MGB Geohazard-Assessment-Mapping
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Transcript of 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