1
S
an
A
n
d
re
a
s
F
a
ult
Displacement
Earth Sciences 1081B:
Resources, Environment and Sustainability in a
Material Society

2
“E” released as crustal plates slip past one another

Elastic rebound
deformed by tectonic
forces
bend and store elastic
energy - strain
Frictional
resistance holds
the rocks together
3
Earthquakes
A. Original Position
B. Build up of Strain
Earthquakes where and
why?

4
D. Strain Released
What is an Earthquake ?

5
•
direction of
applied stress
•
the sense of
motion relative
to the
fault
Types of faults
and movement
based on:

“E” moves in waves
Interior :
P-waves “Primary”
S-waves “Secondary
Exterior:
Surface waves
6
Energy radiates in all directions from the source
Focus
earthquake waves
originate
Epicentre
location on the surface
directly
above
the focus

Body waves: travel through Earth’s interior
Primary (P) waves:
7

Body waves: travel through Earth’s interior
Secondary (S) waves
8

9
Surface; R- waves

Seismology
The study of
earthquake waves
,
Seismometers
are instruments that record seismic
waves
10
Records the
movement of Earth
in relation to a
stationary mass on
a rotating
drum
or
magnetic tape

11

12
A Time Travel Graph:
used to locate
Distance
to
epicentre
triangulation used to
locate epicentre
Locating the
epicentre of an
earthquake

13
Mid-Atlantic
Ridge
Locating the
epicentre
Triangulation
from 3
stations


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- Fall '11
- SamRussell
- Earthquakes