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Publications tagged with [rockfalls]
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<p>Ermenek is one of the curious settlement areas because of its topographical features in Karaman (Turkey). The city is located in northern side of the very steep cliffs formed by jointed limestone which are suddenly increased from 1250m to 1850 m. Moreover, ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Nat. Hazards Earth Syst. Sci. Discuss., doi:10.5194/nhess-2015-337, 2016 Manuscript under review for journal Nat. Hazards Earth Syst. Sci. Published: 19 January 2016
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
<p>This paper describes landslides and slope stability evaluation in the urban area of Kruja, Albania. Kruja is a historical and heritage center, due to the existence of many important cultural monuments, including “Skanderbeg” castle and Bazaar ...
Filed under:
Rock Mechanics -
Rock Slope Stability
Reference:
Nat. Hazards Earth Syst. Sci., 14, 545–556, 2014
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
Ferrari F.
,
Gianni G. P.
et al.
Rockfalls frequently occur in Alpine areas, creating serious risks to population and buildings; the protection measures against rockfalls cannot be adequately designed unless the comprehensive understanding of rockfall phenomenon. Some experimental rockfall ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
IJEGE.2013-06.B-13
Ferrari F.
,
Gianni G. P.
et al.
<p>In this paper results of experimental field tests carried out on a scree slope, located in Northern Italy, are presented. On Alpine talus cones the motion of blocks is typically characterized by impacts and rebounds, which in modelling are described using ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Rend. Online Soc. Geol. It., Vol. 24 (2013), pp. 122-124, 1 fig.
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)
The protective effect of forests against rockfall cannot be neglected in risk management. This is, of course, under the condition that a considerable slope length in the transit area is forested and that a tree diameter distribution which can provide sufficient ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Landslides and engineered slopes: protecting society through improved understanding. Taylor and Francis Group, London: pp 117 – 127.
Potentially, increasing rockfall hazards triggered by climate change are a major concern expressed both in scientific and non-scientific media. An existing rockfall inventory for Austria including 252 events from ca. 1900 to 2010, mainly from non-permafrost ...
Filed under:
Rock Mechanics -
Rock Falls
Reference:
Nat. Hazards Earth Syst. Sci., 12, 3209–3216, 2012