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platetectonics theory.ppt
Explain the Plate Tectonic theory.
Describe the distribution of active
volcanoes, Earthquake epicenters,
and major mountain belts.
1. What is the theory of plate
tectonics?
2. What are the three types of
plate boundaries?
• The Earth’s crust and
upper mantle(Lithosphere)
are broken into sections
called plates
• Plates move around on top
of the mantle like rafts
• A section of the lithosphere
that slowly moves over the
asthenosphere, carrying
pieces of continental and
oceanic crust.
The theory which states that pieces of Earth’s
lithosphere are in constant motion, driven by
convection currents in the mantle.
• Plates move
slowly in
different
directions
Cause different
geologic events
(like
earthquake,
volcano, etc.)
platetectonics theory.ppt
Convection Currents in the mantle move the plates as the core heats
the slowly-flowing asthenosphere (the elastic/plastic-like part of the
mantle).
platetectonics theory.ppt
The edges of Earth’s plates
meet at plate boundaries.
Extended deep into the
lithosphere
Divergent Boundaries
 Convergent Boundaries
 Transform Boundaries
A plate boundary where two plates move away from each other.
 
RIFTING
causes
SEAFLOOR SPREADING
platetectonics theory.ppt
platetectonics theory.ppt
• A geologic feature or event…
May form RIFT
VALLEYS on continents
SEA-FLOOR
SPREADING in the
ocean
• Divergent is like “dissecting” or “dividing”
• If you pull warm bubble gum or silly putty, it will thin in the
middle until it is stressed so much that it breaks.
• Happens on land
& under H2O
• Mid-ocean ridges
• rift valleys
• fissure volcanoes
A plate boundary where two plates
move towards each other.
Boundaries between two
plates that are colliding
 
This stress is called COMPRESSION
 Places where
plates crash (or
crunch) together
or subduct (one
sinks under)
Ocean plate colliding with a less dense
continental plate
Subduction Zone: The process by which
oceanic crust sinks beneath a deep-ocean
trench and back into the mantle at a
convergent plate boundary.
platetectonics theory.ppt
What else happens at Convergent Boundaries?
VOLCANOES
occur at
subduction
zones
platetectonics theory.ppt
• Ocean plate colliding with another ocean plate
• The less dense plate slides under the more dense plate creating a
subduction zone called a TRENCH
platetectonics theory.ppt
A continental plate colliding with another
continental plate
Have Collision Zones:
A place where folded and thrust faulted
mountains form.
• May form Mountain Ranges.
These are Folded Mountains, like the Himalayas or the Rockies.
A REVERSE FAULT
Rock is forced upward as it is
squeezed.
• Convergent = “Connecting” boundaries
• May work like a trash compactor smashing rock.
– Rock goes crunches up to make folded mountains.
– Rock goes down “under” @ subduction zone.
A plate boundary where two plates move past each other in opposite
direction.
Rock is pushed
in two opposite
directions (or
sideways, but no
rock is lost)
This stress is
called
SHEARING
• May cause Earthquakes
when the rock snaps from
the pressure.
• A famous fault @ a
Transform Boundary is
the San Andreas Fault in
California.
platetectonics theory.ppt
A STRIKE-SLIP FAULT
Rocks on each side of the fault slip
past each other as they break.
 Shearing means cutting (“Shears” are like scissors)
 Transform boundaries run like trains going past each other in
different directions & they shake the ground!
Can you match
the boundary
name correctly
with its
diagram?
A._____________
B._____________
C._____________
•Correct
Answers:
A.Divergent
B.Convergent
C.Transform

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platetectonics theory.ppt

  • 2. Explain the Plate Tectonic theory. Describe the distribution of active volcanoes, Earthquake epicenters, and major mountain belts.
  • 3. 1. What is the theory of plate tectonics? 2. What are the three types of plate boundaries?
  • 4. • The Earth’s crust and upper mantle(Lithosphere) are broken into sections called plates • Plates move around on top of the mantle like rafts • A section of the lithosphere that slowly moves over the asthenosphere, carrying pieces of continental and oceanic crust.
  • 5. The theory which states that pieces of Earth’s lithosphere are in constant motion, driven by convection currents in the mantle. • Plates move slowly in different directions Cause different geologic events (like earthquake, volcano, etc.)
  • 7. Convection Currents in the mantle move the plates as the core heats the slowly-flowing asthenosphere (the elastic/plastic-like part of the mantle).
  • 9. The edges of Earth’s plates meet at plate boundaries. Extended deep into the lithosphere
  • 10. Divergent Boundaries  Convergent Boundaries  Transform Boundaries
  • 11. A plate boundary where two plates move away from each other.   RIFTING causes SEAFLOOR SPREADING
  • 14. • A geologic feature or event… May form RIFT VALLEYS on continents SEA-FLOOR SPREADING in the ocean
  • 15. • Divergent is like “dissecting” or “dividing” • If you pull warm bubble gum or silly putty, it will thin in the middle until it is stressed so much that it breaks. • Happens on land & under H2O
  • 16. • Mid-ocean ridges • rift valleys • fissure volcanoes
  • 17. A plate boundary where two plates move towards each other. Boundaries between two plates that are colliding   This stress is called COMPRESSION
  • 18.  Places where plates crash (or crunch) together or subduct (one sinks under)
  • 19. Ocean plate colliding with a less dense continental plate Subduction Zone: The process by which oceanic crust sinks beneath a deep-ocean trench and back into the mantle at a convergent plate boundary.
  • 21. What else happens at Convergent Boundaries? VOLCANOES occur at subduction zones
  • 23. • Ocean plate colliding with another ocean plate • The less dense plate slides under the more dense plate creating a subduction zone called a TRENCH
  • 25. A continental plate colliding with another continental plate Have Collision Zones: A place where folded and thrust faulted mountains form.
  • 26. • May form Mountain Ranges. These are Folded Mountains, like the Himalayas or the Rockies.
  • 27. A REVERSE FAULT Rock is forced upward as it is squeezed.
  • 28. • Convergent = “Connecting” boundaries • May work like a trash compactor smashing rock. – Rock goes crunches up to make folded mountains. – Rock goes down “under” @ subduction zone.
  • 29. A plate boundary where two plates move past each other in opposite direction.
  • 30. Rock is pushed in two opposite directions (or sideways, but no rock is lost) This stress is called SHEARING
  • 31. • May cause Earthquakes when the rock snaps from the pressure. • A famous fault @ a Transform Boundary is the San Andreas Fault in California.
  • 33. A STRIKE-SLIP FAULT Rocks on each side of the fault slip past each other as they break.
  • 34.  Shearing means cutting (“Shears” are like scissors)  Transform boundaries run like trains going past each other in different directions & they shake the ground!
  • 35. Can you match the boundary name correctly with its diagram? A._____________ B._____________ C._____________