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The evaluation of geological structures by the vector analysis of valley axes

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00088382%3A_____%2F14%3AN0000001" target="_blank" >RIV/00088382:_____/14:N0000001 - isvavai.cz</a>

  • Result on the web

    <a href="https://www.schweizerbart.de/papers/zfg/detail/58/82764/The_evaluation_of_geological_structures_by_the_vector_analysis_of_valley_axes" target="_blank" >https://www.schweizerbart.de/papers/zfg/detail/58/82764/The_evaluation_of_geological_structures_by_the_vector_analysis_of_valley_axes</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1127/0372-8854/2013/0113" target="_blank" >10.1127/0372-8854/2013/0113</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    The evaluation of geological structures by the vector analysis of valley axes

  • Original language description

    The paper describes the methodology of evaluating geological structures by the vector analysis of valley axes. Both geological structures and valley axes were determined by the azimuth and the dip which corresponds with the angle of the slope in the selected catchment in the central Czech Republic. The determination of the dip of valley axes has formed a base for the quantitative classification of valley axes analogous to geological structures. The following five types of valley axes were distinguished: sub-horizontal, gently inclined, moderately inclined, steeply inclined and sub-vertical. The orientations of both the valley axes and the geological structures were evaluated by the construction of outline diagrams in the programme Spheristat. The directions of valley axes were compared with geological structures by the statistical relationship using the chi square test. The directions of sub-horizontal valley axes correspond with the dip azimuth of foliations in contrast to the dip azimuth of joints in the model area. The evaluation of geological structures by the vector analysis of valley axes is practicable in all kinds of landscape.

  • 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

    10505 - Geology

Result continuities

  • Project

  • Continuities

    V - Vyzkumna aktivita podporovana z jinych verejnych zdroju

Others

  • Publication year

    2014

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Zeitschrift für Geomorphologie

  • ISSN

    0372-8854

  • e-ISSN

    1864-1687

  • Volume of the periodical

    58

  • Issue of the periodical within the volume

    2

  • Country of publishing house

    DE - GERMANY

  • Number of pages

    15

  • Pages from-to

    201-215

  • UT code for WoS article

    000337116900005

  • EID of the result in the Scopus database

    2-s2.0-84973467738