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Published byGeoffrey Cross Modified over 9 years ago
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Challenger expedition 1872-1876
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Woods Hole, Massachusetts Hopkins Marine Station, Stanford Scripps Institute of OceanographyFriday Harbor Labs, Washington
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Submersibles
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R/V FLIP, floating instrument platform
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Scientific Method What? Why? How?
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Inductive approach: from specific observations to the general Deductive approach: use general principles in predicting specific outcomes
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Ocean Basin Geography
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Interconnected World Ocean system
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How did we get these ocean basins? Continental drift –all the continents had once been joined in a single ‘supercontinent’ called Pangaea Plate tectonics Sea floor spreading
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Mid Ocean Ridge Continuous chain of submarine volcanic mountains encircling the globe –Largest geological feature on earth –Is not static; slips and slides
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Sea floor spreading As ridges separate, molten mantle rises up through rift
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Moving plates
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Collisions Creates trenches or subduction zones –Earthquakes & volcanos –Less dense continental crust floats on top; lasts forever –Form volcanic islands
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Kilauea, Hawai’i
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