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Radiometric Dating Continuation of Journal Entry #5.

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Presentation on theme: "Radiometric Dating Continuation of Journal Entry #5."— Presentation transcript:

1 Radiometric Dating Continuation of Journal Entry #5

2 Radiometric Dating A technique used to date materials such as rocks based upon a comparison between the observed abundance of a naturally occurring radioactive isotope and its decay products using known rates of decay. Some elements have isotopes that predictably decay over time to more stable forms

3 Types of radioactive decay Alpha decay – Isotope emits 2 n 0 and 2 p + Beta decay – Isotope emits 1 e - Neutron decay – Isotope emits 1 n 0

4 Common radioactive isotopes and their products C-14  N-14 (beta decay) K-40  Ar-40 (beta decay) U-235  Pb-207 (all three forms of decay)

5 Radioactive Half-life The rate at which an isotope decays can be precisely measured in the lab and have been found to occur at a constant, predicable rate. An isotopes half-life is the amount of time necessary for ½ of the original amount of the radioactive isotope to decay to the more stable form.

6 Commonly used half-lives C-14 = 5,730 years U-235 = 704 million years K-40 = 1.25 billion years

7 Question: If I found a bone with 12.5% of the expected amount of C-14, approximately how old is the bone?

8 Answer: 5,730 years x 3 half-lives = 17,190 yrs

9 U-235 decay The geologic processes that form uranium are very different than those that form lead. Therefore, any lead found in a rock containing uranium must have been formed by decay. A measurement of the ratio of the two will reveal how many half-lives have passed – and thus will determine the age of the fossil.

10 Say hello to your lab partner!

11 Analysis Question If I found a fossil sample with 12 m&m’s remaining from the original sample, how old would it be if m&mdium has a half-life of 4.7 million years?

12 #2 – Explain how an evolutionary biologist would use radiometric dating, relative dating, and fossils to determine something about how species have changed over time. #3 – Personal thoughts and reflections


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