WPR 2 Vocab Flashcards
interplate boundary
earthquake at boundary of 2 plates
elastic rebound theory
rocks on either side of fault bending or deforming instead of slipping. continue until slip and straighten out, releasing energy
intraplate boundary
earthquake at the interior of a plate
convergent boundary
tectonic plate boundary along 2 plates. comes together by subduction (one goes under other, lighter goes over) or collision
force = compression
depth = 400km deep
magnitude = highest
divergent boundary
spreading plate boundaries, force = tension
depth = <10km
weakest magnitude
transform boundary
fault boundary where 2 plates slide past each other, force = shear
intermediate depth
intermediate magnitude
focus
origin of where fault first slipped, center of seismic waves
epicenter
point on map directly above focus, strongest shaking occurs
S Wave
secondary wave, shear waves or wiggling motion, moving at 90 degree angles 2nd to arrive 3.5km/s velocity force = shear change in shape travels through solids
p waves
primary waves: compressional waves, sudden jolt
velocity = 6 km/s
1st to arrive
motion parallel, force = compression
change in volume and travel through all mediums
surface waves
along surface, series of rolling motions
travel only at earth’s crust
most destructive, but slower than P or S waves
Body waves
travels through the earth
period
cycle between peak to peak
wavelength
distance between wave crest
amplitude
amount of positive or negative shift in the earth
frequency
number of peaks per second
seismograph
records shaking of earthquakes on record. time travel graph helps find epicenter
tool
seismology
scientific study of earthquakes and propogation of elastic waves through earth