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Publications tagged with [rockfall hazard]
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<p>Using a dataset of preexisting mapped landslides, we create two maps that provide a firstorder approximation of rockfall susceptibility for the state of New Mexico. In natural hazard assessments, the term 'susceptibility' is used to describe the natural ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
New Mexico Bureau of Geology and Mineral Resources Open-file Report 595
Rockyfor3D is a simulation model that calculates trajectories of single, individually falling rocks, in three dimensions (3D). The model combines physically-based, deterministic algorithms with stochastic approaches, which makes Rockyfor3D a so-called ‘probabilistic ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Dorren L.K.A., 2015. Rockyfor3D (v5.2) revealed –Transparent description of the complete 3D rockfall model. ecorisQ paper (www.ecorisq.org): 32p., date 25.01.2015
The paper deals with the assessment of the rockfall risk for a road stretch, in southern Italy, affected by high traffic intensity. Three qualitative rockfall risk rating systems (QRSs) which use an exponential scoring with a base of 3 were employed, and then ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Nat. Hazards Earth Syst. Sci., 13, 1643–1653, 2013
Guerin Α.
,
Rossetti J.-P.
et al.
Terrestrial Laser Scanner has been used to detect rock falls which have occurred in a limestone cliff during some years, in the difficult configuration of the Subalpine Chains. In a rock wall of width 750m and height 200 m, 130 rock falls larger than 0.1 ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
"First International Conference on Landslides Risk, Tabarka : Tunisia (2013)
Horton P.
,
Jaboyedoff M.
et al.
The development of susceptibility maps for debris flows is of primary importance due to population pressure in hazardous zones. However, hazard assessment by processbased modelling at a regional scale is difficult due to the complex nature of the phenomenon, ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Nat. Hazards Earth Syst. Sci., 13, 869–885, 2013
Lekkas E.
,
Alexoudi V.
et al.
<p>The Teleferik area of Santorini Volcanic Complex, is characterized by rockfall risk due to existing morphological, geological, geotechnical and geodynamic conditions. It is therefore considered a high risk area because of the huge number, in annual base, ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Bulletin of the Geological Society of Greece, vol. XLVII 2013 Proceedings of the 13 th International Congress, Chania, Sept. 2013
<p>The geological structure of Greece (frequent occurrence of rock formations, existence of faults and fracturing of rocks), the steep topography and mountainous terrain as well as its high seismicity, creates a significant rockfall hazard. During the last ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Bulletin of the Geological Society of Greece, vol. XLVII 2013 Proceedings of the 13th International Congress, Chania, Sept. 2013
Christchurch City Council requested GNS Science to carry out geomorphic mapping of the near-surface materials and processes present in the Port Hills of Christchurch. The purpose of this work is to provide information relating to near-surface geological materials ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
GNS Science Consultancy Report 2012/15. 21 p + maps (91 p)
Rock falls from cliffs and other steep slopes present numerous challenges for detailed geological characterization. In steep terrain, rock-fall source areas are both dangerous and difficult to access, severely limiting the ability to make detailed structural ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
GeoCongress 2012 © ASCE 2012
Walter M.
,
Schwaderer U.
et al.
In this study we describe the seismic analysis of precursory patterns of a rockfall in the “Rappenlochschlucht”, a gorge located in the Vorarlberg Alps, Austria. The rockfall with an estimated volume of 15 000m<sup>3</sup> occurred on 10 May 2011 (10:48:43 ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Nat. Hazards Earth Syst. Sci., 12, 3545–3555, 2012