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Great Tohoku Earthquake and Tsunami, March 11, 2011

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Presentation on theme: "Great Tohoku Earthquake and Tsunami, March 11, 2011"— Presentation transcript:

1 Great Tohoku Earthquake and Tsunami, March 11, 2011
Image from "SH-60B helicopter flies over Sendai" by U.S. Navy photo. This Image was released by the United States Navy with the ID N-0000X-003 (next). Licensed under Public Domain via Commons - Great Tohoku Earthquake and Tsunami, March 11, 2011 Version: Sept 10, 2015

2 Tohoku Earthquake & Tsunami Facts
Magnitude 9.0 – March 11, 2011 Societal preparation had been for ~Mag 8 ~20,000 people dead or missing Fukushima nuclear disaster >1 million buildings damaged or destroyed In 2015, >200,000 people still displaced Image source: (public domain)

3 Hazard versus Risk Hazard: Physical process that has the potential to cause loss or damage to something valued by an individual or a society Risk: Likelihood of asset or life damage/loss due to an extreme event It is critical that students understand the difference between hazard and risk. Societies do not have control over the geohazards that exist. However, decisions we make most definitely determine the risk to our valued assets (including human life). Modified from InTeGrate module “Natural Hazards and Risk” Unit 1

4 HAZARD RISK Show the class one of the better videos that students find, which depicts ongoing damage from the tsunami or earthquake. Example: Ask them to identify what things they see are the HAZARD and which are the RISK. If you choose, you can come out of presentation mode and type what students say directly into the pptx OR write on a nearby chalk or white board. Types of answer to look for: Hazard (the main process being observed): in most cases this will be a visual of the tsunami itself or possibly earthquake shaking Risk: the placement of the city where it is, the way the city and maybe sea wall were constructed, the mobility of boats and other items being moved, the strength of the buildings, etc.

5 Shaking-Related Hazard
Potential questions: How many people were exposed to shaking that has the potential to cause moderate to heavy damage to resistant structures? How is this illustrated in the figure in the upper right? All images from USGS PAGER alert: in public domain Gray scale: Population per ~1 sq. km. from LandScan USGS PAGER

6 Financial cost of damage
Potential questions: Start by NOT showing the graph and asking students to predict the most costly type of damage from the earthquake and tsunami. Discuss briefly and then show the graph. Were they correct or not? Data from Cabinet Office of Japan. Figure modified from Additional details can be found at Total = >$200 billion (16.9 trillion yen) Damage estimate as of June 2011 Subsequent estimates are as high as $300 billion Source: Cabinet Office of Japan, 24 June 2011

7 Fukushima Nuclear Disaster
Potential questions: How many times higher than natural background radiation was the average for the 20 km evacuation area? What type of health effects could have occurred for unprotected people on the Fukushima plant grounds? Left image: "Towns evacuated around Fukushima on April 11th, 2011" by User:Mayhewderivative work: derived from original work by User:Lincun - File:Iitate_vs_Fukushima_evacuation_zones_large.svgderivative work: original source is File:Iitate_in_Fukushima_Prefecture_Ja.svg. Licensed under CC BY-SA 3.0 via Commons - Right image: "Fukushima7" by Rama C. Hoetzlein (Rchoetzlein at en.wikipedia) - Own work. Released in public domain.. Licensed under CC0 via Commons -

8 Tectonic Setting The earthquake occurred along the bounding fault between the Pacific and Amur (Eurasian) plates. Potential questions: What sort of plate boundary is this? What are at least two lines of evidence for this? Source: USGS event poster: in public domain

9 Tsunami Potential questions:
How many prefectures accounted for most of the life loss? Where are the highest observed tsunami heights? When did the tsunami arrive at these locations? Tsunami due largely to static (long-term) displacements. Left image source: (Permission for non-commercial use) Right image source: public domain

10 Rupture Model 100 km Seismic waves (and GPS displacements) can be used to model the slip on the fault surface at depth. Potential questions: What was the maximum slip? What was the length of the portion of fault that slipped in the strike direction? Use the 1m contour to define the main slip patch. What was the length of the portion of fault that slipped in the dip direction? Use the 1m contour to define the main slip patch. What was the area of the fault that slipped? Note that moment = slip * Area * stiffness of the surrounding rock. This is a measure of the size of the earthquake. The moment magnitude is based on the log of the moment. Source: in public domain

11 Coseismic Displacements
Horizontal Vertical In addition to shaking the ground also experienced long-term (static) displacement. Potential questions: How far, and in what direction, did the east coast of Japan, near Sendai, move horizontally? How far, and in what direction, did the east coast of Japan, near Sendai, move vertically? Images source: UNAVCO Preliminary highly smoothed model of coseismic slip for the 11 March main shock. Red and yellow vectors show horizontal (left) and vertical (right) predicted and observed displacements respectively. Model is constrained by both GPS displacements and 12 DART buoy tsunami records. GPS offsets are derived from 5 minute epoch time series processed by the ARIA team at JPL and Caltech. Displacements due aftershocks have been isolated and removed. This model was generated by Caltech Tectonics Observatory as part of the ARIA project. All original GEONET RINEX data provided to Caltech by the Geospatial Information Authority (GSI) of Japan. (

12 Reflecting on what you have learned
What surprised you most in what you have learned about the 2011 Tohoku Japan Earthquake? What else would you like to know about this earthquake? These questions are included to help students reflect on their learning process. Reflection on learning (or “metacognition”) is a critical component of solidifying learning.


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