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A case study of shallow landslide occurrence and magnitude-frequency due to rainfall events after earthquakes in northwestern California /Hayhurst, Cheryl A. January 1900 (has links)
Thesis (M.S.)--Humboldt State University, 2006. / Includes bibliographical references (leaves 42-46). Also available via Humboldt Digital Scholar.
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Drowned and partially drowned landslide deposits off Tai O and their engineering implicationTam, Chi-kan., 譚志勤. January 2000 (has links)
published_or_final_version / abstract / toc / Applied Geosciences / Master / Master of Science
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A comparative analysis of emergent group behavior in disaster : a look at the United States and Sweden /Neal, David Miller January 1985 (has links)
No description available.
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The prediction of ground sliding induced by strong earthquakesSrbulov, Milutin January 1994 (has links)
No description available.
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Progressive failure as a possible mechanism of deep-seated failures insaprolite cut slopes in Hong KongTsang, Lai-yan, Ada., 曾麗欣. January 2001 (has links)
published_or_final_version / Applied Geosciences / Master / Master of Science
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Loess and loess instability in north ChinaMeng, Xing - Min January 1998 (has links)
No description available.
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The geochemistry of pyritic shale weathering within an active landslideVear, Alwyn January 1981 (has links)
Intense chemical weathering accompanies physical instability at the site of a repeatedly active landslide in North Derbyshire. In order to describe and quantify the chemical weathering, a programme of water sampling and analysis was devised. A sequence of reactions are proposed, based on theresults of this work, to account for the observed concentrations of chemical species in the drainage waters. It is thought that pyrite oxidation, accelerated by the presence of catalytic bacteria, is responsible for the considerable acidity of these waters. Additional reactions involving carbonates and silicates occur at strictly comparable rates and consume over 99% of the acidity prior to the water's emergence in a number of ochre-precipitating springs. Analysis of the solid reactants and products confirms the suggested sequence of events and suggests a number of ways in which chemical weathering might be related to slope stability. Clay minerals appear to be little affected by weathering, and the growth of precipitate minerals such as gypsum in joints and on bedding planes might be a more important mechanism in shale breakdown. After this initial rapid physical disintegration, chemical weathering, at the surface, proceeds relatively slowly. Chemical processes build up stresses within the rocks and possibly help to maintain any inherent planes of weakness. Ultimately landslide movement is triggered by increases in porewater pressures brought about by fluctuations in local ground water levels.
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Geotechnical analysis of horizontal drains as a landslide mitigation method in western Washington /McKay, Sara E. January 2006 (has links)
Thesis (M.S.)--University of Nevada, Reno, 2006. / "August, 2006." Includes bibliographical references (leaves 93-97). Library also has microfilm. Ann Arbor, Mich. : ProQuest Information and Learning Company, [2006]. 1 microfilm reel ; 35 mm. Online version available on the World Wide Web.
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Relationship between geology and spatial distribution of landslidesLo, Ming-yan., 老明恩. January 2010 (has links)
published_or_final_version / Applied Geosciences / Master / Master of Science
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Remedies for landslides and slips on the Kanawha and Michigan RyBlack, Ralph Peters 08 1900 (has links)
No description available.
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