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CHapter 18 and 19 (Volcanoes and Earthquake) Review

Use this review as a guide... you still need to understand your notes.

AB
viscositythe internal resistence to flow
basaltic magmaforms when rocks in the upper mantle melt
andesitic magmafound along continental margins where oceanic crust is subducted into Earth's mantle
Rhyolitic magmaforms when molten material rises and mixes with the overlying silica- and water-rich continental crust
ventwhere lava erupts through an opening in the crust
craterlocated at the top of a volcano, around the vent
calderascan be up to 50km in diameter, can form when the summit or the side of a volcano collapses into the magma chamber that once fueled the volcano
shield volcanomountain with broad, gently sloping sides and a nearly circular base
cinder-cone volcanoforms when material ejected high into the air falls back to Earth and piles up around the vent
composite volcanoforms when layers of volcanic fragments alternate with lava
tephrarock fragments thrown into thte air during a volcanic eruption
pyroclastic flowrapidly moving volcanic material
hot spotsunusually hot regions of Earth's mantle where high-temperature plumes of mantle material rise toward the surface
stressthe forces per unit area acting on a material
strainthe deformation of materials in response to stress
faultthe resulting fracture or system of fractures, along which movement flows
reverse faultsfractures the form as a result of horizontal compression
normal faultsfractures caused by horizontal tension
strike-slip faultsfractures caused by horizontal shear
P-wavessqueeze and pull rocks in the same direction along which the waves are traveling
S-wavescause rocks to move at right angles in relation to the direction of the waves
surface wavesmove in two directions as they pass through rock
focusthe point where the earthquake originates
epicenterthe point on Earth's surface directly above the focus
seismometersvibrations from earthquakes are detected and recorded by sensitive instruments
seismogramthe recors produced by a seismogram
magnitudethe amount of energy released during as earthquake
Richter Scalehow an earthquake is rated based on the size os the largest seismic waves
Mercalli Scalerates the types of damage and other effects of an earthquake as noted by observers during and after its occurence
tsunamilarge ocean wave generated by vertical motions of the seafloor during an earthquake


Katherine Ewing

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