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GEOL 4110 Advanced Earth Science For Teachers Jim Miller
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Plate Tectonic Theory The Earth’s outer shell (lithosphere) is composed of rigid plates that are moving relative to one another.
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Physical and Chemical Structure of the Earth Chemical Layers Physical Layers Lithosphere Compositional Components of the Lithosphere Continental Crust – ~62% SiO 2, low density rocks, “felsic” Oceanic Crust - ~ 48% SiO 2, high density rocks, “mafic” Lithospheric Mantle - ~ 40% SiO 2, very high density rocks, “ultramafic” Lithospheric Mantle
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Plate Tectonics drives 2 Stages of Crust-making 1. Mantle partially melts to make ocean crust 2. Ocean crust melts to make continental crust
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What moves the Plates? Slab Pull - densification of subducted plate pulls the plate into the mantle Mantle Push - Upwelling of the asthenospheric mantle pushes the plates apart Ridge Slide – Thermal upwelling at ridges causes plates to separate by sliding downhill (by gravity) Problem - we are not sure how the mantle is structured.
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Types of Plate Boundaries
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Divergent Plate Boundaries Mid-ocean Ridges Where Stage 1 Crust is Made
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Youthful Oceanic Crust
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Basalt – Rock Type of the Oceanic Crust Remember: Melting the mantle makes mafic magma!! Always
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Continental Rifting The creation of new ocean basins
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Continental Rifting and The Break-up of Pangea
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Convergent Boundaries Making 2 nd Stage Crust Ancient Continental Crust
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Convergent Boundaries- Where the Action Is!! Ocean- Continent Continent - Continent Ocean - Ocean Earthquakes Volcanoes
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Mt. St. Helens May 18, 1980 Consequences of Convergence Explosive Volcanism
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Consequences of Convergence Mountain Building and Rock Deformation
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Consequences of Convergence - Earthquakes 1326 Aftershocks
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OROGENESIS The Culmination of Convergence
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San Francisco Earthquake April 18, 1906 Mag 7.8 Transform Boundaries
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Mantle Hotspots Creation of overthickened oceanic crust
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Famous Hotspots Hawaii Yellowstone? Iceland
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The Grand Unifying Theory of the Earth
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