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Geology Plate Tectonics Mid-Ocean Ridge System

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Geology Plate Tectonics Mid-Ocean Ridge System Discovered from sea floor mapping with SONAR during and after World War II Largest geological feature on Earth Ridges displaced in some areas by transform faults Trenches Conspicuous sea floor features Especially common in the Pacific Ocean.

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Presentation Transcript
slide1
Geology
    • Plate Tectonics
      • Mid-Ocean Ridge System
        • Discovered from sea floor mapping with SONAR during and after World War II
        • Largest geological feature on Earth
        • Ridges displaced in some areas by transform faults
      • Trenches
        • Conspicuous sea floor features
        • Especially common in the Pacific Ocean
slide4
Geology
    • Plate Tectonics - Evidence
      • “Ring of Fire”
        • Geological activity (e.g. earthquakes, volcanoes) associated with mid-ocean ridges and with trenches
slide6
Geology
    • Plate Tectonics - Evidence
      • “Ring of Fire”
        • Geological activity (e.g. earthquakes, volcanoes) associated with mid-ocean ridges and with trenches
      • Closer to ridges
        • Younger rock
        • Thinner covering of sediment
      • Magnetic anomalies
        • Caused by magnetic field reversals
        • Symmetrical on either side of ridge axis
slide8
Geology
    • Plate Tectonics - Mechanism
      • Sea-Floor Spreading
        • Mid-ocean ridges contain rifts where two pieces of crust are moving apart and new oceanic crust is being created (spreading rate ca. 2-18 cm y-1)
        • As rift widens, hot mantle material rises through rift, cools and solidifies to form new oceanic crust
        • Ridges = spreading centers
        • Theory generated by induction explains observations
          • Younger rock closer to ridges
          • Thinner sediment closer to ridges
          • Patterns of magnetic anomalies
slide10
Geology
    • Plate Tectonics - Mechanism
      • Sea-Floor Spreading
        • Lithosphere made up of lithospheric plates
        • Plates may contain continental crust, oceanic crust, or both
        • Plates rest on asthenosphere (plastic upper mantle)
        • Plate boundaries correspond to locations of mid-ocean ridges and to trenches
        • Not all plates completely characterized yet

Fig. 2.9

slide11
Geology
    • Plate Tectonics - Mechanism
      • Subduction
        • Old crust destroyed when one plate dips below another
          • Oldest oceanic crust ~200 million years old
        • Denser plate subducted beneath less dense plate
        • Locations – oceanic trenches = subduction zones
        • Recycles crust and supports volcanic activity
        • May result from collisions between
          • Continental plate and oceanic plate (oceanic plate subducted; usually forms volcanoes)
          • Two oceanic plates (denser plate subducted; usually forms island arc)
slide14
Geology
    • Geological History
      • Continental Drift
        • All continents joined together ~200 mya
          • Pangaea – “supercontinent”
          • Panthalassa – single ocean  Pacific Ocean
          • Tethys Sea – Shallow sea between Eurasia & Africa  Mediterranean Sea
          • Sinus Borealis  Arctic Ocean
        • Laurasia separated from Gondwana ~180 mya
slide20

Global Plate TectonicsJurassic to Present Day

By

L.A. Lawver, M.F. Coffin, I.W.D. Dalziel

L.M. Gahagan, D.A. Campbell, and R.M. Schmitz

2001, University of Texas Institute for Geophysics

February 9, 2001

slide44

We wish to thank the PLATES’ sponsorsfor their support:Conoco, TotalFinaElf, Exxon-Mobil, Norsk Hydro, and Statoil.

slide45

For more information, contact:Lisa M. GahaganInstitute for Geophysics4412 Spicewood Springs Rd., Bldg. 600Austin, TX [email protected]

slide51
Geology
    • Geological Provinces
      • Continental Margins
        • Boundaries between continental and oceanic crust
        • Accumulate sediment deposits from rivers and streams
        • Continental shelf
        • Continental slope
        • Continental rise
      • Deep-Ocean Basins
      • Mid-Ocean Ridges
      • Hot Spots
slide53
Geology
    • Geological Provinces
      • Continental Margins
        • Continental shelf
          • Shallowest part of continental margin
          • Underlie ~8% of ocean surface
          • Richest, most productive parts of ocean
          • Some parts exposed during times of low sea level and eroded by rivers and glaciers now are submarine canyons
slide54

California Coastline

Monterey Canyon

Fig. 2.19

slide55
Geology
    • Geological Provinces
      • Continental Margins
        • Continental shelf
          • Shallowest part of continental margin
          • Underlie ~8% of ocean surface
          • Richest, most productive parts of ocean
          • Some parts exposed during times of low sea level and eroded by rivers and glaciers now are submarine canyons
          • Varies in width from 1 km (Pacific coast of S Am) to 750+ km (Arctic coast of Siberia)
          • Ends at shelf break, usually at 120-200 m but up to 400+ m depth.
slide56
Geology
    • Geological Provinces
      • Continental Margins
        • Continental slope
        • Transition from continent to ocean
        • Furrowed with submarine canyons in many areas
          • Canyons channel sediment and debris to deep sea floor
        • Continental rise
        • Accumulated sediment, including deep-sea fans
          • May be extensive in areas where large rivers discharge into ocean
slide57
Geology
    • Geological Provinces
      • Continental Margins
        • Active margins
        • Geologically active
          • Usually subduction or transform fault
        • Steep, rocky shoreline
        • Narrow continental shelf
        • Steep continental slope
        • Usually lack well-developed continental rise
          • Sediment removed by geological activity

Fig. 2.20

slide58
Geology
    • Geological Provinces
      • Continental Margins
        • Passive margins
        • Not geologically active
        • Flat coastal plain
        • Wide continental shelf
        • Gentle continental slope
        • Usually well-developed continental rise

Fig. 2.20

slide60
Geology
    • Geological Provinces
      • Deep-Ocean Basins
        • Mostly between 3000 and 5000 m
        • Predominantly abyssal plain
slide61
Geology
    • Geological Provinces
      • Deep-Ocean Floor
        • Mostly between 3000 and 5000 m
        • Predominantly abyssal plain
        • Seamounts – Undersea mountains
        • Guyots – Flat-topped seamounts
        • Rises – Large table-like features
          • Common in Pacific
slide62

California Coastline

Monterey Canyon

Fig. 2.19

slide63
Geology
    • Geological Provinces
      • Mid-Ocean Ridges
        • Central region – rift valley
          • Fractures allow sea water to seep into crust
slide65
Geology
    • Geological Provinces
      • Mid-Ocean Ridges
        • Central region – rift valley
          • Fractures allow sea water to seep into crust
        • Water is heated by rock and rises back to surface of sea floor
          • Hot water picks up dissolved minerals (iron, manganese, sulfides)
        • Hot, mineral-rich water contacts cold sea water
          • Precipitate forms
          • Black smokers
          • May be very hot (350 oC or more)
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