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CONVECTION CURRENTS and the Movement of the Earth’s Crust HEAT TRANSFER – Heat is passed from HOT/Warmer regions, to COLD/Cooler regions. This happens in 3 ways… 1. CONDUCTION – when heat is transferred by DIRECT CONTACT of matter particles (touching) 2. CONVECTION – when heat is transferred by the MOVEMENT of a fluid (liquid or gas). 3. RADIATION – when heat is transferred through EMPTY SPACE (in the form of electromagnetic waves) RECALL…… LITHOSPHERE = The SOLID, RIGID outer portion of the Earth that is composed of the CRUST and UPPERMOST MANTLE. ASTHENOSPHERE = The HOT, SOFT, WEAK, SLOW MOVING portion of the UPPER MANTLE. Lithosphere FLOATS on top of the Asthenosphere **CONVECTION CURRENTS** take place in the slow moving ASTHENOSPHERE So, the Lithosphere CONVECTION CURRENTS are the circular flow or movement within a liquid or gas, due to a variation in DENSITY caused by TEMPERATURE differences. o DENSITY FLOATS on these CURRENTS . is the ‘amount of matter’ (mass) in a given ‘space’ (volume). How do density and floating relate? Relative to Surroundings: More dense things SINK and Less dense things FLOAT When a liquid or gas is HEATED , it becomes LESS dense. - It becomes LESS dense because when it is heated, the substance EXPANDS (spreads out) When a liquid or gas is COOLED , it becomes MORE - This is because when an liquid or gas is cooled, the substance dense. CONTRACTS (squeezes down) . CONVECTION CURRENTS and the Movement of the Earth’s Crust LITHOSPHERE 4. Soft Rock COOLS because it is FAR from the CORE. 5. COOL Rock SINKS in the Asthenosphere, because it is MORE DENSE. 3. Soft Rock reaches Lithosphere and SPREADS OUT. 2. HOT, Soft Rock in the Asthenosphere RISES because it is LESS DENSE. 4. Soft Rock COOLS because it is FAR from the CORE. 5. COOL Rock SINKS in the Asthenosphere, because it is MORE DENSE. 1. SOFT ROCK deep in the Asthenosphere is HEATED by the EARTH’s INTERIOR. 6. Cool Rock sinks down in the Asthenosphere and REPEATS 6. Cool Rock sinks down in the Asthenosphere and REPEATS