2. •
> Relative: Placing events in a sequence based
on their positions in the geologic
record.
> Absolute: Placing a specific number of years
on an event or rock sample.
• Two ways to relate time in geology:
> Relative
> Absolute
Important concepts
3.
4. 4
Tools used to determine
• Using radiometric
dating
• Principle of
superposition
• Principle of cross-
cutting
• Principle of lateral
continuity
• Principle of faunal
succession
Absolute Age Relative Age
8. Relative Dating
Principle of Cross - Cutting
An event that crosses several layers of rocks must be
younger than the rocks it affects, and older than the
rocks it does not.
Types of events: folds, faults, magmatic intrusions (dykes), inclusions (one
rock type included in another rock type), erosion….
14. Relative Dating
Principle of Faunal/Floral Succession
Each period in the history of the Earth can be
associated with a group of characteristic fossils.
16. 16
Guide Fossils
• Index Fossils—the ones used to date sedimentary
strata
• Their characteristics are:
– Fossils from creatures that existed for a geologically
short period of time
– Fossils from creatures that had a wide geographic
distribution
17. Location A Location B Location C
Rock layer 1 W W W Z
Rock layer 2 W Z Y Z
Rock layer 3 W X X X Z
ACTIVITY
Which letter would make a good guide fossil?
18. Relative Dating
Principle of Lateral Continuity
• Strata are deposited
in a basin and are
continuous from end
to end
• Any breaks are due to
erosion or
deformation after
deposition
19. Rocks with the same fossils can be correlated as the same
age, even if the rocks occur in widely separated locations
or are of a different rock type.
CORRELATION
20. 1. Which layers are the same?
2. Which layer is older E or F?
3. What is correct sequence of rock layers from oldest to youngest?
4. What has happened between C and B?
ACTIVITY