Reversefault - also known as thrustfault, sliding one block of crust on top of another. This fault is commonly found in collisionszones.
Normal faults - two blocks of crust pull apart create space, stretching the crust into a valley. In a normal fault, the hanging wall drops down.
PHIVOLCS – (PHILIPPINE INSTITUTE OF VOLCANOLOGY AND SEISMOLOGY) mandate to mitigate to disasters that may arise from volcanic eruptions, earthquakes, tsunami and other related geotectonic phenomena.
Earthquake - An earthquake is a shaking of the ground caused by movements of the earths crust.
The lithosphere is composed of the crust layer and the upper portion of the mantle.
Tectonic plates are massive, irregularly shaped slabs of solid rock, generally composed of both continental and oceanic lithosphere.
Plate boundaries - edges where two plates meet
Focus is the areainside the Earth where an Earthquake starts. It is also known as the focalpoint.
Epicenter is the point on the Earth's surface directly above the focus.
Magnitude measures the energy being released from the focus.
A seismograph is an instrument that measures the earthquake's magnitude.
Richter (Magnitude) Scale - measures the seismic energy released by the earthquake.
Intensity is the strength of the trembling made by the earthquake at a place or on the surface.
MercalliScale measures the intensity of an earthquake
Active faults are areas along which displacement is expected to occur.
Inactive faults are areas which can be identified but which do not have the occurrence of an earthquake.