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Challenger expedition 1872-1876. Woods Hole, Massachusetts Hopkins Marine Station, Stanford Scripps Institute of OceanographyFriday Harbor Labs, Washington.

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Presentation on theme: "Challenger expedition 1872-1876. Woods Hole, Massachusetts Hopkins Marine Station, Stanford Scripps Institute of OceanographyFriday Harbor Labs, Washington."— Presentation transcript:

1 Challenger expedition 1872-1876

2 Woods Hole, Massachusetts Hopkins Marine Station, Stanford Scripps Institute of OceanographyFriday Harbor Labs, Washington

3 Submersibles

4 R/V FLIP, floating instrument platform

5 Scientific Method What? Why? How?

6 Inductive approach: from specific observations to the general Deductive approach: use general principles in predicting specific outcomes

7 Ocean Basin Geography

8 Interconnected World Ocean system

9 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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12 Mid Ocean Ridge Continuous chain of submarine volcanic mountains encircling the globe –Largest geological feature on earth –Is not static; slips and slides

13 Sea floor spreading As ridges separate, molten mantle rises up through rift

14 Moving plates

15 Collisions Creates trenches or subduction zones –Earthquakes & volcanos –Less dense continental crust floats on top; lasts forever –Form volcanic islands

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17 Kilauea, Hawai’i


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