Plate Tectonics Living with a Dynamic Planet. Alfred Wegener: a man before his time Meteorologist...
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![Page 1: Plate Tectonics Living with a Dynamic Planet. Alfred Wegener: a man before his time Meteorologist Research on arctic climates – Greenland Evidence for.](https://reader036.fdocuments.net/reader036/viewer/2022062322/56649d555503460f94a32c6c/html5/thumbnails/1.jpg)
Plate Tectonics
Living with a Dynamic Planet
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Alfred Wegener:a man before his time
• Meteorologist
• Research on arctic climates – Greenland
• Evidence for past climates preserved in rocks
• A super-continent: Pangea
• Pangea broke apart 200 million years ago
• Continents drifted to their present locations
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Wegener’s Continental Drift
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Evidence for Pangea: glaciation
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Evidence for Pangea: paleontology (fossils)
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How Science Works:Continental Drift Disputed
• Lack of Mechanism – what makes continents move?
• Alternate explanations possible
• Anti-German sentiments in the U.S.
• What are the credentials of Wegener?
• Continental Drift largely dismissed until 1960’s
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Oceanography: a new scienceand new evidence
• Following WW II – a convergence of questions, technology, manpower and money
• Defense needs – mapping the seafloor• Anti-submarine technology• GI Bill – a wave of scientists and engineers• Booming postwar economy and support for
science
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A new view of the Seafloor
• Completely surprising!
• Mountains on the sea floor
• Trenches – near some continental edges, near islands
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More puzzles: Magnetic stripes near the Mid-Ocean Ridges
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A new hypothesis: Sea-Floor Spreading – Making New Oceanic Lithosphere
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Continental Drift Revised:the New Global Tectonics
• Earth’s lithosphere is made of crust and uppermost mantle
• Lithosphere is broken into plates
• Plates float on moving asthenosphere (upper mantle)
• Plate motion driven by heat in mantle
• Plates interact – especially at edges
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Lithosphere and Asthenosphere
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Plates
• Made of Continental and Oceanic Crust – attached to uppermost part of mantle
• Plates move
• Plate interactions produce specific features (e.g., mountains, etc.) and processes (e.g., earthquakes)
• Motion is also related to heat dissipation and density differentiation
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Balancing the System
• Sea Floor (oceanic lithosphere) is created at MOR (divergence)
• Either Earth is expanding (no evidence!) or
• Sea Floor must be destroyed somewhere – where plates converge
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Subduction – destroying sea floor
The sinking of cold, dense, oceanic lithosphere into the asthenoshere, beneath an over-riding plate.
• Associated: Trenches, Volcanoes, Mountains, Earthquakes
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Convergence Brings Continents into Collision – Forming Mountains
• Subduction of oceanic lithosphere brings landmasses together
• Collision of continents (or continent/island arc)
• Due to low densities, neither can subduct
• Crash!!
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TRANSFORM BOUNDARIES – Two Plates Passing
• Transform boundaries link other types of plate boundaries:
• Transform boundaries allow a single plate edge to have multiple types of interactions w/other plates
• Transforms are major Faults – Earthquakes!
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The Big Picture of Plate Interactions
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Plate Tectonics Explains:• Formation of Oceans• Formation of Mid-ocean Ridges• Formation of Trenches• Formation of Mountains
• Formation of Metamorphic Rocks• Formation of Sedimentary Rocks as mountains
erode
• Earthquakes: cause and distribution• Volcanos: cause, types and distribution
• Formation of Igneous Rocks