I. What is an earthquake? Earthquake defined A. • • 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… ○ ○ ○ ○ B. C. Volcanic activity Landslides Meteorite impacts Major explosions Fractures and faults Some terminology I. What is an earthquake? Earthquake defined Fractures and faults A. B. • • • 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. Strike-Slip Thrust Normal Slide source: Lisa Wald – USGS Pasadena 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 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 Faults: Strike-slip fault near Valley of Fire (Clark Co, NV) East of Las Vegas: image from M.B. Miller I. What is an earthquake? Earthquake defined Fractures and faults Some terminology A. B. C. • • 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) M5 M6 M7 Magnitude scale is logarithmic M7 = 32*M6 = 1024*M5 Slide source: Lisa Wald – USGS Pasadena Earthquake Intensity – Shake Maps