Hazard - any source of potential damage, harm or adverse health effects on something or someone
Geohazards - any geological activity that poses harmful risks or damages
Earthquake - any ground shaking activity due to fault movement, volcanic activity, combination of both, and other factors that deforms the Earth’s lithosphere or crust
Focus - point within the earth where an earthquake rupture starts
Epicenter - point on the surface vertically above the focus
Magnitude - quantifies the energy of an earthquake
Surface-wave Magnitude Scale
Moment Magnitude Scale
Intensity- strength of an earthquake felt by people in a certain locality
Intensity - strength of an earthquake felt by people in a certain locality
Seismic Waves - vibrations (waves of energy) generated by earthquakes
Surface Waves - seismic waves that travel across the Earth’s surface
Love waves - surface waves that move side-to-side or horizontally
Rayleigh Waves - surface waves that move in a ”rolling motion”
Body Waves - seismic waves that travel beneath the Earth’s surface
Primary Wave - a body wave that can travel through gases, liquids, and solids
Secondary Wave - a secondary body wave that cannot travel through fluids (gases and liquids)
Volcanic-Tectonic Earthquake - caused by movement of faults or fractures beneath active volcanoes
Tectonic Earthquake - caused by movement of faults or tectonic plates
Fault - a surface where two blocks of rock slip past one another
Volcanic Earthquake - caused by movement of magma or rock-fracturing beneath volcanoes
Normal fault - a kind of fault where the hanging wall slips downwards with respect to the footwall
Fault scarp - planar geomorphic feature formed by offset of Earth’s surface by earthquakes
Reverse fault - a kind of fault where the hanging wall thrusts upwards with respect to the footwall
Elastic Rebound Theory - Tectonic earthquakes occur via buildup of stress and strain, undergoing different stages of deformation until it results in brittle rupture
Ground rupture - deformation on the ground that marks the intersection of the fault with the earth’s surface
Liquefaction - occurs when underlying water-filled sediments during earthquake release liquids which makes the soil fluid-like
Sinkhole - patches of the earth surface that collapse, forming an abyss
Tsunami - occurs when an underwater earthquake becomes a source of energy in the ocean for large waves to form
Ground Shaking - disruptive up, down and sideways vibration of the ground during an earthquake
... can lead, not only to infrastructure collapses, but fatalities as well
... can trigger the destabilization of a slope which leads to slope failure
Why do earthquakes happen so often in the Philippines?
Pacific Ring of Fire and Bounded by Trenches
1976 Moro Gulf Earthquake - "Midnight Killer" with a magnitude 7.9 Epicenter: Celebes Sea between Mindanao and Borneo Generated by Cotabato Trench
1990 Luzon Earthquake - Magnitude 7.8 Epicenter: Rizal, Nueva Ecija Generated by: strike-slip movements along Northwest segment of Philippine Fault Zone and its splay, Digdig Fault Zone
What are the two Philvolcs Initiatives?
HazardHunter PH
Fault Finder
The recommendations on how to improve disaster risk response on earthquakes all boil down to National, LGU, and Individual levels