Editorial Board

+Volume 56, issue 2, 2023

+Volume 56, issue 1, 2023

+Volume 55, issue 2, 2022

+Volume 55, issue 1, 2022

+Volume 54, issue 2, 2021

+Volume 54, issue 1, 2021

+Volume 53, issue 2, 2020

+Volume 53, issue 1, 2020

+Volume 52, issue 2, 2019

+Volume 52, issue 1, 2019

+Volume 51, issue 2, 2018

+Volume 51, issue 1, 2018

+Volume 50, issue 2, 2017

+Volume 50, issue 1, 2017

+Volume 49, 2016

+Volume 48, 2015 (GRR for 2014)

+Volume 47, 2014 (GRR for 2013)

+Volume 46, 2013 (GRR for 2012)

+Volume 45, 2012 (GRR for 2011)

+Volume 44, 2011 (GRR for 2010)

+Volume 43, 2010 (GRR for 2009)

+Volume 42, 2009 (GRR for 2008)

+Volume 41, 2008 (GRR for 2007)

–Volume 40, 2007 (GRR for 2006)

Regional Geology and Stratigraphy

Quaternary, Engineering Geology

Mineralogy, Petrology, Geochemistry

Research Abroad

Building and Decorative Stones

Mineral Deposits

Radioactive Wastes

+Volume 39, 2006 (GRR for 2005)

+Volume 38, 2005 (GRR for 2004)

+Volume 37, 2004 (GRR for 2003)

+Volume 36, 2003 (GRR for 2002)

+Volume 35, 2002 (GRR for 2001)

+Volume 34, 2001 (GRR for 2000)

+Volume 33, 2000 (GRR for 1999)

+Volume 32, 1999 (GRR for 1998)

+Volume 31, 1998 (GRR for 1997)

+Volume 30, 1997 (GRR for 1996)

+Volume 29, 1996 (GRR for 1995)

+Volume 28, 1995 (GRR for 1994)

+Volume 27, 1994 (GRR for 1993)

+Volume 26, 1993 (GRR for 1992)

+Volume 25, 1993 (GRR for 1991)

Publisher © Czech Geological Survey, ISSN: 2336-5757 (online), 0514-8057 (print)

Disruption of Ondřejník Hill synclinal chine in Podbeskydy hully country

Jan Rybář, Vít Janoš, Jan Klimeš, Tomáš Nýdl

Geoscience Research Reports 40, 2007 (GRR for 2006), pages 92–96

Keywords: Landslide inventory, deep seated creep, sliding, flow

Map sheets: Bělá nad Radbuzou (21-21), Holýšov (21-22)

Full text (PDF, 0.39 MB)

Abstract

The study concerns slope development in the geomorphological region of Ondřejník Hill in Podbeskydy hilly country. Engineering-geological maps 1:10 000 of stability conditions and derived prognostic slope movement susceptibility maps were prepared. The most extensive and complex landslide area was found on slopes oriented to the East. There is a characteristic phenomenon of the Ondřejník deformation - disruption of a flat field at the synclinal chine where even a graben-like structure developed.