How to radiometric dating
Radiometric dating is based on the decay rate of these isotopes into stable nonradioactive isotopes.
To date an object, scientists measure the quantity of parent and daughter isotope in a sample, and use the atomic decay rate to determine its possible age.
Radiometric dating is a method which scientists use to determine the age of various specimens, mainly inorganic matter (rocks, etc.), though there is one radiometric dating technique, radiocarbon dating, which is used to date organic specimens. Basically, scientists take advantage of a natural process by which unstable radioactive “parent” isotopes decay into stable “daughter” isotopes spontaneously over time.
Uranium-238 (U238), for example, is an unstable radioactive isotope which decays into Lead-206 (Pb206) naturally over time (it goes through 13 unstable intermediate stages before it finally stabilizes into Pb206).
Play a game that tests your ability to match the percentage of the dating element that remains to the age of the object.
Understand how decay and half life work to enable radiometric dating.A commonly used radiometric dating technique relies on the breakdown of potassium (Ar in an igneous rock can tell us the amount of time that has passed since the rock crystallized.If an igneous or other rock is metamorphosed, its radiometric clock is reset, and potassium-argon measurements can be used to tell the number of years that has passed since metamorphism.Various exchange processes between the atmosphere, the biosphere, and the hydrosphere result in a dynamic equilibrium between C abundance ratio by counting the isotopes themselves.
This makes it possible to reduce the necessary sample size from over 1 gram to less than 1 milligram of carbon and the measuring time from days to hours.Question: "How does radiometric dating fit with the view of a young earth?