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- Cassie Strickland, Columbia Basin College
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- Geology: The study of the planet Earth
- materials of which it is made
- processes that act on these materials
- products formed
- history of the planet and its life forms since its origin
- Divided into
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- Basic Course Outline:
- Fundamental Concepts of Historical Geology
- Rate of Geologic Change
- Important theories & people
- Fossils & Evolution
- Geologic Time and Dating Methodologies
- Origin of Earth & Movement of Continents
- Time Periods in Detail:
- Archean, Proterozoic, Paleozoic, Mesozoic, Cenozoic
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- Oldest meteorites and moon rocks
- Oldest rocks on Earth
- ~4.1-4.2 billion years old
- Zircon, from Jack Hills, Australia
- Jack Hills metaconglomerate, Enanondoo Hill, Jack Hils region, western
Australia. Photos by SA Wilde.
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- meteorite impacts
- volcanic eruptions and lava flows
- mountain building
- earthquakes
- erosion
- slow movement of continents (plate tectonics)
- formation and destruction of ocean basins (plate tectonics)
- glaciations
- climatic changes
- Human effects (anthropogenic)
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- Catastrophic
- eruption of Mt. Thera; ~1650 B.C.
- ended Minoan culture
- Gradual
- current global warming is flooding coastal areas like Venice, Amsterdam
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- Geologic change can be linear or non-linear
- Geologic change can be repetitive or non-repeating
- Periodic
- Episodic
- Non-repeating change
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- Catastrophism
- Dominated human beliefs until ~1850
- Believed in 6,000 year old Earth
- Example: Old Testament Flood
- Uniformitarianism
- Considers episodic events like earthquakes normal and non-catastrophic
- Modern geology dates Earth to ~4.5 billion years of age
- Example: Daily water erosion
process widens & deepens stream channel
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- Principle of Uniformitarianism
- Scientific Method
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