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Ocean Formation 16 September 2014
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Theory of continental drift: all continents were unified and drifted apart over time to current positions. First proposed by Alfred Wegener in 1912.
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Why do the continents drift in the first place?
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Earth Layers Crust(solid) Mantle (molten) Outer Core (liquid) Inner Core (solid) Lithosphere: the outer shell of the Earth consisting of the crust and upper mantle.
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Tectonic Plates: Large pieces of the Earth’s crust Involved the movement of plates.
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Mid-Ocean Ridge: An underwater mountain range
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The Great Global Rift: A break in the Earth’s crust through which magma emerges. The magma pushes through because of convection. This leads to Sea Floor Spreading.
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Sea-Floor Spreading Sea floor spreading is the outward spreading of the lithosphere from ocean ridges.
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Trenches encircle most of the pacific rim
Trenches encircle most of the pacific rim. They form when 2 plates collide and one plate plunges under the other. This region is also known as a convergent plate boundary
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Earthquakes, tsunamis, volcanic eruptions can result from the friction and stress near trenches.
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Interaction between seawater and magma Seawater soaks through pores and is heated by magma.
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The rising water dissolves minerals and is released through vents near ocean ridges. These minerals include Fe, H2S, Mg, and methane.
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These minerals are necessary for hemoglobin, chlorophyll, and sulfur-fixing bacteria. phytoplankton take in these minerals which makes it available for other organism
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