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Earthquake Hazards Program images.

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Diagram of dipping slab with different focal depth events shown at different depths.
Focal Depth
Focal Depth
Focal Depth

Diagram of dipping slab with different focal depth events. The focal depth refers to the depth of an earthquake hypocenter.

Diagram of dipping slab with different focal depth events. The focal depth refers to the depth of an earthquake hypocenter.

Blurry table of the geologic time scale
Geologic Time Scale
Geologic Time Scale
Geologic Time Scale

The geologic time scale showing each eon, era, period, epoch, and their associated ages.

The geologic time scale showing each eon, era, period, epoch, and their associated ages.

Photo of a bridge over a valley with a semi-transparent textbox labelled "www.worldweb.com. Photo c Jim Forrest"
Bridge (Geotechnical)
Bridge (Geotechnical)
Bridge (Geotechnical)

Photo of bridge.  Geotechnical means referring to the use of scientific methods and engineering principles to acquire, interpret, and apply knowledge of earth materials for solving engineering problems.  

Photo of bridge.  Geotechnical means referring to the use of scientific methods and engineering principles to acquire, interpret, and apply knowledge of earth materials for solving engineering problems.  

Crustal block diagram with the down-dropped blocks labelled as "graben" and the upthrown blocks labelled as "horst" between faults
Horst and Graben Diagram
Horst and Graben Diagram
Horst and Graben Diagram

Horst and graben diagram. A graben is a down-dropped block of the earth's crust resulting from extension, or pulling, of the crust. 

Horst and graben diagram. A graben is a down-dropped block of the earth's crust resulting from extension, or pulling, of the crust. 

Map of Iceland showing plate boundaries
Iceland and Plate Motions (Kinematic)
Iceland and Plate Motions (Kinematic)
Iceland and Plate Motions (Kinematic)

Iceland and plate motions. Kinematic refers to the general movement patterns and directions of the earth's rocks that produce rock deformation.

Iceland and plate motions. Kinematic refers to the general movement patterns and directions of the earth's rocks that produce rock deformation.

Graph with scattered dots with a diagonal line going downward from left to right in between the dots
Least Squares Fit Plot
Least Squares Fit Plot
Least Squares Fit Plot

Plot showing least squares fit. When plotting data points on a graph, the least-squares-fit is the line or curve that comes closest to going through all the points.

Plot showing least squares fit. When plotting data points on a graph, the least-squares-fit is the line or curve that comes closest to going through all the points.

Two fault lines with circles showing their aftershocks
Landers Fault and Hector Mine Fault Aftershocks
Landers Fault and Hector Mine Fault Aftershocks
Landers Fault and Hector Mine Fault Aftershocks

The Landers fault (red lines at left) and the Hector Mine fault and its aftershocks (red lines and circles at right). The Hector Mine earthquake was a magnitude 7.1, and it produced thousands of aftershocks.

The Landers fault (red lines at left) and the Hector Mine fault and its aftershocks (red lines and circles at right). The Hector Mine earthquake was a magnitude 7.1, and it produced thousands of aftershocks.

Two graphs
Natural Frequency
Natural Frequency
Natural Frequency

The natural frequency is the frequency at which a particular object or system vibrates when pushed by a single force or impulse, and not influenced by other external forces or by damping. If you hold a slinky by one end and let it hang down and then give it one push up from the bottom, the rate of up-and-down motion is its natural frequency.

The natural frequency is the frequency at which a particular object or system vibrates when pushed by a single force or impulse, and not influenced by other external forces or by damping. If you hold a slinky by one end and let it hang down and then give it one push up from the bottom, the rate of up-and-down motion is its natural frequency.

Diagram showing P waves (small jolt or light shaking or not felt), S waves (larger jolt or strong shaking), and surface waves (rolling motion))
P Waves
P Waves
P Waves

A P wave, or compressional wave, is a seismic body wave that shakes the ground back and forth in the same direction and the opposite direction as the direction the wave is moving.

A P wave, or compressional wave, is a seismic body wave that shakes the ground back and forth in the same direction and the opposite direction as the direction the wave is moving.

Black background with a green wave and a white arrow pointing across one concave and one convex hump to indicate a period
Period
Period
Period

Diagram of period.  The period is the time interval required for one full cycle of a wave.

Diagram of period.  The period is the time interval required for one full cycle of a wave.

Diagram showing a blob shape with a D and an arrow pointing right and a labelled reupture.  The height is labelled "W" and the length is "L."  The top line is labelled "Surface" and the bottom line is labelled "Base of seismogenic zone"
Seismogenic Zone
Seismogenic Zone
Seismogenic Zone

Moment = ? A D

? = shear modulus = 32 GPa in crust, 75 GPa in mantle

A = LW = area

D = average displacement during rupture

Moment = ? A D

? = shear modulus = 32 GPa in crust, 75 GPa in mantle

A = LW = area

D = average displacement during rupture

Map of the central US (Missouri, Illinois, Kentucky, Tennessee) with red lines and red, yellow, and blue circles representing earthquake magnitude
New Madrid Seismic Zone
New Madrid Seismic Zone
New Madrid Seismic Zone

The New Madrid seismic zone in Central U.S.

A seismic zone is an area of seismicity probably sharing a common cause. 

The New Madrid seismic zone in Central U.S.

A seismic zone is an area of seismicity probably sharing a common cause. 

Seismic waves
Seismic Waves
Seismic Waves
Seismic Waves

A seismogram is a record written by a seismograph in response to ground motions produced by an earthquake, explosion, or other ground-motion sources.

A seismogram is a record written by a seismograph in response to ground motions produced by an earthquake, explosion, or other ground-motion sources.

Diagram showing a descending slab in yellow with the associated dip angle, flow pressure, and gravitational body force vectors
Descending Slab
Descending Slab
Descending Slab

A slab is the oceanic crustal plate that underthrusts the continental plate in a subduction zone and is consumed by the earth's mantle.

A slab is the oceanic crustal plate that underthrusts the continental plate in a subduction zone and is consumed by the earth's mantle.

Photo of large house with damage and debris on the ground
Los Gatos Residence Damage
Los Gatos Residence Damage
Los Gatos Residence Damage

This turn-of-the-century wooden residence in Los Gatos sustained major damage when it moved off its foundation during the October 17, 1989, M7.1 Loma Prieta, California earthquake.

This turn-of-the-century wooden residence in Los Gatos sustained major damage when it moved off its foundation during the October 17, 1989, M7.1 Loma Prieta, California earthquake.

Block diagram showing equal waves throughout
Surface Waves
Surface Waves
Surface Waves

A surface wave is a seismic seismic wave that is trapped near the surface of the earth.

A surface wave is a seismic seismic wave that is trapped near the surface of the earth.

Diagram of a right triangle representing land and a blue sqiggly line representing a sea wave
Tsunami Diagram
Tsunami Diagram
Tsunami Diagram

A tsunami is a sea wave of local or distant origin that results from large-scale seafloor displacements associated with large earthquakes, major submarine slides, or exploding volcanic islands.

A tsunami is a sea wave of local or distant origin that results from large-scale seafloor displacements associated with large earthquakes, major submarine slides, or exploding volcanic islands.

Map of the Los Angeles region in California with a color gradient of purple to yellow showing amplification values.
Amplification Map of Los Angeles
Amplification Map of Los Angeles
Amplification Map of Los Angeles

This image of the Los Angeles region combines this information to predict the total amplification expected in future earthquakes from local geologic conditions or site effects.

This image of the Los Angeles region combines this information to predict the total amplification expected in future earthquakes from local geologic conditions or site effects.

A diagram on a blue background showing a slice of the Earth's lithosphere, including continental crust (green), oceanic crust (maroon), asthenosphere (pink), and the upper mantle (yellow).
Asthenosphere
Asthenosphere
Asthenosphere

A diagram showing a slice of the Earth's lithosphere, including continental crust, oceanic crust, asthenosphere, and the upper mantle.

A diagram showing a slice of the Earth's lithosphere, including continental crust, oceanic crust, asthenosphere, and the upper mantle.

An illustration showing two stick figures doing basement excavations, one with a frown that excavated into the labelled hard, stable bedrock on the left and the other with a smile that excavated above the labelled bedrock surface.  There is a bridge overlying water on the right hand side.
Basement
Basement
Basement

An illustration showing two stick figures doing basement excavations, one with a frown that excavated into the labelled hard, stable bedrock on the left and the other with a smile that excavated above the labelled bedrock surface.  

An illustration showing two stick figures doing basement excavations, one with a frown that excavated into the labelled hard, stable bedrock on the left and the other with a smile that excavated above the labelled bedrock surface.  

A diagram of blind thrust fault with arrows on the left and right pointed inward to indicate movement and resulting in labelled ductile rock layers folding.
Blind Thrust Fault
Blind Thrust Fault
Blind Thrust Fault

A diagram of a blind thrust fault resulting in ductile rock layers folding over the fault and leaving the fault under the surface.

A diagram of a blind thrust fault resulting in ductile rock layers folding over the fault and leaving the fault under the surface.

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