Radiometric Dating

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Radiometric decay is the constant predictable decay of unstable atoms into more stable isotopes or elements. Measurements of atomic decay are generally considered one of the most accurate ways of measuring the age of an object, and these measurements form the basis for the scientifically accepted age of the earth. There are many different variations of the radiometric dating technique such as radiocarbon, argon-argon, iodine-xenon, lanthanum-barium, lead-lead, lutetium-hafnium, neon-neon, potassium-argon, rhenium-osmium, rubidium-strontium, samarium-neodymium, uranium-lead, uranium-lead-helium, uranium-thorium, and uranium-uranium, of which every single one will date objects far older than 10,000 years1.(2)

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