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JH22-EARTH SYSTEMS II VOCAB-PLATE BOUNDARIES

ASSIGNED MONDAY (10/17) --LOG 15 MINUTES BY 10 PM THURSDAY

AB
FOLDED MOUNTAINScreated where two continental plates are pushed together EX: Mt. Everest
TRENCHlong and deep valley on the ocean floor created by subduction; ex: Mariana Trench
SUBDUCTIONprocess when one tectonic plate moves under another tectonic plate
DIVERGENT BOUNDARYwhen two tectonic plates move away from each other
MID OCEAN RIDGEan underwater mountain range created by diverging tectonic plates
RIFT VALLEYA deep valley that forms where two continental plates move apart
TRANSFORM BOUNDARYboundary where two tectonic plates shear past each other
SHEARINGprocess where plates slide past each other
FAULTa break in the Earth's crust caused by shearing; San Andreas
CONVECTION CURRENTSCircular currents in the mantle that causes oceanic & continental plates to move.
SEAFLOOR SPREADINGThe process that creates new sea floor as plates move away from each other at the mid-ocean ridges
OCEANIC-CONTINENTAL CONVERGENCEboundary where the more dense oceanic plate subducts under the less dense continental plate creating trenches or volcanic mountains
CONTINENTAL-CONTINENTAL CONVERGENCEboundary where two continental plates collide creating folded mountains
OCEANIC-OCEANIC CONVERGENCEboundary where denser plate is sub-ducted, deep trenches or volcanic islands formed
FOLDINGProcess caused by compression of rock to form a mountain
PLATE BOUNDARY TYPESdivergent, convergent, transform
DIVERGENT BOUNDARYboundary along which volcanoes form
TRANSFORM BOUNDARYboundary along which earthquakes occur
MID-OCEAN RIDGElong underwater volcanic mountain chain created when plates move apart
SUBDUCTION ZONEthe area of the asthenosphere where the plates melt
PACIFIC RING OF FIREa line of volcanoes that occurs along where the pacific plate is being subducted underneath other plates
DIVERGENT BOUNDARYwhere new ocean crust is formed?
CONVERGENT BOUNDARYWhere old ocean crust is destroyed?
FOCUSthe place inside the earth where an earthquake starts
EPICENTERthe place on the earth's crust directly above the place where and earthquake starts
SEISOMOGRAPHrecord of the movements of the earth's crust
PRIMARY (P) WAVEStravel through gases, liquids and solids push-pull waves fastest waves used to find the epicenter used to find travel time
SECONDARY (S) WAVEStravel through solids used to find the epicenter used to find travel time
SURFACE WAVEStravel through solids slowest waves cause the most damage
VISCOSITYability of a fluid to resist flowing
TEPHRAall pieces of all fragments of rock ejected into the air by an erupting volcano
BASALTIC MAGMAlow viscosity
VISCOSITYcontrols the character of eruptions--when higher lavas flow more slowly covering smaller area--when lower lava flows are more rapid and cover larger area
PYROCLASTIC FLOWa dense, destructive mass of very hot ash, lava fragments, and gases ejected explosively from a volcano and typically flowing downslope at great speed.
TEPHRAvolcanic bombs


Physical Science/Biology Instructor
Winston Jr/Sr High School
Winston, MO

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