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Labs Start Next Week Don’t forget your lab book!!!

Labs Start Next Week Don’t forget your lab book!!!. Read through labs ahead of time Exploring the Deep: GEO/OC 103 Lab Manual by Hall-Wallace et al. TA assignments now updated on web dusk.geo.orst.edu/oceans/103labs.html. Shape of the Seafloor Chapter 2. Techniques of Bathymetry - 1.

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Labs Start Next Week Don’t forget your lab book!!!

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  1. Labs Start Next WeekDon’t forget your lab book!!! • Read through labs ahead of time • Exploring the Deep: GEO/OC 103 Lab Manual by Hall-Wallace et al. • TA assignments now updated on web • dusk.geo.orst.edu/oceans/103labs.html

  2. Shape of the SeafloorChapter 2

  3. Techniques of Bathymetry - 1 • Challenger expedition (1872-1876) -1st systematic bathymetric survey • ocean floor not flat - significant topographic relief • German ship Meteor (1920’s) - 1st echosounding survey • sounds travels through water much better • velocity = distance/time • SONAR (Sound Navigation and Ranging)

  4. Bathymetry - 2 • WWII - U.S. Navy further developed SONAR technology • knowledge of the enemy • knowledge of the ocean • 1950’s - 1960’s - single, focused high-frequency, short wavelength sound beam • “wide-beam” bathymetry • sound beam spreads out as it reaches bottom • range of depths - fuzzy estimate

  5. single, focused high-frequency, short wavelength sound beam

  6. Bathymetry - 3 • 1970’s - revolution in bathymetric mapping with multibeam bathymetry • multiple, focused, high-frequency, short wavelength sound beams • “narrow-beam” or “multibeam” bathymetry • sound beam stays narrow and focused all the way to the bottom • depths much more precise • e.g., Sea Beam has 16 beams, Sea Beam 2000 has 121, Simrad EM120 has 191

  7. multiple, focused, high-frequency, short wavelength sound beams A Gigabyte of data an hour A Gigabyte of data a day

  8. Bottom Coverage & Data Density by Survey Method Leadline Single Beam Multibeam 1-2 K soundings per survey 500 - 750 K soundings per survey 400,000 – 1,000,000 K soundings per survey Image courtesy of NOAA & UNH

  9. N

  10. N

  11. Shallow Water Multibeam

  12. Shallow Water Multibeam (cont.)

  13. Tutuila Surveys

  14. Tutuila Surveys

  15. Fagatele Bay National Marine Sanctuary

  16. FBNMS Benthic Habitat

  17. Need for Mapping Oregon Territorial Seafloor Siletz Bay Goldfinger et al., OSU Active Tectonics & Seafloor Mapping Lab Oregon Department of Fish & Wildlife

  18. Applications for Mapping

  19. dusk.geo.orst.edu/3mile/consensus_statement.pdf

  20. “Fine Scale” Mapping • on the order of tens of meters to meters • features the size of a can of beer!

  21. Study Area Image courtesy of Dan Fornari, Woods Hole Oceanographic Institution

  22. 2005 HURL Sub & ROV surveys Ka‘imikai-o-Kanaloa Pisces IV or V HURL = Hawaii Undersea Research Lab ROV= remotely-operated vehicle RCV-150

  23. Sonar Also Used as... • a “catscan” of oceans to see water structure ABOVE seafloor • an “x-ray” of seafloor to see structure BENEATH seafloor • seismic reflection & seismic refraction • low frequency, long-wavelength sound • sidescan sonar to get pictures of seafloor in addition to depth • backscatter strength as opposed to traveltime

  24. Sidescan Sonar Image courtesy of USGS Woods Hole

  25. DSL-120 Vehicle Image courtesy of WHOI Deep Submergence Lab and Dr.Dan Fornari Image courtesy of USGS Woods Hole

  26. Resolution • with multibeam bathymetry can see things on seafloor the size of this room • swath width of 6 km or 3.7 miles • good, high-resolution maps possible only since 1980’s • other instruments needed to see things smaller than size of room • remotely-operated vehicles (ROVs) • submersibles

  27. Seafloor Features: Continental Margins • continental shelf - extends from shore to a point marked by great increase in slope • continental slope - steep slope beyond the continental shelf break • slopes often cut by submarine canyons • turbidity currents - dense flows of sediment-laden water • deepsea fans • continental rise • abyssal plain - extensive, flat

  28. Seafloor Features: Deep Ocean • seamounts - underwater volcanoes 500 m to 1000 m high • flat-topped ones are called guyots • volcanic features (buoyed up by hot rock, lava) • abyssal hills - features around 200 m high • pervasive on seafloor • volcanic AND tectonic in origin - still debated

  29. Seafloor Features: Deep Ocean • Plate Boundaries • Ridges (Rises), Trenches, Transform Faults, Fracture Zones

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