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Published byAlexia Hudson Modified over 9 years ago
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The Geosphere
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What is the GEOSPHERE? All solid parts of Earth – Rocks, soils, minerals, sediments, magma The Grand Canyon, AZ
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Remember… CruManCo Chemical Company
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Layers of the Earth 1.Crust- O, Si, Al 2.Mantle- O, Si, Mg, Fe 3.Core- Fe, Ni Geologists classify Earth’s layers two ways: chemically and physically Chemical – by composition Physical- by structure Chemical Layers of the Earth
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Physical Layers of the Earth Lithosphere – Crust and upper mantle combined – Broken in chunks called tectonic plates – Oceanic plates are thinner and denser than continental plates Asthenosphere -Layer of Jello-like magma in the mantle -Tectonic plates move due to convection currents in the asthenosphere
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Physical Layers, cont. Mesosphere – The rest of the mantle; molten rock Outer Core – Liquid metal – Surrounds inner core Inner Core – Densest layer – Solid metal
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Remember… LAMOI, The physical trainer
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http://www.youtube.com/watch?v=Q9j1xGax YzY http://www.youtube.com/watch?v=Q9j1xGax YzY earth layer song
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Theory of Plate Tectonics Lithosphere (upper mantle and crust) is divided into pieces called tectonic plates. These plates glide across the underlying asthenosphere like ice drifts across a pond. Continents are located on tectonic plates and move around with them
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Plate Boundaries The area where two plates meet is called a plate boundary. Most earthquakes and volcanoes occur at or near plate boundaries Three main types of plate boundaries: 1.Divergent- separating 2.Convergent- colliding 3.Transform- scraping past
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Earthquakes Worldwide Tectonic Plates Active Volcanoes
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Transform Boundaries 2 plates slide past each other This sliding is not smooth. Plates lock and build up tension. After too much tension builds, the plates “snap” and move against each. Causes earthquakes
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Divergent Boundaries When two plates separate Most common on ocean floor Creates Mid-Atlantic Ridge which is visible on land in Iceland
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Divergence Forms New Ocean Floor
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Convergent Boundaries Three Main Types: 1.Continental & Oceanic- causes deep ocean trench and land volcanoes Ex: Andes Mountains 2. Oceanic & Oceanic- causes deep ocean trench and island arc (chain of volcanic mountains) Ex: Mariana islands and Mariana trench 3. Continental & Continental- causes large land mountain ranges Ex: Himalayan Mountains
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Subduction Zone Continental + Oceanic Crust
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Subduction Zone Oceanic + Oceanic Crust
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Subduction Zone Oceanic + Oceanic Crust (another view)
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Continental + Continental Crust
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Some videos for your viewing pleasure… Plate Movement: http://www.youtube.com/watch?v=ryrXAGY1 dmE&feature=endscreen&NR=1 http://www.youtube.com/watch?v=ryrXAGY1 dmE&feature=endscreen&NR=1 San Andreas Fault: http://www.youtube.com/watch?NR=1&v=Zx PTLmg0ZCw&feature=endscreen http://www.youtube.com/watch?NR=1&v=Zx PTLmg0ZCw&feature=endscreen
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