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LESSONS LEARNED FROM
PAST NOTABLE DISASTERS
          JAPAN
  PART 1A: EARTHQUAKES
NATURAL HAZARDS THAT PLACE JAPAN’S
         NATURAL HAZARDS THAT PLACE JAPAN’S
               COMMUNITIES AT RISK
                COMMUNITIES AT RISK

                              EARTHQUAKES/TSUNAMIS
GOAL: DISASTER
GOAL: DISASTER
RESILIENCE
RESILIENCE                    TYPHOONS

ENACT AND IMPLEMENT
ENACT AND IMPLEMENT           FLOODS
  POLICIES HAVING HIGH
   POLICIES HAVING HIGH
  BENEFIT/COST FOR
   BENEFIT/COST FOR           LANDSLIDES
  COMMUNITY
   COMMUNITY
  RESILIENCE
   RESILIENCE
                              VOLCANIC ERUPTIONS


                              GLOBAL CLIMATE CHANGE
THE TECTONIC PLATES
REGIONAL MAP
EARTHQUAKES


EARTHQUAKES OCCUR FREQUENTLY IN
  THE PHILIPPINES AS A RESULT OF
  COMPLEX INTERACTIONS OF THE
 PHILIPPINE AND EURASIAN PLATES
EARTHQUAKE RISK
                                             ACCEPTABLE RISK
•     QUAKE HAZARDS
•                              RISK
      BLDG. INVENTORY
•     VULNERABILITY                          UNACCEPTABLE RISK
•     LOCATION



                                             GOAL: EARTHQUAKE
                          PHILIPPINES’       DISASTER RESILIENCE
     DATA BASES
     AND INFORMATION      COMMUNITIES



                                                 POLICY OPTIONS
                                         •   PREPAREDNESS
    HAZARDS:                             •   PROTECTION
       GROUND SHAKING
       GROUND FAILURE                    •   EARLY WARNING
       SURFACE FAULTING
       TECTONIC
                                         •   EMERGENCY RESPONSE
       DEFORMATION                       •   RECOVERY and
       TSUNAMI RUN UP
       AFTERSHOCKS                           RECONSTRUCTION
CAUSES OF DAMAGE
                    CAUSES OF DAMAGE




                                        INADEQUATE RESISTANCE TO HORIZONTAL
                                                   GROUND SHAKING




                                             SOIL AMPLIFICATION

                                        PERMANENT DISPLACEMENT
                                           (SURFACE FAULTING &
                                             GROUND FAILURE)

                                       IRREGULARITIES IN ELEVATION
EARTHQUAKES                                      AND PLAN
 EARTHQUAKES

   “DISASTER
    “DISASTER                               TSUNAMI WAVE RUNUP
  LABORATORIES”
   LABORATORIES”


                                          POOR DETAILING AND WEAK
                                           CONSTRUCTION MATERIALS


                                       FRAGILITY OF NON-STRUCTURAL
                                                  ELEMENTS
SOME OF JAPAN’S NOTABLE
EARTHQUAKE EXPERIENCES

           1923
       JUNE 16, 1964
     JANUARY 17, 1995
      MARCH 11, 2011
LESSONS LEARNED FOR
 DISASTER RESILIENCE
          • ALL NOTABLE
            EARTHQUAKES
          • PREPAREDNESS
            PLANNING FOR
            THE INEVITABLE
            GROUND
            SHAKING IS
            ESSENTIAL FOR
            COMMUNITY
            RESILIENCE.
LESSONS LEARNED FOR
 DISASTER RESILIENCE
          • ALL NOTABLE
            EARTHQUAKES
          • PROTECTION OF
            BUILDINGS AND
            INFRASTRUCTURE
             IS ESSENTIAL
            FOR COMMUNITY
            RESILIENCE.
LESSONS LEARNED FOR
 DISASTER RESILIENCE
         • ALL NATURAL
           HAZARDS
         • CAPACITY FOR
           INTELLIGENT
           EMERGENCY
           RESPONSE IS
           ESSENTIAL FOR
           COMMUNITY
           RESILIENCE.
THE GREAT KANTO
  EARTHQUAKE: SEPT 1, 1923

• The Mw7.9 Great Kanto earthquake, the
  worst in Japanese history, struck the
  Kanto Plain near Tokyo in 1923 and
  resulted in the deaths of 140,000
  people.
• The fiery conflagration that followed
  the earthquake was more deadly than
  the earthquake’s ground shaking.
THE NIIGATA EARTHQUAKE:
         JUNE 16, 1964

• The M7.5 Niigata earthquake devastated
  Niigata, located 50 km south of the epicenter,
  mainly as a result of massive soil failure and
  tsunami waves.
• Although the quake only left 36 dead or
  missing and 385 injured, the material damage
  was great: 3,534 houses destroyed, 11,000
  houses damaged.
THE GREAT HANSHIN (KOBE)
 EARTHQUAKE: JAN. 17, 1995

• The M6.8 Kobe devastated Kobe.
• Ground shaking and fires together
  destroyed over 150,000 buildings
  and left about 300,000 people
  homeless, 6,434 dead, 415,000
  injured, and economic losses of
  $200 billion
THE TOHOKU EARTHQUAKE:
       JAN. 17, 1995

• The M9.0 Tojoku earthquake was
  huge, but its ground shaking did
  NOT cause the disaster that killed
  an estimated 21,000 people …
• The tsunami generated by the
  earthquake did!
TOHOKU QUAKE: THE RESULT OF
     PLATE TECTONICS
AN OFFSHORE EPICENTER
• It only took seconds for the P-
  and S-waves to reach Sendai,
  and about 15 minutes for the
  tsunami waves, but what a
  difference in damage..
THE GROUND SHAKING

• Strong ground shaking lasted 300
  seconds (compared with about 10 - 20
  seconds for the 1995 Kobe, Japan
  quake).
• But, the ground shaking did not cause
  the disaster this time; the tsunami did.
TOHOKU: SUMMARY OF
    SOCIETAL IMPACTS
• The earthquake ground shaking and the
  tsunami wave run up together caused
  major damage to 1.2 million buildings.
• Simultaneously, wide spread fires
  burned out of control.
• Economic losses were estimated at
  $574 billion.
LESSONS LEARNED FOR
 DISASTER RESILIENCE
         • ALL NATURAL
           HAZARDS
         • CAPACITY FOR
           RECOVERY AND
           RECONSTRUCTION
           IS ESSENTIAL FOR
           COMMUNITY
           RESILIENCE.
WHAT COULD BE THE NEXT EARTH-
  QUAKE DISASTER FOR JAPAN

• A difficult question, but ---
• It is one that was being asked
  before the March 11, 2011
  TOHOKU earthquake disaster.
LOCATION OF TOKAI
TOKAI EARTHQUAKE
        TECTONICS
• The Nankai trough marks the
  boundary where the
  Philippines tectonic plate is
  subducting beneath Japan
  (part of the Eurasian plate).
TOKAI EARTHQUAKE
        TECTONICS

• The section along Tokai has
  not ruptured since 1854.
TOKAI EARTHQUAKE
       TECTONICS
• The recurrence interval of
  large- magnitude
  earthquakes along this
  boundary is believed to be
  100-150 years.
TOKAI EARTHQUAKE
          TECTONICS
• At present, the land near Shizuoka
  is sinking toward the Nankai
  trough at about 5 mm/yr.
• Japan’s Earthquake Research
  Institute is on record that the
  Tokai earthquake could happen
  anytime.
TOKAI EARTHQUAKE
• Before the March 11, 2011
  Tohoku earthquake, the
  Government of Japan
  expected its next great
  earthquake to be “the Tokai
  Earthquake.”
TOKAI EARTHQUAKE

• The precise area along the
  Pacific coast- about 160 km (100
  mi) southwest of Tokyo-- that is
  expected to be affected has been
  delineated by scientific studies,
• And, by law, this area is the
  focus of intensive preparations.
FORECASTS: TOKAI
       EARTHQUAKE
• Estimated deaths — between
  7,900 and 9,200 depending on
  the amount of advance warning
  people have, the time of day
  when it occurs, and the
  tsunami.
FORECASTS: TOKAI
       EARTHQUAKE

• Estimated property damage –-
  as much as $310 billion.
FORECASTS: TOKAI
       EARTHQUAKE
• Landslides -- 6,449 specific
  locations
• Structures susceptible to
  quake-related fires – 58,402
  specific houses
TOKAI EARTHQUAKE
• The Government of Japan has an
  “early warning action plan based on
  the concept of “pre-slip.”
• Pre-slip is based on laboratory
  experiments, which indicate that a rock
  slips for a short time before it
  ultimately fails and generates a big
  quake.
MONITORING: TOKAI
         EARTHQUAKE
• The Government of Japan is currently
  deploying strain meters throughout the
  Tokai area to record the slip in order to
  provide as much advance warning as
  possible.

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Japanese earthquakes 1911 2011 lessons learned

  • 1.
  • 2. LESSONS LEARNED FROM PAST NOTABLE DISASTERS JAPAN PART 1A: EARTHQUAKES
  • 3. NATURAL HAZARDS THAT PLACE JAPAN’S NATURAL HAZARDS THAT PLACE JAPAN’S COMMUNITIES AT RISK COMMUNITIES AT RISK EARTHQUAKES/TSUNAMIS GOAL: DISASTER GOAL: DISASTER RESILIENCE RESILIENCE TYPHOONS ENACT AND IMPLEMENT ENACT AND IMPLEMENT FLOODS POLICIES HAVING HIGH POLICIES HAVING HIGH BENEFIT/COST FOR BENEFIT/COST FOR LANDSLIDES COMMUNITY COMMUNITY RESILIENCE RESILIENCE VOLCANIC ERUPTIONS GLOBAL CLIMATE CHANGE
  • 5.
  • 7. EARTHQUAKES EARTHQUAKES OCCUR FREQUENTLY IN THE PHILIPPINES AS A RESULT OF COMPLEX INTERACTIONS OF THE PHILIPPINE AND EURASIAN PLATES
  • 8. EARTHQUAKE RISK ACCEPTABLE RISK • QUAKE HAZARDS • RISK BLDG. INVENTORY • VULNERABILITY UNACCEPTABLE RISK • LOCATION GOAL: EARTHQUAKE PHILIPPINES’ DISASTER RESILIENCE DATA BASES AND INFORMATION COMMUNITIES POLICY OPTIONS • PREPAREDNESS HAZARDS: • PROTECTION GROUND SHAKING GROUND FAILURE • EARLY WARNING SURFACE FAULTING TECTONIC • EMERGENCY RESPONSE DEFORMATION • RECOVERY and TSUNAMI RUN UP AFTERSHOCKS RECONSTRUCTION
  • 9. CAUSES OF DAMAGE CAUSES OF DAMAGE INADEQUATE RESISTANCE TO HORIZONTAL GROUND SHAKING SOIL AMPLIFICATION PERMANENT DISPLACEMENT (SURFACE FAULTING & GROUND FAILURE) IRREGULARITIES IN ELEVATION EARTHQUAKES AND PLAN EARTHQUAKES “DISASTER “DISASTER TSUNAMI WAVE RUNUP LABORATORIES” LABORATORIES” POOR DETAILING AND WEAK CONSTRUCTION MATERIALS FRAGILITY OF NON-STRUCTURAL ELEMENTS
  • 10. SOME OF JAPAN’S NOTABLE EARTHQUAKE EXPERIENCES 1923 JUNE 16, 1964 JANUARY 17, 1995 MARCH 11, 2011
  • 11. LESSONS LEARNED FOR DISASTER RESILIENCE • ALL NOTABLE EARTHQUAKES • PREPAREDNESS PLANNING FOR THE INEVITABLE GROUND SHAKING IS ESSENTIAL FOR COMMUNITY RESILIENCE.
  • 12. LESSONS LEARNED FOR DISASTER RESILIENCE • ALL NOTABLE EARTHQUAKES • PROTECTION OF BUILDINGS AND INFRASTRUCTURE IS ESSENTIAL FOR COMMUNITY RESILIENCE.
  • 13. LESSONS LEARNED FOR DISASTER RESILIENCE • ALL NATURAL HAZARDS • CAPACITY FOR INTELLIGENT EMERGENCY RESPONSE IS ESSENTIAL FOR COMMUNITY RESILIENCE.
  • 14. THE GREAT KANTO EARTHQUAKE: SEPT 1, 1923 • The Mw7.9 Great Kanto earthquake, the worst in Japanese history, struck the Kanto Plain near Tokyo in 1923 and resulted in the deaths of 140,000 people. • The fiery conflagration that followed the earthquake was more deadly than the earthquake’s ground shaking.
  • 15. THE NIIGATA EARTHQUAKE: JUNE 16, 1964 • The M7.5 Niigata earthquake devastated Niigata, located 50 km south of the epicenter, mainly as a result of massive soil failure and tsunami waves. • Although the quake only left 36 dead or missing and 385 injured, the material damage was great: 3,534 houses destroyed, 11,000 houses damaged.
  • 16. THE GREAT HANSHIN (KOBE) EARTHQUAKE: JAN. 17, 1995 • The M6.8 Kobe devastated Kobe. • Ground shaking and fires together destroyed over 150,000 buildings and left about 300,000 people homeless, 6,434 dead, 415,000 injured, and economic losses of $200 billion
  • 17.
  • 18.
  • 19.
  • 20.
  • 21. THE TOHOKU EARTHQUAKE: JAN. 17, 1995 • The M9.0 Tojoku earthquake was huge, but its ground shaking did NOT cause the disaster that killed an estimated 21,000 people … • The tsunami generated by the earthquake did!
  • 22. TOHOKU QUAKE: THE RESULT OF PLATE TECTONICS
  • 23. AN OFFSHORE EPICENTER • It only took seconds for the P- and S-waves to reach Sendai, and about 15 minutes for the tsunami waves, but what a difference in damage..
  • 24. THE GROUND SHAKING • Strong ground shaking lasted 300 seconds (compared with about 10 - 20 seconds for the 1995 Kobe, Japan quake). • But, the ground shaking did not cause the disaster this time; the tsunami did.
  • 25. TOHOKU: SUMMARY OF SOCIETAL IMPACTS • The earthquake ground shaking and the tsunami wave run up together caused major damage to 1.2 million buildings. • Simultaneously, wide spread fires burned out of control. • Economic losses were estimated at $574 billion.
  • 26. LESSONS LEARNED FOR DISASTER RESILIENCE • ALL NATURAL HAZARDS • CAPACITY FOR RECOVERY AND RECONSTRUCTION IS ESSENTIAL FOR COMMUNITY RESILIENCE.
  • 27. WHAT COULD BE THE NEXT EARTH- QUAKE DISASTER FOR JAPAN • A difficult question, but --- • It is one that was being asked before the March 11, 2011 TOHOKU earthquake disaster.
  • 29. TOKAI EARTHQUAKE TECTONICS • The Nankai trough marks the boundary where the Philippines tectonic plate is subducting beneath Japan (part of the Eurasian plate).
  • 30. TOKAI EARTHQUAKE TECTONICS • The section along Tokai has not ruptured since 1854.
  • 31. TOKAI EARTHQUAKE TECTONICS • The recurrence interval of large- magnitude earthquakes along this boundary is believed to be 100-150 years.
  • 32. TOKAI EARTHQUAKE TECTONICS • At present, the land near Shizuoka is sinking toward the Nankai trough at about 5 mm/yr. • Japan’s Earthquake Research Institute is on record that the Tokai earthquake could happen anytime.
  • 33. TOKAI EARTHQUAKE • Before the March 11, 2011 Tohoku earthquake, the Government of Japan expected its next great earthquake to be “the Tokai Earthquake.”
  • 34. TOKAI EARTHQUAKE • The precise area along the Pacific coast- about 160 km (100 mi) southwest of Tokyo-- that is expected to be affected has been delineated by scientific studies, • And, by law, this area is the focus of intensive preparations.
  • 35. FORECASTS: TOKAI EARTHQUAKE • Estimated deaths — between 7,900 and 9,200 depending on the amount of advance warning people have, the time of day when it occurs, and the tsunami.
  • 36. FORECASTS: TOKAI EARTHQUAKE • Estimated property damage –- as much as $310 billion.
  • 37. FORECASTS: TOKAI EARTHQUAKE • Landslides -- 6,449 specific locations • Structures susceptible to quake-related fires – 58,402 specific houses
  • 38. TOKAI EARTHQUAKE • The Government of Japan has an “early warning action plan based on the concept of “pre-slip.” • Pre-slip is based on laboratory experiments, which indicate that a rock slips for a short time before it ultimately fails and generates a big quake.
  • 39. MONITORING: TOKAI EARTHQUAKE • The Government of Japan is currently deploying strain meters throughout the Tokai area to record the slip in order to provide as much advance warning as possible.