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Published byAugustus Lambert Modified over 9 years ago
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Chapter 4 Lesson 1 Plate Tectonics
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What Are Earth’s Layers
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Earth’s Layers Core- central part –Inner Core – solid metals –Outer Core – liquid metals Mantle – thick layer of solid and molten rock that surrounds the core Lower – solid rock Upper – 2 parts Lithosphere – solid- upper mantle & crust Asthenosphere – upper mantle – melted rock
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Crust –Thin layer of solid rock that makes up the outermost layer. –Where we live Atmosphere – –All gases that surround the Earth Hydrosphere –All of Earth’s liquid and solid water (lakes, oceans, rivers, glaciers) –Covers 70% of the Earth
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Landforms – a physical feature of the Earth’s surface
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Earth ~200 million years ago
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The Continental Drift Hypothesis Geologist – person that studies rocks Thought of by Alfred Wegener in 1915. Continents "drifted" to their present positions. Supercontinent Pangaea started to break up about 200 million years ago.
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Continental Drift: Evidence Geographic fit of South America and Africa Fossils match across oceans Rock types and structures match across oceans Ancient glacial features
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Tight fit of the continents, especially using continental shelves. Continental Drift: Evidence
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Continental Drift: Evidence Fossil critters and plants
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Continental Drift: Evidence Correlation of mountains with nearly identical rocks and structures
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Continental Drift: Evidence Glacial features of the same age restore to a tight polar distribution.
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Presumably, Pangaea was ripped apart by such continental rifting & drifting.
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What causes the continents to move? Plate Tectonics Theory to explain how forces deep within Earth can cause seafloors to spread and continents to move.
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Tectonic Plates
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Continental Divergent Boundary Example: Red Sea / E. African Rift
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Magma – hot melted rock Tension – push or a stretch on the plates Seafloor Spreading – caused by magma pushing on the plates
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Mid Ocean Ridges - underwater mountain ranges
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Subduction – when one tectonic plate can sink under another plate- crust gets recycled back into the mantle
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Mountain Formation Compression – a squeezing or pushing together of the crust This creates folded mountains.
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Fault – deep cracks in the Earth’s crust where rocks move in the opposite direction Fault Block Mountain –Caused by tension when one block of rock moves down –Sierra Nevada Mountains
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