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Distinguish between relative dating and radioactive dating

distinguish between relative dating and radioactive dating-82

Sedimentary rock is made of particles derived from other rocks, so measuring isotopes would date the original rock material, not the sediments they have ended up in.However, there are radiometric dating methods that can be used on sedimentary rock, including luminescence dating.

Geologists use radiocarbon to date such materials as wood and pollen trapped in sediment, which indicates the date of the sediment itself.Others measure the subatomic particles that are emitted as an isotope decays.Some measure the decay of isotopes more indirectly.The table below shows characteristics of some common radiometric dating methods.Geologists choose a dating method that suits the materials available in their rocks. Measuring isotopes is particularly useful for dating igneous and some metamorphic rock, but not sedimentary rock.Typically commonly occurring fossils that had a widespread geographic distribution such as brachiopods, trilobites, and ammonites work best as index fossils.

If the fossil you are trying to date occurs alongside one of these index fossils, then the fossil you are dating must fall into the age range of the index fossil. In a hypothetical example, a rock formation contains fossils of a type of brachiopod known to occur between 410 and 420 million years.

The same rock formation also contains a type of trilobite that was known to live 415 to 425 million years ago.

Since the rock formation contains both types of fossils the ago of the rock formation must be in the overlapping date range of 415 to 420 million years.

For example, fission track dating measures the microscopic marks left in crystals by subatomic particles from decaying isotopes.

Another example is luminescence dating, which measures the energy from radioactive decay that is trapped inside nearby crystals.

Scientists can use certain types of fossils referred to as index fossils to assist in relative dating via correlation.