MGB Geohazard-Assessment-Mapping

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    The MGBThe MGB GeohazardGeohazard Assessment &Assessment &

    LIZA SOCORRO J. MANZANO

    Supervising Science Research Specialist

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    Objectives

    identifying areas susceptibleor vulnerable to various

    types of flood and landslidehazards

    increase public awareness ofsuch hazards in order tomitigate the negative

    impacts.

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    Major Activities Geohazard mapping at 1:50,000 scale

    and 1:10,000 scale

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    High landslide

    susceptibility

    Moderate landslide

    susceptibility

    Low landslide

    susceptibility

    Low to moderate flood

    Examples of Geohazards Maps (1:50K) covering

    Metro Manila and vicinity

    Areas affected by less than 1 m

    high flood. These are usually

    inundated during prolonged and

    intense rainfall or extreme weather

    condition.

    High floodsusceptibility

    Areas affected by greater than 1 m

    high flood. These areas are usually

    flooded for several hours during heavy

    rainfalls. Included are landforms of

    topographic lows such as active and

    abandoned river channels and areas

    along river banks.

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    Landslide Susceptibility Zones

    These are areas where landslide debris could accumulate.These are areas where landslide debris could accumulate.

    Areas with low to gentle slopes and lacking tension cracks haveAreas with low to gentle slopes and lacking tension cracks have

    low landslide susceptibility rating.low landslide susceptibility rating.

    Areas with moderate landslide susceptibility rating haveAreas with moderate landslide susceptibility rating have

    inactive/old landslides and tension cracks which are located awayinactive/old landslides and tension cracks which are located away

    from the community. These areas usually have moderate slopes.from the community. These areas usually have moderate slopes.

    Areas with high landslide susceptibility rating have active/recentAreas with high landslide susceptibility rating have active/recent

    landslides and tension cracks that would directly affect thelandslides and tension cracks that would directly affect the

    community. Those with steep slopes and drainages that are pronecommunity. Those with steep slopes and drainages that are prone

    to landslide damming are also highly susceptible to landslides.to landslide damming are also highly susceptible to landslides.

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    Status of the National

    Geohazards Assessment

    and Mapping

    (1:50,000 scale)

    Good news

    100%

    (December 2010)

    www.mgb.gov.ph

    All 1:50K geohazards

    (landslide and flood) maps

    can now be downloaded for

    free at the following website:

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    Objective: Complete thedetailed geohazards mapping

    at 1:10,000 scale

    Detailed Geohazards

    Assessment and Mapping

    at 1:10,000 scale

    n verse , c esmunicipalities

    Accomplishment to date 950

    (2011-172, 2012-230, 2013-548)

    Target for 2014- 648

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    Methodology

    Interpretation and analysis of Remote Sensing Data

    (aerial photographs & satellite images) and other thematic maps such as

    geologic map, drainage map, slope map, vegetation map

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    Geomorphological/Geological

    Assessment

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    Ground Penetrating Radar surveys

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    Anecdotal accounts

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    Province- and municipal-wide IEC on

    Geohazards

    Production of IEC materials on

    geohazards (posters, flyers, comics,videos)

    Making people aware through IEC

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    Provided geohazard maps to local government units and advisories to

    communities identified as prone to landslide and flood hazards

    Enhance awareness on geohazard

    maps and information

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    Establishment of the Geohazards Operations Center

    and Disaster Response Protocols

    Updating of the Geohazards Web Portal

    Operationalize the early warning and monitoring system of

    geohazards

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    Assess relocation/ resettlement

    sites of communities affected by

    disasters nationwide

    Assess relocation sites of areas

    affected by Typhoon Pablo in

    Compostela valley and Davao

    Assessment of identified relocation

    sites/temporary shelters/evacuation centers

    by LGUs

    r en a , yp oon o an a n

    Region VIII and Subsidence in

    Bohol

    Assess the suitability of existing

    temporary shelters and evacuation

    centers by LGUs

    ew ataan, omposte a a ey

    Relocation Site Assessment

    Tubigon, Bohol

    Temporary Shelter Site

    Assessment

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    LANDSLIDE HAZARDS

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    Guinsaugon Landsl ide, SouthernL eyte,2006

    Compos tela Valley,2002

    LANDSLIDE OR MASS WASTING IS

    THE DOWNWARD MOVEMENTS OF

    EARTH MATERIALS AIDED BYGRAVITY

    Cherry Hil l , An tipo lo,1999

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    What are the types of mass wastinghat are the types of mass wasting

    TYPEVery Slow

    (4km/hr)

    Flow CREEP EARTH OR MUDFLOWDEBRIS

    AVALANCHE

    Slip DEBRIS SLIDE OR SLUMP

    Fall ROCKFALL

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    Debris FlowDebris Flow

    2Real, Quezon, 2005

    ,, ,,

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    MudflowMudflow

    ,, ,,

    Former location of chapel

    KapataganKapatagan,, LanaoLanao del Norte,2006del Norte,2006KapataganKapatagan,, LanaoLanao deldel

    Norte,2006Norte,2006