Mass Wasting (from Ch. 15) 1. 2 mass wasting The relatively rapid movement of bedrock, debris,...

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3 Angle of repose –talus 30 to 37° –dry sand 28 to 30° ~32 ° mass wasting

Transcript of Mass Wasting (from Ch. 15) 1. 2 mass wasting The relatively rapid movement of bedrock, debris,...

Mass Wasting (from Ch. 15) 1 2 mass wasting The relatively rapid movement of bedrock, debris, regolith, and/or soil down a slope a short distance Landform scale Unweathered rock resists forces; weathered rock does not Gravity dominates No transporting medium required Requires a trigger Produce colluvium 3 Angle of repose talus 30 to 37 dry sand 28 to 30 ~32 mass wasting 4YearLocationNameCauseDeaths 1949 Tadzhik Russia Kahit slide7.5 EQ200, PeruHuascaran debris aval.7.7 EQ18, PeruHuascaran debris aval. ?? EQ5, Virginia, USAHurricane Camille30 in. in 8 hrs Alberta, CanadaFrank slide?? WashingtonOso mudslide??43 5 mass wasting 6 United States landslide incidence and susceptibility map. National Atlas of the United Statesmass wasting 2. Youtube 3. Youtube 4. Youtube 5. Youtube 1. Youtube 8 mass wasting triggers Vibration earthquakes meteor impact nuclear testing trucks / trains volcanic eruptions Rain, heavy or light Watering / leaky pipes Oversteepening Cut banks in streams Road cuts Foundations Deforestation / planting When shear stress exceeds shear strength, mass wasting occurs. What about bedding planes, joints, and faults? mass wasting shear strength vs. shear stress Shear strength 10 mass wasting factor of safety Shear Strength / Shear Stress = 1, critical threshold > 1, slope stability < 1, slope instability 11 mass wasting types 12 1.fall fastest; a rock falls and becomes talus; rocks float on air, grus, water and avalanche 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide 3.flow slow; with water; earthflow; mudflow; debris flow 4.creep very slow; wet/dry; freeze/thaw; solifluction mass wasting types 13 1.fall fastest; a rock falls and becomes talus mass wasting types 14 1.fall fastest; a rock falls and becomes talus mass wasting types 15 1.fall fastest; a rock falls and becomes talus mass wasting types 16 1.fall fastest; a rock falls and becomes talus mass wasting types 17 1.fall fastest; a rock falls and becomes talus mass wasting types On Tuesday, May 23, 2006 at 5:00pm on the Wall Street section of the Navajo Loop Trail there was a significant rock fall. The rock fall was caused by erosion and weathering, which have shaped Bryce Canyon into what visitors see today. The primary weathering force at Bryce Canyon is frost wedging. Here we experience over 200 freeze/thaw cycles each year. Image from: 18 1.fall fastest; a rock falls and becomes talus mass wasting types 1982 rockfall in Yosemite. 19 mass wasting types 1.fall fastest; a rock falls and becomes talus Image from: 20 mass wasting types 1.fall fastest; a rock falls and becomes talus 21 1.fall fastest; a rock falls and becomes talus mass wasting types An estimated 7,000 tons of rock came down during the Monday afternoon slide, which officials said is enough to fill about 30 average-sized swimming pools. About 300 truckloads of rock will be hauled away before the road is clear. mass wasting types 1.fall fastest; a rock falls and becomes talus 3/8/2010 The largest hole in the roadway was 10 feet by 20 feet. About 20 boulders ranging from three to 10 feet long were scattered on the highway, with the largest weighing 66 tons, officials said. A 1995 rock slide on I-70 in Glenwood Canyon killed three people. A slide on Thanksgiving Day in 2004 closed the highway and required nearly $700,000 worth of repairs. Info./image from: 23 mass wasting types 1.fall fastest; a rock falls and becomes talus Image from: 24 mass wasting types 1.fall fastest; a rock falls and becomes talus mass wasting types 25 Head scarp accumulation zone toe 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide 26 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types fast slide slow slide 27 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types Frank Slide, Alberta, Can 1903; 76 died 28 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types The 17 ka Blackhawk Landslide, San Bernardino County, CA. Photo: Kerry Sieh A sturzstrom! 29 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types The Marcus Rockslide: 500,000 years old. A sturzstrom! 30 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types Anza-Borrego Desert SP, CA Photo by Bob Knapp A sturzstrom! 31 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types Anza-Borrego Desert SP, CA Photo by Bob Knapp A sturzstrom! 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types The Gros Ventre slide of In 3 mins., 50,000,000 cubic yards of rock slid down and 300 ft. up the other side of the valley. 2.slide fast; with/without water; regolith and sometimes bedrock too slow; slumping; rotational slide mass wasting types The Gros Ventre slide of In 3 mins., 50,000,000 cubic yards of rock slid down and 300 ft. up the other side of the valley. 34 2.slide mass wasting types 35 2.slide mass wasting types 36 2.slide mass wasting types May 26, 2014 37 2.slide mass wasting types 38 2.slide mass wasting types 39 2.slide mass wasting types 40 2.slide mass wasting types 41 2.slide mass wasting types 42 3.flow slow; with water; earthflow; mudflow; debris flow mass wasting types 43 3.flow slow; with water; earthflow; mudflow; debris flow mass wasting types Flows are almost always associated with excessive rainfall and oversaturation flow slow; with water; earthflow; mudflow; debris flow mass wasting types 3.flow slow; with water; earthflow; mudflow; debris flow mass wasting types 3.flow slow; with water; earthflow; mudflow; debris flow mass wasting types 4.75 km^2 47 4.creep very slow; wet/dry; freeze/thaw; solifluction mass wasting types 48 4.creep very slow; wet/dry; freeze/thaw; solifluction mass wasting types Photo taken at Red Rock Canyon Open Space, Colorado Springs, CO. Sept., 2015 494.creep very slow; wet/dry; freeze/thaw; solifluction mass wasting types 50 4.creep very slow; wet/dry; freeze/thaw; solifluction mass wasting types 51 mass wasting typeswaterlogged sediment moves over an impermeable surface 4.creep very slow; wet/dry; freeze/thaw; solifluction 52 mass wasting types waterlogged sediment moves over an impermeable surface 4.creep very slow; wet/dry; freeze/thaw; solifluction Your job Risk of mass wasting hazards can be reduced with careful planning and increased understanding Geologic / surficial geology mapping, detection of slope hazards and prediction will aid planners and engineers Physical geographers / soil scientists play a central role More info on mass wasting Lab Three is due next week at the start of class 55 Lab Three is due next week at the start of class