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EnglandGeologyQuick questions

Time, past life and past climates

Quick questions on Radiometric dating and half-life: decay, parent-daughter ratios and absolute ages - Eduqas A-Level Geology

5short Q&A pairs drawn directly from our worked dot-point answer. For full context and worked exam questions, read the parent dot-point page.

What are parent-to-daughter ratios?
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You cannot measure N0N_0 directly, but in a closed system every daughter atom came from a decayed parent, so:
What is building the absolute time scale?
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The geological time scale was first built by relative dating (the order of strata and their fossils), then calibrated in years by dating igneous rocks (lavas, ashes and intrusions) interbedded with or cutting the fossil-bearing strata. Combining the two gives absolute ages for the boundaries of the eras, periods and epochs.
What is q1?
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After three half-lives, what fraction of the original parent isotope remains? [1 mark]
What is q2?
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A mineral has a parent-to-daughter ratio of 1:1 and a half-life of 700 million years. Calculate its age. [2 marks]
What is q3?
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State one assumption that must hold for a radiometric date to be reliable. [1 mark]

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