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Published byRhoda Davidson Modified over 9 years ago
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Earth’s Interior
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Crust OOOOutermost layer of solid rock that includes both dry land and ocean floor 5555-70 kilometers thick TTTTwo Types Oceanic Crust - made of mostly basalt- Thinnest Crust - 7 km avg Continental Crust - made of mostly granite- Thickets crust - 35 km avg
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Mantle MMMMade of very hot, but solid rock AAAAbout 3000 kilometers thick MMMMoho - the boundary between the mantle and the crust LLLLithosphere - crust & upper mantle AAAAsthenosphere - soft layer of mantle, like road tar LLLLower mantle - solid, hot rock
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The mantle exhibits plasticity, where molten rock bends and flows
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Convections currents exist in the mantle.
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Cooler, denser mantle material sinks toward the core and warmer, less dense mantle material rises toward the crust.
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Outer Core Molten, liquid metal
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Inner Core Dense ball of solid metal
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STRESS
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As rocks undergo STRESS, the DEFORM SSSStress - the forces that push and pull on the Earth’s crust DDDDeformation - an change in the original shape or volume of rocks
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Types of Stresses CCCCompression - type of stress that squeezes rocks together TTTTension - type of stress that pulls rocks apart SSSShearing - type of stress that pushes rocks in two opposite horizontal directions
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STRESS can cause rocks to FRACTURE Fracture - break or crack in rocks
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STRESS can also cause FAULTS FAULT - a break or crack along which rocks move
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Faults HHHHanging Wall - the block of rock above a fault. Longer at the top FFFFoot Wall - the block of rock below a fault. Longer at the bottom
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Types of Faults NNNNormal Fault - a fault in which the hanging wall moves down relative to the foot wall
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Reverse Fault - a fault in which the foot wall moves down relative to the hanging wall
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Example - Thrust Fault - a reverse fault in which the hanging wall slides over the foot wall Example - Thrust Fault - a reverse fault in which the hanging wall slides over the foot wall
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Lateral (Strike slip) fault - a fault along which the rocks move horizontally past each other
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Fault block mountain A mountain formed by blocks of rocks uplifted from normal faults
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Rift Valley A valley formed when the block of land between two normal faults slides downward.
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STRESS can also cause FOLDING FOLD - a bend in rock
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Types of Folds Anticline - an upward fold in rocks Syncline - an downward fold in rocks
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The 4 factors that determine whether a rock will fault or fold: TTTTemperature PPPPressure RRRRock type HHHHow the stress is applied
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Geographic Features PPPPlateau - a large area of flat land that is raised high above sea level and consists of horizontal rock layers
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Domes - a raised area shaped like the top of a sphere often formed by magma pushing rock layers upward.
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