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Plate Tectonics
Review   Inside the Earth      The Earth is divided into four main layers:         Crust         Mantle         Outer...
The Crust The crust makes up 1% of the  Earth. The crust of the Earth is broken  into many pieces called plates. Two ty...
The Mantle   The upper part of    the mantle and the    crust make up the     Lithosphere.   The mantle is the    larges...
Lithosphere   The outermost ridge of the Earth.
Asthenosphere   Soft layer of the mantle on which    pieces of the lithosphere move.
Mesosphere   Beneath the    Asthenosphere    is the    strongest part    of the mantle    —the    Mesophere.
The CoreThe core extends fromthe bottom of themantle to the centerof the Earth.The outer core is liquid.The inner core is ...
Tectonic Plates   Pieces of the lithosphere that move    around on the top of the    asthenosphere.
Restless Continents   Drifting continents:Theory of Continental Drift
Continental Drift*Continents candrift apart fromone another andhave done so in thepast.*The continentsare still slowlymovi...
   Alfred Wegener suggested that    all continents were joined    together at some time in the    past. This is called th...
The Break up of Pangaea            *180 million years            ago
65 Million years ago
Evidence   1. Landforms   2. Fossils   3. Evidence from climate    changing
Landforms• Mountains in  South Africa  line up with  mountains in  Argentina• Coal mines  line up on  different  continents
Mountain Structures   Similar rock structures    are found on different    continents.   For example, parts of    Appala...
Appalachian Mountainsstrike through the easternUnited States andCanada then end at thesea off of Newfoundland.The Caledoni...
Fossils   Besides the puzzlelike fit of continents, fossils provided    support for continental drift.   For example: fo...
   Another fossil that supports the continental    drift is Glossopteris which has been found in    Africa, Australia, In...
Climate Clues   Fossils of tropical plants were found in    Spitsbergen, an ice covered island in the    Arctic Ocean (no...
Glacier Activity   Glacial deposits and rock    surfaces scoured and polished by    glaciers are found in South    Americ...
Why was it not accepted?   Wegener could not provide an    adequate explanation for the force    that pushes or pulls the...
Although Wegener provided evidence to support hishypothesis, he couldn’t answer two questions:1. What was causing the cont...
2. How were the continents moving?  Wegener proposed that the continents were  plowing through a stationary ocean floor. B...
And the rest of the story….Undaunted by rejection, Wegener devoted the restof his life to doggedly pursuing additionalevid...
The controversy continues!Plate tectonics has proven to be as important to the earthsciences as the discovery of the struc...
Plate TectonicsSeafloor Spreading    Harry    Hess
Sea-floor Spreading*How oceanic lithosphere is created asolder materials are pulled away.
   http://youtu.be/ryrXAGY1dmE   <iframe width="560" height="315"    src="http://www.youtube.com/embed/ryrXAG    Y1dmE" ...
Mapping TheOcean Floor   Scientists began using sound waves on moving    ships to map large areas of ocean floor in detai...
Mapping the Mid-Ocean Ridge Also known as the Mid-  Atlantic Ridge Longest mountain  chain in the world Divided by a tr...
   Most is hundreds of meters under water, but part    reaches above the ocean surface.   It is almost twice as deep as ...
   In the early 1960s, Harry Hess proposed that hot,    less dense material below Earth’s crust rises    toward the surfa...
   In 1968, a research ship, Glomar Challenger, began    gathering rock samples from mid-ocean ridges.   They made a rem...
Evidence of Sea-Floor Spreading   Molten Material   Magnetic Stripes   Drilling Samples
Magnetic Clues   Iron-bearing minerals,    such as magnetite, that    are found in the rocks of    the seafloor can recor...
SeafloorSpreading
Subduction of Deep-Ocean              Trenches   Subduction is the    process by which    the ocean floor    sinks beneat...
Subduction and Earth’s Ocean   Subduction and sea-floor spreading can    change the size and shape of the oceans.   The ...
   The Pacific Ocean is shrinking; a trench swallows    more oceanic crust than the mid-ocean ridge can    produce.   Th...
Section 3:           theory of Plate              tectonicS   In the 1960s, scientists developed a new theory that    com...
Where did the theory come               from?   J. Tuzo Wilson combined Earth’s plates,    continental drift, and sea-flo...
A Theory of Plate Tectonics   Plate tectonics states that pieces of Earth’s    lithosphere are in constant, slow motion, ...
Basically….   The plates on the lithosphere float on the    asthenosphere, convection currents rise in the    asthensophe...
   Earth’s crust and a part of upper mantle combined    are the lithosphere.     (100km=62 mile thick)   The plastic-lik...
Causes of Plate Tectonics   Convection currents cause the movements of plates   Hot, less dense liquid or gas is forced ...
   No plate can budge without affecting    the other plates surrounding it!
Plate Boundaries   When plates move, they can interact in several    ways. Three different moving types of plates are:   ...
 Faults break in Earth’s crust  where rocks have slipped past each  other. Plate boundaries are where the  edges of diff...
Gummy Time   Boundary Activity
Transform Boundary   Two plates slip past each other, moving in    opposite directions. (Do not push or pull)   Crust is...
Divergent Boundary   Two plates move apart or diverge.   Most occur at the mid-ocean ridge; they can also    occur on la...
Convergent Boundary   Two plates come together or collide (converge)   Results: earthquakes, trenches, volcanoes,    mou...
3 types of convergent boundary                 outcomes1)    Oceanic crust meets continental crust:
   Oceanic crust meets oceanic crust:
   Continental crust meets continental crust:   Example: Folded Mountains
The continents’ slow dance   The plates move at slow rates about 1 to 10 cm    per year.http://youtu.be/hSdlQ8x7cuk
To prevent confusion   Not all volcanoes    occur at plate    boundaries. For    example, the    Hawaiian islands    form...
Summary    Theories:     Continental Drift     Theory of Plate                      Theory              TectonicsForces of...
Cookie Time   Boundary Activity
2013 updated plate tectonics new one use this one
2013 updated plate tectonics new one use this one
2013 updated plate tectonics new one use this one
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Transcript of "2013 updated plate tectonics new one use this one"

  1. 1. Plate Tectonics
  2. 2. Review Inside the Earth  The Earth is divided into four main layers:  Crust  Mantle  Outer Core  Inner Core
  3. 3. The Crust The crust makes up 1% of the Earth. The crust of the Earth is broken into many pieces called plates. Two types of crust:  Oceanic (made of basalt)  Continental (made of granite)
  4. 4. The Mantle The upper part of the mantle and the crust make up the Lithosphere. The mantle is the largest layer of the Earth. The mantle can be divided into two regions: the upper and lower mantle.
  5. 5. Lithosphere The outermost ridge of the Earth.
  6. 6. Asthenosphere Soft layer of the mantle on which pieces of the lithosphere move.
  7. 7. Mesosphere Beneath the Asthenosphere is the strongest part of the mantle —the Mesophere.
  8. 8. The CoreThe core extends fromthe bottom of themantle to the centerof the Earth.The outer core is liquid.The inner core is thesolid dense center ofour planet.
  9. 9. Tectonic Plates Pieces of the lithosphere that move around on the top of the asthenosphere.
  10. 10. Restless Continents Drifting continents:Theory of Continental Drift
  11. 11. Continental Drift*Continents candrift apart fromone another andhave done so in thepast.*The continentsare still slowlymoving, at aboutthe speed yourfingernails grow.
  12. 12.  Alfred Wegener suggested that all continents were joined together at some time in the past. This is called the hypothesis of “continental drift”. According to continental drift, continents have moved slowly to their current locations. He called this large landmass as Pangaea (“all land”)
  13. 13. The Break up of Pangaea *180 million years ago
  14. 14. 65 Million years ago
  15. 15. Evidence 1. Landforms 2. Fossils 3. Evidence from climate changing
  16. 16. Landforms• Mountains in South Africa line up with mountains in Argentina• Coal mines line up on different continents
  17. 17. Mountain Structures Similar rock structures are found on different continents. For example, parts of Appalachian mountains are similar to those found in Greenland and western Europe.
  18. 18. Appalachian Mountainsstrike through the easternUnited States andCanada then end at thesea off of Newfoundland.The CaledonidesMountains are found ineastern Greenland,Ireland, Great Britainand Norway.These two mountainranges are the same agewith the same rock typesand structures.
  19. 19. Fossils Besides the puzzlelike fit of continents, fossils provided support for continental drift. For example: fossils of the reptile Mesosaurus have been found in South America and Africa.
  20. 20.  Another fossil that supports the continental drift is Glossopteris which has been found in Africa, Australia, India, South America, and Antarctica.
  21. 21. Climate Clues Fossils of tropical plants were found in Spitsbergen, an ice covered island in the Arctic Ocean (north of Norway).
  22. 22. Glacier Activity Glacial deposits and rock surfaces scoured and polished by glaciers are found in South America, Africa, India and Australia.
  23. 23. Why was it not accepted? Wegener could not provide an adequate explanation for the force that pushes or pulls the continents.
  24. 24. Although Wegener provided evidence to support hishypothesis, he couldn’t answer two questions:1. What was causing the continents to move? Wegener said that this force might be the rotation of Earth, however, physicists were able to show that this force was not great enough to move continents.
  25. 25. 2. How were the continents moving? Wegener proposed that the continents were plowing through a stationary ocean floor. But, his peers argued that continents could not push through the ocean floor without fracturing, because crustal rock is too brittle. And no evidence of fracturing had been found.
  26. 26. And the rest of the story….Undaunted by rejection, Wegener devoted the restof his life to doggedly pursuing additionalevidence to defend his theory. He froze to death in1930 during an expedition crossing the Greenlandice cap, but the controversy he spawned raged on.However, after his death, new evidence fromocean floor exploration and other studies rekindledinterest in Wegeners theory, ultimately leading tothe development of the theory of plate tectonics.http://bumileluhur.blogspot.com/2011/01/this-dyniamic-earth-story-of-plate.html
  27. 27. The controversy continues!Plate tectonics has proven to be as important to the earthsciences as the discovery of the structure of the atom was tophysics and chemistry. Even though the theory of platetectonics is now widely accepted by the scientificcommunity, aspects of the theory are still being debatedtoday. Ironically, one of the chief outstanding questions is theone Wegener failed to resolve: What is the nature of theforces propelling the plates? Scientists also debate how platetectonics may have operated (if at all) earlier in the Earthshistory and whether similar processes operate, or have everoperated, on other planets in our solar system. Will you be the one to solve the mystery?
  28. 28. Plate TectonicsSeafloor Spreading Harry Hess
  29. 29. Sea-floor Spreading*How oceanic lithosphere is created asolder materials are pulled away.
  30. 30.  http://youtu.be/ryrXAGY1dmE <iframe width="560" height="315" src="http://www.youtube.com/embed/ryrXAG Y1dmE" frameborder="0" allowfullscreen></iframe>
  31. 31. Mapping TheOcean Floor Scientists began using sound waves on moving ships to map large areas of ocean floor in detail. Sound waves echo off the ocean bottom – the longer the sound waves take to return to the ship, the deeper the water is.
  32. 32. Mapping the Mid-Ocean Ridge Also known as the Mid- Atlantic Ridge Longest mountain chain in the world Divided by a trench
  33. 33.  Most is hundreds of meters under water, but part reaches above the ocean surface. It is almost twice as deep as the Grand Canyon. Iceland is part of the mid-ocean ridge
  34. 34.  In the early 1960s, Harry Hess proposed that hot, less dense material below Earth’s crust rises toward the surface at the mid-ocean ridges. Then, it flows sideways, carrying seafloor away from the ridge in both directions. This theory is known “seafloor spreading”.
  35. 35.  In 1968, a research ship, Glomar Challenger, began gathering rock samples from mid-ocean ridges. They made a remarkable discovery as they studied the ages of rock samples. The younger rocks are closer to the mid-ocean ridges and older rocks are farther from the ridges.
  36. 36. Evidence of Sea-Floor Spreading Molten Material Magnetic Stripes Drilling Samples
  37. 37. Magnetic Clues Iron-bearing minerals, such as magnetite, that are found in the rocks of the seafloor can record Earth’s magnetic field direction when they form. The magnetic alignment in the rocks reverses back and forth over time in strips parallel to the mid-ocean ridges.
  38. 38. SeafloorSpreading
  39. 39. Subduction of Deep-Ocean Trenches Subduction is the process by which the ocean floor sinks beneath a deep-ocean trench and back into the mantle.
  40. 40. Subduction and Earth’s Ocean Subduction and sea-floor spreading can change the size and shape of the oceans. The ocean floor is renewed about every 200 million years.
  41. 41.  The Pacific Ocean is shrinking; a trench swallows more oceanic crust than the mid-ocean ridge can produce. The Atlantic Ocean is expanding. There are only a few trenches in the Atlantic. The continental crust is attached to the ocean floor, so as the Atlantic expands and moves, the continents move with it.
  42. 42. Section 3: theory of Plate tectonicS In the 1960s, scientists developed a new theory that combined continental drift and seafloor spreading . According to the theory of plate tectonics, Earth’s crust and part of upper mantle are broken into sections. These sections are called plates, move on a plastic-like layer of the mantle.
  43. 43. Where did the theory come from? J. Tuzo Wilson combined Earth’s plates, continental drift, and sea-floor spreading into a single theory---PLATE TECTONICS
  44. 44. A Theory of Plate Tectonics Plate tectonics states that pieces of Earth’s lithosphere are in constant, slow motion, driven by convection currents in the mantle, and it explains the formation, movement, and subduction of Earth’s plates.
  45. 45. Basically…. The plates on the lithosphere float on the asthenosphere, convection currents rise in the asthensophere and spread out beneath the lithosphere. http://youtu.be/ryrXAGY1dmE
  46. 46.  Earth’s crust and a part of upper mantle combined are the lithosphere. (100km=62 mile thick) The plastic-like layer below the lithosphere is called asthenosphere. The rigid plates of the lithosphere float and move around on the asthenosphere.
  47. 47. Causes of Plate Tectonics Convection currents cause the movements of plates Hot, less dense liquid or gas is forced upward, as it reaches the surface, it cools down and sinks back down. This entire cycle of heating, rising, cooling and sinking is called a convection current.
  48. 48.  No plate can budge without affecting the other plates surrounding it!
  49. 49. Plate Boundaries When plates move, they can interact in several ways. Three different moving types of plates are:  Plates moving apart (Divergent)  Plates moving together (Convergent)  Plates slide past each other (Transform)
  50. 50.  Faults break in Earth’s crust where rocks have slipped past each other. Plate boundaries are where the edges of different pieces of the lithosphere meet.
  51. 51. Gummy Time Boundary Activity
  52. 52. Transform Boundary Two plates slip past each other, moving in opposite directions. (Do not push or pull) Crust is neither created nor destroyed near a transform boundary. Earthquakes occur frequently along these boundaries.
  53. 53. Divergent Boundary Two plates move apart or diverge. Most occur at the mid-ocean ridge; they can also occur on land (poor Africa). A rift valley is a deep valley that forms along the divergent valley. The Great Rift Valley in Africa marks a deep crack in the African continent that runs for about 3,000 km. When divergent boundaries develop on land, two of Earth’s plates pull apart.
  54. 54. Convergent Boundary Two plates come together or collide (converge) Results: earthquakes, trenches, volcanoes, mountains When two plates collide the denser of the two plates will sink or slide beneath the other.
  55. 55. 3 types of convergent boundary outcomes1) Oceanic crust meets continental crust:
  56. 56.  Oceanic crust meets oceanic crust:
  57. 57.  Continental crust meets continental crust: Example: Folded Mountains
  58. 58. The continents’ slow dance The plates move at slow rates about 1 to 10 cm per year.http://youtu.be/hSdlQ8x7cuk
  59. 59. To prevent confusion Not all volcanoes occur at plate boundaries. For example, the Hawaiian islands formed from a hot spot volcano. As the Pacific plate moves across a fixed hot spot (mantle plume), new volcanoes (and islands) form.
  60. 60. Summary Theories: Continental Drift Theory of Plate Theory TectonicsForces of Plate Cycle of Gravity Heated CoreMovement: Convection CurrentsTypes of Plate Divergent Convergent TransformMovement/Interactions:(Boundary)Processes or Sea-floor Subduction EarthquakesTypes of Spreading (Volcanoes) andMovement Mountains(Results):Stress: Tension Compression ShearingFaults: Normal Reverse Strike Slip
  61. 61. Cookie Time Boundary Activity
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