8.2 Measuring Earthquakes A) Seismographs - instruments that record earthquake waves. B) Seismograms electronically recorded ground motion made by seismographs. I. Instruments
Seismograph
Seismogram
II. Earthquake Waves 8.2 Measuring Earthquakes A) Body Waves 1) P waves - Have the greatest velocity of all -Are push-pull waves that push (compress) and pull (expand) - Travel through solids, liquids, and gases
Earthquake Waves 8.2 Measuring Earthquakes S waves - Slower velocity than P waves - Travel only through solids
8.2 Measuring Earthquakes Surface waves seismic waves, travel along Earth’s outer layer.
Seismic Waves
Locating an Earthquake 8.2 Measuring Earthquakes Earthquake Distance Travel-time graphs from 3 or more seismographs can be used to find the exact location of an earthquake epicenter. The epicenter is located using the difference in the arrival times between P and S wave Earthquake Direction
Measuring Earthquakes 8.2 Measuring Earthquakes Richter Scale Richter Scale Based on the amplitude of the largest seismic wave. Increases 32 times each increase
Measuring Earthquakes 8.2 Measuring Earthquakes Moment Magnitude Moment magnitude is the most widely used - estimates the energy released by earthquakes.
Earthquake Magnitudes
- The majority of all earthquakes that occur on Earth are found at or near plate boundaries. 8.2 Earthquake locations
Some Notable Earthquakes