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38 Cards in this Set

  • Front
  • Back

Seismic waves

body waves (p and s waves)
surface waves

Surface to center order...

Crust (solid)
Mantle(plastic-like/solid)
lower (rigid/solid)
Core (outer=liquid, inner=solid)



Minerals

Naturally-occurring, inorganic solid with a definite atomic structure and chemical composition.

mineral properties

hardness, cleavage, fracture, color streak, luster

rock types

igneous - forms from cooling of magma


sedimentary - forms from lithificationof rock fragments


metamorphic rocks - forms from changes in rock temp/pressure





Burial

when additional sediment accumulates on top burying original sediment



compaction

weight of overlying sediment reduces the pore space between sediment particles

cementation

precipitation of minerals within pores that effectivelhy binds (glues) sediment together (CaCO3, Si)



clastic

made from particles of preexisting rocks

non-clastic

formed from chemical solution o from organic deposition

clastic rocks

conglomerate
sandstone
shale
non-clastic rocks

limestone
rock salt
chalk



strata

layer of sedimentary rockor soil



unconformity

gap in the rock record

3 factors that determine the violence of an eruption
composition, temp, dissolved gases

lahars

viscous mudflow of pyroclastic debris and water, may be triggered by rapid snow melt or rain



pyroclastic flows

composed of hot ash, pumice, rock fragments, and volcanic gas

focus

the location where earthquakes originate

epicenter

the oint directly above the focus on the earth


s surface

magnitude

measure sthe amount of energy released

intensity

measures the amount of shaking that has occurred
intensity

Mercalli Scale)))) based on damage sustained. factors that determine structural damage

liquefaction

saturation of ground material turning into a fluid

fault

fracture in crustal rock where one side is displaced with respect to the other side

sublimation

solid to gas

deposition

gas to solid
stability of air

determines cloud types, intensity of precipitation

relative humidity
amount of water vapour in air

saturated

air is filled to 100% capacity

stable air

cooler/denser than surrounding air (sinks),

resists vertical displacement, light to moderate precipitation

unstable air

warmer and less dense than surrounding air (rises), clouds are often "towering", heavy precipitation

earth's axis tilt

23.5 degrees

O3
OZONE, 3 OXYGENS

2 types of heat

solar + terrestial

atmospheric pressure

weight of the air (decreases with altitude)_

adiabatic temperature
changes when air is compressed (warm) or expand (cools)

heat

measured in calories

states of matter

solid, liquid, gas