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Geology 1 MT2: EQs
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earthquake
the sudden slip on a fault (release of elastic energy) and the resulting ground shaking and radiated seismic energy caused by the slip
hypocenter (focus)
the first point on a fault that moves in an EQ
the EQ originated at the hypocenter
epicenter
the point on the earth's surface that is directly above the hypocenter
rupture area
the portion of a fault that slips in an EQ
surface trace
where the fault breaks the earth's surface
blind fault
a fault that does not break the earth's surface
elastic rebound theory
1.
stresses
(force/area) are
applied
to a fault
2.
strain
(deformation)
accumulates
in the vicinity of friction-locked faults
3. strain accumulation reaches a
threshold
and fault slips suddenly
4.
rupture
(slip) continues over some portion of the fault
2 types of seismic waves
body waves - move through the earth's interior
surface waves - through earth's surface
2 types of body waves
p-wave
: (primary wave)
the first wave to arrive following an EQ
propogate by alternately compressing/expanding material
can move through solids, liquids, gases
s-wave
: (secondary wave)
shear wave
can only move through solids
2 types of surface waves
Love wave
: horizontal shearing of the earth's surface
Rayleigh wave
: "rolling" of the earth's surface
calculating the distance to an EQ
depends on the time gap b/t p-waves and s-wave arrivals (∆ t)
∆ t = ts - tp
[ts= s-wave arrival time, tp= p-wave arrival time]
D= (Vp x Vs) / (Vp - Vs) x ∆ t
what is Richter magnitude based on?
the amplitude of the largest s-wave
4 steps to find Richter magnitude:
Find distance
Measure amplitude and find log
Find log A
0
from graph
Find difference
: M
L
= logA - logA
0
A fault that has both horizontal and vertical offset
oblique fault
Fault that moves without an EQ
fault creep
Author
kjel
ID
80826
Card Set
Geology 1 MT2: EQs
Description
Geology 1 MT2: EQs
Updated
2011-05-09T17:06:31Z
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