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ch 14 voacb

February 10th, 2006 · No Comments
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1. core-interior of the earth.

2. mantle- surrounding the molten outer core is a hot pliable layer of rock.

3. cruts- outter layer of the earth is a cool, light weight, brittle rock that floats on the mantle.

4. tectonic plates- upper layer mantle as a huge convection currents that break the over laying cruts into mosaic huge blocks.

5. mineral- naturally occuring, inorganic soild element or compound with a definate chem comp and reg internal crystal structure.

6.rock- soild cohesive aggreate of one or more minerals.

7. igneous rock- most common rock-type ine the earth’s cruts is solidfied from magma welling up from the earth’s interior.

8.wethering- exposure to air, water changing temperature amd reactive chemicals slowly breaks down

9. sedimentation- particles of rock are transported by wind water ice and gravity until they come to rest again in a new location.

10.sedmentary rock- deposited material that remians in place long enough or is coered with enough material to compact it may once again become rock

11. metamorphic rock- preexisting rocks can be modified by heat pressure and chemial agents to create new forms.

12.smelting- roasting ore to relase metals.

13. heap-leach extraction- invloves piling curshed ore in huge heaps and spraying it with a dilute alcakine soultion.

14. earthquakes- sudden movements in earth’s crust that occur along faults.

15. tsunami- giant sea wells that move away from the center of an earthquake.

16.volcanoes- undersea magma vents produce much of the earths curts

17. mass wasting- geological materials are moved downslope from one place to another.

18. magma- molten rock.

19.rock cycle- ceration destruction and metamorphsis

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