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Voyage to the Bottom of the Sea
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EQ: Have you ever wondered how the ocean would look without all that water? How it would look if it were just dry land?
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It has mountains and valleys and ridges and volcanoes and just about any other land feature you could name.
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The Ocean Floor Plate Tectonics Map the Ocean Floor - Bathymetry
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PLATE TECTONICS
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Convection Currents - The force responsible for plate movement
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Plate Boundaries Divergent Boundary – moving _____ Convergent Boundary – moving ________ Transform Fault Boundary – moving ________________________ apart together sideways past each other
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Divergent boundary of two continental plates. Creates a __________. Example: _____________ rift valley East African Rift
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Convergent boundary of two oceanic plates. Creates an ________ and a _____. Example: _____ island arctrenchJapan
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Convergent boundary of an oceanic plate and a continental plate. Forms a _______ mountain range and a ______. Examples: _______ or _______ Mts volcanic trench Cascades Andes
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Convergent boundary of two continental plates. Forms a ______ mountain range. Examples: ___________, Alps, ______________ folded Himalayas Appalachians
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Transform-fault boundary where the North American and Pacific plates are moving ____ each other. Example: ________________ in California past San Andreas Fault
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How do we explore the Ocean floor?
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How was the Titanic located? Using sonars and submersibles. 1934 Dr. William Beebe reached a depth of 900 meters in a steel chamber called a Bathysphere ( fits 2 people). In 1960 a Swiss team of Auguste and Jacques Piccard, made the deepest dive in a submersible (bathyscaphe) to the bottom of the Mariana Trench (10,852 meters- 4 hrs.). Alvin is a submersible that has logged in over 1000 dives. It holds a crew of 3. Dr. Sylvia Earle holds the record for the deepest solo dive- 380 meters. (Jim Suit)
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Beebe’s Bathysphere
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The Jim Suit
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How do Modern Submersibles Explore the Ocean Floor? Using unmanned vehicles called Robots. Using personal submersibles. Using high tech submersibles specially outfitted to withstand the cold temperatures and high pressure of the deep ocean. Using Sonar (sound navigation and ranging).
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Alvin
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Sonar Sonar stands for sound navigation and ranging. Sonar uses a beam of sound waves and directs them downward. After the sound wave hits the bottom of the ocean (ocean floor), or an object, it will bounce off and return back causing an echo. This is then recorded on a depth recorder on the ship. Some marine organisms use Echolocation, which is a form of sonar (dolphins, whales, porpoises).
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Sonar http://oceanexplorer.noaa.gov/okeanos/ed u/collection/hdwe.htmlhttp://oceanexplorer.noaa.gov/okeanos/ed u/collection/hdwe.html
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SUBMARINES /SUBMERSIBLES http://oceanexplorer.noaa.gov/te chnology/subs/subs.html
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NOAA RESEARCH VESSELS http://oceanexplorer.noaa.gov/technology/vessels/vessels.html
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Bathymetry – Mapping the Ocean Floor www.topozone.com http://erg.usgs.gov.isb/pubs/booklets/sy mbols
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The term bathymetry is defined as the depth of water relative to sea level. Bathymetric mapping involves the production of ocean and sea maps based upon bathymetric data. Bathymetric maps represent the ocean depth. The most popular type of bathymetric maps are ones on which lines of equal depths (called isobaths) are represented.
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SYMBOLS
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Atlantic Ocean Floor
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Digital Data for Maps of Hawaiian Islands
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Earthquakes and Faults in the San Francisco Bay Area
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http://oceanexplorer.noaa.gov/explorations/0 7fire/welcome.html http://oceanexplorer.noaa.gov/explorations/1 0sanandreas/logs/slideshow/flash_slidesho w.html
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Internet – www.google earth/ocean
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http://oceanexplorer.noaa.gov/explorations/ 02hawaii/welcome.html
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