FINAL Flashcards
Earthquakes
ground shaking caused when the pressure in the earth is stronger than the rock, which breaks it at a fault
Fault
fracture in earth’s surface on which sliding occurs, most are at an angle
“stick-slip”
when a fault overcomes the friction between them
focus/hypocenter
pointy at which original rupture occurs and energy is released during an earthquake
epicenter
point on earth’s surface directly above focus
3 types of waves
come in this order: P, S, surface
P- Primary, fastest, can move through any medium
S- Secondary, can only move through solid
seismograph
measures ground motion from an earth quake, uses 3, 1 vertical and 2 horizontal
how to find epicenter
time lag between types of waves increases the farther away you are
Mercalli intensity scale
defines intensity by AMOUNT OF DAMAGE, on a scale from I to XII
Richter magnitude scale
based on amount of GROUND MOTION, on a scale from 1-9 ish, logarithmic so every value is 10x more powerful
Raleigh waves
pass like waves, (arrows pointing in 2 directions)
Love waves
waves move laterally, (towards each other)
Damage due to ground motion depends on…
- closeness to epicenter
- underlying ground being solid or soft
- building construction
Landslides / Avalanches
ground on steep slope gives way and tumbles downhill
Sediment liquefaction
sediment containing poe water becomes a slurry, can create sand volcanoes
Fires (damage due to earthquakes)
spread from lamps and broken gas lines
What can cause a tsunami?
submarine fault, landslide, volcano
Deep water tsunami
height is 1/2 a meter, but WHOLE BODY of ocean is moving, lots of energy, very fast
Shallow water tsunami
piles up due to friction, gets up to 10 meters high (30 feet)
megatsunami
10 to 20 times bigger
tsunami prediction
seismograph records earthquake, sensors pick up speed of water, warning issued.
tsunami runup
size of tsunami wave when it gets to shore, unpredictable by tsunami warning system
steps to minimize damage
- avoid runup areas
- evacuation plan
- avoid new development in high risk areas
- design construction to minimize damage
Earthquakes at divergent boundaries
not very dangerous, shallow focus
earthquakes at Transform boundaries
between shallow and deep, could be minor or major
locked fault
section of fault where its stuck, so stress is spread out over more fault
earthquakes at convergent boundaries
subduction zones, deep - shallow focus, could be minor or major
Benioff-Wadati zone
subduction zone where plate is forced under
intraplate earthquakes
- Collision zone
- ancient weak fracture zones
- extensions of mid ocean fracture zones
Collision zones
convergent zone where neither plate goes down
Ancient weak fracture zones
many are failed rift valleys,
fracture zones
created as transform faults between segments of spreading ridges
induced earthquakes are due to
- changing stress field
2. increasing pore pressure underwater
examples of induced earthquakes
- reservoirs
- withdrawal of oil or water
- rockbursts
- underground nuclear testing
- deep well injection
predicting an earthquake
- identify seismic zones, or clusters of epicenters
2. identify seismic gaps, a gap of years where an active fault has not shaken
foreshocks
lil earthquakes before a big one
Earthquake warning system
Japan uses it, measures P waves and sends out an alert, slows bullet train and turns off gas lines.
Differential stresses
- compression (squeezing)
- tension (stretching)
- shear (twisting)
Deformation
small scale, foliation and joints
large scale, folds and faults
Kinds of deformation
- brittle - material breaks
2. ductile - material changes shape
Behavior of crust depends on…..
- composition
- rate - fast=brittle
- temp - higher temp=more ductile
- pressure - higher pressure=more ductile
hanging wall v. foot wall
hanging wall hangs over and foot wall is under
strike
angle bw horizontal line and true north measuring a fault
dip
angle b/w horizontal and steepest slope (gives slope)
dip slip
sliding up or down in dip direction
strike slip
sliding horizontally