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    EARTHQUAKE/GEMPABUMI

    (dan tsunami)

    Subagyo PramumijoyoLaboratorium Geologi Dinamik, Jurusan Teknik Geologi FT UGM

    E-mail: [email protected]

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    X

    Z

    Y

    PARTS OF OUR GLOBE

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    SEISMIC WAVES

    Hypocentrum

    Primary /

    Longitudinal wave

    Secondary /

    Transversal wave

    Hypocentrum

    Shadow zones

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    Distribution of EQ EpicentrumMb>4, Periode 1961-1967

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    PLATES BOUNDARIES

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    Convergent plate boundary

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    ACTIVE dynamic Factor : PASSIVE dynamic Factor :1. Gravitation2. Climate3. Biologic action

    4. ACTIVE TECTONICS

    5. Lithology6. Geologic structure7. Position on surface

    (Campy & Macaire, 1989)

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    SOIL FORMATION AND SEDIMENT

    TRANSPORTATION

    (Campy & Macaire, 1989)

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    USGS

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    TYPE OF EQ WAVES

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    P wave

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    S wave

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    R wave

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    L wave

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    PRINSIPLE of SEISMOGRAPH

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    Sumber :

    Bumi-Pustaka Alam LIFE

    1979

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    Sumber :Bumi-Pustaka Alam LIFE, 1979

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    TYPES OF FAULTS

    Normal fault Reverse fault

    Strike-slip fault

    Dextral strike-slip fault Sinistral ss fault

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    FAULTING AND EQ

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    Modified Mercalli Scale of Earthquake Intensity

    IV Felt indoors during the day by many people. Windows, dishes, and doors rattle,

    glassware and crockery clink and clash.

    V Felt indoors by nearly everyone. Frightens many, some run outdoors. Some

    broken dishes, glassware, and windows. Minor cracking of plaster. Moves small

    objects, spill liquids, ring small bells, and sways tall objects.

    VI Felt by all, many frightened and run outdoors. Dishes, glassware, and windows

    break in considerable quantities. Book and pictures fall. Furniture moves oroverturns. Weak plaster walls and some brick walls crack. Damage is slight.

    VII Frightens all, difficult to stand. Damage slight to moderate in well-built

    ordinary buildings. Numerous windows and chimneys break. Small landslides

    occur. Waves on ponds, water becomes turbid.

    VIII Fright is general. Disturbs drivers of automobiles. Heavy furniture overturns.Damage considerable in ordinary substantial building, partial collapses. Most walls,

    chimneys, towers, and monuments fall. Well water levels change. Cracks appear.

    IX General panic. Damage considerable in masonry structures. Ground cracks

    conspicuously. Underground pipes break. Liquefactions occur in soft sediment areas.

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    YOGYAKARTA EQ

    2006

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    GEOLOGIC MAP OF

    YOGYAKARTA AND

    SUROUNDING

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    GEOLOGICAL MAP OF SOUTHERN YOGYAKARTA

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    SURFACE WAVE AMPLIFICATION

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    SURFACE WAVE AMPLIFICATION

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    Liquefaction

    Landslide at Cermai Cave

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    Landslide at Cermai Cave

    LANDSLIDE AT SENGIR VILLAGE

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    TSUNAMI

    Shallow EQ at the bottom of sea, lake

    Magnitude > 6

    Vertical movement

    Tsunami hazard map of Indonesia

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    H t i f d?

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    How tsunami formed?

    Indo-Australian plate

    Eurasian plate

    CIAMIS - CILACAP

    TEKNIK GEOLOGI FAKULTAS TEKNIK UGM

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    CIAMIS - CILACAP

    Eurasian plate

    Indo-Australian plate

    TEKNIK GEOLOGI FAKULTAS TEKNIK UGM

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    Rising up wave

    CIAMIS - CILACAP

    Eurasian plate

    Indo-Australian plate

    TEKNIK GEOLOGI FAKULTAS TEKNIK UGM

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    Tsunami

    CIAMIS - CILACAP

    Eurasian plate

    Indo-Australian plate

    TEKNIK GEOLOGI FAKULTAS TEKNIK UGM

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    TSUNAMI ACEH

    2004

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    Tsunami wave simulation

    10 minutes after main shock

    http://localhost/var/www/apps/conversion/PRAMUMIJOYO/My%20Documents/AcehTsunami-2.gifhttp://localhost/var/www/apps/conversion/PRAMUMIJOYO/My%20Documents/AcehTsunami-2.gifhttp://localhost/var/www/apps/conversion/PRAMUMIJOYO/My%20Documents/AcehTsunami-2.gif
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    BANDA ACEH

    and

    Sourounding

    Area

    Source: Digital Globe

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    BANDA ACEH City Area

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    y

    Source: Digital Globe

    BANDA ACEH CITY

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    Source: Digital Globe

    BANDA ACEH CITY

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    Source: Digital Globe

    W part of BANDA ACEH City

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    p y

    Source: Digital Globe

    W part of BANDA ACEH City

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    Source: Digital Globe

    p y

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    CAN WE PREDICT EQ ?

    Java Earthquake Potential

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    On land earthquakes 1600-1921 (Dr. Visser, 1922)

    Jogyakarta earthquake (1867)

    SUMARY OF JAVA EARTHQUAKE 1840 2005

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    SUMARY OF JAVA EARTHQUAKE 18402005(Newcomb and McCann, 1987)

    1994 (Pancer) M 7.4

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    Next?2000

    2007

    2007

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    MITIGATION AND PREPARDNESS

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    ANXIETYTRAUMA..

    NEED OF PUBLIC HEALING .

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    How to survive an earthquake

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    How to survive an earthquake

    Stay under strong objects, like desk or cars. Get down beside a large bulky object.

    If you are in bed, roll off it near the bottom of the

    bed.

    If in a car, get out and lie next to the vehicle.

    Never go to stairs.

    Dont shelter under the doorway arch.

    Wooden building are safer than brick building.

    pace an t me mens on n naturaphenomena

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    phenomena

    (John, 1995)

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    GEOHAZARD

    EVENT

    RESPONSESRESPONSES

    REHABILITATIONREHABILITATIONMITIGATIONMITIGATION

    PREVENTION &PREVENTION &

    PREPARDNESSPREPARDNESS

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    LANDSLIDE ATLEMBAH BALIEM

    PAPUA

    LEMBAH BALIEM

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    JEMBER FLOODING

    2006

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