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All solid parts of Earth
What is the GEOSPHERE? All solid parts of Earth Rocks, soils, minerals, sediments, magma The Grand Canyon, AZ
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What are the layers of the Earth?
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Chemical Layers of the Earth
Geologists classify Earth’s layers two ways: chemically and physically Chemical – by composition Physical- by structure Chemical Layers of the Earth Crust- O, Si, Al Mantle- O, Si, Mg, Fe Core- Fe, Ni
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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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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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Seafloor Spreading Magma rises from asthenosphere
Creates new oceanic lithosphere Pushes tectonic plates apart
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Seafloor-Spreading
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If new crust is being created by the process of seafloor spreading, is the Earth growing!?
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Subduction Subduction zones: A region where old crust is destroyed as it is pulled back down into the mantle
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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: Divergent- separating Convergent- colliding Transform- scraping past
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Transform Boundaries 2 plates slide past each other
Not smooth. Plates lock, and build up tension. After too much tension builds, the plates “snap” causing earthquakes
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Divergent Boundaries When two plates separate
Most common on ocean floor Creates Mid-Ocean Ridge
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Divergence Forms New Ocean Floor
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Convergent Boundaries
Three Main Types: Continental & Oceanic- causes deep ocean trench and land volcanoes Ex: Andes Mountains 2. Continental & Continental- causes large land mountain ranges Ex: Himalayan Mountains 3. Oceanic & Oceanic- causes deep ocean trench and island arc (chain of volcanic mountains) Ex: Mariana trench and islands
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Subduction Zone Continental + Oceanic Crust
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Continental + Continental Crust
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Subduction Zone Oceanic + Oceanic Crust (another view)
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Subduction Zone Oceanic + Oceanic Crust
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Some videos for your viewing pleasure…
Plate Movement: ndscreen&NR=1 San Andreas Fault: een
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Exit Ticket 1. Arrows in the block diagram below show the relative movement along a tectonic plate boundary. What is this type of plate boundary called? transform plate boundary convergent plate boundary divergent plate boundary subduction plate boundary
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Exit Ticket 2. When two tectonic plates collide, oceanic crust usually subducts beneath continental crust because oceanic crust is primarily composed of igneous rock that is: thin and less dense thick and less dense thin and more dense thick and more dense
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Exit Ticket 3. The block diagram below shows the boundary between two tectonic plates. Which type of plate boundary is shown? divergent transform convergent complex
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Exit Ticket 4. The Himalaya Mountains were formed in a collision at a:
divergent boundary convergent boundary transform boundary fracture zone
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Exit Ticket 5. In which Earth layer are most convection currents that cause seafloor spreading thought to be located? crust outer core asthenosphere inner core
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Earthquakes Worldwide
Tectonic Plates Active Volcanoes Earthquakes Worldwide
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