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Astronomy
Meteorology
Geology
NATS 1003
Syllabus
Topic Outlines
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Topic 10 Geologic Time
Primary goals
- Describe geologic history from relative geologic features.
- Arrange layers and events in a geologic cross-section in relative
time order.
- Understand the general mechanism of absolute
dating using radiometric decay.
Topics
10.1 Introduction
10.2 Relative
dating
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Rule: Sedimentary layers are deposited/formed horizontally
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Rule: In undisturbed sedimentary rock layers, older stuff is below
younger stuff
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Rule: Geologic features that cut across rocks must
have occurred after the rocks
were formed
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Rule: Fragments of one rock contained in another rock tell us that the
included rock is older
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Analytical: Be able to apply the relative dating rules to rock
cross-sections
10.3
Unconformities
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Terms: unconformity; disconformity; angular unconformity; nonconformity
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Story: How could a disconformity have occurred?
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Story: How could an angular unconformity have occurred?
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Story: How could a nonconformity have occurred?
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Analytical: Be able to recognize the type of unconformity on a rock
cross-section
10.4 Absolute
dating
10.5
Correlation
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Explanation: How are rock types used to correlate rock sequences?
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Explanation: How are index fossils used to correlate rock sequences?
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Explanation: How are key beds used to correlate rock sequences?
10.6 Geologic
Time Scale
Resources for students
Entire course
Links for
further interest 10.2 Relative dating
10.3 Unconformities
10.4 Absolute dating
10.5 Geologic
time scale
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