Islands and mountains in the Philippines were the result of the collision of the Pacific Plate in the east and the Eurasian Plate in the west
Fault lines
Cracks on the Earth's surface along which smaller plates move or slip against each other
Tsunami is a series of large waves resulting from the disturbance of seawater commonly due to an earthquake, with wave heights reaching five meters or higher
Liquefaction takes place when there is an increase in water pressure in saturated soil because of ground shaking
Movement of active faults can be shown by fault slips based on displaced rocks or soil of known age, or through displaced landforms
Ground Shaking is caused by the passage of seismic waves beneath structures, leading to tilting, splitting, toppling, or collapsing of structures
Focus and Epicenter
The place where the energy is released like an explosion is called the focus, while the epicenter is the point that is immediately above the focus (Cramer, 1991)
Earthquake
The weak or violent shaking of the earth's surface caused by the sudden movement of rock materials beneath it
Ground subsidence or the lowering of the land surface can occur due to various reasons such as extraction of groundwater, natural gas, mining, and earthquakes
As the Pacific Plate was forced against the Eurasian Plate, the crust crumbled
Effects of Earthquakes
Ground Shaking
Ground Rupture
Liquefaction
Ground Subsidence
Tsunami
Signs of an approaching local tsunami include a felt earthquake, extreme lowering of sea level, noticeable rise and fall of coastal water, and the rumbling sound of approaching waves (DOST-PHIVOLCS, n.d.)
GroundRupture is the displacement of the ground due to the violent shaking of the surface, which can be vertical or horizontal
PHIVOLCS defines an active fault as a fault that has moved within the last 10,000 years, indicating historical seismicity