Your single point of reference for all your Geotechnical Inquiries

Publications by [Harp E. L.]

Total Items found:
<p>At least 135 rock falls have occurred from Glacier Point in Yosemite Valley since 1870. Rock falls in 1996 and 1998&ndash;1999 led to hypotheses that these events were triggered by water system discharges from visitor facilities (leachfield and storage ...
Filed under: Rock Mechanics -  Rock Falls
Reference: Landslides and Engineered Slopes: Protecting Society through. Improved Understanding – Eberhardt et al. (eds) © 2012 Taylor & Francis Group, London, ISBN 978-0-415-62123-6
Shaking from the January 12, 2010, Haiti earthquake (M 7.0) caused devastating structural damage and triggered many landslides that blocked roads, dammed rivers and streams, and threatened infrastructure in many parts of Haiti. The earthquake had a complex ...
Reference: Open-File Report 2011–1023
Progressive rock-fall failures in natural rock slopes are common in many environments, but often elude detailed quantitative documentation and analysis. Here we present high-resolution photography, video, and laser scanning data that document spatial and temporal ...
Filed under: Rock Mechanics -  Rock Falls
Reference: EARTH SURFACE PROCESSES AND LANDFORMS Earth Surf. Process. Landforms (2011)
The 8 October 2005 Kashmir earthquake triggered several thousand landslides. These were mainly rock falls and debris falls, although translational rock and debris slides also occurred. In addition, a sturzstrom (debris avalanche) comprising ∼80 million m3 ...
Reference: Geomorphology 94 (2008) 1–9
<p>We examine rockfall susceptibility of folded strata in the Sevier fold-thrust belt exposed in American Fork Canyon in north-central Utah. Large-scale geologic mapping, talus production data, rock-mass-quality measurements, and historical rockfall data indicate ...
Filed under: Rock Mechanics -  Rock Falls
Reference: Nat. Hazards Earth Syst. Sci., 7, 1–14, 2007
The October 8, 2005, Kashmir earthquake (M 7.6) triggered several thousand landslides, mainly rock falls and rock slides, in the epicentral area near the cities of Muzafarrabad and Balakot, Pakistan. Most of these were shallow, coalescing rock slides emanating ...
Reference: USGS Open-File Report 2006–1052