Lecture #9 [Earthquakes-Mass Wasting] Flashcards
Faulting
lithospheric plates moving past one another, slowed by friction, rocks along boundary undergo stress/strain
when stress overcomes strength rocks rupture along a fault
Focus
point of initial rupture within earth
Epicenter
place on surface directly above focus
Earthquake magnitude
moment magnitude (originally richter scale) determined from rigidity of rocks,the are that ruptured along fault plane and amount of movement along the fault
Earthquake intensity
10 categories to examine
relies on how people percieve the shaking and the extent of the damge to buildings
which plates are we dealing with in the PNW
juan de fuca and north american potential cascadian subduction zone “megathrust” earthquake
Mass wasting
downslope movement of earth materials, “landslides” major types of mass wasting in BC: falls,flows,slides
Falls
at the base of most cliffs theres an accumulation of fallen material known as talus or scree
Rock avalanche
a massive rock fall explodes apart on contact with a slope, thousands of rocks flying downslope. Transitional: changes to rapid flow of material beyond base of slope
Slides
material slips over one or more surfaces
wet tectonically active earthquake prone areas
Flows
internal movement of individual grains within flow
variables in mass wasting
earth material type slope angle and topography climate veg water time