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Earth

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Earth
Core- (inner & outer) iron, nickel, sulfur
- Mantle- silicate materials
- Crust- granitic, basaltic rocks
- Mantle- silicate materials
HEAT Sources:
- Primordial Heat- 5%
- Crystallization/Differentiation/Friction- heat cools, crystallizes, moves, friction=heat
- Radioactive Decay: 90%, unstable isotopes decay radioactively into other more stable elements, releasing energy and radiation
- Least to Most Radioactive: Banana, Nuts, Salt, Nuclear Waste, Smoke Detector, Granite
- Radioactive Decay: 90%, unstable isotopes decay radioactively into other more stable elements, releasing energy and radiation
- Crystallization/Differentiation/Friction- heat cools, crystallizes, moves, friction=heat
- Primordial Heat- 5%
Unconfortmities:
- Disunconformity- unconformity between parallels of sedimentary rocks
- Angular Unconformity- uplift, tilt, followed by erosion and new disposition
- Nonconformity- igneous or metamorphic rock eroded and sedimentary rock
Law of Faunal Succession- over time, life forms change, old ones disappear and new ones appear in the geologic record
Uniformitarism- geologists can infer much about how rocks were formed/changed in the past bc the same physical laws have operated through history
Relative Age Dating
- Stratigraphy-studies rock layer (strata) and layering (stratification)
- Principle of Original Horizontality- sediments are deposited in horizontal, flat layers
- Stratigraphy-studies rock layer (strata) and layering (stratification)
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- Mind Map on Earth, created by Rachel Thornton on 06/10/2015.
- Created by
- Rachel Thornton
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