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Geology of the Ocean

Geology of the Ocean. Origin of Earth. 4.6 billion years ago began as giant disk of dust and gases orbiting the sun grains came together forming comets, asteroids, planets (The Nebular Theory). Earth Structure Density Stratification. core – very dense (iron & nickel) inner core is solid

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Geology of the Ocean

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  1. Geology of the Ocean

  2. Origin of Earth • 4.6 billion years ago • began as giant disk of dust and gases orbiting the sun • grains came together forming comets, asteroids, planets (The Nebular Theory)

  3. Earth StructureDensity Stratification • core– very dense (iron & nickel) • inner core is solid • outer core is liquid (viscous); creates magnetic field • mantle – dense rock, mostly solid does NOT melt because of rapidly increasing pressure

  4. Earth Structure (cont.) • asthenosphere – upper part of mantle, nearly molten, flows very slowly • Hot, partially melted • lithosphere– rigid outer layer (60-125 mi. thick) – floats in the asthenosphere • Comprised of crust and uppermost portion of the mantle

  5. Earth Structure (cont.) • crust– upper part of lithosphere – rigid because of low temperature two types: • continental crust –thicker than oceanic crust, lighter in color, less dense • oceanic crust – thinner, darker, more dense

  6. Kontinentalverschiebung • Theory of Continental Drift Proposed in 1912 byAlfred Wegener • continents fit together like pieces of a jigsaw puzzle. • Suggested that 200 million years ago, continents formed one big land mass Pangaea similarities in fossils and rock formations on different continents bordered by the Atlantic Ocean

  7. Continental Drift • Geologists ignored his theory initially…continents did not fit together exactly like “puzzle pieces”. • Harry Hess – Continents floated on asthenosphere (semi-fluid) Usedthe end of the continental shelf to put continent pieces together—fit exactly

  8. Isostasy • Lithospheric plates float in the asthenosphere in a balance called • Thicker (less dense rocks) continental crust floats higher than thin oceanic crust • Large glaciers weigh down crust, when glaciers melt, plates rise (can be measured).

  9. Plate Tectonics • Lithosphere (crust) is made of several very large plates which move. Theory explains geological changes and features and events such as earth quakes, continental drift and volcanoes.

  10. Plate Boundaries (3 types) • Divergent boundaries – Found at Mid-ocean ridges – • plates move awayfrom each other • new crust formed • seafloor spreading • crust forms from magma at a rift valley

  11. Divergent Boundaries

  12. Divergent boundaries • Midocean Ridges • Mid-Atlantic Ridge • most prominent feature steep-sided, very tall mountains • rift valley 25-50 km wide • small e-quakes occur frequently on crests

  13. Divergent boundaries • Rises • Shorter than ridges because plates spread apart faster than @ridges • Have less time to accumulate • Frequently found in Pacific Ocean

  14. Convection Currents • Causes molten magma to rise through mantle and into crust creating oceanic ridges

  15. Magnetic Reversals • Magnetic bands show that new crust is formed and moves away from the ridge over time, has allowed us to date oceanic crust

  16. Convergent Boundaries • Plates converge (come together) • Crust is destroyed-(recycled into mantle) or pushed up to form mountains.

  17. Convergent Boundaries

  18. Convergent boundaries • Subduction –zone where dense lithosphere (crust) sinks into mantle and is reabsorbed • Occurs widely in western Pacific basin

  19. Convergent boundaries • Trenches • Deepest part of the ocean floor • Most occur in Pacific (esp. western Pacific) • Most of Pacific Ocean bordered by trenches

  20. Transform Boundaries • Transform faults – plates slide past each other. • Result in earthquakes • Ex. San Andreas fault in California

  21. Seafloor Features • Principal boundary between continents and ocean basins is called the continental margin … • Continental shelf • Continental slope • Continental rise

  22. Continental shelves • The relatively flat, submerged margin of a continent between the shoreline and depth of 200 meters.

  23. Continental slope • steep portion at the end of the continental shelf that ends at the beginning of the ocean basin

  24. Continental rises • Occur at the base of the continental slope… slopes gently…connects with the deep-sea floor

  25. Seafloor Features • Submarine canyons • Are formed by turbidity currents • Began with a large earthquake off of the Grand Banks in the late 1920’s

  26. Deep-Ocean Floor(30% or Earth’s surface) • abyssal hills – cover about 80% of Pacific floor and half of the Atlantic • typically 200m high (many extinct volcanoes) • Are very short compared to midocean ridge mountains • abyssal plains– flat deep ocean floor

  27. Hot spots • midoceanridges (Iceland) • in middle of lithospheric plates (Hawaii) • remain fixed for a very long time

  28. Hot Spots Example: Hawaii • plates move over hot spots and form chains of volcanoes • youngest islands remain active while near hot spot • after crust moves away, volcano becomes extinct

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