earthquakes and tsunamis - environmental engineering - lecture slides pdf
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8/15/2019 Earthquakes and Tsunamis - Environmental Engineering - Lecture Slides PDF
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What is an Earthquake?
• Ground movement caused by the sudden release of
seismic energy due to tectonic forces.
The focus of an earthquake is theactual location of the energy
released inside the Earth’s crust.
The epicentre is the point on the
Earth’s surface directly above the
focus.
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Why do earthquakes occur?• Seismic energy is usually caused by the brittle
failure (fracturing) of rocks under stress.
• This commonly occurs due to movement along
tectonic plate boundaries
Figure showing the
distribution ofearthquakes
around the globe
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Earthquake Magnitude
Magnitude Earthquake Effects Approx. number
each year
< 2.5 Usually not felt, but recorded 900,000
2.5-5.4 Often felt, only minor damage 30,000
5.5-6.0 Slight damage to buildings andother structures
500
6.1-6.9May cause a lot of damage in very
populated areas 100
7.0-7.9 Major earthquake. Seriousdamage.
20
> 8.0 Great earthquake. Can be totallydestructive near the epicentre.
1 every 5-10 years
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Earthquake Hazards
• These are important hazards to understand: – the natural hazard that on average kills the highest
number of people per year (> 1 million during the pastcentury)
– commonly strikes without warning
– no time for evacuation
– not a predictable trend to earthquake numbers,magnitude or location
• 1000's of large earthquakes every year
• ~ 20 are > M7.0 and these account for 90% of the energyreleased and 80% of all the fatalities
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How do we mitigate the hazard from
earthquakes?
• Reinforce buildings
• Education
• Disaster plan
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Earthquakes and Tsunami’s
• An earthquake under the ocean has the
potential to form a tsunami.
• The earthquake must vertically displaceoverlying water (extensional or
compressional faults - not transform)
Extension Compression
TransformD o c s i t y . c o m
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How does an earthquake form a
tsunami?
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2004 South Asian
Boxing Day event
• Biggest earthquake in40 years!
• Magnitude 9.2
• 150 km off the westof Northern Sumatra
• Generated adisastrous tsunami in12 countries
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Second largest recorded earthquake• The earthquake occurred at a convergent tectonic
plate boundary (subduction zone)
• An estimated 1,600 km (994 miles) of faultline slipped about 15 m (50 ft)!
• The earthquake released 20 x 1017 Joules ofenergy
– Equivalent to:• 475,000,000 kg of TNT
• 23,000 Hiroshima atomic bombs!
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How do we mitigate the hazard from
tsunamis?
• Monitoring – process is very technology-
intensive• high costs for many poorer countries
– often no technology available tomonitor local tsunamis
• for example,
• Papua New Guinea has no monitoringstations
– reliant on the Pacific TsunamiWarning Center
• tsunami in 1998 was not detected
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How do we mitigate the hazard from
tsunamis?
• Building restrictions in
hazard prone areas – In Hawaii, Hilo harbor anddowntown was destroyed bythe tsunamis of 1946 and
1960 – The town is now rebuilt on
higher ground and thedevastated area is a park
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How do we mitigate the hazard from
tsunamis?
• Seawall construction – cause early wave breaking
– prevent wave run up into urban areas
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How do we mitigate the hazard from
tsunamis?
• Education – warning systems
– evacuation plans – general understanding of
the hazards involved
Punishment
From God
45%
Natural event
35%
Bomb 20%
Population reaction:Papua New Guinea (1998)
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