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acloutier copyright 2013
Plate Tectonics
Ann C. Cloutier
Pangaea
Continental Drift
Sea Floor Spreading
Isochron Maps – Geomagnetic Core
GPS
Sonar
acloutier copyright 2013
Continental Drift
from a Hypothesis by Alfred Wegener and was
developed into a Theory with supporting evidence
 Super continent called Pangaea >Greek for “all land”
 Began to brake apart over 200 million years ago
 Puzzle fit of South America and Africa
 Collected evidence in rocks, fossils, and climatic data to
support his hypothesis
acloutier copyright 2013
Evidence to collect to support hypothesis but, no means to
explain how the continents were moved…yet !
acloutier copyright 2013
Glossopteris and Mesosaurus
acloutier copyright 2013
Ancient climates
evidence of coal deposits found in Antarctica
 coal is formed from swamp plant or other vegetation that
has decomposed
 this meant a temperate rainy climate was once on the
surface of Antarctica
 glacial deposits of till and striation scratches on bedrock
found in Afrrica, 290 million year old land formations
 today Africa is covered by huge deserts where the
evidence of continental glaciers was documented
acloutier copyright 2013
How is coal formed ?
acloutier copyright 2013
Today 290MYBP
acloutier copyright 2013
Seafloor Spreading
 Technology sonar echo-
location > sound beams /
time returned
 WWII submarine warfare
developed technology to
detect more than an
enemy sub
 Detailed maps and a safe
way to navigate the
bottom
acloutier copyright 2013
Seafloor spreading Harry Hess
acloutier copyright 2013
Mid Ocean Ridges & Trenches
 Ocean ridges are long
mountain ranges
 Continuous wrap around
planet
 Deepest and longest
mountain range on the
planet
 ~46,000 miles long (~ 72km)
 Mariana Trench
 11 km deep deepest
trench in all oceans
acloutier copyright 2013
Continental Crust - Oceanic Crust
 Oldest age 3.8 BYBP
 Billions of years before
present
 Less dense than oceanic
crust
 Continental mountains
keep getting folded and
faults break up crust
 Young age ~ today’s lava
>180 MYBP
 Millions of years before
present
 More dense than
continental crust
 The further away from the
ridge the thicker and
older the oceanic crust
becomes
acloutier copyright 2013
Earth quakes occur at plate boundaries
acloutier copyright 2013
Seismic information
acloutier copyright 2013
Richter Scale
Earthquake magnitude of seismic wave data
acloutier copyright 2013
Safety for Earthquake
acloutier copyright 2013
acloutier copyright 2013
Causes of Plate Movement
 Mantle convection are thought to be the driving mechanism of plate tectonic
movement
(continental drift caused by seafloor spreading and subduction)
 The transfer of heat, called thermal energy is the cause of the movement of
hot matter (magma) moving to cold matter; this is called convection
 Warm matter move toward cold matter
 Cooler matter sinks because it is more dense
 “G force” gravity pulls it down into the mantle
 Ridge push and slab pull are the results of this process of heat moving away
from the radiation of the core out towards the crust
acloutier copyright 2013
Convection current of Earth’s mantle
the bulldozer pushes plates around the planet surface
acloutier copyright 2013
Isochron Map
maps with magnetic fields showing Earth’s polarity for
magnetic north
 A line graph defined by data
for rocks of the same age;
 With the same isotopic
composition
 Polarity event is recorded in
rocks a period of no more
than 100,000 years when
Earth’s magnetic polarity was
opposite to the existing
polarity
acloutier copyright 2013
Check out and watch this movie on your iPad
 http://science.discovery.com/tv-shows/greatest-
discoveries/videos/100-greatest-discoveries-magnetic-field-
reversal.htm
acloutier copyright 2013
http://www.youtube.com/watch?
v=1sNL-XaBmBk
acloutier copyright 2013
http://mysciencebox.org/files/images/magnetic_reversal_animation.gif
acloutier copyright 2013
Questions?
Going further time for the iPad technology
 Do scientist know if convection currents stay in
the same places ?
 Are hot spots located in the same places ?
For how long ?
 Is Cape Cod located on a hot spot?
 What state is located over a hot spot ?
 When was the last earthquake Cape Cod felt ?

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Plate tectonics power point 2012 acloutier

  • 1. acloutier copyright 2013 Plate Tectonics Ann C. Cloutier Pangaea Continental Drift Sea Floor Spreading Isochron Maps – Geomagnetic Core GPS Sonar
  • 2. acloutier copyright 2013 Continental Drift from a Hypothesis by Alfred Wegener and was developed into a Theory with supporting evidence  Super continent called Pangaea >Greek for “all land”  Began to brake apart over 200 million years ago  Puzzle fit of South America and Africa  Collected evidence in rocks, fossils, and climatic data to support his hypothesis
  • 3. acloutier copyright 2013 Evidence to collect to support hypothesis but, no means to explain how the continents were moved…yet !
  • 5. acloutier copyright 2013 Ancient climates evidence of coal deposits found in Antarctica  coal is formed from swamp plant or other vegetation that has decomposed  this meant a temperate rainy climate was once on the surface of Antarctica  glacial deposits of till and striation scratches on bedrock found in Afrrica, 290 million year old land formations  today Africa is covered by huge deserts where the evidence of continental glaciers was documented
  • 6. acloutier copyright 2013 How is coal formed ?
  • 8. acloutier copyright 2013 Seafloor Spreading  Technology sonar echo- location > sound beams / time returned  WWII submarine warfare developed technology to detect more than an enemy sub  Detailed maps and a safe way to navigate the bottom
  • 9. acloutier copyright 2013 Seafloor spreading Harry Hess
  • 10. acloutier copyright 2013 Mid Ocean Ridges & Trenches  Ocean ridges are long mountain ranges  Continuous wrap around planet  Deepest and longest mountain range on the planet  ~46,000 miles long (~ 72km)  Mariana Trench  11 km deep deepest trench in all oceans
  • 11. acloutier copyright 2013 Continental Crust - Oceanic Crust  Oldest age 3.8 BYBP  Billions of years before present  Less dense than oceanic crust  Continental mountains keep getting folded and faults break up crust  Young age ~ today’s lava >180 MYBP  Millions of years before present  More dense than continental crust  The further away from the ridge the thicker and older the oceanic crust becomes
  • 12. acloutier copyright 2013 Earth quakes occur at plate boundaries
  • 14. acloutier copyright 2013 Richter Scale Earthquake magnitude of seismic wave data
  • 17. acloutier copyright 2013 Causes of Plate Movement  Mantle convection are thought to be the driving mechanism of plate tectonic movement (continental drift caused by seafloor spreading and subduction)  The transfer of heat, called thermal energy is the cause of the movement of hot matter (magma) moving to cold matter; this is called convection  Warm matter move toward cold matter  Cooler matter sinks because it is more dense  “G force” gravity pulls it down into the mantle  Ridge push and slab pull are the results of this process of heat moving away from the radiation of the core out towards the crust
  • 18. acloutier copyright 2013 Convection current of Earth’s mantle the bulldozer pushes plates around the planet surface
  • 19. acloutier copyright 2013 Isochron Map maps with magnetic fields showing Earth’s polarity for magnetic north  A line graph defined by data for rocks of the same age;  With the same isotopic composition  Polarity event is recorded in rocks a period of no more than 100,000 years when Earth’s magnetic polarity was opposite to the existing polarity
  • 20. acloutier copyright 2013 Check out and watch this movie on your iPad  http://science.discovery.com/tv-shows/greatest- discoveries/videos/100-greatest-discoveries-magnetic-field- reversal.htm
  • 23. acloutier copyright 2013 Questions? Going further time for the iPad technology  Do scientist know if convection currents stay in the same places ?  Are hot spots located in the same places ? For how long ?  Is Cape Cod located on a hot spot?  What state is located over a hot spot ?  When was the last earthquake Cape Cod felt ?