded stage of development. Boulder accumulations at the downslope side of the hollow probably represent a relic of terminal moraines, and the grain size distribution of clasts together with micromorphology of quartz grains fromthe hollowindicate the glacial environment of a small glacier. This glacier represents the lowermost located such systemin central Europe and provides evidence for the presence of niche or small cirque glaciers probably during pre-Weichselian glacial periods. The glaciation limit (1000 m asl) and paleo-ELA (900 m asl) proposed for the Jizerské hory Mountains implies that central European ranges lower than 1100 m asl were probably glaciated during the Quaternary.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10508 - Physical geography

Result continuities

  • Project

    <a href="/en/project/GAP209%2F10%2F0519" target="_blank" >GAP209/10/0519: Paleogeographic reconstruction of Quaternary deglaciation in mountain areas of the Bohemian Massif</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2017

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Geomorphology

  • ISSN

    0169-555X

  • e-ISSN

  • Volume of the periodical

    neuveden

  • Issue of the periodical within the volume

    280

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    12

  • Pages from-to

    39-50

  • UT code for WoS article

    000393931400004

  • EID of the result in the Scopus database

    2-s2.0-85006152390