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37 Terms
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what is mass wasting?
* gravitational downslope transport of rock, regolith (unconsolidated material), snow or ice * also called mass movement
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factors that affect slope shape?
* material strength * ability to avoid failure * material strength depends on if it is coherent or unconsolidated or has planes of weakness * roundedness plays a part too * climate * affects which agents or erosion are at work (ice, water, wind) and how fast; also affects soil and vegetation formation on slopes * more veg → more stability * process of formation * ex. glacially carved valley have a ‘U’ shape * river erosion causes a ‘V’ shaped valleys
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factors controlling downslope movement of material?
* slope angle * critical angle of repose * cohesion & water Saturation * Material Strength
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slope angle stress?
* Shear Stress (σd): stress resulting from application of force parallel to a surface (force pulling the boulder/grain downslope) * Normal Stress σn): component of stress perpendicular to the Earth’s planar surface (force keeping the boulder/grain from moving)
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when is a slope stable?
* when σd
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when is slope unstable?
* when σd>σr * shear stress bigger than resistance
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what is the critical angle of repose?
* max angle at which sediment particles can stand w/o falling depends on:
* grain size * grain angularity * rounded grains (more friction) < angular grains * moisture content * dry sediments typic is less stable than damp sediment * oversat sediment becomes less stable
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what is cohesion?
* attraction between small soil particles that is provided by the surface tension of water between the particles * friction and surface tension of water can provide some resistance to sliding
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material strength categories?
* loose, poorly cemented, dry material → weak * solid, well-cemented material → stronger * weak between sedimentary layers & along well dev factures * diff types of rocks layer up → change between one type of rock to other can be failure
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what are the diff types of slope failure?
* creep and solifluction * slumps * debris flows & mud flows * rockslides and rockfalls * sturzstroms (rock avalanches)
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what is a creep?
* extremely slow downslope flow of sediment on the surface * caused by cycles of freeze-thaw, wetting-drying and/or warming-cooling * when water freeze, expands ground (rises) n continues * so winter slope is higher than summer slope
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how do creep occur?
* slow, so loss is mostly from damage to buildings and infrastruct, rather than casualties
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what is solifluction?
* downslope creep driven by sequential freezing and thawing in tundra regions * results in soggy layer of ground above frozen permafrost that then moves downhill * this water can’t go back down
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what are translational slump?
* landslide that moves along a regular sloping planar surface * typic occurs when a block of material is underlain by a weak surface that is more or less parallel to the slope * planes between sedimentary beds * old faults and fractures * debris or cohesive mud over underlying bedrocks * block can travel down slope as a cohesive unit or lose internal cohesion and break up as it travels downslope * if it breaks, turns into diff landslide
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what are rotational slumps?
* landslide in which the mass rotates on a concave failure surface
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examples of slumps?
* Slumps dev along the South Saskatchewan River near Medicine Hat, Alberta * Slump destroyed Holbeck Hall in Scarborough, England, 1993
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what are flows?
* slope failures involving material that has lost internal cohesion
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what is mud flow?
* flow of mud, rock, and water dominated by clay-sized particles * includes lahars
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what is debris flow?
* slurry of rock, sand, and water flowing downslope; water usually makes up less than half of the flow vol
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what does speed of flow depend on?
* steepness of the slope * water content
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example of debris flow?
* Andres of Northwest Argentina that was rich in cobble and boulders
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example mudflow?
* Afghanistan, 2014 * heavy rain turned a slump into a mudflow * buried part of a village in Afghanistan
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Rio De Janeiro and landslides
* highly weathered Sugarloaf mountains surround the city * poor communities (favelas) built on material where landslides are common * 8 million mostly poor Brazilians face mudflow risk * wealthy communities build homes on stable ground
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Vargas Tragedy - Venezuela 1999
* several debris and mudflows over a 2-day period caused by heave rainfall * towns were built on debris from past flows * 30,000 deaths * 75,000 people displaces * dutch helped out (Netherlands) * Some buried to death * mudline on clothes suggest that the landslide was much higher than what videographer saw next day
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what is quick clay?
* water-sat mud deposited in salty water composed of clay flakes with large pore spaces between the flakes * highly unstable
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example of quick clay landslides?
* Led Clay in the ST. Lawrence, Saguenay, and Ottawa Valleys * Lemieux Landslide 1993 → * The headscarp retrogressed 680 m into level
ground above the riverbank. About 2.8 million tons of clay and silt liquefied and flowed \n into the South Nation River valley, damming the river * Alta, Norway 2020
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what is a rockslide?
* sudden movement of rock and debris down a non-vertical slope
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Vaiont Slide
* October 9, 1963; Southern alps in northwest Italy * dam changed water tables (raised it) → caused surface above to get wet, making it unstable → cause slide + river was blocked * slide displaced all the water in downstream half of the reservoir * 125m high wave crashed over the dam * tsunami rushed upstream * 2500 lives lost due to water spilling over dam
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what is a rockfall?
* slope failure that occurs when a mass free-falls down a cliff or a steep slope; slope is often vertical
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rock fall examples?
* Swiss Alps * India
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what is frost wedging?
* splitting of rock thru pressure exerted when water freezes * freezing water expands by 9.2% * coastal areas prone to frost wedging where temperature oscillates around freezing pnt * example: cliff in Torbay, Newfoundland and Labrador
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what is Sturzstrom?
* extremely rapid downslope movement of large vols or rocks and debris * largest and most destructive * typic being as a rock slide, but breaks up, entraining air n water * travel velocities as high as 100-300 km/hr * can travel distances up to 20x their vertical fall * mecha that causes sturzstroms to have such hig velocity and long flow paths is still under debate * sturzstrom may flow as a fluid composed of rock fragment suspended in air (fluidization)
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examples of struzstroms?
* 1903 Frank, Alberta * 1965 Hope, BC
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Frank, Alberta
* started as a translational slide * grained speed and dev into sturzstrom * event lasted less than 100 secs * slope failure occurred along fractured limestone planes * based on the speed and distance of the sturzstrom, it is thought to have traveled on a cushion of compressed air * The rock moved from Turtle Mountain (lower \n left), buried the town of Frank, crossed the river and surged 120m up the other slope. * The river eventually cut through and opened the channel again
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hazard mapping & assessment
* GIS software can help identify areas of past and potential failures by mapping attributes that contribute to slope failures * slope * bedrock type (lithology) * sediment texture and depth * vegetation * drainage * historic slope failures
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reducing or mitigating risk?
* roots of plants * reservoir lowering * river undercutting flow * retaining wall * pipes * metal screening * debris basin * rock bolt
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how to reduce risk from slope failures?
* installation of detection devices, such as acoustic flow monitors * only gives a couple of mins of warning * not enough time to evacuate peep downslope * prohibit building at the base of mountains and is dangerous areas along steep slopes * zone hazardous area as open space for parks, golf courses and agriculture * construct walls and dams to deflect or slow debris flows * construct debris basins large enough to channel and contain debris