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HISTORY OF LIFE ON EARTH Physical conditions - last 4 billion years major changes: oxygen in atmosphere climate change ocean currents sea level changes
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History, Theory, Current Methods, Problems SRJC, Physics 43, Spring 2011 Aaron Krive, Kevin Chee
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Whats the oldest thing you have ever touched?. Evolution of Landforms and Organisms Continued – Part Two
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Dating with Radioactivity Chapter 12, Section 3. Basic Atomic Structure Each atom has a nucleus containing protons and neutrons and that nucleus is orbited
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Half-Life Pg. 870-874. Half-Life Half-life = the time needed for half of the radioisotope sample to decay into products Half-live can have varying lengths
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1.Relative age dating العمر النسبى It could be done by the following: a) Principle of superposition---Initial horizontality: In normal geologic section,
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Grand Canyon in Arizona (stratification, bedding) stratification, bedding, stratum (strata) Rock Record and Geologic Time
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James Ussher (mid 1600's) Georges Buffon (mid 1700s) Lord Kelvin (late 1800's) 75,000 yr 100 m.y. Charles Walcott (1893) 75 m.y. 4004 B.C
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Fossils are usually formed when an organism is covered by sediments that then harden into sandstone, slate, mudstone or flint. Most organisms do not fossilize
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Fossils Lecture
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Geology. The study of the solid Earth and the processes that shape it – Plate tectonics – Past climates – Natural disasters – Fossil Record – Evolution
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What’s the oldest thing you have ever touched?. Evolution of Landforms and Organisms
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