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    Exercise 2 relative and absolute dating of geologic events

    Like the other kind of dating, geologic dating isn’t always simple.

    Activity: Further discussion: Good overview as relates to the Grand Canyon: age dating: Use with this cross section of the Grand Canyon from the USGS’s teaching page: Canyon Have students reconstruct a simple geologic history — which are the oldest rocks shown? Are there any that you can’t tell using the Rule of Superposition?

    Chart of a few different isotope half lifes: In reality, geologists tend to mix and match relative and absolute age dates to piece together a geologic history.

    If a rock has been partially melted, or otherwise metamorphosed, that causes complications for radiometric (absolute) age dating as well.

    In a way this field, called geochronology, is some of the purest detective work earth scientists do.

    There are two basic approaches: relative age dating, and absolute age dating.

    That’s because zircon is super tough – it resists weathering. Each radioactive isotope works best for particular applications.

    The half-life of carbon 14, for example, is 5,730 years.

    They are both important in terms of Earth's history and its geological timeline, and they work together in concert to build the planet's geological record.

    Relative age dating also means paying attention to crosscutting relationships.

    Say for example that a volcanic dike, or a fault, cuts across several sedimentary layers, or maybe through another volcanic rock type.

    What’s more, if the whole rock is badly weathered, it will be hard to find an intact mineral grain containing radioactive isotopes.

    You might have noticed that many of the oldest age dates come from a mineral called zircon.

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