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Earthquakes Earth Science. What is an Earthquake?  A vibration of the Earth produced by a rapid energy release  The point within the earth where an.

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Presentation on theme: "Earthquakes Earth Science. What is an Earthquake?  A vibration of the Earth produced by a rapid energy release  The point within the earth where an."— Presentation transcript:

1 Earthquakes Earth Science

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3 What is an Earthquake?  A vibration of the Earth produced by a rapid energy release  The point within the earth where an earthquake starts is called the focus  Energy travels from the focus in all directions- think of a stone being tossed into a pond  Stone sets waves of motion in water just as seismic waves move through earth The point on the surface of the Earth above the focus is called the epicenter

4 The Epicenter  The epicenter is the location directly above the focus

5 Earthquakes over a 10 yr. period  Pacific Ring of fire

6 Faults  Faults are fractures in the Earth where plate movement has occurred  There are three types of forces that create faults.  Compression - squeezes  Tension - stretches  Shear – causes slippage  Each of these three forces can create a different kind of fault.

7 Earthquake causes  Elastic Rebound hypothesis  Rock is bending causing elastic stress  Eventually the rock will slip and break at the weakest point (the focus)  The vibrations we feel occur as the rock returns to its original shape

8 Types of faults  Normal Faults- caused by tension forces  Reverse Faults- compression  Strike-Slip Faults- shear forces

9 Normal Faults  Tension causes rocks to be pulled apart.  Rock above the fault surface moves downward in relation to rock below the fault surface.  Can help to form mountains such as the Sierra Nevada Mountain Range

10 Reverse Fault  Compression causes rock to break.  Rocks above the fault surface are forced up and over the rocks below the faults.  Can form mountains such as the Rockies.

11 Strike-Slip Fault  Two of Earth’s plates move past each other due to shear forces.  There is very little vertical movement  Ex: San Andreas Fault

12 Earthquake Info  Seismic waves – waves that move through the Earth’s crust  Seismic waves travel outward from the focus of an earthquake  Surface Waves- these travel along Earth’s outer layer  Body waves- travel through Earth’s interior  Primary Waves (P) – waves that travel in the same direction the wave is moving  Secondary Waves (S) – move through the Earth causing particles to move at right angles to the direction of the wave.

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15 Wave Facts  Surface waves (S) are the slowest waves, primary (P Waves) are the fastest. P Waves can only travel through solids.  P waves travel 1.7 times faster than S waves  Surface waves cause the most destruction during an earthquake.

16 Measuring Earthquakes  Seismologists use seismographs to measure earthquakes.  The more energy that an earthquake releases, the greater its magnitude.  One of the largest earthquakes occurred in Haiti very recently and killed over 200,000 people

17 Finding the Epicenter- Distance  Remember P Waves travel faster than S waves  The greater the distance between the P wave and S wave the farther the source  1) find the time interval between the first P wave and first S wave using the seismogram  2) use the graph to find distance from the seismogram

18 Finding the Epicenter- Direction  Can use 3 or more seismograms to do this  Create a circle using direction found on graph  Where circles intersect is the exact location of the epicenter

19 Richter  Earthquakes are ranked on the Richter Scale – measures amount of energy released  1-10  For each increase of 1.0, amplitude of the largest surface wave is 10 times greater  About 32 times as much energy is released

20 Tsunami  Means “Harbor Wave”  If an earthquake happens underwater, it can create a huge wave.  This wave travels to the surface  After it reaches the surface, it can spread out for thousands of kilometers in every direction  As the wave approaches the shore, it can form a towering crest that can reach 30m high.

21 Earthquake Safety  Be prepared – know if an area has had earthquakes in the past or if it is near a pate boundary.  Make your home earthquake safe  Take heavy objects down from high shelves  Hot water heaters and gas appliances should be securely in place  During earthquakes, stay away from windows or anything that could fall on you.

22 Living on a Fault  Seismic Safe structures  Resistant to vibrations  Buildings with bases of alternating rubber and steel can withstand quakes of up to 8.3 on the Richter scale without major damage  Buildings and highways can be made so they will bend but not break  Seismic safe structures are more expensive to build than regular structures.

23 More Earthquake Damage Anchorage, Alaska 1964 – Magnitude 9.2

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29 Oakland, CA 1989

30 Northridge, CA 1994 – 62 killed

31 Former hospital in Mexico City 1985 – Magnitude 8.1 with 7.5 aftershock 18 hours later

32 Turkey 1999


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