Tensional stress-rocks are stretched away from each other.
Compressionalstress - rocks are pushed toward each other
Shearstress - rocks are pushed perpendicular to the axis.
2 Types of Faults: Active Faults & Inactive Faults
Activefaults - faults that are generated earthquakes within the last 10,000 years and may still continue to do so
Inactive faults – those without a record of having generated earthquakes within the last 10,000 years, but may possible generate an earthquake in the future
Philippine Institute of Volcanology and Seismology (PHIVOLCS) - is a Philippine national institution dedicated to provide information on the activities of volcanoes, earthquakes, and tsunamis