final - ch 4 Flashcards
lisbon earthquake 1755
2 major earthquakes: 1st caused fires, 2nd caused sea waves, 70k ppl killed
what causes earthquakes
volcanic activity, metoerite impacts, movement of land,
fault
fracture in the earth where both sides move relative to eachother
stresses
build up to crack the rock and send waves of seismic energy causing earthquake
Steno (1669)
discovered law of original horizontality
law of original horizontality
sediments are
originally deposited in
horizontal layers
law of superposition
in an unformed layer of sedimentary rock, each layer is younger than the one below it
law of original continuity
sediment layers are continuous
fault - jointing
brittle lithosphere rocks fracture and crack
strike and dip
method to describe location of rock in 3D
fault - dip slip
dominated by vertical movement, caused by a push or pull
normal fault
where dominant force is pulling (type of dip slip)
reverse fault
dominant force is pushing (type of dip slip)
strike slip fault
dominated by horizontal movement
right/left lateral fault
If the right or left side has moved towards you
foreshock
smaller events before the earthquake
aftershock
smaller events after earthquake
seismology
study of earthquakes
seismometer
detects earthquake waves
seismograph
records earthquake waves
seismogram
visual created by sesimograph
2 categories of seismic waves
body waves and surface waves
body waves
pass through entire earth, faster, shorter periods
surface waves
move near surface only, created by body waves disturbing the surface
2 types of body waves
p and s waves
p waves
primary, first to reach the recording station, travels through solid liquid or gas
s waves
secondary, second to reach recording station, travels only through solids
2 types of surface waves
love and rayleigh
love waves
travel faster, side to side
rayleigh
backwards rotating
how to find the arrival time of an earthquake
S-P
how many stations are needed to identify an earthquake location
3
richter scale
measuring amplitude of an earthquake
in what order is the feedback presented on a seismogram
aftershock, mainshock, foreshock