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Earthquakes. Causes of Earthquakes An earthquake is a shaking of Earth’s crust caused by a release of energy Mostly caused by the strain that builds.

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Presentation on theme: "Earthquakes. Causes of Earthquakes An earthquake is a shaking of Earth’s crust caused by a release of energy Mostly caused by the strain that builds."— Presentation transcript:

1 Earthquakes

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3 Causes of Earthquakes An earthquake is a shaking of Earth’s crust caused by a release of energy Mostly caused by the strain that builds up along faults which are breaks in the lithosphere Strain becomes great enough to overcome friction and land moves

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5 Where do earthquakes happen? (pg528-529) Earthquakes can happen anywhere that there is stress and strain resulting in a crack in the Earth’s crust. This most often occurs at plate tectonic boundaries, but they can also occur in the middle of plate tectonics that are under a lot of stress.

6 How often do earthquakes occur? Earthquakes happen everyday around the world, some can’t even be felt http://earthquake.usgs.gov/earthquakes/

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8 Types of faults (pg531)

9 Parts of Earthquakes FOCUS: Point at which the first movement occurs during an earthquake –M–Many miles below the Earth’s surface EPICENTER: Point on the Earth’s surface directly above the focus

10 Body Waves Body waves: Are waves that travel from the focus through the Earth –E–Every Earthquake produces 2 types of body waves P-Waves: Primary Waves (Come First and travel faster) –C–Can travel through solids, liquids and gases S-Waves: Secondary Waves ( Come Second and are slower) –C–Can only travel through solids

11 Locating and Measuring Earthquakes Seismograph: Detects and records waves produced by earthquakes Seismogram: Record sheet on seismograph – P waves will arrive at the seismograph station first –T–The farther away the earthquake is from the seismograph station the greater the difference in arrival times

12 Locating the Epicenter Scientists need to know the distances from at least three different stations in order to plot an epicenters location

13 Why do you need three stations?

14 Measuring Magnitude of Earthquake Magnitude is the strength of the Earthquake ranges 1-10 –Richter Scale: For each increase of 1 whole number represents a 31-fold increase in energy –Example: A reading of a 6 on the Richter scale is 31 times stronger than a 5 on the Richter scale

15 Richter Scale: Related to power or strength

16 Mercalli Scale The Mercalli scale measures the earthquakes destruction or how much damage it has produced Ranges 1-12

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18 Earthquake Hazards

19 Tsunamis Fire Flooding Ground displacement Destruction

20 Welcome! Get out your Volcano and Earthquake notes. On your whiteboard answer the following: –What are the two types of seismic waves related to earthquakes –Which travels faster and which travels slower


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