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Landslides, Part 2 Beverly Hills slide, Feb 2005
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Outline Slide examples Flows Avalanches
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Block Slide The rapid movement of large blocks of detached bedrock sliding more or less as a unit.
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Block Slide
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Debris Slide Rock material and soil move largely as one or more units along planes of weakness.
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Debris Slide
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1925 Gros Ventre Slide, Wyoming
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Gros Ventre Slide, Wyoming
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Fig. 12.17 Vaiont Reservoir Slide Debris slide caused reservoir wall to collapse, sent water downstream
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Lateral Spreading
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Turnagain Heights, Alaska
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Flows Mass movements behave like fluids Materials include boulders, sand, ice, mix Speed varies - barely moving to ~200 mph Various types of flow, depending on material, slip surface
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Loess Flow Dry flows of fine silt deposits Example: 1920 China –160 by 275 km hill of loess flowed after earthquake –Killed ~200,000 people by burying villages very rapidly
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Earth Flow A fluid movement of relatively fine-grained material (soils, clays)
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Earthflow
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Debris Flow A fluid mass movement of rock fragments supported by a muddy matrix. May move a speeds of up to 100 km/hr!
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Mudflow A flowing mass of material (mostly finer than sand, along with some rock debris) containing a large amount of water. May travel large distances and high speeds Can carry particles as large as a house!
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Debris Avalanche Fast (up to 280 km/hr) downhill movements of soil and rock, usually occurring in humid mountainous regions
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Mt Huascaran, Peru (before 1970) Mountain region in Peru, before a Mw 7.7 occurred in the subduction zone offshore
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Mt Huascaran, Peru (after 1970)
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Combination of Processes: Mt. Huascaran
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Snow Avalanches Snow has same pull from gravity –Can fail in creep, fall, slide, flow Snowfall, wind-blown snow load slope towards failure –Also skiers
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Snow Avalanche Large events - slab of snow breaks away Occurs because each layer of snow has different properties –Layers deposited at different times, vary in strength, hardness, density, thickness
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Snow! Can travel at very high speeds, trapping skiers
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Ways to Reduce Losses Due to Landslides Include: Avoid construction in areas prone to mass movement Build in a way that does not make naturally stable slope unstable Engineer water drainage to prevent strata to become water saturated and prone to fail
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Note dipping beds undercut by excavation for house
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Box 12.1 Failure occurs when water- saturated strata slide along slippery clay unit, breaching thin retaining wall
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Submarine Movements Same types of failures occur underwater Example: Hawaii has significant slumps, debris avalanches Volcanic flank collapse - whole side of volcano falls off –Leads to tsunami
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Hawaii
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Big Island, Hawaii Motion along blocks near Kilauea today!
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Next Time Subsidence and review for midterm
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