Disaster Readiness and Risk Reduction Notes
Disaster Readiness and Risk Reduction: Other Related Geologic Hazards
Unit Overview
This unit discusses different geological hazards, their causes, signs, and mitigation strategies for preventing loss of lives and properties.
Learning Targets
Discuss the different geological hazards.
Analyze the causes of geological hazards.
Recognize signs of impending geological hazards.
Interpret geologic maps.
Apply mitigation strategies to prevent loss of lives and properties.
Lesson 1: Ground Subsidence
Causes and Effects
The Philippines is highly vulnerable to natural disasters like floods, typhoons, landslides, earthquakes, volcanoes, and droughts due to:
Location at the intersection of two main tectonic plates.
Position within a typhoon belt.
The Philippines is among the top three nations for population exposure and hazard vulnerability.
The government has developed coping methods due to its history of dealing with disasters.
There are gaps in disaster management capabilities across different regions.
Local disaster preparedness and resilience information is extremely limited.
Central Question
What is the difference between the preparation for hydrometeorological and geological hazards?
Ground Subsidence: A Silent Hazard
Ground subsidence is a phenomenon where the land gradually or suddenly sinks.
It is caused by excessive water extraction below the ground, which the environment cannot replenish quickly enough.
From 1979 to 2009, some areas in Metro Manila sank 0.68 meters to 1.34 meters.
CAMANAVA (Caloocan City, Malabon City, Navotas City, and Valenzuela City) is affected by groundwater subsidence due to excessive groundwater pumping by fishpond operators.
Continued sinking may cause dikes protecting CAMANAVA from seawater incursion to be overtopped, leading to unexpected floods.
What Is Ground Subsidence?
Ground subsidence, including sinkholes, can result from excessive groundwater extraction in urban areas.
Sinkholes form in karst terrain, characterized by bedrock made of limestones, dolomite, or gypsum.
Types of Sinkholes
Dissolution Sinkholes: Occur where bedrock is exposed or very shallow, resulting from rainfall and surface water.
Cover-Subsidence Sinkholes: Develop gradually where covering sediments are permeable and contain sand.
Cover-Collapse Sinkholes: Occur in soil or loose material overlying soluble bedrock.
Human-Induced Sinkholes: Result from land use practices, especially construction and water pumping.
Causes of Ground Subsidence
Natural processes or human activities can cause ground subsidence.
Dissolution and diversion of natural water drainage patterns or dewatering.
Compaction of soil.
Subterranean mining.
Thawing permafrost.
Effects of Ground Subsidence
Impacts agricultural lands, industrial processes, and infrastructure.
Farmlands, irrigation systems, and groundwater wells can be destroyed.
Infrastructures on subsiding ground can be damaged or destroyed.
Mining areas, tunnels, and surrounding areas can collapse.
Can cause injuries and fatalities.
Tips to Mitigate Ground Subsidence
Find alternative sources of groundwater.
Avoid building infrastructure near land fissures.
Route drainage away from cracks.
Prohibit residential zones in or near fissure areas or ground with high subsidence susceptibility.
Lesson 2: Rainfall-Induced Landslide
What is Rainfall-Induced Landslide?
Rainfall-induced landslide involves downslope movement of soil, rock, and organic materials due to gravity.
It also refers to the resulting landform from such movement.
Factors That Influence Landslide Development
Morphological factors
Geological factors
Human factors
Water (rainfall)
Seismic activity
Volcanic activity
Major Types of Landslides
Fall: Material on cliffs or steep slopes loses support or becomes fractured.
Topple: A block of material detaches from a steep slope and rotates forward and downward.
Slide: A detached mass of rocks, soil, and organic matter moves along a downward-sloping surface.
Flow: Materials from gentle slopes detach and flow like a viscous liquid.
Includes debris flow
Debris avalanche
Earth flow
Spreads: Mass of soil or rocks extends or spreads laterally.
Types of Landslides (Detailed)
Rotational Landslide: Ground rotates and slides along a curved failure plane.
Translational Landslide: Ground slides with little rotation along a flat plane parallel to the surface.
Block Slide: A type of translational landslide made of mostly one block of surface material that moves downslope.
Rockfall: Pieces of a cliff or rock face fall forward as large blocks due to gravity.
Earthflow: Forms on moderate slopes when fine-grained material liquefies and runs out in an hourglass shape.
Lateral Spread: Surface material extends or spreads on gentle slopes, often associated with earthquake shaking.
Debris Flow: Rapidly moving mix of water, mud, trees, and other materials that flows downvalley.
Debris Avalanche: An extremely large and fast-moving debris flow.
Creep: Soil and surface material that slowly moves down a slope.
Best Practices for Landslide Mitigation
Hazard mapping
Public information
Engineering intervention measures of slope protection measures
Early warning system (EWS)
Lesson 3: Coastal Erosion
What Is Coastal Erosion?
Coastal Erosion involves breaking and removing materials from the coastline due to wave action, tidal currents, and human activities.
Types of Coastal Erosion
Mechanical erosion of waves
Bioerosion
Weathering
Mass Movements
Factors That Influence Coastal Erosion
Lithology of rocks
Climate
Global sea level rise
Man-made interventions
Lesson 4: Bolide Impact
What Is Bolide Impact?
A bolide is a generic term for celestial bodies entering the Earth's surface and creating a fireball.
A superbolide is a relatively larger bolide that can cause cratering impacts.
Superbolides can increase the incidence of climate change and sea-level change.
Near-Earth Objects (NEOs)
Near-Earth Objects (NEOs) define the rocky or metallic asteroids and icy comets between Jupiter and Mars.
Hazards of Bolide Impact
Increased incidence of climate change and sea-level change.
Intense tectonic activities, earthquakes, and increased volcanism.
Trigger global mass extinction and global environmental dangers.
Deflection Techniques
Use a laser beam to move the NEO.
Use large lenses or mirrors to refocus the sun’s energy on a NEO.
Use another object to collide with a NEO to deflect or change its velocity.
Integration Steps for Bolide Impact Analysis
Step 1: Search for pictures of celestial bodies entering the Earth’s surface.
Step 2: Enumerate the possible hazards they may cause.
Step 3: Compare the hazards based on the rock’s sizes and shapes if they enter the Earth’s surface.
Project NOAH Integration: Fireball vs. Bolide
A fireball is a very bright meteor, generally brighter than magnitude -4 (same magnitude as Venus).
A bolide is a special fireball that explodes in the atmosphere with a bright flash before impacting the Earth and is often observed with visible fragmentation.
Perspectives in DRRR (Disaster Risk Reduction and Management) in the Philippines
The Philippines is located in the Pacific Ring of Fire and the typhoon belt, making it one of the most hazard-prone countries.
The country experiences natural hazards like earthquakes, volcanic eruptions, typhoons, floods, and droughts.
These hazards can be classified as geophysical disturbances, meteorological and hydrological events, and slow-onset disasters.
Due to increasing population and urbanization, natural disasters have resulted in unprecedented devastation.
From 2001 to the present, the country experienced some of the most destructive disasters, including Typhoon Yolanda and the Bohol Earthquake in 2013.