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NOTABLE EVENTS AND DISASTERS OF 2014 HIGHLIGHTS OF EARTHQUAKES. Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA .
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NOTABLE EVENTS AND DISASTERS OF 2014 HIGHLIGHTS OF EARTHQUAKES Walter Hays, Global Alliance for Disaster Reduction, Vienna, Virginia, USA
EARTHQUAKES are small to awesome manifestations of energy released in the form of seismic waves and tsunamis as tectonic plates of the Earth’s crust slowly converge, diverge, or slide by each other
2014: EARTHQUAKES ARE A GLOBAL NATURAL HAZARD CONTINUUM • FLOODS • SEVERE WINDSTORMS • EARTHQUAKES • DROUGHTS • VOLCANIC ERUPTIONS • ETC.
2014: THE TECTONIC PLATES THAT HAVE BEEN MOVING FOR 200 MILLION YEARS CONTINUED TO MOVE
TSUNAMI FAULT RUPTURE DAMAGE/ LOSS TECTONIC DEFORMATION DAMAGE/ LOSS DAMAGE/LOSS FOUNDATION FAILURE EARTHQUAKE DAMAGE/ LOSS SITE AMPLIFICATION DAMAGE/ LOSS LIQUEFACTION DAMAGE/ LOSS LANDSLIDES DAMAGE/ LOSS DAMAGE/LOSS AFTERSHOCKS DAMAGE/ LOSS SEICHE DAMAGE/ LOSS GROUND SHAKING
NOTE: GROUND SHAKING BECOMES A POTENTIAL DISASTER AGENT WHEN IT INTERACTS WITH A COMMUNITY’S VULNERABLE AND UNPROTECTED BUILDINGS AND INFRASTRUCTURE
CAUSES OF DAMAGE INADEQUATE RESISTANCE TO HORIZONTAL GROUND SHAKING SOIL AMPLIFICATION PERMANENT DISPLACEMENT (SURFACE FAULTING & GROUND FAILURE) IRREGULARITIES IN ELEVATION AND PLAN EARTHQUAKES FIRE FOLLOWING RUPTURE OF UTILITIES “DISASTER LABORATORIES” LACK OF DETAILING AND CONSTRUCTION MATERIALS INATTENTION TO NON-STRUCTURAL ELEMENTS
2014: SUB-OCEAN EARTHQUAKES CONTINUED TO OCCUR; SOME LARGE ENOUGH TO GENERATE TSUNAMIS
NOTE: TSUNAMI WAVE RUNUP BECOMES A POTENTIAL DISASTER AGENT WHEN IT INTERACTS WITH AN UN-WARNED, UN-EVACUATED AND UN-PREPARED COASTAL COMMUNITY
CAUSES OF DAMAGE HIGH VELOCITY IMPACT OF INCOMING WAVES INLAND DISTANCE OF WAVE RUNUP VERTICAL HEIGHT OF WAVE RUNUP INADEQUATE RESISTANCE OF BUILDINGS TSUNAMIS FLOODING “DISASTER LABORATORIES” INADEQUATE HORIZONTAL AND VERTICAL EVACUATION PROXIMITY TO SOURCE OF TSUNAMI
2014: EARTHQUAKE/TSUNAMI DISASTER OF THE YEAR THE DISASTER OF THE YEAR OCCURRED IN IQUIQUE, CHILE WHERE THE NAZCA PLATE IS SUBDUCTING BENEATH CHILE-PERU
Moment Magnitude 8.2 • On April 1, the mega-thrust Iquique earthquake struck off the coast of Chile approximately 95 km (59 mi) northwest of Iquique. • The main shock was followed by a large number of moderate to very large aftershocks, including a M7.7 event.
A TSUNAMI WAVE OF 2.1 M WAS GENERATD BY THE MEGATHRUST EARTHQUAKE
IQUIQUE: NOT THE FIRST EARTHQUAKE EXPERIENCE REMEMBERING MAY 9, 1877
THE HISTORICAL RECORD • The 1877 Iquique earthquake occurred on May 9 with a magnitude estimated at 8.5-9.0 on the surface wave magnitude scale. • The earthquake shaking caused significant damage over most of the coastal parts of the Tarapaca and Antofagasta regions.
THE HISTORICAL RECORD • The earthquake triggered a devastating 10 m (33 ft) tsunami wave along about 500 km (310 mi) of coast, from Arica in the north to Meiillones in the south.
M6.1 EARTHQUAKE STRIKES NORTHERN YUNNAN PROVINCE 4:30 pm, JULY 22, 2013
VULNERABLE BRICK HOUSES • The homes that collapsed in Ludian (a population of about 429,000), were mostly old brick houses having little resistance to strong ground shaking.
A M6.0 EARTHQUAKE STRIKES NAPA, CA(USA’S WINE COUNTRY) 3:20 AM, AUGUST 24, 2014
SAN FRANCISCO BAY AREA The Bay Area is prone to moderate- to large- magnitude earthquakes because it straddles the boundary between two major tectonic plates — the North American and Pacific plates.
NAPA: SURROUNDED BY SAN ANDREAS, HAYWARD, AND OTHER FAULT ZONES
The M6.0 Napa earthquake was the strongest in the San Francisco Bay area since the 1989 M6.9 Loma Prieta quake, BUT it only had about 1/30th of Loma Prieta’s energy release
SOCIOECONOMIC IMPACTS • Loss of power, gas, and water for 70,000 people. • Injuries, but no deaths
SOCIOECONOMIC IMPACTS • Local damage to buildings and houses, infrastructure, and interior contents of homes and stores. • $ Millions from extensive loss of product (wine)
BEYOND 2014: Communities throughout the world know why it is urgent for their stakeholders to continue working on becoming EARTHQUAKE- and TSUNAMI- DISASTER RESILIENT
Each community knows that it is only a matter of time until the inevitable earthquake occurs that can expose its physical and social vulnerabilities
PREPAREDNESS • PROTECTION • EM RESPONSE • RECOSTRUCTION AND RECOVERY EARTHQUAKE DISASTER RESILIENCE ACCEPTABLE RISK RISK UNACCEPTABLE RISK BOOKS OF KNOWLEDGE • MONITORING • HAZARD MAPS • INVENTORY • VULNERABILITY • LOCATION DATA BASES AND INFORMATION YOUR COMMUNITY HAZARDS: GROUND SHAKING GROUND FAILURE SURFACE FAULTING TECTONIC DEFORMATION TSUNAMI RUN UP AFTERSHOCKS
SEISMICITY TECTONIC SETTING & FAULTS EARTHQUAKE HAZARD MODEL
FAULTS, EARTHQUAKES, AND RECURRENCE INTERVALS • A LONG FAULT IS NEEDED TO GENERATE A LARGE-MAGNITUDE EARTHQUAKE. • LARGE-MAGNITUDE EARTHQUAKES HAVE RECURRENCE INTERVALS OF 100 YEARS OR MORE; SEVERAL TIMES LONGER THAN THOSE FOR SMALL- TO MODERATE- MAGNITUDE EARTHQUAKES
THE USA’S OTHER NOTABLE PLATE BOUNDARY FAULT ZONE • THE JUAN DE FUCA PLATE • SUBDUCTING BENEATH WASHINGTON AND OREGON; • POTENTIAL FOR M9.0
CHILE’S NOTABLE PLATE BOUNDARY FAULT ZONE • THE NAZCA PLATE • SUBDUCTING BENEATH CHILE AND PERU • HAS GENERATED M8-9.5 QUAKES