Plate Tectonics

Cards (22)

  • Lithosphere 
    • Crust and uppermost mantle 
    • Rigid
  • Asthenosphere
    • relatively weak
  • Continental drift hypothesis
    • Alfred Wegener
    • German meteorologist and geophysicist
    • The origin of continents and oceans; Pangaea
    • Pangaea = "all land” 
    • Laurasia: North America, Europe and Asia
    • Gondwanaland: South America, Africa, India, Australia, and Antartica 
    • Panthalassa - “all sea” 
  • Evidence of the Continental Drift Hypothesis
    • Continental jigsaw puzzle fit
    • Africa and South America fit if Atlantic Ocean is closed
    • Fossil match across continents
    • Fossils of animals and plants that could not have traveled through the oceans: Mesosaurus, Glossopteris, and Lystrosaurus
    • rock type and geologic features
    • Similarities across continents (e.g., Appalachian-Caledonian Mountains)
    • Paleoclimatic evidence
    • Coal seams in Northern Hemisphere with tropical trees
    • Glacial till and striations in Southern Africa, South America, Australia, and India
  • Opposition for the CDH
    • no explanation for the mechanism for such movement
    • According to Wegener
    • suggested that it was moving because of tidal waves, continents broke through oceanic crust
  • Seafloor Spreading
    • Introduced by Harry Hess in the early 1960s
    • Extensive mapping of the ocean floor during the WW II
    • Submarine volcanoes: mid-oceanic ridges (longest chain of volcanoes), guyots, and seamounts
    • Earth’s crust is moving away from MORs (mid-oceanic ridges)
    • New material is being formed along MORs
  • Where do old materials go?
    - Gets melted as it goes further down (trenches)
    - It will be reworked in the mantle
  • Additional Evidence for Plate Motion
    • Paleomagnetism and polar wandering 
    • Magnetic Reversals
    • Hot spot volcanism
    • Seismicity and plate boundaries
  • Paleomagnetism
    • Old magnetism of the earth
    • ‘Paleo’ = old
    • The compass will point to the North Pole
  • Polar wandering 
    • Pertains to the North Pole moving
  • Paleomagnetism and polar wandering
    • uses curie point - T at which a minerals magnetic properties change (e.g., magnetite 585C)
    • small magnetite minerals point to the magnetic north during their birth (Paleomagnetism)
  • Magnetic Reversals 
    • Magnetic strips on the ocean floor 
    • Magnetic minerals will point to the north or South Pole 
    • These strips move 
  • Hot spot volcanism 
    • Localized; long-lasting hot regions below the lithosphere
    • Frame of reference for tracking plate motion 
    • Age of volcanism corresponds to the time elapsed since it was on top for the hotspot/mantle plume 
    • The lithosphere moves (bc of volcanos), while the asthenosphere stays in place 
  • Seismicity and plate boundaries
    • Deep earthquakes (>150km): location of subjecting slabs
    • Shallow earthquakes: regions rifting 
  • Plate Tectonics Theory
    • UNifying theory of geology
    • lithosphere composed of segments (tectonic plates)
    • PLates in constant motion relate to one another
    • Major Plates
    • North American
    • South American
    • Pacific
    • Eurasian
    • Australian
    • Indian
    • Antarctic
    • Minor PLates
    • Philippine Sea Plate
  • Plate boundaries - where most movement occurs
  • plate boundaries types
    1. divergent
    2. convergent
    3. transform
  • Divergent boundaries or constructive 
    • Where two plates move apart creating new oceanic crust as seafloor 
    • Spreading centers: oceanic ridges and continental rifts 
    • The rift widens, eventually forming a valley 
    • It will forms a sea, as it widens even more 
    • Valley --> sea —> oceans 
    • Will become a separate island 
  • Convergent boundaries or disruptive boundaries
    • Where two plates move together forming wither arcs or mountain systems 
    • Continental volcanic arc 
    • Continental plate — oceanic plate = subduction 
    • Oceanic will subduct 
    • Forms subduction zones when oceanic lithosphere is involved
    • Orcogenic belts form in continental vs continental plates
    • Orogenic belts — mountain belts 
    • Why is there no subduction
    • Both solid, same density 
    • Oceanic — oceanic 
    • The more dense plate will subduct 
    • Density — depends on the age of the crust 
  • Transform boundaries or conservative boundaries
    • Where two plates grind past each other 
    • Connects oceanic ridge systems into a continuous networks 
  • Philippine Tectonics
    • Volcanism
    • Pacific ring of fire; 25 active volcanoes
    • Earthquakes
    • Everywhere besides Palawan, why?
    • not located in the fault line, it is in another tectonic plate
    • Convergent Plate Boundary
    • Oceanic vs Oceanic (mature island arc): Philippine mobile belt+ Philippine Fault zone
    • Continental vs oceanic: Palawan micro continental block and suture zones
    • Plates
    • eurasian plate, philippine mobile belt, philippine sea plate
    • trenches
    • west - manila trench, negros ternch, cotobato trench, sulut trench
    • east - east luzon trough, philippine trench
  • Philippine tectonic plates moves towards the northwest