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Dating Fossils in the Rocks

The five categories included in the peer review process are. This activity has benefited from input from faculty educators beyond the author through a review and suggestion process. This review took place as a part of a faculty professional development workshop where groups of faculty reviewed each others’ activities and offered feedback and ideas for improvements.

Students don’t have to be passively taught the important principles geologists use to do relative age- dating of rocks and geologic events. By careful analysis and critical thinking about photos and illustrations of rock outcrops, they can discover these principles themselves, and present their discoveries to the class!

The age of a rock is determined by stratigraphy, a branch in geology which by relative dating , only the order of deposits has been determined, i.e. the events in​.

The oldest mineral grains yet identified on Earth are about 4. Rocks brought back from the moon by astronauts, and meteorites that have fallen to Earth, are about 4. Because the moon, Earth, and the meteors probably formed at the same time concurrently with the rest of the solar system , we can conclude that the Earth itself is about 4. How do we know that the Morton gneiss is older or younger than other rocks?

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How do we know the age of any rock? Using relative age, geologists can show that a particular rock unit is older than some other rock unit without knowing how old either one is in calendar years. They understand the processes by which rocks form, and have developed logical rules based on observable field relationships to establish the relative ages among rock units.

Although we may not be used to thinking of them this way, calendars and clocks are simply convenient devices for counting orbital revolutions and Earth rotations, respectively. The calibration of human history depends on people who counted and recorded orbital revolutions in some systematic way. For the vast majority of geologic time, however, humans were not around to keep track with astronomical calendars and clocks.