GEOLOGIC TIME
Geologic Time
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Two ways to view geologic time:
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Relative time
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"older" vs. "younger"
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placed in order
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Absolute time
Relative Time
Basic Rules
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Relative Time - places the rock
record within a sequence of events
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Basic Rules
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Law of Superposition - in undeformed
strata:
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lowest unit oldest
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units become younger upward
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Principle of Original Horizontality
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Strata generally deposited horizontally
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tilting post-dates deposition
Relative Time
Basic Rules (cont.)
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Principle of Original Horizontality
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Strata generally deposited horizontally
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tilting post-dates deposition
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Cross-cutting relations
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the geologic feature that cuts across or penetrates
another rock body must be younger than the rock unit it penetrates
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Inclusions
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older than the rock in which they are included
Unconformities
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Unconformities
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When sedimentation is continuous
without interruption, it is said to be conformable
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Gaps in time in the stratigraphic
record are called unconformities
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May represent erosion surface
or just a period of non-deposition
Types of Unconformities
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May represent erosion surface or just a period of
non-deposition
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Two types of unconformities are:
Types of Unconformities (cont.)
Relative Time Problem
Correlation and Stratigraphy
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While seas were flooding Texas and Colorado in the Cretaceous,
was Europe flooded? (Implications?)
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Did the extinction of the dinosaurs
in North America occur at the same time in Europe? (Implications?)
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To answer these questions, need
to correlate sedimentary rocks in one area with those in another.
Stratigraphic Units
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First need to define units of strata
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Three classification schemes
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Rock Units
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defined based on observable characteristics of
rock
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Fundamental rock unit is a formation
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mappable, lithologically distinct
body of rock having recognizable boundries (contacts) with other formations
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formations subdivided into members
or grouped into groups
Stratigraphic Units
Correlation and Time

Stratigraphic Units (cont.)
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Time units
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the Geologic Time Scale divides geologic time
into time units -- Eras, Periods, Epochs
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Time-rock units
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classification of sedimentary layers deposited
during a particular time interval (which corresponds to a time unit)
Stratigraphic Correlation
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Correlate By:
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lithology - type of layered sedimentary
or igneous rock
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fossils - remains and traces of
organisms
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first occurrence, last occurrence
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index fossils
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Principle of Faunal and Floral
Succesion
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layer of strata has a particular fossil assemblage
associated with it (faunal assemblage changes with time).
Stratigraphic Correlation