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By Prof. Liwayway Memije-Cruz
Plate Tectonics
The Continental Drift Theory
According to Alfred Wegener had once been joined together
forming a single supercontinent landmass called Pangaea that
divided into individual continents as they are now.
The Seafloor Spreading Theory
This theory states
that the oceanfloor
are spreading
outward from vast
underwater ridges.
This was proposed
by an American
geologist named
Harry H. Hess in
early 1960’s.
Seafloor Spreading
What is Plate Tectonics Theory?
Plate tectonics is the theory that the outer rigid layer of
the earth (the lithosphere) is divided into a couple of
dozen "plates" that move around across the earth's surface
relative to each other, like slabs of ice on a lake.
TYPES OF PLATE BOUNDARY
Divergent boundary or divergent plate boundary
(also known as a constructive boundary or an
extensional boundary) is a linear feature that exists
between two tectonic plates that are moving away
from each other.
Convergent boundary, also known as a destructive
plate boundary (because of subduction), is an actively
deforming region where two (or more) tectonic plates
or fragments of the lithosphere move toward one
another and collide.
Transform boundary (or conservative boundary) is where
two of the tectonic plates slide alongside each other. When
this happens, the scraping of the two plates causes
earthquakes. And since these faults neither create nor destroy
lithosphere, is a type of fault whose relative motion is
predominantly horizontal in either sinistral or dextral
direction.
Transform boundary (or conservative boundary) is where
two of the tectonic plates slide alongside each other. When
this happens, the scraping of the two plates causes
earthquakes. And since these faults neither create nor destroy
lithosphere, is a type of fault whose relative motion is
predominantly horizontal in either sinistral or dextral
direction.

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Plate tectonics

  • 1. By Prof. Liwayway Memije-Cruz Plate Tectonics
  • 2. The Continental Drift Theory According to Alfred Wegener had once been joined together forming a single supercontinent landmass called Pangaea that divided into individual continents as they are now.
  • 3.
  • 4. The Seafloor Spreading Theory This theory states that the oceanfloor are spreading outward from vast underwater ridges. This was proposed by an American geologist named Harry H. Hess in early 1960’s.
  • 6. What is Plate Tectonics Theory? Plate tectonics is the theory that the outer rigid layer of the earth (the lithosphere) is divided into a couple of dozen "plates" that move around across the earth's surface relative to each other, like slabs of ice on a lake.
  • 7. TYPES OF PLATE BOUNDARY Divergent boundary or divergent plate boundary (also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates that are moving away from each other.
  • 8. Convergent boundary, also known as a destructive plate boundary (because of subduction), is an actively deforming region where two (or more) tectonic plates or fragments of the lithosphere move toward one another and collide.
  • 9. Transform boundary (or conservative boundary) is where two of the tectonic plates slide alongside each other. When this happens, the scraping of the two plates causes earthquakes. And since these faults neither create nor destroy lithosphere, is a type of fault whose relative motion is predominantly horizontal in either sinistral or dextral direction.
  • 10. Transform boundary (or conservative boundary) is where two of the tectonic plates slide alongside each other. When this happens, the scraping of the two plates causes earthquakes. And since these faults neither create nor destroy lithosphere, is a type of fault whose relative motion is predominantly horizontal in either sinistral or dextral direction.