Plate Boundaries - are made up of many faults, and most of the earthquakes around the world occur on these faults.
Subduction Zones - are areas where tectonic plates converge.
Subduction - causes a tectonic plate to slide under another and sink into the mantle because the denser oceanic crust slides beneath the lighter continental crust
Earthquake - is what happens when two blocks of the earth suddenly slip past one another
Fault or Fault plane - is the surface where 2 blocks of Earth slip
Hypocenter - The location below the surface where the earthquake starts.
Epicenter - Location on the surface right on top of the hypocenter.
Foreshocks - These are smaller earthquakes that happen in the same place as the larger earthquake that follows.
Foreshocks - Scientists can’t tell that an earthquake is a ______ until the larger earthquake happens.
Mainshock - is called the largest main earthquake.
Aftershocks - These are smaller earthquakes that occur afterwards in the same place as the mainshock.
Seismic Waves - The energy radiates outward from the fault.
Seismographs - instruments that record vibrations from eathquakes.
Seismogram - the recording that comes from the seismograph
Magnitude - size of the earthquake
Intensity - the shaking of the eartquake
Active Faults - as any fault that is likely to have another earthquake sometime in the future. If they have moved one or more times in the last 10,000 years.
West Valley Fault -
Rodriguez (Rizal)
San Mateo (Rizal)
Marikina
Pasig
Taguig
Muntinlupa
San Pedro
Biñan
Carmona
Santa Rosa
Calamba
Tagaytay
Oriental Mindoro
Western Philippine Fault -
Luzon Sea
Mindoro Strait
Panay Gulf
Sulu Sea
Central Philippines Fault - Ilocos Sur, Ilocos Norte, La Union, Pangasinan, Nueva Ecija, Aurora, Quezon, Masbate, Eastern Leyte, Southern Leyte, Agusan Del Norte, Agusan del Sur, Davao del Norte, Davao Oriental