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Building Resilience by Addressing the Challenges of a Strong Earthquake (BRACE) February 25, 2015 Renato U. Solidum, Jr. Philippine Institute of Volcanology and Seismology Department of Science and Technology

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Page 1: Building Resilience by Addressing the Challenges of a ...carlospromulo.org/wp-content/uploads/2015/02/Dr.-Renato-Solidum.pdf · Building Resilience by Addressing the Challenges of

Building Resilience by Addressing

the Challenges of a Strong

Earthquake (BRACE)

February 25, 2015

Renato U. Solidum, Jr.

Philippine Institute of Volcanology and Seismology

Department of Science and Technology

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PHILIPPINE HAZARDSCAPE

Earthquake Tsunami Volcanic eruption

Typhoon Storm surge Flood Landslide

The Philippines is 3rd in the world most exposed

and at risk to natural hazards (World Risk Report, 2013)

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M7.8 1990 Luzon Earthquake

M6.9 2012 Negros Or Earthquake

(~90 destructive earthquakes for past 400 years)

EARTHQUAKE ACTIVITY IN THE PHILIPPINES

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WEST

PHILIPPINE

SEA

SULU

SEA

CELEBES

SEA

PHILIPPINE

SEA

Local Tsunami-Affected Areas in the Philippines

Local Tsunami in

the Philippines

Epicenter of tsunamigenic

earthquake

(~ 40 tsunamis for past 400 years – 1 in 10 years)

Coastal areas at eastern

and western margins

fronting major seas and

inland seas have been

affected by tsunamis

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M7.2 2013 BOHOL EARTHQUAKE

Affected Bohol and Cebu Casualties:

Dead - 222

Missing - 8

Injured - 976 Houses damaged:

Total - 14,512

Partial - 58,490

Roads, bridges, seaports

damaged

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Can strong earthquakes affect

Metro Manila and vicinity?

YES

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LATEST DAMAGING EARTHQUAKE

IN METRO MANILA

• M 7.3 Casiguran, Aurora

Earthquake, 02 August

1968

• Ruby Tower in Manila

collapsed – 268 killed, 260

injured

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HISTORICAL CHURCH WITH

EARTHQUAKE ACCOUNTS

• “partially destroyed by

earthquake of 1600”

• “destroyed by the earthquake

of 1645”

• “destroyed by the earthquake

of 3 June 1863”

Manila Cathedral

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• “withstood the earthquakes of

1645, 1658, 1754, and 1863”

• “the masonry roof of the

Church collapsed in the

earthquake of 1880”

Guadalupe Church - Makati

HISTORICAL CHURCH WITH

EARTHQUAKE ACCOUNTS

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EARTHQUAKE GENERATORS IN

METRO MANILA AND VICINITY

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THE VALLEY FAULT SYSTEM

• West Valley Fault

(WVF) movement

mainly horizontal

• WVF moved 4 times in

past 1400 years;

movement interval ~

400 years

• Last major earthquake

from Valley Fault in

1658

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HISTORICAL TSUNAMIS IN

METRO MANILA

• November 9, 1828 – estimated tsunami height 1

meter

“At the port (of Manila), people on board ship felt the shocks

strongly as if they struck a hard object. The river level rose quickly

after the quake to rainy day water level and inundated lowlands

near its banks.”

• June 3, 1863 – estimated tsunami height 1-2 meters

“In Manila Bay, the wave action was observed by the captains on

board two English frigates. They described the wave as coming

from SE to NW. It then struck their ships forcefully and water

completely covered the deck.”

From Bautista and others, 2013

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Hazards and Risk Scenarios for

Metro Manila

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The Worst Case

Scenario Earthquakes

for Metro Manila

Model M Characteristics

08 – West

Valley Fault 7.2 Severe Damage

13 – Manila

Trench 7.9 Tsunami

West

Valley

Fault

Manila

Trench

Metro Manila Earthquake Impact Reduction Study (JICA-MMDA-PHIVOLCS

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EARTHQUAKE-RELATED HAZARDS

Tsunami Fire

Ground Shaking Liquefaction

Landslide

Faulting (Ground)

Rupture

Fault

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FAULTS

Strike Slip (Horizontal)

Normal

Thrust

• fractures where rock

movement has taken

place and earthquakes

have been produced

• active faults are

those that have

produced earthquakes

historically or has

moved for the last

10,000 years

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GROUND RUPTURE HAZARD MAP FOR

METRO MANILA

Metro Manila cities

transected by the

West Valley Fault:

• Quezon City

• Marikina

• Pasig

• Makati

• Taguig

• Muntinlupa

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AVOIDING EFFECTS OF GROUND RUPTURE

• Avoid

construction of

structures on

top of an active

fault

• House or

building should

be at least 5

meters away

from the trace

of the fault

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GROUND SHAKING

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MAGNITUDE

Energy released during

earthquake.

INTENSITY

Effect or felt strength at the surface

STRENGTH OF EARTHQUAKE:

MAGNITUDE VERSUS INTENSITY

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GROUND SHAKING M7.2 West Valley Fault Earthquake

(Risk Analysis

Project, 2013)

NCR

BULACAN

RIZAL

CAVITE LAGUNA

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GROUND SHAKING M6.5 West Valley Fault Earthquake

(Risk Analysis

Project, 2013)

NCR

BULACAN

RIZAL

CAVITE LAGUNA

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INTENSITY VIII (VERY DESTRUCTIVE)

GROUND SHAKING

1995 Kobe Earthquake

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BUILDING AND CASUALTY ESTIMATES (1) FOR METRO MANILA FROM A M7.2 WEST VALLEY FAULT EARTHQUAKE

Residential Building (1,325,896)

Damage Heavy -168,300 (12.7%) Partly - 339,800 (25.6%)

Public Buildings

Damage Heavy - 8-10% Partly - 20-25% 10-30 Storey Building

Damage Heavy - 11% Partly - 27%

30-60 Storey

Damage Heavy - 2% Partly - 12%

Population (9,932,560)

Casualty Dead 33,500 (0.3%)

Injured 113,600 (1.1%)

Additional Deaths by Fire 18,000

Metro Manila Earthquake Impact Reduction Study, 2004 – JICA, PHIVOLCS, MMDA

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BUILDING AND CASUALTY ESTIMATES (2) FOR METRO MANILA FROM A WEST VALLEY FAULT EARTHQUAKE

Risk Analysis Project, 2013 – PHIVOLCS, UP-ICE, GA (AusAID)

M7.2 M6.5

Total Floor Area in Complete 88,142,000 65,407,000

to Collapsed Damage (sqm)

Total Floor Area in Slight 172,924,000 162,799,000

to Extensive Damage (sqm)

Total Fatalities (Death) 31,000 23,000

Total Injuries Very Serious 14,000 10,000

Serious 112,000 85,171

Slight 385,000 302,000

Total Economic Losses (millions of PhP) 2,269,000 1,773,000

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• Loose, water-rich sediments behave like

liquid during strong ground shaking.

• Sediments are rearranged into a more

compact state.

LIQUEFACTION

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LIQUEFACTION

Subsidence of bridge column Subsidence of building, roads

Dagupan 1990

Fissuring of roads

Mindoro 1994

Dagupan 1990

La Union, 1990

Damage to buried pipes, tanks

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(READY for GMMA Project, 2013)

LIQUEFACTION POTENTIAL M7.2 West Valley Fault Earthquake

Localities prone to liquefaction

a) water-saturated (shallow water table), low-lying

b) Have loose

(unconsolidated), sand or silt deposits

• river banks, abandoned

rivers, flood plains

• coastlines

• swamps

• reclaimed land

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(MMEIRS, 2004)

FIRE AFTER THE EARTHQUAKE M7.2 West Valley Fault Earthquake

*MMEIRS, 2004

Pasig Manila

Marikina

Muntinlupa

Taguig

Pasay

Paranaque

Las Pinas

Quezon

City

Makati Mandaluyong

Navotas

Malabon Caloocan

Valenzuela

San Juan

Pateros Maximum Burnt Number

500 - 1,000

200 - 500

100 - 200

50 - 100

20 - 50

1 - 20

• Fire outbreak by

electrical short circuit;

toppling of lamps,

candles

• Explosion of

petroleum, gas tanks

may cause spreading

of fire

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• West

• Fire, Building Damage

• North

• Bridge Damage

• South

• Bridge Damage

• East

• Building Damage, Bridge Damage

POSSIBLE

ISOLATION DUE

TO EARTHQUAKE

IMPACTS (West Valley Fault Scenario)

(MMEIRS, 2004)

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TSUNAMI SCENARIO M8.3 Earthquake from Manila Trench

Estimated Tsunami

Height in Manila Bay:

• 3.5 meters (mean sea

level)

• 5.5 meters (+ 2m from

tide)

Arrival Time:

• > 1 hour

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TSUNAMI HAZARD

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GOALS FOR RISK REDUCTION IN

METRO MANILA (MMEIRS, 2004)

• Develop local and national governance and

business system resistant to strong earthquakes

• Improve resiliency of urban structures and

settlements

• Enhance current risk and emergency

management

• Enhance community disaster management

capacities

• Formulation of reconstruction system

• Promotion of research and technology

development

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PRIORITY STRATEGIC APPROACH TO

CONTEND WITH STRONG EARTHQUAKE

Focus Concept

1 – Strengthen

Legal

Framework and

Institutional

Capacity for

Disaster

Management

• Enhance Legal Basis and

support

• Strengthen Institutional

Capacity for Mitigation,

Preparedness and Response

as well as Inter-Institutional

Coordination

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PRIORITY STRATEGIC APPROACH TO

CONTEND WITH STRONG EARTHQUAKE

Focus Concept

2 – Build

Capacity for

Relief and

Recovery

• Enhance Emergency Health

and Medical Response

System

• Establish Emergency

Transportation System

• Secure sea ports, airports

• Secure water source and

supply

• Secure power and

communication systems

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PRIORITY STRATEGIC APPROACH TO

CONTEND WITH STRONG EARTHQUAKE

Focus Concept

3 – Strengthen

Community

Preparedness

for Earthquakes

and Tsunamis

• Enhance self-reliance and

mutual help for efficient risk

management capacity

• Inculcate Disaster Mitigation

Culture among populace

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PRIORITY STRATEGIC APPROACH TO

CONTEND WITH STRONG EARTHQUAKE

Focus Concept

4 – Reduce

Seismic

Dangers of

Residential

Structures

• Strengthen Buildings,

Structures

• Promote and Institute Fire

Safety

• Promote and support further

researches on seismic

hazards and better building

technology

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PRIORITY STRATEGIC APPROACH TO

CONTEND WITH STRONG EARTHQUAKE

Focus Concept

5 – Enhance

National System

to Become

Resistant to

Impact of

Earthquakes

• Protect stability of

government function

• Ensure continuity of socio-

economic systems

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KEY MESSAGES

• Metro Manila and surrounding provinces are prone to

extreme natural events, such as strong earthquakes

and tsunamis. • A large earthquake from the West Valley Fault can

significantly affect Metro Manila and vicinity. A large

earthquake from the Manila Trench can generate a

tsunami that can affect the coastal areas of the

metropolis. • Disaster risk reduction and management efforts must

take into account appropriate science-based

scenarios.

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/PHIVOLCS

@phivolcs.dost

www.phivolcs.dost.gov.ph

Earthquake & Tsunami (24/7):

Tel. Numbers

+632 929-9254

+632 426-1468 loc 124 / 125

Fax number

+632 927-1087

Volcano (24/7):

Tel. Numbers

+632 426-1468 loc 127

Telefax number

+632 927-1095

IEC materials:

+632 426-1468 loc 128

+632 927-4524