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Earth’s Interior. Crust OOOOutermost layer of solid rock that includes both dry land and ocean floor 5555-70 kilometers thick TTTTwo Types.

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Presentation on theme: "Earth’s Interior. Crust OOOOutermost layer of solid rock that includes both dry land and ocean floor 5555-70 kilometers thick TTTTwo Types."— Presentation transcript:

1 Earth’s Interior

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3 Crust OOOOutermost layer of solid rock that includes both dry land and ocean floor 5555-70 kilometers thick TTTTwo Types Oceanic Crust - made of mostly basalt- Thinnest Crust - 7 km avg Continental Crust - made of mostly granite- Thickets crust - 35 km avg

4 Mantle MMMMade of very hot, but solid rock AAAAbout 3000 kilometers thick MMMMoho - the boundary between the mantle and the crust LLLLithosphere - crust & upper mantle AAAAsthenosphere - soft layer of mantle, like road tar LLLLower mantle - solid, hot rock

5 The mantle exhibits plasticity, where molten rock bends and flows

6 Convections currents exist in the mantle.

7 Cooler, denser mantle material sinks toward the core and warmer, less dense mantle material rises toward the crust.

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9 Outer Core  Molten, liquid metal

10 Inner Core  Dense ball of solid metal

11  STRESS

12 As rocks undergo STRESS, the DEFORM SSSStress - the forces that push and pull on the Earth’s crust DDDDeformation - an change in the original shape or volume of rocks

13 Types of Stresses CCCCompression - type of stress that squeezes rocks together TTTTension - type of stress that pulls rocks apart SSSShearing - type of stress that pushes rocks in two opposite horizontal directions

14 STRESS can cause rocks to FRACTURE  Fracture - break or crack in rocks

15 STRESS can also cause FAULTS  FAULT - a break or crack along which rocks move

16 Faults HHHHanging Wall - the block of rock above a fault. Longer at the top FFFFoot Wall - the block of rock below a fault. Longer at the bottom

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18 Types of Faults NNNNormal Fault - a fault in which the hanging wall moves down relative to the foot wall

19  Reverse Fault - a fault in which the foot wall moves down relative to the hanging wall

20 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

21  Lateral (Strike slip) fault - a fault along which the rocks move horizontally past each other

22 Fault block mountain  A mountain formed by blocks of rocks uplifted from normal faults

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24 Rift Valley  A valley formed when the block of land between two normal faults slides downward.

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26 STRESS can also cause FOLDING  FOLD - a bend in rock

27 Types of Folds  Anticline - an upward fold in rocks  Syncline - an downward fold in rocks

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29 The 4 factors that determine whether a rock will fault or fold: TTTTemperature PPPPressure RRRRock type HHHHow the stress is applied

30 Geographic Features PPPPlateau - a large area of flat land that is raised high above sea level and consists of horizontal rock layers

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32  Domes - a raised area shaped like the top of a sphere often formed by magma pushing rock layers upward.

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