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Publications tagged with [debris flow]
Total Items found:
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
Mainsant G.
,
Larose E.
et al.
Given that clay-rich landslides may become mobilized, leading to rapid mass movements (earthflows and debris flows), they pose critical problems in risk management worldwide. The most widely proposed mechanism leading to such flow-like movements is the increase ...
Filed under:
Engineering Geology -
Landslides
Reference:
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 117, F01030, doi:10.1029/2011JF002159, 2012
Abancó C.
,
Hürlimann M.
et al.
Debris flows are fast mass movements formed by a mix of water and solid materials, which occur in steep torrents, and are a source of high risks for human settlements. Geophones are widely used to detect the ground vibration induced by passing debris flows. ...
Filed under:
Engineering Geology -
Landslides
Reference:
Sensors 2012, 12, 4870-4891
This report presents an emergency assessment of potential debris-flow hazards from basins burned by the 2011 Motor fire in the Sierra and Stanislaus National Forests,Calif. Statistical-empirical models are used to estimate the probability and volume of debrisflowsthat ...
Filed under:
Engineering Geology -
Landslides
Reference:
Open-File Report 2011–1251
Water-related disasters most perceived by the public are those caused by large-scale riverine floods. There is evidence, however, that the most deadly events, which are driven by extreme precipitation, are those that are difficult to predict, such as debris ...
Filed under:
Engineering Geology -
Geological Hazards
Reference:
ASSOCIATED PROGRAMME ON FLOOD MANAGEMENT February 2011
Tillery A. C.
,
Darr M. J.
et al.
In June 2011, the Track Fire burned 113 square kilometers (km2) in Colfax County, northeastern New Mexico, and Las Animas County, southeasternColorado, including the upper watersheds of Chicorica and Raton Creeks. The burned landscape is now at risk of damage ...
Filed under:
Engineering Geology -
Landslides
Reference:
Open-File Report 2011–1257
Franzi L.
,
Giordan D.
et al.
The papers that are here presented and sum-marised represent the recent scientific contributions of someauthors coming from different countries and working in the fields of monitoring, modelling, mapping and design of mitigation measures against mass movements. ...
Filed under:
Engineering Geology -
Landslides
Reference:
Nat. Hazards Earth Syst. Sci., 11, 1583–1588, 2011
Hsu S. M.
,
Chiou L. B.
et al.
The objective of this study is to propose new approaches that can improve hazard zone delineationaccuracy and simulate hazard zones in response to different rainfall intensity. In this study, a two-dimensionalcommercial model FLO-2D, physically based and taking ...
Filed under:
Engineering Geology -
Landslides
Reference:
"Nat. Hazards Earth Syst. Sci., 10, 535-545, 2010"
Lagasse P. F.
,
Clopper P. E.
et al.
This report explores guidelines to help estimate the quantity of accumulated, flow event debris, based on the density and type of woody vegetation and river bank condition upstream and analytical procedures to quantify the effects of resulting debris-induced ...
Filed under:
Soil Mechanics -
Deep Foundations
Reference:
NCHRP Report 653, TRB
Hasegawa S.
,
Dahal R. K.
et al.
Geologically and tectonically active Himalayan Range is characterized by highly elevated mountains and deep river valleys. Because of steep mountain slopes, and dynamic geological conditions, large scale landslides are very common in Lesser and Higher Himalayan ...
Filed under:
Engineering Geology -
Landslides
Reference:
EnvironmentalGeology, 57(6):1423‐1434, 2009