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Page 1: Earthquake hazards

Earthquake hazards

Ground Rupture

Ground rupture from the M8.1 2001 Tibet earthquake

Alaskan pipe after the Denali quake ruptured through

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Earthquake hazards (cont.)

Shaking Wave

amplitude Wave

frequency Duration of

shaking

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Earthquake hazards (cont)

Liquefaction Saturated sand

loses strength upon shaking

1964 Nigata Japan

Tsunami Wave wavelength

ocean waves that can travel vast distances

2004 Sumatra earthquake

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Sumatra Earthquake tsunami

QuickTime™ and aSorenson Video decompressorare needed to see this picture.

QuickTime™ and aVideo decompressor

are needed to see this picture.

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Seismic Hazard of MA

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Cape Ann Earthquake 1755

Woodcut illustration depicting damage in Boston from the earthquake

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Hazard vs risk

1989 Macquarie Ridge, New Zealand M 8.3 No losses

1960 Agadir, Morocco M 5.5 12,000 deaths

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Earthquake Risk

Risk = hazard x vulnerabilityThe amount of damage and numbers of

earthquake related deaths do not correlate to magnitude of the earthquake.

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Products of hazard assessment

Active fault mapHistorical seismicityEarthquake likelihood

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3D models assess seismic hazard in Los Angeles, CA

SCEC Community Fault Model

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Acceptable Risk

Level of acceptable risk depends on the structure

Cannot design for maximum earthquake with low probability

Social question

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How would you mitigate damages from….

Ground RuptureLiquefactionGround ShakingTsunami

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Ground Rupture

Avoid constructionRelocate sensitive facilitiesImplement low use facilities

Playing fields Green space

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Portola Valley California

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Liquefaction

Recognize liquefaction potentialIn-situ remediationAvoid construction in liquefaction prone

areas

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Tsunami mitigation

Early warning system Broadcast signal to beaches after a major

earthquake anywhere in the ocean basin

Saftey guidelines Go to high ground Climb a tree

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Ground Shaking

Recognize the degree of probable ground shaking in the area

Improve construction methods to accommodate shaking without collapse


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