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Transcript
Layers of the Earth Earth’s layers Divided 2 different ways: 1. Composition (What it’s made of) 2. Physical Structure (Ex: solid or liquid) Three layers based on composition: 1) Crust 2) Mantle 3) Core Note: Denser material collects in the core because denser objects always sink due to gravity. Continental Crust Oceanic Crust • • Thin & solid, outer most layer (5 – 100 km thick) up to 870oC (increasing with depth) Continental crust Often composed of granite mostly Al, Si, O, Ca, Na, K thick (32 km) Oceanic crust Usually composed of basalt mostly Si, O, Fe, Mg thin (8 km) Why does oceanic crust sit lower than continental crust? - Basalt is more dense (heavier) than rocks in continental crust. A. Between the core and crust B. Most of the Earth’s mass is in the mantle (thickness = 2900 km or 1800 miles) C. Made of Si, O, Fe & Mg Contains more Mg, which is denser than Al in the crust D. Temperature = 870oC – 2200oC (1600oF – 4000oF) The top layers of the mantle are hot enough to be plastic or semi-liquid, which allows it to… FLOW (10,000 times slower than the hour hand on a clock!) There are places in the ocean where the mantle pushes through to form new rock along the ocean floor. As a result, the ocean floor has a similar composition to the mantle. Makes up 1/3 of the Earth’s mass Made mainly of iron and nickel (the denser elements) Almost no silicon, oxygen, and aluminum Why the Earth is so hot Five layers based on physical properties: 1) 2) 3) 4) 5) Lithosphere Asthenosphere Mesosphere Outer core Inner core 1 2 3 5 4 Lithosphere litho = “rock” • 2 parts: rocky crust and rigid, outermost mantle • TECTONIC PLATES!!!! Asthenosphere astheno = “weak” • Plastic (flowing) upper mantle directly beneath the lithosphere – Due to heat and pressure Mesosphere meso = “middle” • Strong, dense lower layer of the mantle Outer Core Surrounds Inner Core • molten Fe & Ni – produces Earth’s magnetic field • Temperature = 2200-5000C • Less pressure than inner core Inner Core • • • Solid Fe & Ni Temperature = 5000oC Extreme pressure Why do you think the outer core is liquid, when the inner core is solid? The intense pressure at the center of the Earth squeezes it into a solid! • • • Pieces of the lithosphere that move around, floating on top of the denser asthenosphere Each plate fits together with the plates around it. There are 10 or so major plates, but around 50 or more total, including all of the smaller ones. The South American plate is a single plate containing both continental and oceanic crust. It is surrounded by several other oceanic plates. 1) Both oceanic and continental plates float on top of the asthenosphere, like ice cubes floating in water, because of their… Lower density 2) Just like ice cubes, the plates can move around and often bump into each other. 3) Some of the plate sits below the level of the asthenosphere, just like The thicker continental crust displaces ice displacing water. more of the asthenosphere than does oceanic crust. When earthquakes occur, seismic waves (vibrations) are sent out in all directions, through the earth. These vibrations reach different places at different times because of the ways the waves… BEND and CHANGE SPEED as they pass through the internal layers.