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Published byBertha Townsend Modified over 9 years ago
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Slope stability I EOSC316 Engineering Geoscience
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Landslip trigger processes Water Toe removal –Natural –Artificial Head loading Vibration
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Folkestone Warren, Kent Toe erosion due to extension of harbour wall, 1905 Since 1915 slide –mass concrete toe weights –drainage adits
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Mt. Huascaran, Peru, 1970 earthquake triggered hit towns of Yungay and Ranrahirca, 18 km away, at around 150 km/hr Yungay completely buried, 66,000 dead
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Types of landslide Rock failure –failure plane pre- determined Soil failure –failure plane along line of max stress
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Rock failure
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Planar translational slip in rock = angle of repose (= angle of friction) Factor of safety = shear force at failure / shear force
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Wedge failure in rock
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Toppling failure, Masada, Israel
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Effect of cohesive strength on bench height in rock Shear stress on sliding plane: Failure occurs when: Thus Area of wedge
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Half dome, YosemiteCarrara marble quarries, Italy
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Rock failure – remedial measures
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Slope failure in ‘unconsolidated’ material
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Planar versus rotational slip in unconsolidated material Planar slip –frictional –cohesionless –C = 0 Rotational slip –frictional –cohesional –C ≠ 0
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La Conchita, Santa Barbara, California, Spring 1995
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Planar translational slip = angle of repose (= angle of friction) Factor of safety = shear force at failure / shear force
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Planar slip - analysis
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Planar slip in soils Cohesionless soils (φ=0) Soils with cohesion (φ≠0)
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