Download presentation
Published byBryan Thompson Modified over 9 years ago
1
I. What is an earthquake? Earthquake defined Fractures and faults
An earthquake is a series of vibrations (shaking) at the earth’s surface produced by the sudden release of energy by movement along a fault. Other mechanisms of earthquake generation… Volcanic activity Landslides Meteorite impacts Major explosions Fractures and faults Some terminology
2
I. What is an earthquake? Earthquake defined Fractures and faults
Faults are fractures within the earth (rocks and soils) along (across) which movement has occurred Faults are 2 dimensional planes within the 3D earth Faults appear as 1 dimensional lines at the earth’s 2D surface, on maps of the earth’s surface and on vertical cross-sections [the fault is a plane, the surface is a plane where two plane intersect you get a line] Fractures with no movement are called joints.
3
Three Types of Faults Strike-Slip Thrust Normal
Form depending on type of plate motion and complex reaction of earth’s lithospheric blocks Strike-slip Normal Thrust Normal Slide source: Lisa Wald – USGS Pasadena
4
Near Kingman AZ; image from R.J. Varga
Faults: Normal faults offsetting layers in volcanic ash deposits 2D cross-section view of fault in road cut (plane of the faults intersect the plane of the vertical road cut, looks like a line) Faults cutting layered volcanic rocks Near Kingman AZ; image from R.J. Varga
5
(right-lateral strike-slip fault)
San Andreas Fault (right-lateral strike-slip fault) Wallace Creek, Carrizo Plain, CA 2D map view of fault from above (plane of vertical fault intersects plane of the surface of the earth = line SERC and USGS
6
Faults: Strike-slip fault near Valley of Fire (Clark Co, NV)
East of Las Vegas: image from M.B. Miller
7
I. What is an earthquake? Earthquake defined Fractures and faults
Some terminology Seismology – field of study of earthquakes Seismic waves – vibration energy transmitted through earth materials (rocks and soils) Earthquake focus (or hypocenter) – site within the earth where fault fails, source of seismic waves Earthquake epicenter – position on the earth’s surface above the focus Magnitude – calculated energy released at the earthquake focus Intensity – experienced effects of seismic waves on people and materials (varies with location and materials, type of building, rocks vs. loose soils)
8
Earthquake Magnitude M5 M6 M7 Magnitude scale is logarithmic
Slide source: Lisa Wald – USGS Pasadena
9
Earthquake Intensity – Shake Maps
Similar presentations
© 2025 SlidePlayer.com. Inc.
All rights reserved.