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Energy Transformation in the form of Seismic Waves

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Presentation on theme: "Energy Transformation in the form of Seismic Waves"— Presentation transcript:

1 Energy Transformation in the form of Seismic Waves
Earthquakes and waves Energy Transformation in the form of Seismic Waves

2 New Island < >

3 What do you know about Earthquakes?

4 Earthquakes Earthquakes transfer stored energy into kinetic energy in form of seismic waves. These waves are MECHANICAL waves Waves are an oscillation or vibration that transfers energy

5 Earthquake Identification and Location
Earthquakes are located and identified by their focus, epicenter and magnitude Focus: The point where the fracture in rock occurs, (under ground). Epicenter: The point, on land, directly above the focus point. Magnitude: The amount of energy or destruction that has been released/caused

6 Seismographs

7 Seismographs

8 Explain the difference between a Focus and an Epicenter?
If earthquakes are mechanical waves, what are the other types of waves called?

9 Magnitude Richter Scale: Measures the total amount of energy released by the earthquake. Magnitude 7 or greater is a major quake Magnitude 6 or less is a minor quake Magnitude 2 or less is a micro quake or tremor

10 Magnitude Continued 2. Mercalli Scale:
Measures the degree of destruction that has been caused. This is a scale that is far more subjective in nature. Mercalli scale rates on a scale of I – XII (I) is little damage and (XII) is extreme destruction

11 Seismic Waves Primary or P waves Secondary or S waves
Fastest moving seismic wave Arrive at recording stations first Moves in a spring like way Travel through both liquid and solid material Slower moving wave Arrives at recording stations after the P wave Moves in an up and down way Cause buildings to shake Travels through solid material only

12 Primary and Secondary Waves
P waves oscillate through compression and expansion, in the same direction of movement S waves oscillate in a direction that is perpendicular to direction of movement

13 L-Waves L waves are also known as surface waves
They are the slowest but most destructive waves They are the waves that cause surface rolling

14 Which is the fastest moving seismic wave?
Which seismic wave is most destructive?

15 Distance to Epicenter Seismologists determine the distance to the earthquake’s epicenter through analyzing the difference in arrival times at the recording station. When arrival times are close, with little difference, the distance to the epicenter is very small. The greater the difference in arrival times, the further away the epicenter is Use information from 3 recording stations to triangulate the location

16 Triangulation


18 Location of Earthquakes
3 major locations where earthquakes occur Ring of Fire

19 Earthquake location continued
Mid ocean ridges

20 Earthquake locations continued
The Eurasian-Melanesian Mountain Belt

21 What is the different plate activity at each of the locations where seismic activity takes place? Ring of Fire, Mid-Ocean Ridge, and Eurasian-Melanesian Mountain Range

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