lecture11 earthquakes

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Earthquakes

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Page 1: Lecture11 earthquakes

Earthquakes

Page 2: Lecture11 earthquakes
Page 3: Lecture11 earthquakes

Global Seismicity

Page 4: Lecture11 earthquakes

Continental Drift Animationbased on paleomaps from University of Texas Arlington

Page 5: Lecture11 earthquakes

Plate tectonics: predicting the future

Page 6: Lecture11 earthquakes

Plate tectonics in the future: 50 my

• Australia will straddle the equator• E. Africa will form new continent• Antarctica will swing off the south pole• Mediterranean will close off• Atlantic Ocean will grow• Pacific Ocean will shrink

Page 7: Lecture11 earthquakes

Global Seismicity

Page 8: Lecture11 earthquakes

Rocks are stressed too…

Rock stress: from tectonic forces, gravity, and weight of rocks above

Types of stress4. Tension (stretching)5. Compression (shortening)6. Shear (twisting or tearing)

Page 9: Lecture11 earthquakes

Strain

= how rocks respond to stress

2 types4. folding (bending)5. faulting (breaking)

depends on rock composition, pressure, and rock characteristics (brittle vs. ductile)

Page 10: Lecture11 earthquakes

Types of folds1. Anticline

• simple upfold• layers slope down from

axis• younger on outside

2. Syncline• simple downfold• layers slope up from

axis• younger on inside

younger

older

younger

older

Page 11: Lecture11 earthquakes

Types of folds

synclineanticline overturned

anticline

Page 12: Lecture11 earthquakes

Types of Faults

Tension

Compression

Shear

Stretching

Shortening

Twisting

Page 13: Lecture11 earthquakes

Faulting

= rocks on either side of a fracture are displaced relative to each other

Earthquake: caused by sudden release of energy along a fault

Page 14: Lecture11 earthquakes

Anatomy of a faultFault scarp = steep cliffs that make up the

edge of a displaced block

Page 15: Lecture11 earthquakes

3 Types of Faults

1. Normal• tension

2. Reverse• compression

3. Strike-slip (transcurrent)• shearing• lateral displacement

Page 16: Lecture11 earthquakes

3 Types of Faults

Page 17: Lecture11 earthquakes

3 Types of Faults

Divergent Plate Boundaries

Page 18: Lecture11 earthquakes

3 Types of Faults

Convergent Plate Boundaries

Page 19: Lecture11 earthquakes

3 Types of Faults

Transform Plate Boundaries

Page 20: Lecture11 earthquakes

Earthquakes

= vibration in the Earth• produced by shockwaves from sudden

movements along faults

Seismic= pertaining to earthquakes

Page 21: Lecture11 earthquakes

Focus vs epicenterFocus = center of fault motionEpicenter = surface directly above focus

Page 22: Lecture11 earthquakes

Seismometer

Page 23: Lecture11 earthquakes

Seismogram

Page 24: Lecture11 earthquakes

Richter ScaleScale is exponentialFor every increase of 1 in the Richter scale, the wave amplitude increases x10

Exponential decay

Exponential growth

y = y0e-kx y = ekx

Page 25: Lecture11 earthquakes

a = 10M

Where M is Richter magnitude, and a is wave amplitude

M = log10(a)Which is the same as

Richter ScaleScale is exponentialFor every increase of 1 in the Richter scale, the wave amplitude increases x10

Page 26: Lecture11 earthquakes

But wave amplitude is not the same as energy released. (see pg 408 in Strahler)

E = 10(4.8+1.5M) = 104.8 ·101.5M

Where M is Richter magnitude, and E is energy released

So for every increase of 1 in the Richter magnitude, energy increases x 32

Richter Scale

Page 27: Lecture11 earthquakes

How much energy is released?For example, the earthquake that caused the Indian Ocean tsunamis on Boxing Day 2004 (12/26/04) measured 9 on the Richter scale

How much energy was released by this quake?

E = 10(4.8 + 1.5M)

Page 28: Lecture11 earthquakes

The Boxing Day Quake

How much energy was released by this quake?

E = 10(4.8 + 1.5M)

= 10(4.8 + 1.5(9))

= 10(4.8 + 13.5)

= 10(18.3) = 1.99 x 1018J

For comparison, the average U.S. electric power consumption rate is 3 x 1012J/sec