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- Landslides_vs._Rock_strength abstract "Landslides are a major geologic hazard in many locations around the globe. They are considered a mass-wasting process, the most common of which are debris flows, hill slides, and rock falls. These events can take place over the course of several years of creeping but powerful movement, or in a matter of a few devastatingly destructive moments. There are several factors relating to structural geology that correlate directly to landslide occurrences. One major factor pertaining to landslides is rock strength. Rock strength is defined by stress/strain relationships, pore fluid pressure, and confining pressure. Stronger, more dense rocks are not as likely to be involved in a rock slide or landslide than porous less dense rocks that can be easily saturated with water. In Utah the groundwater level is continually fluctuating, making the area particularly susceptible to landslides. As water saturates the ground, making it softer and heavier, the stress/strain relationships experienced by the rocks increases considerably. The strength of a rock can be defined by its Mohr Circle, and its corresponding failure envelope. Once conditions are reached which place a rock over its failure envelope, it will experience deformation.There are two main types of deformation which rocks undergo and both are pertinent to landslides. If a rock behaves elastically and experiences micro fractures involved with tiny slip movements in the rock, cohesive strength is still somewhat maintained, and a slide might be temporarily prevented. However, if a rock undergoes brittle deformation and breaks into pieces, a landslide is much more likely to occur. Stress and strain conditions associated with rocks and their failure envelopes differ between rock types, but they have been studied extensively in laboratories because the implications of these data have relevance in every scope of geology.".
- Landslides_vs._Rock_strength thumbnail LS-usgs.gif?width=300.
- Landslides_vs._Rock_strength wikiPageExternalLink thistle.htm.
- Landslides_vs._Rock_strength wikiPageExternalLink index.htm.
- Landslides_vs._Rock_strength wikiPageExternalLink IMWA2005_072_Li.pdf.
- Landslides_vs._Rock_strength wikiPageID "31440196".
- Landslides_vs._Rock_strength wikiPageLength "7840".
- Landslides_vs._Rock_strength wikiPageOutDegree "16".
- Landslides_vs._Rock_strength wikiPageRevisionID "616594833".
- Landslides_vs._Rock_strength wikiPageWikiLink Category:Environmental_soil_science.
- Landslides_vs._Rock_strength wikiPageWikiLink Category:Geological_processes.
- Landslides_vs._Rock_strength wikiPageWikiLink Category:Landslides.
- Landslides_vs._Rock_strength wikiPageWikiLink Confining_pressure.
- Landslides_vs._Rock_strength wikiPageWikiLink Debris_flow.
- Landslides_vs._Rock_strength wikiPageWikiLink Debris_flows.
- Landslides_vs._Rock_strength wikiPageWikiLink Landslide.
- Landslides_vs._Rock_strength wikiPageWikiLink Mohrs_Circle.
- Landslides_vs._Rock_strength wikiPageWikiLink Mohrs_circle.
- Landslides_vs._Rock_strength wikiPageWikiLink Mohr–Coulomb_theory.
- Landslides_vs._Rock_strength wikiPageWikiLink Mudflow.
- Landslides_vs._Rock_strength wikiPageWikiLink Mudslides.
- Landslides_vs._Rock_strength wikiPageWikiLink Overburden_pressure.
- Landslides_vs._Rock_strength wikiPageWikiLink Pore_fluid_pressure.
- Landslides_vs._Rock_strength wikiPageWikiLink Pore_water_pressure.
- Landslides_vs._Rock_strength wikiPageWikiLink Rock_slide.
- Landslides_vs._Rock_strength wikiPageWikiLink Shale.
- Landslides_vs._Rock_strength wikiPageWikiLink Stress-strain_curve.
- Landslides_vs._Rock_strength wikiPageWikiLink Stress–strain_curve.
- Landslides_vs._Rock_strength wikiPageWikiLink Thistle,_Utah.
- Landslides_vs._Rock_strength wikiPageWikiLink File:Cedar_Hills_Landslide.jpg.
- Landslides_vs._Rock_strength wikiPageWikiLink File:LS-usgs.gif.
- Landslides_vs._Rock_strength wikiPageWikiLink File:Thistle_2010_from_US6_rest_area.JPG.
- Landslides_vs._Rock_strength hasPhotoCollection Landslides_vs._Rock_strength.
- Landslides_vs._Rock_strength wikiPageUsesTemplate Template:Orphan.
- Landslides_vs._Rock_strength wikiPageUsesTemplate Template:Reflist.
- Landslides_vs._Rock_strength subject Category:Environmental_soil_science.
- Landslides_vs._Rock_strength subject Category:Geological_processes.
- Landslides_vs._Rock_strength subject Category:Landslides.
- Landslides_vs._Rock_strength hypernym Hazard.
- Landslides_vs._Rock_strength type Article.
- Landslides_vs._Rock_strength type Lighthouse.
- Landslides_vs._Rock_strength type Article.
- Landslides_vs._Rock_strength comment "Landslides are a major geologic hazard in many locations around the globe. They are considered a mass-wasting process, the most common of which are debris flows, hill slides, and rock falls. These events can take place over the course of several years of creeping but powerful movement, or in a matter of a few devastatingly destructive moments. There are several factors relating to structural geology that correlate directly to landslide occurrences.".
- Landslides_vs._Rock_strength label "Landslides vs. Rock strength".
- Landslides_vs._Rock_strength sameAs m.0glsyk5.
- Landslides_vs._Rock_strength sameAs Q6485198.
- Landslides_vs._Rock_strength sameAs Q6485198.
- Landslides_vs._Rock_strength wasDerivedFrom Landslides_vs._Rock_strength?oldid=616594833.
- Landslides_vs._Rock_strength depiction LS-usgs.gif.
- Landslides_vs._Rock_strength isPrimaryTopicOf Landslides_vs._Rock_strength.