1. Elastic strain energy builds up in the deforming rocks on either side of the fault until it overcomes the resistance posed by any irregularity on the fault plane
2. When the slippage does occur energy is released
3. The elastic energy released is transported by seismic waves that travel throughout the earth
Landslides - occur when soil becomes saturated with water and loses its cohesion due to heavy rainfall or rapid snowmelt.
Tsunami - is a series of ocean waves generated by sudden displacement of water on the seafloor.
Tectonic - Earthquake produces by sudden movement along faults and plate boundaries
Volcanic - Earthquake produces by sudden movement of magma beneath volcanoes
Intensity - it is the perceived strength of an earthquake
Magnitude - based on instrumentally derived information and correlated strength
Secondary waves - This is a body wave with low frequency and can only pass through rocks
Primarywaves - The fastest seismic wave and are the first to reach any particular location after an earthquake occurs
Secondary waves - These seismic waves move along the earth's crust and make the ground roll up and down or shake from side to side
0.1 - This g value is sufficient to produce some damage to weak construction
Liquefaction - Takes place when loosely packed, water logged sediments at or near the ground surface lost their strength in response to strong ground shaking
Strike - slip fault - Involves a dominantly horizontal shifting of the ground
Types of Liquefaction features:
Ground oscillation
Settlement
Flow Failure
Lateral Spread
Loss of Bearing Strength
Types of Landslides
TOPPLES - Type of landslide that occur suddenly when massive part of every steep slopes loose and rotate forward
ROCK FALLS - a landslide that involve chunks of detached rock that fall freely for some distance or bounce and roll down the steep slope
LATERAL SPREADS - a landslide that are triggered by earthquakes and affect gentle slopes with less than 10 degrees inclination. Slope materials lose cohesion through liquefaction caused by shaking during earthquake
FLOWS - Type of landslide that involve downslope motion of fine-grained clay, silt, and fine sand made mobile by water saturation. These flows include mudflows and earthflows, and are common during the rainy season
SLIDES - a landslide that involve large blocks of bedrock that break free and slide down along a planar or curved surface
COMPLEX SLIDES - a landslide which are combination of two or more types of movements
Type of landslide that involve downslope motion of fine-grained clay, silt, and fine sand made mobile by water saturation. These flows include mudflows and earthflows, and are common during the rainy season
Type of landslide that are triggered by earthquakes and affect gentle slopes with less than 10 degrees inclination. Slope materials lose cohesion through liquefaction caused by shaking during earthquake
A sea wave of local or distant origin that results from large-scale seafloor displacements associated with earthquakes, major submarine slides, or exploding volcanic islands
A methodology to determine the nature and extent of risk by analyzing potential hazards and evaluating existing conditions of vulnerability that together could potentially harm exposed people, property, services, livelihood, and the environment on which they depend