Geodynamic effects detected in the Stolowe Góry Mountains investigated originally for gravitational mass movements

Title:

Geodynamic effects detected in the Stolowe Góry Mountains investigated originally for gravitational mass movements

Creator:

Cacoń, Stefan, Blahoslav Košťák, and Mąkolski, Krzysztof

Identifier:

https://cdk.lib.cas.cz/client/handle/uuid:0ad818d5-2ee5-4eb7-9643-0a5614aebe04
uuid:0ad818d5-2ee5-4eb7-9643-0a5614aebe04
issn:1214-9705

Subject:

Geologie. Meteorologie. Klimatologie, geodynamika, národní parky, geodetické výpočty, geodynamics, national parks, geodetic networks, recent crust movements, tectonic processes, rock block displacements, table hills, precise levelling, gravity measurements, crack gauging, 7, and 551

Type:

article, články, model:article, and TEXT

Format:

print, bez média, and svazek

Description:

Rock block forms of the Szczeliniec Wielki (919 m a.s.l.) in the border area of the Stolowe Mountains massif originated due to various exogenous and endogenous pro cesses. The processes had started in the Upper Cretaceous, culminated in Late Tertiary, and continue till the present day with much lower intensity. Such processes were indica ted by historical earthquakes and different tectonic events in the Sudeten Mountains and adjacent areas. Results of geodetic geodynamic studies are presented. Several sectors of the Sudeten Mountains which include the Table Hills - Stolowe Mountains, show horizontal and vertical movements. Results of periodic precise levelling in three geodetic micro-networks established on the Szczeliniec Wielki: "Przy Schronisku", "Piekielko" and "Tarasy Poludniowe / Schody" are presented. Investigations have been augmented wit h TM-71 crack gauging in rock blocks. These studies started in 1972 increasing gradually effectiveness of monitoring. Levelling changes, as well as displaceme nts resulting from 3D monthly records of three TM-71 crack gauges have been confronted with recent investigations into tectonic micro-deformations along the Sudeten Fault in the Bohemian Massif. It is suggested that aseismic geotectonic processes participated in the deformations found in investigated networks., Stefan Cacoń, Blahoslav Košťák and Krzysztof Mąkolski., and Obsahuje bibliografické odkazy

Language:

English

Rights:

http://creativecommons.org/licenses/by-nc-sa/4.0/
policy:public

Source:

Acta geodynamica et geomaterialia : | 2012 Volume:9 | Number:4 (168)

Harvested from:

CDK

Metadata only:

false