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Earthquake Hazards Program images.

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Three graphs with the x-axis labelled "Time (s)": the first labelled "Acceleration (cm/s^2)," the second labelled "Velocity (cm/s)," and the third labelled "Displacement (cm)."
Acceleration, Velocity, and Displacement Graphs
Acceleration, Velocity, and Displacement Graphs
Acceleration, Velocity, and Displacement Graphs

Acceleration, velocity, and displacement records. 

Displacement is the difference between the initial position of a reference point and any later position. The amount any point affected by an earthquake has moved from where it was before the earthquake.

Acceleration, velocity, and displacement records. 

Displacement is the difference between the initial position of a reference point and any later position. The amount any point affected by an earthquake has moved from where it was before the earthquake.

First motion diagram: a circle split into quadrants with hollow white circles in the upper left and lower right and solid black circles in the upper right and lower left.  There is an arrow pointing down and another pointing right from the upper left quadrant, and an  arrow pointing up and another pointing left from the lower right quadrant.
First Motion
First Motion
First Motion

First motion mechanism. On a seismogram, the first motion is the direction of ground motion as the P wave arrives at the seismometer. Upward ground motion indicates an expansion in the source region; downward motion indicates a contraction.

First motion mechanism. On a seismogram, the first motion is the direction of ground motion as the P wave arrives at the seismometer. Upward ground motion indicates an expansion in the source region; downward motion indicates a contraction.

Seismic record with red, blue, and black waves.  The largest seismic wave is labelled "Main shock," the second largest is labelled "Aftershock," and the third largest is labelled "foreshock.""
Foreshock
Foreshock
Foreshock

Small foreshocks on a seismic record. Foreshocks are relatively smaller earthquakes that precede the largest earthquake in a series, which is termed the mainshock. Not all mainshocks have foreshocks.

Small foreshocks on a seismic record. Foreshocks are relatively smaller earthquakes that precede the largest earthquake in a series, which is termed the mainshock. Not all mainshocks have foreshocks.

Photo of mountains in Zion Canyon with trees in the foreground
Photo of Zion Canyon (Geology)
Photo of Zion Canyon (Geology)
Photo of Zion Canyon (Geology)

Photo of Zion Canyon located in Zion National Park in Utah, United States. (Image courtesy of Justin Gould)

Photo of Zion Canyon located in Zion National Park in Utah, United States. (Image courtesy of Justin Gould)

A map of Asia with colored dots. The earthquakes (colored dots) in the middle of the continent are intraplate events. Those near the ocean boundary are at the boundary between two plates (interplate).
Interplate and Intraplate Events
Interplate and Intraplate Events
Interplate and Intraplate Events

The earthquakes (colored dots) in the middle of the continent are intraplate events. Those near the ocean boundary are at the boundary between two plates (interplate).

The earthquakes (colored dots) in the middle of the continent are intraplate events. Those near the ocean boundary are at the boundary between two plates (interplate).

Block diagram showing the left coastal block moving forward and parallel as the right block moves away
Left-Lateral Motion Diagram
Left-Lateral Motion Diagram
Left-Lateral Motion Diagram

Diagram of left-lateral motion on fault. If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the left block moves toward you and the right block moves away. See also right-lateral. 

Diagram of left-lateral motion on fault. If you were to stand on the fault and look along its length, this is a type of strike-slip fault where the left block moves toward you and the right block moves away. See also right-lateral. 

Diagram of a figure with a cube form made up of smaller cubes bent into waves and then going straight
Love Wave
Love Wave
Love Wave

A Love wave is a surface wave having a horizontal motion that is transverse (or perpendicular) to the direction the wave is traveling.

A Love wave is a surface wave having a horizontal motion that is transverse (or perpendicular) to the direction the wave is traveling.

Photo of ripples in a pond with the reflection of a cloudy sky
Pond Ripples (Attenuation)
Pond Ripples (Attenuation)
Pond Ripples (Attenuation)

Ripples on a pond are attenuated as they move away from the source. Q is the inverse of attenuation. A high Q means a low attenuation.

Ripples on a pond are attenuated as they move away from the source. Q is the inverse of attenuation. A high Q means a low attenuation.

Geologic time scale showing eras, periods, and notable events in terms of millions of years ago
Geologic Time Scale 3
Geologic Time Scale 3
Geologic Time Scale 3

Geologic time scale showing eras, periods, and notable events in terms of millions of years ago.

Geologic time scale showing eras, periods, and notable events in terms of millions of years ago.

Photo of snowy mountains in the background with pine trees in the foreground
Secular Mountains
Secular Mountains
Secular Mountains

Secular refers to long-term changes that take place slowly and imperceptibly. Commonly used to describe changes in elevation, tilt, and stress or strain rates that are related to long-term tectonic deformation.

Secular refers to long-term changes that take place slowly and imperceptibly. Commonly used to describe changes in elevation, tilt, and stress or strain rates that are related to long-term tectonic deformation.

Block diagram with a labelled earthquake source shown as a circle on the fault plane and directly underneath the center of the produced circular, seismic waves
Earthquake Source Diagram
Earthquake Source Diagram
Earthquake Source Diagram

The source is the term for the released forces that generate acoustic or seismic waves, also called the earthquake source.

The source is the term for the released forces that generate acoustic or seismic waves, also called the earthquake source.

3 diagrams: At the top is a crustal block diagram showing how strike direction from North along a fault.  At the bottom left is a figure showing the strike angle as the angle between North and the fault plane with dip direction pointing away from the fault plane.  At the bottom right is a circle with North, East, South, and West and their respective strikes when going clockwise from North: 0, 90, 180, 270.
Strike
Strike
Strike

The strike is the trend or bearing, relative to north, of the line defined by the intersection of a planar geologic surface (for example, a fault or a bed) and a horizontal surface such as the ground.

The strike is the trend or bearing, relative to north, of the line defined by the intersection of a planar geologic surface (for example, a fault or a bed) and a horizontal surface such as the ground.

Picture showing 3 stages of a tsunami forming and growing
Tsunamigenic
Tsunamigenic
Tsunamigenic

Tsunamigenic is referring to those earthquakes, commonly along major subduction zone plate boundaries such as those bordering the Pacific Ocean, that can generate tsunamis.

Tsunamigenic is referring to those earthquakes, commonly along major subduction zone plate boundaries such as those bordering the Pacific Ocean, that can generate tsunamis.

A figure with text titled "Years before present (YBP)".  The text is: "Formation of Earth: 4.6x10^9 YBP. Dinosaur extinction: 6.5x10^7 YBP. First hominids: 2x10^6 YBP. Last great ice age: 1x10^4 YBP. Declaration of Independence: 2x10^2 YBP. Establishment of UWB: 1x10 YBP."
YBP
YBP
YBP

YBP is an abbreviation for "years before present".

Formation of Earth: 4.6x10^9 YBP

Dinosaur extinction: 6.5x10^7 YBP

First hominids: 2x10^6 YBP

Last great ice age: 1x10^4 YBP

Declaration of Independence: 2x10^2 YBP

Establishment of UWB: 1x10 YBP

YBP is an abbreviation for "years before present".

Formation of Earth: 4.6x10^9 YBP

Dinosaur extinction: 6.5x10^7 YBP

First hominids: 2x10^6 YBP

Last great ice age: 1x10^4 YBP

Declaration of Independence: 2x10^2 YBP

Establishment of UWB: 1x10 YBP

Graph with 3 seismic waves:  The blue wave has the highest peaks and is labelled "high amplitude," the green has medium peaks and is labelled "medium amplitude," and the red has the smallest peaks and is labelled "low amplitude."
Amplitude (1)
Amplitude (1)
Amplitude (1)

High, medium, and low amplitude. The amplitude is the size of the wiggles on an earthquake recording.

High, medium, and low amplitude. The amplitude is the size of the wiggles on an earthquake recording.

Seismicity of Hawaii from 2021 Hawaii National Seismic Hazard Map
Figure 3. Seismicity of Hawaii from 2021 Hawaii National Seismic Hazard Map
Figure 3. Seismicity of Hawaii from 2021 Hawaii National Seismic Hazard Map
Figure 3. Seismicity of Hawaii from 2021 Hawaii National Seismic Hazard Map

Seismicity of Hawaii: earthquakes M>5 from the 1840-1899, 1900-1959, 1960-2019 catalogs shown separately. While earthquake activity remains high today, it seems to have decreased over the past 60 years, which could be related to less volcanic activity at Mauna Loa. 

Seismicity of Hawaii: earthquakes M>5 from the 1840-1899, 1900-1959, 1960-2019 catalogs shown separately. While earthquake activity remains high today, it seems to have decreased over the past 60 years, which could be related to less volcanic activity at Mauna Loa. 

Chance of earthquakes in Hawaii
Chance of earthquakes in Hawaii
Chance of earthquakes in Hawaii
Chance of earthquakes in Hawaii

Figure 1. Chance of minor or greater damaging earthquake shaking in the next 100 years. Population exposure estimates are rounded to the nearest 1000. 

Figure 1. Chance of minor or greater damaging earthquake shaking in the next 100 years. Population exposure estimates are rounded to the nearest 1000. 

digging machine on grassy meadow with large white windmills in background
Sediment Investigations in the San Joaquin – Sacramento Delta
Sediment Investigations in the San Joaquin – Sacramento Delta
Sediment Investigations in the San Joaquin – Sacramento Delta

USGS Geologists R. Sickler, J. Willard, and B. Philibosian observe as an excavator digs a pit used to investigate sediments uplifted by active tectonic activity in the San Joaquin – Sacramento Delta, California, November 29, 2021.

USGS Geologists R. Sickler, J. Willard, and B. Philibosian observe as an excavator digs a pit used to investigate sediments uplifted by active tectonic activity in the San Joaquin – Sacramento Delta, California, November 29, 2021.

Infographic on the 2011 Virginia Earthquake and East Coast Earthquake Hazards
2011 Virginia Earthquake - Infographic
2011 Virginia Earthquake - Infographic
2011 Virginia Earthquake - Infographic

USGS infographic on the magnitude 5.8 earthquake that struck central Virginia August 23, 2011, east coast earthquake hazards and how the USGS is helping inform critical decisions to protect lives and property. 

Full Text Description:

10-YEAR ANNIVERSARY OF THE M5.8 EARTHQUAKE IN VIRGINIA
America’s Most Widely Felt Earthquake

USGS infographic on the magnitude 5.8 earthquake that struck central Virginia August 23, 2011, east coast earthquake hazards and how the USGS is helping inform critical decisions to protect lives and property. 

Full Text Description:

10-YEAR ANNIVERSARY OF THE M5.8 EARTHQUAKE IN VIRGINIA
America’s Most Widely Felt Earthquake

USGS scientist with yellow visibility safety vest on talking to the camera with people working in the background.
Joanne Chan - Seismic Survey
Joanne Chan - Seismic Survey
Joanne Chan - Seismic Survey

Joanne Chan conducting a seismic survey in San Carlos, California, looking for traces of the Serra Fault. 

Joanne Chan conducting a seismic survey in San Carlos, California, looking for traces of the Serra Fault. 

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