Geologic Hazards Flashcards
why do earthquakes form?
sudden movement of plate causes rock to break at the hypocenter and release energy in the form of seismic waves. Waves spread from the epicenter
Difference between focus and epicenter
Focus or hypocenter is the origin of the earthquake at depth while epicenter is the point at the surface directly above the hypocenter
Elastic rebound theory
Original position - buildup of strain - rupture/slippage - release of energy
Def
Seismic waves
body waves
surface waves
seismic waves - form of propagation of energy released in an earthquake
body waves - emanate from the focus in all directions through the interior of earth
surface waves - travels at earth’s surface
cc
Seismic waves
body waves
surface waves
body waves primary - push pull (solid and liquid) secondary - transverse (up/down) solid only surface waves rayleigh - cyclical up and down love - cyclical side to side
Difference between seismograph and seismogram
seismograph - instrument
seismogram - graph
difference between magnitude and intensity
magnitude - amount of energy released by the earthquake
intensity - strength felt by people/destruction or damage caused by the earthquake
how to locate earthquake
measure S-P interval, determine distance, determie magnitude by measuring amplitude, locate the epicenter
Factors promoting mass wasting:
ssg
slope, soil cover, geologic feature slope: g(to downslope) > g (stay in place) geologic feature: Type of rock; presence of joints, fractures, or bedding planes Dips upslope, horizontal, dips downslope
If direction of slope is the same as direction of *: daylighting slope
planar features
Types of mass wasting
Fall, topple
Slide, Slump
Flow
Granular flow (debris avalanche, earthflow, creep) and slurry flow
sudden movement of rock, separated along fractures or bedding planes no fluidity in the motion, only bouncing, rolling and free fall
Fall
blocks of material fall over as a unit, similar to falling dominos
Topple
result when rocks and debris slide down a pre-existing surface, such as a bedding plane, foliation surface, or joint
Slides (Translational)
downward rotation of rock or regolith occurs along a concave-upward curved surface leave arcuate scars or depressions on the hill slope
Slumps (Rotational slides)