Topic 2 Part 2 Flashcards

1
Q

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.

A

Intensity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

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.

A

Intensity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

It is a descriptive method which has been
traditionally used to establish earthquake size,
especially for pre-instrumental events.

A

Intensity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

It is a descriptive method which has been
traditionally used to establish earthquake size,
especially for pre-instrumental events.

A

Intensity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

It is a subjective damage evaluation metric
because of its qualitative nature, related to
population density, familiarity with earthquake
and type of constructions.

A

Intensity

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

is a measure of the total energy
released by an earthquake at its source
(hypocenter or focus).

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

is a measure of the total energy
released by an earthquake at its source
(hypocenter or focus).

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

• It is a quantitative, objective measure that does
not change with distance from the earthquake’s
epicenter.

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

• It is a single, objective value that is used to
compare the size of earthquakes globally

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

is calculated based on seismic data
recorded by seismographs, which capture the
amplitude of seismic waves.

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

is calculated based on seismic data
recorded by seismographs, which capture the
amplitude of seismic waves.

A

Magnitude

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

three different ways to measure the
size of an earthquake, each with its own
applications and methods for calculation.

A

Local Magnitude Scale, Surface Wave
Magnitude Scale, and Moment Magnitude
Scale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

three different ways to measure the
size of an earthquake, each with its own
applications and methods for calculation.

A

Local Magnitude Scale, Surface Wave
Magnitude Scale, and Moment Magnitude
Scale

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

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.

A

Local Magnitude Scale,

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

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.

A

Local Magnitude Scale,

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Primarily used to measure small to
medium-sized earthquakes in a local region,
generally within 600 km of the epicenter

A

Local Magnitude Scale,

17
Q

The scale is most effective for
earthquakes of magnitude 3 to 7 and becomes less
accurate for larger earthquakes or those occurring
at great depths.

A

Local Magnitude Scale,

18
Q

The scale is most effective for
earthquakes of magnitude 3 to 7 and becomes less
accurate for larger earthquakes or those occurring
at great depths.

A

Local Magnitude Scale,

19
Q

measures
the size of earthquakes based on surface waves
(specifically Rayleigh waves) that travel along
the Earth’s surface.
• These waves tend to cause the most damage
during an earthquake because they have large
amplitudes and affect the Earth’s surface.

A

SURFACE WAVE MAGNITUDE SCALE,Ms

20
Q

measures
the size of earthquakes based on surface waves
(specifically Rayleigh waves) that travel along
the Earth’s surface.
• These waves tend to cause the most damage
during an earthquake because they have large
amplitudes and affect the Earth’s surface.

A

SURFACE WAVE MAGNITUDE SCALE,Ms

21
Q

It is most effective for large earthquakes
(magnitude 5.5 and above), but it is less accurate for
deep or distant earthquakes.

A

SURFACE WAVE MAGNITUDE SCALE,Ms

22
Q

is the most
modern and widely used earthquake magnitude
scale.
• It measures the total energy released by an
earthquake, including energy from both body and
surface waves, and is especially effective for
large and deep earthquakes.

A

MOMENT MAGNITUDE SCALE,Mw

23
Q

is the most
modern and widely used earthquake magnitude
scale.
• It measures the total energy released by an
earthquake, including energy from both body and
surface waves, and is especially effective for
large and deep earthquakes.

A

MOMENT MAGNITUDE SCALE,Mw

24
Q

Designed to overcome the limitations of
the Richter and Surface Wave Magnitude scales,
Mw provides the most accurate measurement for
all earthquake sizes and depths

A

MOMENT MAGNITUDE SCALE,Mw

25
Q

Works for all earthquake magnitudes, including
very large events (Mw 8 or higher) where the Richter
scale becomes less accurate.
• Can measure energy release more accurately for
deep-focus earthquakes and those that don’t
generate large surface waves.

A

MOMENT MAGNITUDE SCALE,Mw

26
Q

calculated based on the
seismic moment (M₀), which is a function of the fault
area, the average slip on the fault, and the rigidity of the
rocks

A

MOMENT MAGNITUDE SCALE,Mw

27
Q

calculated based on the
seismic moment (M₀), which is a function of the fault
area, the average slip on the fault, and the rigidity of the
rocks

A

MOMENT MAGNITUDE SCALE,Mw

28
Q

is the standard
scale used by seismologists today, especially for
large or significant earthquakes, such as those
above magnitude 6.
• It is also the scale reported by the United States
Geological Survey (USGS) and other global seismic
monitoring agencies.

A

MOMENT MAGNITUDE SCALE,Mw

29
Q

is the standard
scale used by seismologists today, especially for
large or significant earthquakes, such as those
above magnitude 6.
• It is also the scale reported by the United States
Geological Survey (USGS) and other global seismic
monitoring agencies.

A

MOMENT MAGNITUDE SCALE,Mw