Fresh surface fractures (black arrows) along Brawley Fault Zone and across Ralph Road in response to the 2010 El Mayor-Cucapah earthquake; view to the north. Slight vertical component of slip (2 mm, up on east [right] side) more noticeable at white arrow.
Can the ground open up during an earthquake?
Shallow crevasses can form during earthquake-induced landslides, lateral spreads, or from other types of ground failures, but faults do not open up during an earthquake. An earthquake occurs when two blocks of the earth’s crust slide past one another after having been stuck together in one place for a long time, because of friction on the fault, while the rest of the crust away from the edges has been slowly moving. If a fault could open up, no earthquake would occur in the first place because there would be no friction locking the two blocks together.
Learn More: Glossary of earthquake terms
Related
Can you predict earthquakes?
Can animals predict earthquakes?
Why are we having so many earthquakes? Has naturally occurring earthquake activity been increasing? Does this mean a big one is going to hit? OR We haven't had any earthquakes in a long time; does this mean that the pressure is building up for a big one?
Can "MegaQuakes" really happen? Like a magnitude 10 or larger?
Can some people sense that an earthquake is about to happen (earthquake sensitives)?
Will California eventually fall into the ocean?
Is there earthquake weather?
Do solar flares or magnetic storms (space weather) cause earthquakes?
Are earthquakes associated with variations in the geomagnetic field?
Fresh surface fractures (black arrows) along Brawley Fault Zone and across Ralph Road in response to the 2010 El Mayor-Cucapah earthquake; view to the north. Slight vertical component of slip (2 mm, up on east [right] side) more noticeable at white arrow.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
View southeast along the Totschunda fault.
View southeast along the Totschunda fault.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.
Aftershock seismicity of the 2010 Maule Mw=8.8 Chile, earthquake: Correlation between co-seismic slip models and aftershock distribution?
Co-seismic ruptures of the 12 May 2008, Ms 8.0 Wenchuan earthquake, Sichuan: East-west crustal shortening on oblique, parallel thrusts along the eastern edge of Tibet
Where's the San Andreas fault? A guidebook to tracing the fault on public lands in the San Francisco Bay region
The USGS Earthquake Hazards Program - investing in a safer future
ANSS-Advanced National Seismic System
Faulting apparently related to the 1994 Northridge, California, earthquake and possible co-seismic origin of surface cracks in Potrero Canyon, Los Angeles County, California
Winnetka deformation zone: Surface expression of coactive slip on a blind fault during the Northridge earthquake sequence, California
The co-seismic slip distribution of the Landers earthquake
Related
Can you predict earthquakes?
Can animals predict earthquakes?
Why are we having so many earthquakes? Has naturally occurring earthquake activity been increasing? Does this mean a big one is going to hit? OR We haven't had any earthquakes in a long time; does this mean that the pressure is building up for a big one?
Can "MegaQuakes" really happen? Like a magnitude 10 or larger?
Can some people sense that an earthquake is about to happen (earthquake sensitives)?
Will California eventually fall into the ocean?
Is there earthquake weather?
Do solar flares or magnetic storms (space weather) cause earthquakes?
Are earthquakes associated with variations in the geomagnetic field?
Fresh surface fractures (black arrows) along Brawley Fault Zone and across Ralph Road in response to the 2010 El Mayor-Cucapah earthquake; view to the north. Slight vertical component of slip (2 mm, up on east [right] side) more noticeable at white arrow.
Fresh surface fractures (black arrows) along Brawley Fault Zone and across Ralph Road in response to the 2010 El Mayor-Cucapah earthquake; view to the north. Slight vertical component of slip (2 mm, up on east [right] side) more noticeable at white arrow.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
View southeast along the Totschunda fault.
View southeast along the Totschunda fault.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.
At pass west of Delta River. Here there was roughly 5 m of offset. Note the push up in the background. There is permafrost at the bottom of the cracks.