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
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!
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.