Geological activities - basis of scientists in dividing lithosphere
Earthquakes are not randomly scattered. they are located on the edges of plates or near water. there are no earthquakes to places far from the edges of plates.
volcanoes are not randomly distributed. they are located on edges of plates. volcanoes are present where earthquakes are located
volcanoes, mountains, and earthquakes are distributed near each other
to compute the distance in finding the epicenter, use the formula
d = time difference / 8 seconds * 100km
8 seconds is the interval between times of arrival of the P wave and S wave at a distance of 100km
to find the scale in finding the epicenter, use this formula
distance * 1.5 cm / 200km
Triangulation Method - uses distance information from 3 seismic stations in order to locate the epicenter of earthquake.
the method used to determine the depth of an earthquake is called Seismogram Analysis
Geophysical Hazard Maps - includes places that are prone to earthquakes, disasters, and prone to hazards.
Since 1968, PHIVOLCS has recorded 12 destructive earthquakes in the Philippines
Seismology - study of earthquakes and seismic waves that move through and around the earth
Seismologist - person who studies seismology
Fault - the rupture and slippage along fractures of earth's crust which is caused by violent shaking of the earthquake.
Manila trench involves La Union and Pampanga
Philippine Trench involves Surigao del sur and Davao.