reducing earthquake losses in the extended mediterranean ... · losses in the extended...

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R R e e d d u u c c i i n n g g E E a a r r t t h h q q u u a a k k e e L L o o s s s s e e s s i i n n t t h h e e E E x x t t e e n n d d e e d d M M e e d d i i t t e e r r r r a a n n e e a a n n R R e e g g i i o o n n UNESCO-RELEMR XXXV International Workshop 28-31 October 2013 Fuengirola (Malaga), Spain

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Page 1: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

RReedduucciinngg EEaarrtthhqquuaakkee LLoosssseess iinn tthhee EExxtteennddeedd MMeeddiitteerrrraanneeaann RReeggiioonn

UUNNEESSCCOO--RREELLEEMMRR

XXXXXXVV IInntteerrnnaattiioonnaall WWoorrkksshhoopp

28-31 October 2013

Fuengirola (Malaga), Spain

Page 2: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

RReedduucciinngg EEaarrtthhqquuaakkee LLoosssseess iinn tthhee EExxtteennddeedd MMeeddiitteerrrraanneeaann RReeggiioonn

UUNNEESSCCOO--RREELLEEMMRR XXXXXXVV IInntteerrnnaattiioonnaall WWoorrkksshhoopp

28-31 October 2013

Fuengirola (Malaga), Spain

Page 3: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

SC/DRR/2013/1 Paris, France. October 2013

Original: English

United Nations Educational, Scientific and Cultural Organization – UNESCO U.S. Geological Survey – USGS Real Instituto y Observatorio de la Armada in San Fernando – ROA Network of European Research Infrastructures for Earthquake Risk Assessment and Mitigation – NERA

Editorial coordinators: Frederick Simon

Jose Martín Davila Jair Torres

Cover photo credit: Badaoui Rouhban

For further information, please contact:

Cross-Cutting Thematic Unit on Disaster Risk Reduction Natural Science Sector UNESCO 1, rue Miollis 75732 Paris cedex 15 France Phone: + 33-1-45 68 41 22 Fax: + 33-1-45 68 58 21 E-mail: [email protected]

The authors are responsible for the choice and presentation of facts contained in this publication and for the opinions expressed therein, which are not necessarily those of UNESCO and do not commit the Organization. The designations employed and the presentation of the material throughout this publication do not imply the expression of any opinion whatsoever on the part of UNESCO concerning the legal status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.

© UNESCO 2013 Printed in Spain

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XXXV UNEReducing

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XXXV UNEReducing

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XXXV UNEReducing

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XXXV UNEReducing

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XXXV UNEReducing

Tenth S 11:30 – 11:30 –

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XXXV UNEReducing

15:15 –

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XXXV UNEReducing

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Page 18: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

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Page 19: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

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and historwith the bed in the pa

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icity of Nil

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ealed that tthese placeactivity an

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20

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XXXV UNEReducing

In this sboth forzones b Earthqucompilecatalogdeclusteusing ddifferen The parrecent estimat The b-vseismicestimatevents distribuparameseismog The seperformterms oengineeMorocc

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des et Surveent of Physic

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source zoneand seismicsmic, seism

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e seismic ha

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anean Region (R

smogenic -Morocco

Peláez(2), A

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e model forc hazard st

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oped by Kijof the maxazard param

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ed to site-sossible acc

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RELEMR): Fuen

Source Zoo Region

A. Kijko(3) an

mique, CRAity of Jaén, Pretoria, Pre

r the Algeriaudies. The

and geophys

nalyzed usinrthern Algeemoved by udes of comacter of the

ko & Grahaximum posmeters.

relationshing an exteen, we der

ssible magnyzed in dep

computed-Morocco re

pecific seisceleration adence in Tpulated and

ngirola (Malaga)

one Mode

nd A. Talbi(1)

AAG, AlgierJaén, Spai

etoria, Sout

a-Morocco delineationsical data.

ng recent eeria in forme

adapting Gmpleteness

sub-catalo

am (1998, 1ssible earth

ip, taken aension of thrive the acnitude mmax

pth using pd and anaegion.

smic hazardand seismicT years, givd industrial c

), Spain 2013

el in the

)

rs, Algeria. n. thAfrica.

region is pn includes fi

arthquake cer studies. Gardner & mc were esgs obtained

1999), incluhquake ma

as an area-he Aki-Utsu ctivity rate λx and its proarametric alyzed for t

d, which hac hazard cuven a hypocities in the

21

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catalogs In these Knopoff

stimated d for the

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Page 25: Reducing Earthquake Losses in the Extended Mediterranean ... · Losses in the Extended Mediterranean Region UNESCO-RELEMR ... Seismologi ons particip bout the sta e a presen ”

XXXV UNEReducing

A probasequenanalysisand therange b0.03 an The mofractionfractionthat an the mbL

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abilistic modces occurres of two see p-value, ebetween 0.7nd 1.43 ± 0.

odified Bath of the accu of energy 80% of the

g 4.8, Bulladimension Dio, as the re, we havevent, 58% arthquakes.

the correlaed, and the

R International sses in the Exte

atistical aS

M. Ha

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eismicity paexplaining th77 ± 0.05 a10, showing

h’s law is usumulated eis released

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e obtained afor the La .

ations betwAki’s relatio

Workshop ended Mediterra

nalysis ofSouth and

amdache(1),

ent Etudes ent of Physi

ed to analyzh and Soutrameters: the tempora

and 1.18 ± 0g broad reg

sed to analnergy is reld during thrgy is releasd an 87% dated using

e slip occura slip ratio ePaca 2005

ween the fron D=3b/c is

anean Region (R

f some aft Southeas

J.A. Peláez

et Surveillacs, Univers

ze the spatitheastern Sthe b-value l decay rate0.10. The cimes of the

yze the eneeased in the aftershocsed during

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5, 50% for t

ractal dimes discussed

RELEMR): Fuen

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z(2) and A. T

ance Sismiqsity of Jaén,

io-temporalSpain. This

of the freqe of aftersh

computed p-e temporal d

ergy partitiohe main shock sequencthe mbLg 4.

mbLg 4.8, La tion integramary fault s% for the Mthe Lorca 2

ension, the d as well.

ngirola (Malaga)

sequencesin

Talbi(1)

que, CRAAG Jaén, Spai

behavior ostudy focu

quency-maghocks. The -values ran

decay of afte

oning. It suock, and once. For exa.8, Mula 19Paca 2005

al, and then segment toMula 1999, 2011, and 6

b-value an

), Spain 2013

s in

G. in

of eleven aftuses mainlygnitude distcomputed bge betweenershocks.

ggests thatly a relative

ample, we o999, an 88%5, earthquak

used to deo the total s

61% for th63% for the

nd the p-va

22

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t a large ely small obtained % during kes. The erive the slip. For e Bullas e Gador

alue are

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XXXV UNEReducing

De

Algeria Europedestrucaccelercurrentland contype, earecordsderive a The coattenuaBoore Tanakaaccordi Spectraconstituhomogedata onmodel. The obtto 0.32larger mspectragood ag

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rivation of

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is located an plate.

ctive moderarographs nely a very ricntains inforarthquake a

s (2<Ms<6.9an attenuati

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a, 1992]. Tng to magn

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tre National

on the norNorthern Aate-to-stronetwork (335ch data banrmation regand station9 and 7< Dion relations

pectral atteeological sita two-step

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lts show thadata), and and lower dons are stu

with classica

Workshop ended Mediterra

attenuatioegional str

Na

de RecherAl

rthern edgeAlgeria is ng earthqua5 stations), nk. From tharding the s locationshypo <160 Kship for Alg

enuation mote conditionp inversionation modeocentrale dis

re derived fong motionTwo models, and the s

at the PGA the local m

distance. Thdied and do

al published

anean Region (R

on relatiorong motio

asser Laoua

rche Appliqulgiers, Alge

e of the Afra highly skes in the pseveral eais data banmagnitude

s …etc. ActKm). One oeria.

odel accouns. The regr [Fukushiml describesstance, and

from 1155 hn records s are then

second one

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rican plate, seismic arepast. Since arthquakes nk, a strong

(Ms), the tually, the cf the most

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ma and Tas the evolud category o

horizontal c(55%) an

studies, the consider t

deviation derestimates t

values betit any bias. tion attenua

ngirola (Malaga)

eria basedase

nie Parasism

which is cea that exthe installawere recormotion cat

hypocentracatalog conimportant a

ometrical spthod, introd

anaka, 1990ution of spof the site.

componentsnd Europeae first one he whole d

ecreases frothe predicteween obseThe inferre

ation laws.

), Spain 2013

on local a

mique

converging xperienced ation of the Arded and cotalog is esta

al distance, ntains arounapplications

preading, auced by joy0; Fukushi

pectral acce

s. The dataan recordsconsiders A

data called

om 0.33 (loced accelerarved and p

ed regional

23

and

with the several

Algerian onstitute ablished the site

nd 1000 s was to

anelastic yner and ma and eleration

sets are s (45%) Algerian regional

cal data) ation for redicted law is in

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XXXV UNEReducing

Quarry

Groundproblempipelineenvironground (NCC) sof the qcompreof Surfaquarry baccordienvironScaled Pressuranalysisdamage

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d vibrations ms in the ques. Thereformental effevibration

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R International sses in the Exte

AssessmePipelin

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induced byuarrying indre, a vibratiects of blasmeasuremeof Helwan csts on the ves and the(MASW) aresults demInternationa

ects is 650(SD) relatiot) formula (Amum allowaof 12.5 mm/

Workshop ended Mediterra

nt and Thes, South

Ela A. Moh

y Departmef Astronomy

y blasting iustry and mion control sting in quaents inducecity, Egypt. oil pipelinee shear wavare used to monstrate thal Building m, followi

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anean Region (R

eir Enviroeast of He

amed and A

nt, the Natioy and Geop

n the cememay cause sstudy playsarries. Thised by blasThe aim ofs of SUMEve velocity evaluate th

hat, the closCode (IBC

ng the dedV = 440.64152.87 × S

e weight perclosest site

RELEMR): Fuen

onmental Ielwan City

Adel M. E. M

onal Reseaphysics, Egy

ent quarriessevere dams an import research

sting at thef this study ED Companobtained fro

he closest ssest site of C) and theduced Peak4 × SD-1.22

SD-0.071) in dr delay was of the SUM

ngirola (Malaga)

mpacts oy, Egypt

Mohamed

arch Instituteypt

s are one omage to the

ant role in paper pres

e National is to invest

ny. The seom the Mulsite of the twthe two pip

e safe distak Particle V25) in mm/sB. In the ligfound to be

MED pipeline

), Spain 2013

n the Nea

e

of the fundnearby utilithe minimiz

sents the reCement Ctigate the inismic refraclti channel Awo pipelineelines is of ance to avVelocity (PPs and the Aght of the pre 591 m/kg0

es.

24

rby Oil

amental ities and zation of esults of

Company nfluence ction for Analysis

es to the class B,

void any PV) and Air over rediction 0.5 with a

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XXXV UNEReducing

Nor

(1)Dep

North AdevastaconsideNorth-Athe besGroup 2000 udiverse Sudan) In this pstudy, bmaps oThen, win termsaccelerinforma Referen Mou

CheJ., KG.FSeis10.1

ESCO-RELEMREarthquake Los

rth African

pt. of Physic(2)Centre

Africa is oating earthqerable econAfrican Sciest seismic hfor Earthqunder the agroup of

.

paper, we bby the grouof North Afrwe describes of the distration. Thesation necess

nce urabit T. Abeddadi A., CKsentini A.,

F., Peresan smic Hazar1007/s1095

R International sses in the Exte

n Group fohaz

Mo

cs and Cente de Reche

C

ne of the quakes, somnomic damaentists to joihazard assuake and Taegis of ICT

North Afric

briefly presup, that aimrica includine the seismotribution of se thematicsary for the

bou EleneanChourak M., Jabour N

A., Romdrd Assessm

50-013-9375

Workshop ended Mediterra

or Earthquzard asses

urad Bezze

tro de Geoferche en AsCRAAG, Bou

most eartme of themage to the rn their effo

sessment aTsunami stuTP (Triestecan countr

ent the nated at produ

ng five counotectonic comaximum dc maps absustainable

n K. M., Aya., ElGabry M., Magrin Ahane N., Vment in No5-2

anean Region (R

uake and Tssment in

eghoud(1)and

física de Évtronomie, Auzaréah, Al

hquake-prom tsunami-trregion. Thurts in ordernd risk mitudies (NAG

e, Italy). It ries (Moroc

ure, missioucing Neo-dntries: Moroontext of Nodisplacemebout earthqe social and

adi A., BenoM. N., Harb

A., MaoucheVaccari F.aorth-Africa,

RELEMR): Fuen

Tsunami sn North Afr

d Assia Har

vora, ECT, UAstrophysiqugiers, Alger

one areas riggering, ins it was imr to capitalizigation of t

GET, previois structure

cco, Algeria

n and objedeterministiocco, Algerorth Africa ant, maximuuake haza

d economic

ouar D., Bebi A., Hfaiede S., Meghnd ZuccoloJournal of

ngirola (Malaga)

studies anrica

rbi(2)

University oue et Géopria

of the Menflicted heaportant andze on any sthe region. ously NASGed as a paa, Tunisia,

ctives of NAc seismic h

ria, Tunisia,and present m velocity, rd constitudevelopme

en Suleman dh M., Husraoui M., O

o E., 2013.f Seismolog

), Spain 2013

nd the seis

of Évora, Pohysique,

editerraneanavy loss of d necessarysynergies aThe North

G) was fourtnership aLibya, Eg

AGET and hazard asse, Libya, andthe maps oand designte importan

ent of North

A.,Bezzegssein H. M.,Ousadou F. Neo-Detergy, accepte

25

smic

ortugal

n. Many life and

y for the iming at African

unded in among a ypt and

the first essment d Egypt. obtained n ground nt basic Africa.

houd M. , Kacem , Panza rministic ed. DOI

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XXXV UNEReducing

Propo

The resRC infilinterior type of countrieinspectdevelopvulneraassessmbuildingground methodconstruarea grmediumclassifiehorizonand ovebuildingAnalyticinfill wausing nanalysisBasic Cdesign modifielimit CI considebuildingimplies Assessmain cit KeywoRapid analysis

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H

Jo

sidential builed frames.frames bou

f constructioes, is not weion and anapment and ability of exment methogs as adeq

motions ad is only ccted betweroups wher

m rise (4-6 sed into regtal irregulaerhangs ongs were ancal computealls to the lanonlinear dias was carri

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that the bment formsties in Jorda

rds assessmens; capacity

R International sses in the Exte

ndexing Mor Existing

Hanan S. Al-

ordan Unive

ilding stock The exteriound masonon, which cell-defined. alysis requiapplication

xisting resod is a rapiduate, in ternd thereforconcerned

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ateral resistaagonal comed out to adex (BCI) war value (c

at the CapCapacity Ind

ld experiened as in nebuilding uns were desigan.

nt; reinforceindex.

Workshop ended Mediterra

Method forg Residen

-Nimry, Sad

Departmenersity of Sci

k in Jordan or frames ary panels bcould only Identificatires enormo

n of an indidential stod and yet sirms of humre require fwith the

nd 2005. Barea groupght categorirregular suacks and reic performa

arrive at of the reprance and st

mpressive sarrive at thewas obtainecode value)pacity Indexex value be

nce moderaeed for furtnder considgned and u

ed concrete

anean Region (R

r Rapid Asntial Stone

ddam H. Qe

nt of Civil Eence and T

is dominateare infilled wbuilt of concbe found ion of seism

ous time andexing methone-concretimple evalu

man life safefurther detalocal low

Buildings su is further ries. Under ubcategoriee-entrant c

ance of locathe basic

resentative tiffness of ttruts. Using

e capacity ced for each ). This wasx (CI) of theelow the limate damagether detailederation coused to eva

e; infilled f

RELEMR): Fuen

ssessmene-Concrete

eran, Musa

ngineering,Technology,

ed by a locawith stiff stoncrete blocksin Jordan a

mically inaded effort. Thhod for rapte building

uation methoety, or thosailed evaluaand mediubject of theclassified each area-

es. The efforners), ve

al buildings parametersbuildings whe represeng SAP2000curves of thbuilding us

s later mode building wmit value inde during and evaluatio

ould experiealuate twent

frames; sto

ngirola (Malaga)

t of Seisme Building

R. Resheid

, Irbid, Jorda

al type of cone-concretes. Seismic and some equate strucis study is pid evaluats in Jordaod that canse that mayation. The um rise ree study areinto low ris

-height catefects of theertical irregu

are examins of the e

were built. ntative buildN, static nohe represensing its capadified using

which is to bdicates thatn earthqua

on whereasence minoty two samp

one-concret

), Spain 2013

mic Vulnergs

dat

an

onstruction e walls whevulnerabilityof the neigctures with concerned ion of the an. The p be used toy be at riskproposed i

esidential b classified se (1-3 stoegory, builde locally dularities (soned. A totalevaluation Contributiondings was monlinear (puntative buildacity curve g five perfobe comparet the buildin

ake and he a higher Cr damage, ple building

te infills; p

26

rability

of weak reas the y of this ghboring detailed with the seismic

roposed o identify k during indexing buildings into two

ories) or ings are ominant

oft story) l of forty method. n of the modeled ushover) dings. A and the

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if any. gs in two

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XXXV UNEReducing

This proEuropeat An-Nthe Eurand theEUCENcentre collabovisibilitywill be experiegraduatSASPA By deverole willinternata reseathe fieldnetworkactivitie At the preparementionin the encouraacquirinincreas Improveinitiative Note:

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Jalal Al Dab

oject aims tan Researc

Najah Nationropean Cene Institute fNTRE will lein the fieldrate with UPy of UPDRRfundamenta

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eloping a col be fundamtional reseaarch infrastrd of scientifiks of researes will lead U

national leved to respned target wfield of eaage researng and parte their ince

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to reinforce ch Area. Urnal Universntre for Trafor Advanc

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omprehensmental in mearch activitieructure and ic technologrchers and UPDRRC to

vel, an enhpond to eawill be pursurthquake echers to coicipating in ntives to co

itiveness oal public aw

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ect funded by Eu

Workshop ended Mediterra

smic RiskSAS

aola Ceresa

(1)UPDRR(2)EU

(3)IUSS

the cooperrban Planniity (NNU) in

aining and Rced Study oRC to becomc risk mitigdevise a res

national andraining activld of earthqent a distin

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gy and caparesearch in

o a fruitful c

hancement arthquake eued by enhaengineeringompete inteEU Framew

ontinue their

of NNU, crwareness ar

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ration with Eing and Disn Palestine Research inof Pavia (Ime a globagation and search stra

d internationvities for stuuake enginguishing fe

h strategy, national socoject activitieg and enhanacity buildinnstitutes. In cooperation

of capabilengineeringancing the . Furthermoernationallywork projecr research a

eation of nre some of t

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ission through t

RELEMR): Fuen

n in Palesoject

o Germagno

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y, Italy.

Europe’s nesaster Risk

is coordinan EarthquaUSS) in Itally competitdisaster mtegy capab

nal levels. Tudents and

neering and eature of the

the significacio-economies are idenncing internng, i.e. hum

an internatwith EU.

ity will ensg needs ocapability oore, a highy in terms cts related tactivities in

networks othe expecte

Palestinian-adm

the SEVENTH F

ngirola (Malaga)

stine

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eighbours inReduction

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managemenle of increa

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ntified with tational cooan resourcetional frame

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of UPDRRCher visibilityof scientific

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of researched results of

ministrated Area

FRAME WORK

), Spain 2013

arbara Borzi

n the contexCenter (UPoject, suppoering (EUCEupporting aperienced rt. EUCENT

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PROGRAMME

27

i(2)

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action of research TRE will ope and of IUSS

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XXXV UNEReducing

Earthq

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plementatio1. Satellitenication bedata from t

ous earthquold time dog algorithmsimplementeriate servo proper acti

ygnal are thation (IGDA

tion, work dtting up of e earthquak

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rsity, Kaind

on of the eae based atween the rthese statiouakes. A siomain ampls such as Ped as well.

shut-downion based ohe facilities AS). Recent

done over thnew applicke losses in

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ng and RaKO

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illi ObservaIst

rthquake eaand fiber remote statins is used imple and itude levels

PRESTo and. The early

n systems on the alarsuch as Faly construct

he last decaations for e

n quasi-real

anean Region (R

pid Post-EOERI, Turk

r and Musta

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RELEMR): Fuen

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ngirola (Malaga)

ke Assess

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EEWS) in Ission systeion at KOERarning for e

algorithm, implementerunning unto be com

ities, whichprospective

nnel, Istanbric power p

velopment oonse systeake are elab

), Spain 2013

ment Stud

stitute (KOE

tanbul comms are uRI. The con

emerging pobased on

ed. Regionder Seiscom

mmunicatedh will autome end userbul Gas Dislants.

of new appms that funborated.

28

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menced sed for ntinuous otentially

specific nal early mp3 are

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proaches nction to

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XXXV UNEReducing

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Saudi A MashelSeismoKing SaDeparteP.O. BoRiyadh Saudi AE-mail: Spain José MReal I. OHead GCecilio E- 1110E-mail: AntonioReal I. OHead SGeophyCecilio E-1110E-mail: María JCSIC InstituteJose GuE- 2800Tel: +34Fax: +3E-mail: MarianSecretaSeismoEditor-iInstituteMCN loJose GuE-2800Phone: Fax: +3E-mail:

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Turkey Ali PinaKandilli ResearDepartmBogazic81220, IstanbuTurkey E-mail: Dogan BoğaziçEarthquEarthquÇengelTURKEE-mail: Niyazi TProfessDepartmKandilli EarthquBogazic34684 CIstanbuTurkey E-mail: Zehra ÇAssociaMiddle Turkey E-mail: United HussaiNationaSeismoMinistryP.O. BoUnited ATel: +97Fax: +9Email: H

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Ogie KKineme222 VisPasadeCalifornUSA E-mail: UNESC FrederiConsultCross-CRisk ReNatural UNESC11813 SOaktonUnited STel: +1 Fax: +1E-mail:

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