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chapter 22: plate tectonics, earthquakes and volcanoes

geology

AB
geologistsscientists who study the earth and its composition
uniformitarianismthe idea that the earth goes through the same geological changes now as in the past
three layers of the earthcrust mantle and core
lithospherelayer of the mantle with cool,rigid rock
asthenospheresecond layer of the mantle with soft flowing "taffy" rock
mesospherelowest level of mantle with stiff rock to the core
outer corelarge sphere in earth's center -liquid constantly moving causing magnetic field
inner coresolid center of the earth under great pressure
properties of metalscrystal,luster,streal,color,density
plate tectonicstheory that earth's lithoshere moves slowly on top of mantle
Wegner's hypothesistheory that continents were one
Pangaeaancient supercontinent
Wegner's challengeproblem with explaining how continents plow through ocean floor
mid-ocean rangearea in ocean where rocks are the youngest
subductionplates that SINK into the crust
trenchdepression in the ocean floor
sea floor spreadingcreates new ocean crust at the mid ocean ridges
divergent boundariesplates that MOVE AWAY from each other
convergent boundariesplates that come together or collide
transform boundariesplates that SLIDE past each other
stressforce that pushes together and pulls apart plates
faulta break in a mass of rocks
folda bend in a layer of rocks
epicenterlocation on earth's surface that is the center of an earthquake
P wavesseismic waves similar to sound waves (longitudinal) that travel through solid and liquids
S wavesseismic waves cannot pass through liquids travel at right angles
seismographa device to detect earthquake
MMS (moment magnitude scale)scale to measure intensity of earthquakes
magmaamount of mantle rock that melts andis less dense than rock; rises to the surface
pipenarrow vertical chamber where magma collects
craterbowl shaped pit on the top of a volcano
quiet eruptionvolcano magma that is very hot low silica- low viscosity
explosive eruptionhigh silica magma that clogs volcano pipes cause this
shield volcanotype of volcano low flat low viscosity
composite volcanotype of volcano that forms from explosive ash and lava
cinder volcanovolcano formed from ash and cinders in an explosive
batholithlargest type of intrusive igneous rock
igneous rocktype of rock formed from molten material that cools on the earth's surface is extrusive
sedimentary rockrocks that form from minerals or weathering or living organism shells
metamorphic rockrocks formed by heat and pressure deep underground


Intervention Teacher
Barrington High School
Barrington, RI

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