I. Locations of Earthquakes. Announcements. Earthquakes Ch. 5. video Northridge, California earthquake, lecture on Chapter 5 Earthquakes!

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1 Environmental Geology Summer 2006 Tuesday & Thursday 6-9:20 p.m. Dr. Beyer Earthquakes Ch. 5 I. Locations of Earthquakes II. Earthquake Processes III. Effects of Earthquakes IV. Earthquake Risk and Prediction Website: U.S. Geological Survey Earthquake Hazards Program Earthquakes in the Movies 3 Announcements Today: lecture on Chapter 5 Earthquakes! video Northridge, California earthquake, 1994 I. Locations of Earthquakes Figure 5.7 p

2 I. Locations of Earthquakes Earthquakes occur: 1. at plate boundaries (interplate earthquakes) 2. within single plates (intraplate earthquakes) hot spots ancient failed continental rift zones fracture zones Fracture Zone: I. Locations of Earthquakes Charleston, South Carolina, I. Locations of Earthquakes Ancient failed continental rift zone: Figure 5.8 p. 131 New Madrid Fault Zone, earthquakes since II. Earthquake Processes Earthquakes occur due to movement along faults. type of fault depends on sense, or direction, of motion Figure 5.10 p. 134 direction of motion determined by direction of stress on the rocks direction of stress relates to tectonic setting 8 2

3 Types of Faults Normal fault stress: tension extension, stretching Figure 5.10 p Types of Faults Strike-slip fault stress: shear lateral movement Figure 5.10 p Types of Faults Reverse (thrust) fault stress: compression convergence, shortening Figure 5.10 p Types of Faults Buried reverse (thrust) fault folds anticline: upfold over buried fault syncline: downfold Figure 5.11 p

4 II. Earthquake Processes II. Earthquake Processes Figure 5.13 p. 137 Table 5.5 p Seismic waves: P-waves S-waves R-waves 15 II. Earthquake Processes Earthquake terms: epicenter focus rupture surface rupture Figure 5.3 p P (Primary) Waves Figure 5.13 p

5 S (Secondary) Waves Figure 5.13 p Seismograph Figure 5.14 p R (Rayleigh) Waves Seismogram Figure 5.13 p Figure 5.14 p

6 Seismogram Figure 5.14 p Material Amplification Seismic waves travel differently through different rock materials Propagate faster through dense and solid rocks Material amplification: Intensity (amplitude of vertical movement) of ground shaking more severe in unconsolidated materials Seismic energy attenuated more and propagated less distance in unconsolidated materials 23 Locating an Epicenter Material Amplification Figure 5.15 p Figure 5.16 p

7 (San Francisco) Loma Prieta, 1989 Mexico City, 1985 Material Amplification Material Amplification 27 Figure 5.18 p Figure 5.17 p. 141 Loma Prieta, 1989 (San Francisco) Material Amplification Material Amplification 28 Figure 5.20 p Figure 5.17 p

8 Loma Prieta, 1989 Material Amplification Figure 5.19 p. 143 (San Francisco) 29 Northridge, 1994 Directivity and Depth of Focus Figure 5.21 p Material Amplification Loma Prieta, 1989 (San Francisco) Figure 5.19 p Earthquake Magnitude Richter scale: The amplitude of ground motion Increasing one order in magnitude, a tenfold increase in amplitude Moment magnitude scale Measuring the amount of strain energy released Based on the amount of fault displacement Applicable over a wider range of ground motions than Richter scale Earthquake energy: Increase one order in magnitude, about a 32-times increase in energy 32 8

9 Earthquake Magnitude Table 5.3 p Earthquake Intensity Modified Mercalli Scale 12 divisions Qualitative severity measurement of damages and ground movement Based on ground observations, instead of instrument measurement Scale depending on earthquake s magnitude, duration, distance from the epicenter, site geological conditions, and conditions of infrastructures (age, building code, etc.) 35 Earthquake Magnitude Earthquake Intensity Table 5.2 p Table 5.4 p

10 Earthquake Intensity: Northridge, CA 1994 Figure 5.2 p Earthquake Intensity: Seattle, WA 2001 Figure 5.6 p Earthquake Intensity: Northridge, CA 1994 Figure 5.6 p Earthquake Cycles Faulting and elastic rebound Stages of earthquake cycle Inactive and aftershock stage Stress accumulation stage Foreshocks Main shock (major earthquake) Earthquake cycle over time: Recurrence intervals Earthquake cycle in space: Seismic gaps 40 10

11 Seismic Gaps III. Earthquake Effects Primary effects Ground shaking, tilting, and ground rupture Loss of life and collapse of infrastructure Landslides, liquefaction, and tsunamis Secondary effects Fires, floods, and diseases Earthquake Cycle Figure 5.24 p.147 Stages of earthquake cycle Inactive and aftershock stage Stress accumulation stage Foreshocks Main shock (major earthquake) 42 Primary Effects: Surface Ruptures Figure 5.23 p

12 47 Figure 5.27 p.151 Primary Effects: Landslides 45 Figure 5.23 p.146 Primary Effects: Surface Ruptures Figure 5.26 p.149 Primary Effects: Landslides Fault scarp Primary Effects: Surface Ruptures 12

13 Primary Effects: Tsunami Surviving a Tsunami Lessons from Chile, Hawaii, and Japan U. S. Geological Survey Circular 1187, Tsunami Animation 49 III. Earthquake Effects Depending upon the frequency of seismic waves Body waves (P and S) having higher frequency than surface waves High frequency waves posing more threats on low structures Low frequency waves posing more impact on tall structures High frequency waves attenuated faster over distance, higher buildings far away from the epicenter can be damaged 51 Primary Effects: Tsunami Figure 5.30 p IV. Earthquake Risks and Predictions Earthquake risks Probabilistic methods for a given magnitude or intensity Earthquake risk of an area Earthquake risk of a fault segment Seismic hazard maps Conditional probabilities for future earthquakes 52 13

14 IV. Earthquake Risks and Predictions Figure 5.31 p Seismic Gaps 55 IV. Earthquake Risks and Predictions Long-term prediction Earthquake hazard risk mapping Short-term prediction (forecast) Frequency and distribution pattern of foreshocks Deformation of the ground surface: Tilting, elevation changes Emission of radon gas Seismic gap along faults Abnormal animal activities Seismic Gaps

15 IV. Earthquake Risks and Predictions Hazard Reduction Programs Develop a better understanding of the source and processes of earthquake Determine earthquake risk potential Predict effects of earthquakes Apply research results 57 IV. Earthquake Risks and Predictions Technically feasible: But only about a minute warning Warning system Not a prediction tool Can create a false alarm Better prediction and better warning system? 59 IV. Earthquake Risks and Predictions Adjustments to earthquake activities Site selection for critical facilities Structure reinforcement and protection Land-use regulation and planning Emergency planning and management: Insurance and relief measures

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