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Tuesday 5/3/11 How the Earth Was Made
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Content Objectives 1.We will learn about how scientists have determined the age of the Earth. 2.We will learn about the history of Earth over time.
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Language Objectives 1.We will use reading, discussion and writing to learn about the history of Earth.
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Schedule Agenda, objectives 5 min. Intro. to geologic methods for dating rocks 10 min. Video 25 min. Discussion 10 min.
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How do scientists KNOW things? Observations Experiments Inferences
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Relative Dating (this rock is older than that rock) Most of the time the rocks on the top are older than the rocks on the bottom
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Absolute Dating (this rock is 28 million years old) Some atoms are not stable—they break down into “daughter” atoms Ex.: Uranium changes into a form of lead at a constant known rate
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Oldest Rock Oldest rocks on Earth are the Acasta Gniess of northern Canada 4.03 billion years old © NASA Acasta Gneiss Zircon mineral
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Oldest Zircon Grain 4.4 by zircon grain www.geology.wisc.edu/zircon/Earliest%20Piece/Images/2a-team.jpg © NASA Ancient mineral grain found at Jack Hills, Australia Mineral grain eroded from first crust and then deposited in a new rock Dates the Earth’s first crust to around 4.4 billion years
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Meteorites Radiometric age of meteorites date the formation of the Solar System and Earth (4.55 billion years old) en.wikipedia.org/wiki/Image:Canyon-diablo-meteorite.jpg http://upload.wikimedia.org/wikipedia/commons/0/00/Crab_Nebula.jpg Crab Nebula Canyon Diablo meteorite
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