Earthquakes
Study Guide: Earthquakes
Overview of Earthquakes
Definition: Natural events caused by the rapid release of energy in the Earth's crust.
Frequency: Over 1 million detectable earthquakes occur each year.
Earthquake Geography
Regions of Activity: Japan Sea, Pacific Ocean, and volcanic arcs.
Crust Types: Continental & Oceanic Crust.
Earth’s Layers: Contribute to tectonic activity.
Earthquake Mechanism
Cause: Rapid energy release due to tectonic forces.
Process: Rocks bend elastically until they break, producing vibrations.
Impacts of Earthquakes
Most earthquakes are small; significant earthquakes can lead to destruction and fatalities.
Historical Toll: 3.5 million deaths recorded in the past 2,000 years.
Hundreds of significant earthquakes occur annually.
Role of Seismologists
Study causes, effects, and potential damage from earthquakes.
Engage in earthquake prediction (both long-term and short-term).
Types of Faults
Normal Fault: Hanging wall moves down due to extensional forces.
Reverse Fault: Hanging wall moves up due to compressional forces.
Thrust Fault: A low-angle reverse fault associated with mountain formations.
Strike-Slip Fault: Horizontal movement with no vertical motion.
Seismic Waves
Body Waves: Travel through Earth's interior (includes P-waves and S-waves).
Surface Waves: Travel along the surface (includes R-waves and L-waves).
Measuring Earthquakes
Seismographs: Instruments that record ground motion.
Seismogram: Data recording from seismographs, depicting wave behavior and arrival times.
Magnitude and Intensity: Intensity relates to observed damage; Magnitude relates to energy released.
Tsunamis
Definition: Harbor waves resulting from underwater displacements due to earthquakes.
Detection: Increasing need for early-warning systems to save lives.
Earthquake Prediction
Long-term predictions: Possible.
Short-term predictions: Currently unreliable.
Identifying Recent Faults
Historical records and geological dating estimate recurrence intervals of faulting activity.