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Jesse Lawrance, Stanford University Michael Hubenthal, IRIS Consortium

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Presentation on theme: "Jesse Lawrance, Stanford University Michael Hubenthal, IRIS Consortium"— Presentation transcript:

1 Teaching earth science content with iPods, laptops and other portable accelerometers
Jesse Lawrance, Stanford University Michael Hubenthal, IRIS Consortium John Taber, IRIS Consortium

2 Peak acceleration of about 1g at base

3 Peak ground accelerations in region were 0.8g
1995 Kobe earthquake M 6.9 Peak ground accelerations in region were 0.8g

4 How much energy was released?
Could you calculate the amount? Kinetic energy KE = ½ mv2 Distance traveled D = ½ gt2 Landing velocity Vf = gt KE = mass X Distance X gravity constant

5 For example If I jump off a table 1 meter high
KE ~ 100 kg X 1 m X 10 m/s2 = 1000 joules

6 Does the amount of energy released change as the source is moved horizontally?
How does the amplitude recorded by the sensor change as the source is moved further away? How could you modify the experiment to increased the recorded amplitude at each position? We determined that KE = mass X Distance X gravity constant

7 If you add energy to the impact, is this equivalent to changing earthquake magnitude or intensity?
Magnitude – energy released Intensity – amount of shaking at a point

8 Energy release in an earthquake
Seismic Moment Mo = fault length x fault width x displacement x rigidity Can also be determined from seismograms

9 Moment Magnitude = Mw = log Mo/1.5 – 10.7
Energy release in an earthquake Seismic Moment Mo = fault length x fault width x displacement x rigidity Moment Magnitude = Mw = log Mo/1.5 – 10.7

10 Moment Magnitude of my jump
Moment Magnitude = Mw = log Mo/1.5 – 10.7 1000 joules = 1010 ergs Mjump = - 4

11

12 Relationship between Magnitude and Shaking:
The relationship between magnitude and shaking (acceleration) a =13*(e0.67*M)*(D+25) -1.6 Where a is acceleration (in units of m/s/s), M is magnitude, and D is distance (in km) (From Donovan, 1973)

13 Correlated Acceleration and MMI
Modified Mercalli Intensity Acceleration (g) I II III IV V VI VII VIII IX X+ Above 1.24 Trifunac and Brady (1975) and Wald et al. (1999 a, b)

14 ShakeMaps M8.8 at 3:34 AM on Saturday February 27
One of the 5 largest earthquakes ever recorded 577 killed, 12,000 injured and 800,000 displaced Earthquake caused trans-Pacific tsunami

15 ShakeMaps M 7.0 at 4:53 PM on Tuesday January 12, 2010
15 miles WSW of Port au Prince, Haiti 222,570 killed, 300,000 injured and 1.3 million displaced Worst natural disaster since Indian Ocean Tsunami of 2004

16 ShakeMaps M7.0 located 30 m W of Christchurch at 4:36 AM on Saturday September 4 No fatalities (2 serious injuries) Contrast with Haiti earthquake Good buildings and preparedness paid off!

17 Did You Feel it? Vs. ShakeMap

18 Did You Feel it? Intensity Vs. Distance

19 QCN Rapid Detection Maps

20 QCN Rapid Detections


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