Part VII. Dating, Interpreting Geologic Histories, and Geologic Time (Chapter 10 in lecture textbook)

4. The vastness of geologic time. The Earth is 4.5 billion years old and records a long history of evolution of the oceans, atmosphere, and life.

Here is a podcast series from the Open University in the U.K. that illustrates the vastness of geologic time. Check out the one called "The age of rocks".

Diagram showing events

This diagram shows some of the major events in Earth history.

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5. How is Time Recorded in Sedimentary Rocks?

Diagram showing how time is recorded in sediments

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Be sure to learn about gaps in the sedimentary record: Unconformities (know the 3 types, see p. 200-202 in textbook).

6.) Gaps in the Sedimentary rock record = Unconformities = “missing time”

a.) Types:

i.) A boundary that represents a major time break between flat-lying sedimentary layers: Disconformity.

ii.) A boundary between tilted sedimentary layers below + flat- lying ones above: Angular Unconformity.

iii. Contact between crystalline rocks (igneous or metamorphic rocks, ex. granite, schist, gneiss, diorite) below and overlying sedimentary layers = Nonconformity.


What is a Year?

What is a Month =?

Julian Calendar = 365.25 days +

Gregorian Calendar (what we use)

The vastness of Geologic Time is analogous to the vastness of the size of the universe. Compare and explore the relationships of scale here.

Back to the beginning of relative dating, geologic histories, and geologic time.

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