Half-Life Equation:
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Half-life dating is a method used in geology to determine the age of rocks, fossils, and archaeological artifacts by measuring the radioactive decay of isotopes. The half-life is the time required for half of the radioactive atoms present to decay.
The calculator uses the half-life equation:
Where:
Explanation: The equation calculates the time elapsed based on the ratio of remaining radioactive material to the original amount, using the known decay rate (half-life).
Details: Half-life dating is crucial for determining the age of geological formations, fossils, and archaeological artifacts. It helps scientists understand Earth's history and the timing of evolutionary events.
Tips: Enter the isotope's half-life in years, the initial amount of material, and the remaining amount. All values must be positive, and the remaining amount must be less than the initial amount.
Q1: What are common isotopes used in geological dating?
A: Carbon-14 (5730 years), Potassium-40 (1.25 billion years), Uranium-238 (4.47 billion years), and Rubidium-87 (48.8 billion years).
Q2: Why is half-life dating accurate?
A: Radioactive decay is a constant, unaffected by environmental conditions, making it a reliable clock for geological time.
Q3: What is the range of dates possible with this method?
A: From decades (Carbon-14) to billions of years (Uranium-lead dating), depending on the isotope used.
Q4: What are limitations of half-life dating?
A: Requires knowing initial amounts, can be contaminated by additional material, and some isotopes have very long half-lives making them unsuitable for recent dating.
Q5: How is this different from radiocarbon dating?
A: Radiocarbon dating is a specific type of half-life dating using Carbon-14, primarily for organic materials up to about 50,000 years old.