Topic 2 Part 2 Flashcards
is a non-instrumental perceptibility
measure of damage to structures, ground
surface effects, ( e.g. fractures, cracks and
landslides) and human reactions to earthquake
shaking.
Intensity
is a non-instrumental perceptibility
measure of damage to structures, ground
surface effects, ( e.g. fractures, cracks and
landslides) and human reactions to earthquake
shaking.
Intensity
It is a descriptive method which has been
traditionally used to establish earthquake size,
especially for pre-instrumental events.
Intensity
It is a descriptive method which has been
traditionally used to establish earthquake size,
especially for pre-instrumental events.
Intensity
It is a subjective damage evaluation metric
because of its qualitative nature, related to
population density, familiarity with earthquake
and type of constructions.
Intensity
is a measure of the total energy
released by an earthquake at its source
(hypocenter or focus).
•
Magnitude
is a measure of the total energy
released by an earthquake at its source
(hypocenter or focus).
•
Magnitude
• It is a quantitative, objective measure that does
not change with distance from the earthquake’s
epicenter.
Magnitude
• It is a single, objective value that is used to
compare the size of earthquakes globally
Magnitude
is calculated based on seismic data
recorded by seismographs, which capture the
amplitude of seismic waves.
Magnitude
is calculated based on seismic data
recorded by seismographs, which capture the
amplitude of seismic waves.
Magnitude
three different ways to measure the
size of an earthquake, each with its own
applications and methods for calculation.
Local Magnitude Scale, Surface Wave
Magnitude Scale, and Moment Magnitude
Scale
three different ways to measure the
size of an earthquake, each with its own
applications and methods for calculation.
Local Magnitude Scale, Surface Wave
Magnitude Scale, and Moment Magnitude
Scale
also known as the
Richter Scale, was the first widely used method
for measuring earthquakes.
• It was developed by Charles F. Richter in 1935 to
estimate earthquake size based on seismic
waves recorded at a certain distance from the
epicenter.
Local Magnitude Scale,
also known as the
Richter Scale, was the first widely used method
for measuring earthquakes.
• It was developed by Charles F. Richter in 1935 to
estimate earthquake size based on seismic
waves recorded at a certain distance from the
epicenter.
Local Magnitude Scale,