Title: GEO/OC 103 Exploring the Deep
1GEO/OC 103Exploring the Deep .Todays
TuneSink to the BottomFountains of Wayne
2Labs Start Next Week
- Read through labs ahead of time
- See your sections and TAs on the web
- dusk.geo.orst.edu/oceans/103labs.html
3Shape of the Seafloor
4Techniques of Bathymetry - 1
- Challenger expedition (1872-1876) -1st systematic
bathymetric survey - ocean floor NOT flat - significant topographic
relief - German ship Meteor (1920s) - 1st echosounding
survey - sounds travels through water much better
- velocity distance/time
- SONAR (Sound Navigation and Ranging)
5Bathymetry - 2
- WWII - U.S. Navy further developed SONAR
technology - knowledge of the enemy
- knowledge of the ocean
- 1950s - 1960s - single, focused high-frequency,
short wavelength sound beam - wide-beam bathymetry
- sound beam spreads out as it reaches bottom
- range of depths - fuzzy estimate
6single, focused high-frequency, short wavelength
sound beam
7Bathymetry - 3
- 1970s - 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
8multiple, focused, high-frequency, short
wavelength sound beams
A Gigabyte of data an hour
A Gigabyte of data a day
9multiple, focused, high-frequency, short
wavelength sound beams
Multibeam
Movies courtesy of NOAA
10Bottom 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
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14N
15N
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19Shallow Water Multibeam
20Shallow Water Multibeam (cont.)
21Initial Tutuila Surveys
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24Tutuila Surveys
25Fagatele Bay National Marine Sanctuary
26FBNMS Benthic Terrain
27Entire Eastern Samoa
28Need for Mapping Oregon Territorial
Seafloor Siletz Bay
Goldfinger et al., OSU Active Tectonics
Seafloor Mapping Lab Oregon Department of Fish
Wildlife
29Applications for Mapping
Tsunami Runup Models -Evacuation Planning Habitat Restoration
Shoreline Change Analysis Analyzing Storm Impacts -Coastal Erosion
Fisheries Management Commercial Fishing Marine Reserve Design
Emergency Response, Impact Assessment Port Security
Maps and Visualizations Navigation Products, Services
Wave Energy Oil Spill Response, Tracking
Coastal tourism, recreation MANY others
30Fine Scale Mapping
- on the order of tens of meters to meters
- features the size of a can of beer!
31Study Area
Image courtesy of Dan Fornari, Woods Hole
Oceanographic Institution
32HURL Sub ROV surveys
Launch iTunesU
Kaimikai-o-Kanaloa
Pisces IV or V
HURL Hawaii Undersea Research Lab ROV
remotely-operated vehicle
RCV-150
33Sonar 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
34Sidescan Sonar
Image courtesy of USGS Woods Hole
35DSL-120 Vehicle
Image courtesy of WHOI Deep Submergence Lab and
Dr.Dan Fornari
Image courtesy of USGS Woods Hole
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37Sidescan Sonar
Sidescan
Movies courtesy of NOAA
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41Resolution
- 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
1980s - other instruments needed to see things smaller
than size of room - remotely-operated vehicles (ROVs)
- submersibles
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43Seafloor 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
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45Seafloor 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
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47USS San Francisco crashed into2-km tall
uncharted seamount
- Los Angeles class nuclear submarine ran aground
enroute from Guam to Brisbane, Australia - 8
January, 2005 - One sailor killed, 115 injured
- 30-hour trip back to Guam, crew managed to keep
the sub from sinking
Courtesy of Dave Sandwell, Scripps Institution of
Oceanography
48Seafloor Features Deep Ocean
- Plate Boundaries
- Ridges (Rises), Trenches, Transform Faults,
Fracture Zones