Agenda 2/10 Warm-Up: Have you ever seen geologic problems in California on the news? What types of events make life more challenging on the West Coast? Soil Reading/WS Mass Movement Notes Mass Movement flipbook

Mass Movements at Earth’s Surface Part 1

Mass Movements Mass movement: downslope movement of loose sediments and weathered rock resulting from the force of gravity All occur on slopes; since very few places on Earth are flat, almost all Earth’s surface undergoes mass movement Range from extremely slow motions to sudden slides, falls, and flows Materials moved: fine mud to large boulders

Variables that influence Mass Movements: Material’s weight resulting from gravity Material’s resistance to sliding or flowing (friction between material and slope) Trigger: such as an earthquake Erosion and undermining of soil increase potential for earth’s materials to move downhill

Other Variable: Water Too little water: prevents sediment from holding together at all Too much water: can make slope unstable increasing weight of soils and sediment In this case: water not involved as transport agent; moves along with materials vs. materials moving along with water

Types of Mass Movements: Creep Creep: slow, steady downhill flow of loose, weathered materials (soils) Move few cm per year Effects seen over long periods of time Can cause tilting of utility poles, fences, bending of trees, cracking of walls, breaking of underground pipelines Solifluction: slow, downhill movement of loose, water-logged materials in regions of permafrost (mudlike liquid)

Types of Mass Movement: Flows Flows: can move slowly as a few cm per year or hundreds of km per hour Earth flows: slow movements of soil Mudflows: swiftly moving mixtures of mud and water triggered by earthquakes (common in volcanic regions and sloped semi-arid regions) Los Angeles Basin (southern CA) slopes left with little vegetation, heavy rains fall, cause mudflows

Types of Mass Movement: Slides Landslide: rapid downslope movement of materials that occurs when thin block of soil, rock, and debris separates from underlying bedrock Rock Slide: type of landslide that occurs when sheet of rock moves downhill on sliding surface Very destructive form of mass movement!

Types of Mass Movement: Slumps Slump: when mass material in landslide rotates and slides along a curved surface Occur in areas that have thick soils and on moderate to steep slopes Common after rains because water reduces friction between grains of soil; weight of additional water pulls it downhill Triggered by earthquakes

Types of Mass Movement: Avalanches Avalanches: landslides occur in mountainous areas with thick accumulations of snow Usually occur on slope 10,000 avalanches each year in mountains of western US Sun melts surface snow, then refreezes at night, snow falls on top builds up heavy, slip, slide down slope as avalanche

Rock Falls Occur at high elevations, steep road cuts, on rocky shorelines Rocks loosened by physical weathering and plant growth Rocks break up and fall downward

Mass Movements Affect People Dangerous Mudflows: widespread loss of human life primarily result of location of villages both high up and in steep terrain and at foot of unstable, saturated slopes Reducing the Risks: avoid building structures on such steep and unstable slopes Trenches used to divert water from a slope and control drainage Covering steep slopes with steel nets and protective fences

Mass Movement flipbook Make a 6 flap foldable (like our Extreme Weather foldable). Each flap will have the name of one mass movement: Creep, Slump, Flow, Slide, Avalanche Use your notes/internet searches to fill in your foldable   Front Flap: Title and Picture of the mass movement Inside: definition, effects/trigger, what caused by, where these movements occur most often, and any other information you may want to add.