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Lesson 4 Potential Earthquake Hazards
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an earthquake, also called "shock", generates weak to strong shaking due to movement of rock material underneath
Cramer
(1991)
Hays
(1981) waves are classified to 3:
1.)
P
waves or
compressional
waves
the first waves to cause high-frequency vibrations in structures; same direction
2.)
S
waves or
sheer
waves
second waves; cause a structure to vibrate side-to-side
3.)
Surface
waves (
Rayleigh
and
Love
waves)
arrive last and low-frequency vibrations
main shock -> smaller magnitude earthquake experienced after the first one is called
aftershocks
also referred as ground ruptures or fissures
ground movement occurs and surface of ground breaks
Tension
cracks
Tsunami
other term is
harbor wave
the waves increase their height while wavelength decreases
Amplification Process
final stage of tsunami
refers to the approach of the tsunami's leading wave to the shore
Runup
described
Landslides
- mass movement of rock, soil, debris down a slope due to gravity
PHIVOLCS
(2021)
Ex. of various triggers to landslides:
Rainfall
weathering
of
rocks
man-made
activity (excessive mining)
natural
triggers (plant, animal movement)
Triggers that create conditions in an area that make it prone to landslides:
Steep slopes
- increases potential energy of the impending landslide
Weakening
of
slope material
- unstable landmass
Weathering
of
rocks
- alteration of rock condition over time
Overloading
on
the
slope
- may be brought by man made development
The hazard map for tsunamis is straightforward