Bell Ringer When the landscape changes suddenly, it is considered Mass Movement….. Can you list 5 types of Mass movement? What could potentially cause.

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Presentation transcript:

Bell Ringer When the landscape changes suddenly, it is considered Mass Movement….. Can you list 5 types of Mass movement? What could potentially cause this to occur?

Mass Movements/ Wasting

What are they? Mass movements include: Landslides Rock falls Avalanches Mud flows Debris flows Creep

Anatomy of a rotational landslide

<1 cm/year >100 km/year 0%~40%

Mass Movements Material moves downslope due to the pull of gravity Can happen almost anywhere Commonly associated with other events (heavy rainfall or earthquakes, for example) and are therefore under-reported Movements can either be catastrophic (slope failure) or slow and steady (creep) The rate of the mass movement can be increased by various erosive agents (especially water)

Gravity Water Earth Materials Triggering Events Factors in Slope Stability

Gravity & steepening of a slope

How to cause a landslide: add or subtract a mass …in the wrong place Common when building roads Common when building near slopes

Rotational landslide

Angle of Repose Varies for Different Materials

Water decreases rock/soil cohesion

Water circulating underground can dissolve cements that hold sedimentary rocks together

Internal Causes for Slope Failure Water (weight & interaction with clay minerals) Decreasing rock cohesion Incompetent/weak material Adverse geologic structures

The Weight of Water Sedimentary rocks commonly have porosities of % If pore spaces fill with water, the weight of the material is increased substantially, creating instability

La Conchita, CA March 1995

It happened again in 2004… in exactly the same place…

La Conchita, CA

Debris flows or mud flows Mass movements that behave like fluids Unlike slides, flows are not controlled by a failure surface, but instead are dominated by internal movements

Landslides in the Bay Area

1982 San Mateo County

Devil’s slide area on Highway 1 north of Half Moon Bay

Rock Falls

Creep Downslope movement of soil and uppermost bedrock Creep happens at too slow of a rate to observe directly Instead, creep can be identified by it’s effect on objects

Gravity - hill slopes more vulnerable (on top of a hill, on the slope, or at the bottom of a hill), modified slopes (road cut, cut flat area to build on, coastal erosion, etc.) Water - risk is higher when ground is saturated and/or during heavy rains, El Niño events Earth Materials - loose soils (particularly clay-rich) or fractured rock, and old landslides pose greater risk Triggering Events - heavy rain during storm, rain after big storms or fires, earthquakes (when ground is saturated?)…are all triggers Risk factors to increase likelihood of mass movement