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2 | Faults 1, 2,
3, 4, 5
Faults:
A USGS Teacher's Lesson
Application Phase
- Explain that faults are
often (but not always) found near plate boundaries and that each type
of fault is frequently associated with specific types of plate movements.
However, all types of faults can be found at each type of plate boundary.
a. Normal faults are
often associated with divergent (tensional) boundaries.
b. Thrust faults are
often associated with convergent (compressional) boundaries.
c. Strike-slip faults
are often associated with transform (sliding) boundaries.
- Ask the following questions:
a. What kind of faults
would you expect to find in the Himalayas (hih-MAHL-yuz)? Why?
b. What kind of faults
would you expect to find along the Mid-Atlantic Ridge? Why?
c. Is California likely
to "fall into the Pacific Ocean?" Why or why not?
- Explain that not all
faults are associated with plate boundaries. Explain that there is
a broad range of faults based on type, displacement, age, current
or historical activity, and location on contintental or oceanic crust.
Have students research examples of faults that are not at plate boundaries.
- Explain to students that
the stresses and strains in the earth's upper layers are induced by
many causes: thermal expansion and contraction, gravitational forces,
solid-earth tidal forces, specific volume changes because of mineral
phase transitions, etc. Faulting is one of the various manners of
mechanical adjustment or release of such stress and strain.
- Have students research
and report on the types of faults found in your state.
Extensions
- Have students identify
the fault movements in the recent Loma Prieta, California earthquake.
- Have students research
the fault histories and recent theories concerning earthquakes in
Northridge, California (1994), New Madrid, Missouri (1811-12), and
Anchorage, Alaska (1994).
Coloring Key:
Rock Layer X - green
Rock Layer Y - yellow
Rock Layer Z - red
River - blue
Road - black
Railroad tracks - brown
Grass - green
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