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Section 4: Earthquakes and Society
The probability of an earthquake’s occurrence is determined from the history of
earthquakes and knowing where and how quickly strain accumulates.
K
What I Know
W
What I Want to Find Out
L
What I Learned
Essential Questions
•
What factors affect the amount of damage caused by an earthquake?
•
What are some of the factors considered in earthquake-probability studies?
•
How are different types of structures affected by earthquakes?
Copyright © McGraw-Hill Education
Earthquakes and Society
Vocabulary
Review
New
•
•
•
•
geology
Copyright © McGraw-Hill Education
soil liquefaction
tsunami
seismic gap
Earthquakes and Society
Earthquake Hazards
•
Earthquake hazards are factors that determine the severity of damage
produced by an earthquake.
•
Identifying earthquake hazards in an area can sometimes help to
prevent some of the damage and loss of life.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Hazards
Structural failure
•
One type of damage caused by earthquakes is called pancaking;
shaking causes a building’s supporting walls to collapse and the upper
floors to fall one on top of the other like a stack of pancakes.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Hazards
Structural failure
•
If the shaking caused by an earthquake has the same frequency of
vibration as the natural sway of buildings of certain heights, those
buildings will sway the most during the earthquake. Shorter and taller
buildings, however, are less likely to be affected.
Copyright © McGraw-Hill Education
Earthquakes and Society
Structural Engineer
Video
FPO
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Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Hazards
Land and soil failure
•
In sloping areas, earthquakes can trigger massive landslides. In areas
with sand that is nearly saturated with water, seismic vibrations can
cause the ground to behave like a liquid in a phenomenon called soil
liquefaction.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Hazards
Land and soil failure
•
Soil liquefaction can cause trees and houses to fall over or to sink into
the ground and underground pipes and tanks to rise to the surface.
•
The type of ground material can affect the severity of an earthquake in
an area. Ground motion is amplified in some soft materials, such as
unconsolidated sediments. It is muted in more resistant materials, such
as granite.
Copyright © McGraw-Hill Education
Earthquakes and Society
Quakes and Shakes
Video
FPO
Add link to Video from ConnectED here.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Hazards
Tsunami
•
Another type of earthquake hazard is a tsunami—a large ocean wave
generated by vertical motions of the seafloor during an earthquake.
Copyright © McGraw-Hill Education
Earthquakes and Society
Tsunami
Concepts In Motion
FPO
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Earthquakes and Society
Earthquake Forecasting
•
There is currently no completely reliable way to forecast the exact time
and location of the next earthquake. Instead, earthquake forecasting is
based on calculating the probability of an earthquake.
•
The probability of an earthquake’s occurrence is based on two factors:
the history of earthquakes in an area and the rate at which strain builds
up in the rocks.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Forecasting
Seismic risk
•
The probability of earthquakes in seismic belts is much greater than
elsewhere on Earth.
•
The history of an area’s seismic activity can be used to generate
seismic-risk maps.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Forecasting
Recurrence rates
•
Earthquake-recurrence rates along a fault can indicate whether the fault
ruptures at regular intervals to generate similar earthquakes.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Forecasting
Seismic gaps
•
Seismic gaps are sections located along faults that are known to be
active, but which have not experienced significant earthquakes for a long
period of time.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Forecasting
Seismic gaps
•
Earthquakes in 1912 and 1999 happened on either side of Istanbul,
Turkey. The earthquakes around the city leave a seismic gap that
indicates that an earthquake is likely to occur in that area.
Copyright © McGraw-Hill Education
Earthquakes and Society
Earthquake Forecasting
Stress accumulation
•
The stress accumulated in a particular part of a fault, together with the
amount of stress released during the last earthquake in a particular part
of the fault, can be used to develop a stress-accumulation map.
Copyright © McGraw-Hill Education
Earthquakes and Society
Review
Essential Questions
•
What factors affect the amount of damage caused by an earthquake?
•
What are some of the factors considered in earthquake-probability studies?
•
How are different types of structures affected by earthquakes?
Vocabulary
• soil liquefaction
• tsunami
Copyright © McGraw-Hill Education
• seismic gap
Earthquakes and Society