10/10/18 SIO15-18: Lecture 6 Earthquake Hazards Fig. 6.1b Fig. - - PDF document

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10/10/18 SIO15-18: Lecture 6 Earthquake Hazards Fig. 6.1b Fig. - - PDF document

10/10/18 SIO15-18: Lecture 6 Earthquake Hazards Fig. 6.1b Fig. 1.2 (study guide) Hawaii 10/15/06; 7:07 HST Northridge, CA 01/17/94; 4:31 PST Mag. 6.7 Mag. 6.7 0 fatalities 72 fatalities landslides on Hawaii $12.5 billion damage $200


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SIO15-18: Lecture 6 Earthquake Hazards SIO15-18: Lecture 6 Earthquake Hazards

Northridge, CA 01/17/94; 4:31 PST

  • Mag. 6.7

72 fatalities $12.5 billion damage 1g ground acceleration

Hawaii 10/15/06; 7:07 HST

Source: wikipedia.org

  • Mag. 6.7

0 fatalities landslides on Hawaii $200 Mio damage (61 buildings) power outage on Oahu

  • Fig. 1.2 (study guide)
  • Fig. 6.1b
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SIO15-18: Lecture 6 Earthquake Hazards

Hawaii 5/4/18; 12:32 HST

Source: wikipedia.org

  • Mag. 6.9

intensity VIII shaking; 0 fatalities south flank of Kilauea/volcanism minor local tsunami (40 cm) damage to buildings, roads; landslides Hilina slump moved 2 feet

SIO15-18: Lecture 6 Earthquake Hazards

Bam, Iran 12/26/03; 5:26 local time

  • Mag. 6.6

at least 26,000 fatalities displaced 90% of residents destroyed 70% of modern city Northridge, CA 01/17/94; 4:31 PST

Source: wikipedia.org

  • Mag. 6.7

72 fatalities $12.5 billion damage damaged major freeway

  • Fig. 1.x
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SIO15-18: Lecture 6 Earthquake Hazards

Image: S. Marshak “Earth, Portrait of a Planet”

brick

  • Fig. 6.2b

60% of old, poorly-built structures collapsed structures built after 1984 survived 1000 fatalities poor soil (old land fill sites or steep slopes) lack of urban planning and land studies

SIO15-18: Lecture 6 Earthquake Hazards

  • local large tsunami (7 m); Palu
  • landslides/mudflows
  • liquefaction; Palu
  • > 70,000 homes damaged
  • > 2000 fatalities (n1000 missing)
  • tsunami warning issued but the called off
  • power outage/>500 cell phone towers
  • poorly functioning warning system

strike-slip EQ so why tsunami?? -> submarine landslide

source:Wikipedia, NYT

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SIO15-18: Lecture 6 Earthquake Hazards

link for CNN video on liquefaction:

https://www.cnn.com/2018/10/03/asia/liquefaction-earthquake-indonesia-intl/index.html

SIO15-18: Lecture 6 Earthquake Hazards

source:Wikipedia

7 Jun 2008 stratovolcano

  • ne of Sulawesi’s most active

Strombolian style pyroclastic flows; lava flows 10/3/18 ash 6 km high

  • did the earthquake trigger the volcanic eruption?

…. most likely not as volcano was active before EQ

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SIO15-18: Lecture 6 Earthquake Hazards

Compared to long faults, large earthquakes are

  • n shorter faults?

POPQUIZ #2

YOUR FULL NAME AND STUDENT ID# no credit if one is missing

  • less likely
  • more likely
  • equally likely

Code of Conduct: you may ask your neighbor you may consult your notes, book, online you may NOT write and/or submit your friend’s popquiz

SIO15-18: Lecture 6 Earthquake Hazards

source:NOAA

  • Florida panhandle/

Alabama

  • but Georgia, Carolinas

also in path

  • formed in GoM
  • landfall 1 pm Wed
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SIO15-18: Lecture 6 Earthquake Hazards

source:NOAA

  • Florida panhandle/

Alabama

  • but Georgia, Carolinas

also in path

SIO15-18: Lecture 6 Earthquake Hazards

Sumatra-Andaman 26 Dec 2004

  • Mw=9.1; 10m tsunami
  • 3rd largest EQ in 100 years
  • > 240,000 fatalities
  • in ocean, along subduction zone

Tohoku 11 Mar 2011

  • Mw=9.0; 40m tsunami
  • 4th largest EQ in 100 years
  • < 20,000 fatalities
  • in ocean, along subduction zone
  • Fig. 6.11
  • Fig. 6.13

source:Wikipedia source:Wikipedia

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SIO15-18: Lecture 6 Earthquake Hazards

SIO Pier Dec 27 and Dec 29 2006

shallow-water waves (D < λ/20) particle motion elliptical deep-water waves (D > λ/2) waves do not sense bottom particle motion circular v = λ/T or v=g T/(2π)

Chapter 6 (incomplete) λ from cm to n100 m

wave height depends on

  • wind speed
  • duration of wind
  • fetch

SIO15-18: Lecture 6 Earthquake Hazards

Image: S. Marshak “Earth, Portrait of a Planet”

  • 720-800 km/h!!!
  • not noticeable at sea
  • built up coming on shore ( >10m)
  • 15 min between peak and trough

v=√10ms-2•4000m=200m/s=720km/h

  • Fig. 6.17
  • caused by submarine EQs with

vertical displacement

  • extremely long wavelength

(200 km)

  • shallow-water waves -> speed

depends on water depth D

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SIO15-18: Lecture 6 Earthquake Hazards

  • Fig. 6.15

Parking Meters in Hilo, HI SIO15-18: Lecture 6 Earthquake Hazards

  • Fig. 6.23

people ignore warning people forget what to do

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SIO15-18: Lecture 6 Earthquake Hazards

Source: NOAA

partial warning system critical components missing sporadic tsunami history poor tsunami education

  • Fig. 6.20

26 December 2004 Sumatra-Andaman Tsunami

SIO15-18: Lecture 6 Earthquake Hazards

  • Fig. 6.20

link for previous page:

https://upload.wikimedia.org/wikipedia/commons/thumb/4/47/2004_Indonesia_Tsunami_Complete.gif/250px-2004_Indonesia_Tsunami_Complete.gif

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Predicted Heights of Japan Tsunami

Background info: 27 March 1964 Good Friday Alaska EQ 12 fatalities in Crescent City

Source: NOAA/wikipedia

  • Fig. 6.19

SIO15-18: Lecture 6 Earthquake Hazards 23:11

13:11 HST

17:48

21:28 PDT

04:28

Predicted Heights of Samoa Tsunami

Source: NOAA

Crescent City, CA

Mw=8.1; Mercalli intensity VI largest EQ in 2009 tsunami locally up to 14 m > 189 fatalities

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SIO15-18: Lecture 6 Earthquake Hazards

  • Fig. 6.20

link for animation of Samoa tsunami:

https://upload.wikimedia.org/wikipedia/commons/4/4b/Samoa_tsunami_animation_20090929_samoa_a.ogv

SIO15-18: Lecture 6 Earthquake Hazards

29 September 2009 Samoa Tsunami

Source: NOAA

watch tide calendar flee when low tide suspicious you have at least 15min flee when there was an EQ and you are within 1mi of beach you have at least 15min If you felt an EQ If EQ was distant stay away from beach for many hours!!!

  • Fig. 6.24
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SIO15-18: Lecture 6 Earthquake Hazards

Samoa Tsunami Observed at Crescent City Tide Gauge

SIO15-18: Lecture 6 Earthquake Hazards

2010 Tsunami Warning and Preparedness Report by NRC (9/27/10 LA Times)

“since 2004 NOAA improved ability to detect and forecast tsunami” “many coastal communities in U.S. still face challenges in responding to a tsunami that arrives less that 1h after triggering event” “tsunami rare enough to give false sense of security” “if source is close to shore [only minutes to tsunami] public needs to recognize natural cues”