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Take out your notebook Look at the worksheet page you did after the test. Check your answers with those on the next slide!!

Take out your notebook

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Take out your notebook. Look at the worksheet page you did after the test. Check your answers with those on the next slide!!. Forces in the Earth’s crust answers. Reverse fault Compression Hanging wall moves up Normal fault Tension Hanging wall moves down Strike-slip fault Shearing - PowerPoint PPT Presentation

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Page 1: Take out your notebook

Take out your notebook

Look at the worksheet page you did after the test.

Check your answers with those on the next slide!!

Page 2: Take out your notebook

Forces in the Earth’s crust answers

1. Reverse fault 2. Compression

3. Hanging wall moves up4. Normal fault

5. Tension6. Hanging wall moves down

7. Strike-slip fault8. Shearing

9. Blocks move sideways in opposite directions10. Stress that moves rock in two opposite

directions 11. A large area of flat land elevated high

above sea level

Page 3: Take out your notebook

Write what is in yellow in a new page in your notebook.

Add it to your table of contents as “types of faults”

Page 4: Take out your notebook

3 Types of Faults

Normal fault

Reverse fault

Strike-slip fault

Page 5: Take out your notebook

Normal faults

A normal fault occurs when one plate slides down another plate.

Tension is the force causing the plates to move apart

Page 6: Take out your notebook

Reverse Faults

Reverse faults occur when one plate slides up another plate.

The angle is steep usually greater than 45 degrees.

Compression is the force that causing the plates to push together

Page 7: Take out your notebook

Compression causes Anticlines and Synclines

Anticlines are folds in which each half of the fold dips away from the crest.  Synclines are folds in which each half of the fold dips toward the trough of the fold.  You can remember the difference by noting that anticlines form an “A” shape, and synclines form the bottom of an “S.” 

Page 8: Take out your notebook

Strike-slip Faults

Strike-slip faults occur when one plate slides either to the right or to the left of another plate.

Shearing is the force causing the plates to move past each other.

Page 9: Take out your notebook

San Andreas Fault

It is more than 800 miles long and 10 miles deep!

It is an example of a strike-slip fault. Locked sections remain still for about

hundred years until there is enough force to move them. These sections result in massive earthquakes.

Sections that creep move slowly at a constant rate. They result in more subtle earthquakes.

Page 10: Take out your notebook

Images of the SAF

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The Future of CA

The Pacific Plate ismoving northwest of the North AmericanPlate. Eventually California will be further north.

Page 12: Take out your notebook

I live in Louisiana…

Why do I need to know this?

Earthquake game http://www.youtube.com/watch?v=XVrM8dSAtu4

Page 15: Take out your notebook

SEISMOLOGY

THE STUDY OF EARTHQUAKES

THE SCIENCE DEALING WITH ALL EARTH MOVEMENTS AND WAVES

Page 16: Take out your notebook

SEISMOLOGIST

THE SCIENTIST THAT STUDIES THE MOVEMENTS OF THE EARTH

A PERSON WHO STUDIES SEISMOLOGY MUST KNOW FACTS ABOUT GEOLOGY,

PHYSICS, AND CHEMISTRY

Page 17: Take out your notebook

SEISMIC WAVES

CALLED EARTHQUAKE WAVES THERE ARE THREE TYPES OF SEISMIC

WAVES:› PRIMARY WAVES (P-WAVES)› SECONDARY WAVES (S-WAVES)› LONGITUDINAL SURFACE WAVES (L-WAVES)

Page 18: Take out your notebook

SEISMOGRAPH

THE INSTRUMENT THAT MEASURES AND COLLECTS SEISMIC WAVES FOR EACH EARTHQUAKE.

IT SENDS THESE WAVE VIBRATIONS TO THE PRINTER MACHINE WHICH CREATES A GRAPH TO VIEW THE LOCATION OF THE SEISMIC WAVES

http://www.youtube.com/watch?v=VemVX6dQU_k seismograph

Page 19: Take out your notebook

SEISMOGRAM

THE GRAPHED DRAWING OF THE EARTHQUAKE WAVES CAUGHT BY THE SEISMOGRAPH.

SHOWS THE LOCATIONS OF MANY DIFFERENT SEISMIC WAVES SO THAT SEISMOLOGIST CAN DETERMINE WHERE, ON EARTH, THE EARTHQUAKE OCCURRED.