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Warm-Up 11/15 1.What is an index fossil? 2.How are fossils relevant to your daily life? 3.What are some limitations of relative dating? 4.What is radiation?

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Presentation on theme: "Warm-Up 11/15 1.What is an index fossil? 2.How are fossils relevant to your daily life? 3.What are some limitations of relative dating? 4.What is radiation?"— Presentation transcript:

1 Warm-Up 11/15 1.What is an index fossil? 2.How are fossils relevant to your daily life? 3.What are some limitations of relative dating? 4.What is radiation?

2 TO THE LIBRARY! Walk to library in an orderly and quiet fashion! 10 min to pick out a book 5 min to read Return to class in a quiet and orderly fashion! I have a lab planned for today that we can only get to if we don’t waste time! Worksheets are back-up plans!

3 1.What is a parent atom? 2.What is a daughter atom? 3.What is a half life? 4.If you have 10 grams of a radioactive element how many grams of that element will you have after one half life? Warm-Up 11/16 WARM-UPS DUE TODAY! TURN IN AFTER NOTES.

4 Absolute Dating Absolute dating is simply the actual age of a rock layer. The 3 ways of absolute dating we will examine are: Varve count, radioactive decay/half-life, and carbon dating.

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6 1. Varve Count Sort of like counting the rings in a tree trunk to determine tree age. Varves: annual layer of sedimentary deposit on a lake bed. Usually a glacial lake. Sediments are brought in during summer and settle during winter, giving a yearly ring, just like the rings on a tree trunk.

7 True or False… Varve count can be compared to rings in a tree trunk.

8 True or False… Varves are usually found in glacial lakes.

9 2. Radioactive Decay Radioactive elements  unstable elements Unstable means the elements break down into isotopes to try and become stable. Once they reach a stable state this isotope is called the daughter element.

10 True or False… The stable isotope is referred to as the “sister” element.

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12 2. Radioactive Decay Con’t Example of radioactive decay of an element: U-238  emits 2 protons and 2 neutrons Th-234  one neutron changes into a proton and an electron then electron is emitted Pa-234  still unstable, energy is emitted Pb-206  finally reach daughter element

13 2. Half-life Refer back to previous example…Let’s pretend we started with 10 grams of U- 238. Scientists have found a way to calculate the length of time that it takes for HALF of that amount to radioactively decay to Pb-206 (daughter element)

14 2. Half-life Con’t Half-life: the time it takes for HALF the mass of a given amount of a radioactive element to decay into its daughter element.

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16 True or False… For a half-life to exist in an element the element must be radioactive.

17 3. Carbon Dating A common isotope of Carbon is C-14. We know the half-life of this isotope is about 5,730 yrs. C-14 is present in CO2(Carbon Dioxide) which means all things exposed to CO2 will have some amount of C-14 in them. We use C-14 and our knowledge of C-14’s half-life to determine approximate age

18 True or False… The half-life of C-14 is about 3,750 years.


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