Lecture 7: Seismic Waves and EQs Flashcards
Strike
Azimuth or bearing of a horizontal line in the plane
Dip
The slope of the plane in the direction perpendicular to strike
Fractures
Break in rocks or sediments
Faults
Fractures that have motion (slip, displacement) along them in some direction
Fault plane
The plane of the fracture; not usually an flat surface, but curved or irregular
Hypocenter
Where on the fault plane the rupture began (in seconds it can travel over a larger area)
Epicenter
The location on the Earth’s surface projected directly above the hypocentre
Seismic
Related to EQ
Seismograph
Instrument that records vibrations Need one in every direction
Seismogram
Record of vibrations recorded by seismograph
Seismic wave
Any of the waves that are generated by an earthquake
Seismic moment
Direct measure of the energy radiated during an EQ A measure of the size of an earthquake based on the area of fault rupture, the average amount of slip, and the force that was required to overcome the friction sticking the rocks together that were offset by faulting Moment = shear modulus x area of rupture x average displacement during rupture
S waves
Secondary waves, slower
Increases velocity and decreases amplitude
P waves
Primary waves
Can be felt by animals
Increases velocity and decreases amplitude
Use difference between arrival of P and S wave to determine how far away EQ is
Compression waves
Surface waves
Constant velocity
How to locate epicenter
Need 3 seismometers Triangulate position of epicenter and focus
Richter scale
Used for local EQ only
Using seismogram to determine dip slip fault
Will see either initial pull down, or push up depending on what size of fault seismograph is on
Body waves
P and S waves Traveling through the interior of the earth, body waves arrive before the surface waves emitted by an earthquake. These waves are of a higher frequency than surface waves
Surface waves
Travelling only through the crust, surface waves are of a lower frequency than body waves, and are easily distinguished on a seismogram as a result. Though they arrive after body waves, it is surface waves that are almost enitrely responsible for the damage and destruction associated with earthquakes. This damage and the strength of the surface waves are reduced in deeper earthquakes

Normal fault

Reverse fault

Strike-slip fault