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Aim: How is Earth’s interior Structured? Do Now: Why do you think Earth has layers? What material do you think make up those layers? I. Layers of the Earth • layers are defined by their specific composition, temperature and density. Where would the highest temperatures be located? A) Crust - thin outer rocky layer - least dense of all the layers - Oceanic Crust – mostly Basalt bedrock (more dense) - Continental Crust – mostly Granite Bedrock (less dense) The deepest hole drilled by man is 7.6 mi deep (Kola Peninsula, Russia). That is only 1% of the Earth’s entire thickness. B) Mantle - thickest layer consisting plastic fluid-like material. - Meteorites provide clues as to what the interior of earth is made of. (they were made from the same material at the same time) Chondrites: stony (nonmetallic) meteorites that were formed from dust and rocks that were present in the early solar system. C) Core How many cores does - deepest layers of the Earth. Earth have? - composed of iron and nickel. - Inner Core solid iron and nickel - Outer Core liquid iron and nickel II. Physical Properties A) Lithosphere – consists of the crust and uppermost mantle. - Forms a cool, rigid shell made of rock. B) Asthenosphere – - a soft, weak layer beneath the lithosphere. - rocks are close to their melting points in this layer. (plastic-fluid like material) - the lithosphere floats on the asthenosphere. Why does it float? III. Discovering New Layers Moho - (Mohorovicic Discontinuity) - separates the crust from the underlying mantle within the lithosphere. Page 10 - ESRT Closure: • Please complete the worksheet on Layers of the Earth.