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56 Cards in this Set

  • Front
  • Back

elastic deformation

folds. after it breaks, goes back to normal

plastic deformation

slow gradual process, leads to permanent fold

seismic wave

waves that travel through rock

focus point

where the earthquake starts

epicenter

vertical projection of the quake

p wave (primary wave)

4-7 mk in crust. moves through solids, liquids, and gases. spring movement

s wave (secondary wave)

only moves through solids 3-4 km. up and down movement

seismograph

measures ground shaking

seismogram

wiggles from quake

mercalli scale

based on peoples observations

richter scale

standardized graphs (1-10 scale)

moment-magnitude scale

modern scale

time-travel curve

can use to tell how far an earthquake happened

arival of P and S waves

p wave first, s wave second

intersecting arcs

narrows down the area of the earthquake

strike slip fault

happens close to surface, two plates sliding past each other

benioff zone

earthquake at convergent boundary 300 km

moho disontinuity

crust-mantle boundary

how old are continenets

3.9 billion years old

no s-wave beyond what degree?

105

behavior of granitic magma

high in silica and water, low in melting temp.

behavior of basaltic magama

low in silica and water, higher in melting temp.

fissure eruption and type of magama

opens up - basaltic magama

shield volcano

gentle/large in shape, flows basalt, wont erupt wildly

cinder cone volcano

steep, small, symmetrical, explosive/violent

stratovolcano

steep shape, erupts gas, layers of lava form hard surface

insolation decline

cooling- short term

CO2 addition atmosphere

warming- long term

caldera

depression that forms at surface

anticline

compression arch upwards

syncline

arching downward

dome

circular anticline (upward)

basin

circular syncline (downward)

normal fault

extension, distance has become larger

reverse fault

compression- lost horizontal space

thrust fault

low angle reverse fault

strike slip fault

rocks don't move vertically

slip

distance of motion

fault zone

numerous closely spaced fractures

joints

fractures without motion- decrease with depth

orogeny

rocks get smashed together

island arc crust type?

oceanic

mountain belts

parallel mountain ranges

formation of himalayas plate

indian

rocky mountains, when did it occur

100 mya

two names of orogenic events

columbia orogeny


laramide orogeny

weathering

decomposition of rocks

erosion

rocks being picked up and moved

mechanical weathering

any kind of physical force that decomposes rock

pressure-release fracturing

expands because pieces gone

abrasion

bumping against each other

organic activity

trees growing in rocks

hydrolysis

water gets into the rock forming a new mineral

chemical weathering

water, gas, anything in which chem reaction takes place

dissolution in rock

water attacks dissolves ex: limestone

oxidation

reaction w/oxygen, minerals change