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NATSCI4_Intro-to-Hazards
NATSCI4_Earthquakes
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Cards (36)
Earthquake
is a weak to violent shaking of the ground produced by the sudden movement of rock materials below the Earth’s surface.
Identify the ff.
A)
Wave Fronts
B)
Fault
C)
Focus
D)
Epicenter
E)
Fault scarp
5
Types of Earthquakes
Volcanic quakes
Tectonic
quakes
Volcanic quakes
are earthquakes produced by movement of magma beneath volcanoes.
Tectonic quakes
are earthquakes produced by sudden movement along faults and plate boundaries.
Faults
are fractures in the Earth’s crust along which slippage or displacement has occurred or may occur again.
Dip slip faults
move along the direction of the dip plane and are described as either
normal
or
reverse
(thrust), depending on their motion.
Strike-slip faults
are when two blocks slide past one another.
Elastic Rebound Theory
discusses about the gradual accumulation and release of stress and strain.
Seismology
is the study of behavior of seismic waves.
Identify this.
A)
Seismometer
1
Identify this.
A)
Seismogram
1
What are used to describe the strength of an earthquake?
Magnitude
Intensity
Magnitude
is calculated from seismic records and estimates the amount of energy released at the source.
Richter
Scale is used to measure an earthquake's magnitude.
Intensity
is the degree of ground shaking at a given locale based on the amount of damage.
These are used to measure an earthquake's intensity.
Modified Mercalli Intensity Scale
PHIVOLCS
Earthquake
Intensity
Scale
PHIVOLCS Earthquake Intensity Scale
I -
Scarcely
Perceptible
II -
Slightly
Felt
III -
Weak
IV -
Moderately Strong
V -
Strong
VI -
Very
Strong
VII -
Destructive
VIII -
Very
Destructive
IX -
Devastating
X -
Completely
Devastating
These are types of earthquake hazards.
Ground rupture
Ground shaking
Liquefaction
These are the secondary effects of earthquakes.
Landslides
Tsunamis
Ground rupture
is the deformation on the ground that marks, the intersection of the fault with the earth’s surface.
Ground shaking
is the disruptive up, down and sideways vibration of the ground during an earthquake.
Liquefaction
is the phenomenon wherein sediments, especially near bodies of water, behave like liquid similar to a quicksand.
Landslide
is the down slope movement of rocks, solid and other debris commonly triggered by strong shaking.
Tsunamis
are series of waves caused commonly by an earthquake under the sea.
PHIVOLCS stand for
Philippine Institute of Volcanology and Seismology.
Tsunamigenesis
explain how tsunamis work.
Tsunamigenic earthquake events
6.6
Manila Bay
(
November 9, 1828
)
7.5
Manay, Davao Oriental
(
November 11, 1921
)
Not all earthquakes generate tsunamis. (
TRUE
)
All earthquakes generate tsunamis. (
FALSE
)
Shallow earthquakes generate the most destructive tsunamis. (
TRUE
)
Shallow earthquakes generate the least destructive tsunamis. (
FALSE
)
Large tsunamis are likely to be generated by earthquakes with magnitude greater than or equal to 7.0 (
TRUE
)
Large tsunamis are likely to be generated by earthquakes with magnitude less than or equal to 7.0 (
FALSE
)
Structural damage due to earthquake vibrations depends on:
Wave amplitudes
Duration
of vibrations
Nature
of material upon which the structure rests
Design
of structure
Triangulation
is used to locate the epicenter of an earthquake.