Movement ang the ouit ine 7. A river is running though the region represented by the topographic map or V shaped lines The dagram below shows a model of the movement of two tectonic plates. When the plates colide, one plate often moves below the other plate Oceanic Oceanic crust crust O Between Points 1 and 2 The ising magma that can resut from this type of plate movement may produce- O Between Points 2 and 3 F fossil layers G vokcanic slands O Between Points 3 and 4 H deep-sea sediment seafloor spreading Between Points 4 and s

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- STAAR Review- Earth Cycles/PlateBoundaries/TopoM... S ¢ D
The San Andn
whe the tu
anhrm A The ma h a
Sus
w d e ake
whk w boeoed wnsl me
Dossands of ps
best predicts he lkely movement of land along the faut ne ever thousands of
years?
San Andreas
Faut
San Andreas
Faut
Movement toward
the s
Spreading along the
ut ne
San Andreas
Fault
San Andreas
Feult
7.A river is running though the region represented by the topographic map shown her
or V shaped lines
Movement along the
fault ine
Mourtain bulding
The diagram below shows a model of the movement of two tectonic plates. When the plates
colide, one plate often moves below the other plate
Oceanic
Oceanic
crust
crust
chust
O Between Points 1 and 2
The rising magma that can result from this type of plate movement may produce-
O Between Points 2 and 3
F fossil lavers
G volcanic islands
O Between Points 3 and 4
H deep-sea sediment
3seafloor spreading
O Between Points 4 and 5
Transcribed Image Text:- STAAR Review- Earth Cycles/PlateBoundaries/TopoM... S ¢ D The San Andn whe the tu anhrm A The ma h a Sus w d e ake whk w boeoed wnsl me Dossands of ps best predicts he lkely movement of land along the faut ne ever thousands of years? San Andreas Faut San Andreas Faut Movement toward the s Spreading along the ut ne San Andreas Fault San Andreas Feult 7.A river is running though the region represented by the topographic map shown her or V shaped lines Movement along the fault ine Mourtain bulding The diagram below shows a model of the movement of two tectonic plates. When the plates colide, one plate often moves below the other plate Oceanic Oceanic crust crust chust O Between Points 1 and 2 The rising magma that can result from this type of plate movement may produce- O Between Points 2 and 3 F fossil lavers G volcanic islands O Between Points 3 and 4 H deep-sea sediment 3seafloor spreading O Between Points 4 and 5
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