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GRADE 10 SCIENCE
2 LESSON_Q1
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Plate Tectonic Theory
Theory about the distribution of
active volcanoes
,
earthquake epicenters
and
major mountain belts
, which are visibly
evident
in the motion of the
lithosphere
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Three types of plate boundaries
Divergent plate boundary
Convergent plate boundary
Transform fault plate boundary
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Divergent plate boundary
Forces are
pulling apart
where the plates will move
away
from each other
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Divergent plate boundary
Interacting crust can be
oceanic
to oceanic or
continental
to continental
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Convergent plate boundary
Forces will move toward each other and plates will collide
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Convergent
plate boundary
Interacting crust can be oceanic to oceanic, oceanic to
continental
, or
continental
to continental
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Transform fault boundary
Forces move passed each other or at same direction but at different rate, the plates will
slide
or
grind
past each other
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Transform fault boundary
Interacting crust can be
continental
to
continental
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Three types of plate boundary
Divergent
plate type boundary
Convergent
plate type boundary
Transform fault
plate boundary
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Divergent plate type boundary
A boundary that occurs along the spreading centers
Where plates are moving apart as the forces interacting are pulling or moving away from each other
Different geologic events will develop
Happens between the interaction of continental to continental crust and oceanic to oceanic crust
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Convergent plate type boundary
The interacting forces are moving toward or pushing each other thus causing the plates to collide
May occur between continental to continental, continental to oceanic and oceanic to oceanic crust
Several geologic events will also likely to occur
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Transform fault plate boundary
Boundaries at which plates move past one another horizontally in opposite directions or in the
same
direction but at different rates
Most of transform fault plate boundaries are found in the
ocean basins
, only few of which are found in the
continents
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Types of Plate Boundaries
Divergent
Convergent
Transform
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Kinds of Crust
Continental
to Continental
Oceanic
to
Oceanic
Continental
to
Continental
Continental
to
Oceanic
Oceanic
to
Oceanic
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Geologic events
Earthquake
Mid-Atlantic Ridge
New
seafloor
Widening ocean basin
Rift valley
formation to
linear sea
Mountain ranges
Volcanoes
Trenches
Subduction process
occur
Island arc
Zig-zag plate
margins
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