Research of Dolní Zálezly - Dubický Kopec slope deformation, České středohoří Mts.

Result code in IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10192543" target="_blank" >RIV/00216208:11310/13:10192543 - isvavai.cz</a>

Alternative codes found

RIV/67985891:_____/13:00436229

Result on the web

<a href="http://www.geology.cz/zpravy/obsah/2012/Zpravy_2012-25.pdf" target="_blank" >http://www.geology.cz/zpravy/obsah/2012/Zpravy_2012-25.pdf</a>

DOI - Digital Object Identifier

—

Result language

čeština

Original language name

Výzkum svahové deformace Dolní Zálezly - Dubický kopec, České středohoří

Original language description

This paper presents first results of research of the slope deformation Dolní Zálezly - Dubický Hill. The site is situated in the morphologically distinct Labe/Elbe river valley between cities Lovosice and Ústí nad Labem. The locality is built by Tertiaryneovolcanites of České středohoří Mts. The main goal of the ongoing research is to evaluate detailed mapping and geodetic monitoring of the slope deformation, which is potentially danger of important transport communications and buildings. The slope deformation was developed by combination of rock fall and landslide activity probably in the last century. Potentially danger represents especially huge rock blocks in unconsolidated scree accumulation in the middle part of the slope. In this part were found the cracks with ice caves too. Selected morphometric characteristics were derived from DEM based on terrestrial laser scanning and trigonometric measurements.

Czech name

Výzkum svahové deformace Dolní Zálezly - Dubický kopec, České středohoří

Czech description

This paper presents first results of research of the slope deformation Dolní Zálezly - Dubický Hill. The site is situated in the morphologically distinct Labe/Elbe river valley between cities Lovosice and Ústí nad Labem. The locality is built by Tertiaryneovolcanites of České středohoří Mts. The main goal of the ongoing research is to evaluate detailed mapping and geodetic monitoring of the slope deformation, which is potentially danger of important transport communications and buildings. The slope deformation was developed by combination of rock fall and landslide activity probably in the last century. Potentially danger represents especially huge rock blocks in unconsolidated scree accumulation in the middle part of the slope. In this part were found the cracks with ice caves too. Selected morphometric characteristics were derived from DEM based on terrestrial laser scanning and trigonometric measurements.

Type

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

CEP classification

DE - Earth magnetism, geodesy, geography

OECD FORD branch

—

Project

<a href="/en/project/LM2010008" target="_blank" >LM2010008: CzechGeo/EPOS ? Distributed system of permanent observatory measurements and temporary monitoring of geophysical fields in the Czech Republic</a><br>

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

Zprávy o geologických výzkumech v roce 2012

ISSN

0514-8057

e-ISSN

—

Volume of the periodical

46.

Issue of the periodical within the volume

1.

Country of publishing house

CZ - CZECH REPUBLIC

Number of pages

5

Pages from-to

137-142

UT code for WoS article

—

EID of the result in the Scopus database

—