The nuclide half-life tells you what the nuclide is, and if the the decay rate is inconsistet, it can help tell what mix of nulides are presetn in the sample
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Without knowing the element and the specific isotope, this has no answer.
Knowing the half life of carbon-14 the age of an artefact containing an organic material can be evaluated.
This depends on the half-life of the atom
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Half-life is useful to archaeologists for dating artifacts or materials that contain radioactive isotopes. By measuring the remaining amount of radioactive isotope and knowing its half-life, archaeologists can determine the age of the artifact or material. This method is particularly useful for dating organic remains, such as bones or wood, in archaeological contexts.
Half life is useful in knowing about the age of relics.
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Half-life refers to the time required for half of the radioactive atoms in a sample to decay into stable daughter isotopes. By measuring the ratio of parent isotopes to daughter products in a rock or fossil and knowing the half-life of the parent isotope, geologists can calculate the age of the sample. This technique, known as radiometric dating, provides a reliable means to determine the age of geological formations and fossils, allowing scientists to construct a timeline of Earth's history.