Zobrazeno 1 - 10
of 38
pro vyhledávání: '"Mihael Ribičič"'
Publikováno v:
Geologija, Vol 52, Iss 1, Pp 87-104 (2009)
For the area of Slovenia (20.000 sqr. km) a debris-flow susceptibility model at scale 1 : 250,000 was produced.To calculate the susceptibility to debris-flow occurence using GIS several information layers were used such as geology (lithology and dist
Externí odkaz:
https://doaj.org/article/d96656cf562446b8be886e332033b887
Publikováno v:
Geologija, Vol 50, Iss 2, Pp 393-402 (2007)
The Slovenian territory is, geologically speaking, very diverse and mainly composed of sediments or sedimentary rocks. Slope mass movements occur almost in all parts of the country. In the Alpine carbonate areas of the northern part of Slovenia rock
Externí odkaz:
https://doaj.org/article/790346dc3f554efa81e51a868f5e4aa2
Autor:
Marko Komac, Mihael Ribičič
Publikováno v:
Geologija, Vol 49, Iss 2, Pp 295-309 (2006)
Based on the extensive landslide database that was compiled and standardised at the national level, and analyses of landslide spatial occurrence, a Landslide susceptibility map of Slovenia at scale 1 : 250,000 was completed. Altogether more than 6,60
Externí odkaz:
https://doaj.org/article/fe5f0b93c997418f8f99d54397049c60
Publikováno v:
Acta Geographica Slovenica, Vol 45, Iss 2, Pp 93-120 (2005)
The paper gives an overview of the literature on available computer (simulation) models of stone falls and rockfalls, divided into 2D and 3D models. 2D models consider single blocks in the rock-fall mass as lumped mass or a rigid body, and are used t
Externí odkaz:
https://doaj.org/article/0a1da797460544e5b7fc95f069d383c6
Publikováno v:
Geologija, Vol 48, Iss 2, Pp 341-354 (2005)
In the framework of the new Slovenian methodology for determining hazard areas and the classification of land parcels into hazard classes due to land slides and rock falls, a pilot project was carried out on the regional road between Bovec and Vr{i~
Externí odkaz:
https://doaj.org/article/49f3752c5987478f8daed593b19f97c2
Publikováno v:
Geologija, Vol 48, Iss 1, Pp 33-51 (2005)
Theoretical basis and practical legislation (Water Law and regulation acts) would allow in future the determination and classification of endangered territorial zones due to various natural hazards, among them also due to rock collapse and rockfall h
Externí odkaz:
https://doaj.org/article/7a7993a5bb424a95a74b5ed432ed1f54
Autor:
Mihael Ribičič, Renato Vidrih
Publikováno v:
Geologija, Vol 47, Iss 2, Pp 199-220 (2004)
After six years on July 12, 2004 a new earthquake shook again the most seismic dangerous part of Slovenia – the upper Soča valley. This earthquake was about ten times weaker then the earthquake from April 12, 1998. The earthquake was triggered at
Externí odkaz:
https://doaj.org/article/ba7eaccfedf94839b3f6f58af058adae
Autor:
Marko Kočevar, Mihael Ribičič
Publikováno v:
Geologija, Vol 46, Iss 1, Pp 159-166 (2003)
Larger rock falls frequently cause additional secondary phenomena. A lot of them occured after rock fall which happened above Kose~ near Kobarid. Rock fall arose from rock slide, which is even now moving with velocity of 1.2 m per month. The cinetic
Externí odkaz:
https://doaj.org/article/5e04eb587b124c489cd9e9857be6ef81
Autor:
Mihael Ribičič, Marko Kočevar
Publikováno v:
Geologija, Vol 45, Iss 2, Pp 525-530 (2002)
The remediation of such landslide as Slano blato more then 1300 m long and about 1.000.000 m3 of the volume, is very demanding. In the function of water contents the landslide behave as viscosious mud flow when the sliding masses are completely satur
Externí odkaz:
https://doaj.org/article/4b642f700a464435b5363acd73685e1a
Autor:
Marko Kočevar, Mihael Ribičič
Publikováno v:
Geologija, Vol 45, Iss 2, Pp 427-432 (2002)
Landslide Slano blato (Salty mud) is located under the Čaven Mountain on the slope cut by many steep mountains streams and gorges. Creeping at the area of Slano blato started on 18th of November 2000. Creep area is an old landslide. Landslide is 129
Externí odkaz:
https://doaj.org/article/10d73886cdb9427a81cd713c6b28b792