http://equalsmcsquared.livejournal.com/ (
equalsmcsquared.livejournal.com) wrote in
fandomhigh2005-11-28 08:42 am
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Entry tags:
Geology
I hope everyone had a good Thanksgiving. If not, well, I'm sorry. *She smiles pleasantly.* There is leftover pumpkin pie and coffee near the back. Please sign the roll sheet and tell any of your friends who might be skipping that there will be a quiz on Wednesday. Fair warning.
Today, we will be discussing radiometric dating.
Naturally-occurring radioactive materials break down into other materials at known rates. This is known as radioactive decay.
Radioactive parent elements decay to stable daughter elements.
Radioactivity was discovered in 1896 by Henri Becquerel. In 1905, Rutherford and Boltwood used the principle of radioactive decay to measure the age of rocks and minerals (using Uranium decaying to produce Helium. In 1907, Boltwood dated a sample of urnanite based on uranium/lead ratios. Amazingly, this was all done before isotopes were known, and before the decay rates were known accurately.
The invention of the MASS SPECTROMETER after World War I (post-1918) led to the discovery of more than 200 isotopes.
Many radioactive elemtns can be used as geologic clocks. Each radioactive element decays at its own nearly constant rate. Once this rate is known, geologists can estimate the length of time over which decay has been occurring by measuring the amount of radioactive parent element and the amount of stable daughter elements.
Today, we will be discussing radiometric dating.
Naturally-occurring radioactive materials break down into other materials at known rates. This is known as radioactive decay.
Radioactive parent elements decay to stable daughter elements.
Radioactivity was discovered in 1896 by Henri Becquerel. In 1905, Rutherford and Boltwood used the principle of radioactive decay to measure the age of rocks and minerals (using Uranium decaying to produce Helium. In 1907, Boltwood dated a sample of urnanite based on uranium/lead ratios. Amazingly, this was all done before isotopes were known, and before the decay rates were known accurately.
The invention of the MASS SPECTROMETER after World War I (post-1918) led to the discovery of more than 200 isotopes.
Many radioactive elemtns can be used as geologic clocks. Each radioactive element decays at its own nearly constant rate. Once this rate is known, geologists can estimate the length of time over which decay has been occurring by measuring the amount of radioactive parent element and the amount of stable daughter elements.
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[[ooc: let's do it under the right login, shall we?]]
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[ooc: I posted this first to Sara's journal. Don't feel bad. ;)]
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"Ah well, he's one of the lucky ones. We are a special few." Draco laughs.
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[ooc: Because ack, getting sucked into a meeting...]
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