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Geologic Hazards Science Center images.

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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.

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. 

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. 

NSHMP Models, Codes and Catalogs - National Seismic Hazard Mapping Project
The map is based on the USGS models for the conterminous U.S. (2018), Hawaii (1998), and Alaska (2007).
The map is based on the USGS models for the conterminous U.S. (2018), Hawaii (1998), and Alaska (2007).
The map is based on the USGS models for the conterminous U.S. (2018), Hawaii (1998), and Alaska (2007).

2018 Long-term National Seismic Hazard Map. Earthquake hazard map showing peak ground accelerations having a 2 percent probability of being exceeded in 50 years, for a firm rock site.  The map is based on the most recent USGS models for the conterminous U.S.

debris flow deposits blocking road
Debris flow road damage - Macon County, NC
Debris flow road damage - Macon County, NC
Debris flow road damage - Macon County, NC

Debris flow deposits caused by intense rainfall in April 2020 block a highway in Macon County, NC. 

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