Title: Geologic Time Notes
1Geologic Time
2Why is this statement false The caveman had
dinosaur for breakfast.?
- man and dinosaurs
- never lived at the same time
3Laws of geologic history
- SuperpositionOldest rocks on the bottom of an
undisturbed sequence of rock - Law of original horizontalityAll rocks are
initially deposited in flat (horizontal) rows - Cross-cutting relationshipsObjects which
cross-cut rocks are younger than the rocks
themselves (ex fault or intrusion)
4Superposition
5Using superposition, label the strata below from
oldest to youngest.
youngest
oldest
6Horizontality
All rock layers are originally deposited in flat
(horizontal) layers
7Faults are always (older, younger) than the
rocks they cut through.
Cross-cutting relationships
8(No Transcript)
9Which is older F or S How do you know?
F cuts through S S must have been there first
(it's older)
10Uniformitarianism
These laws are based on the assumption that the
forces at work today are the same forces at work
in history uniformitarianism.
11If a geologist finds an igneous sill, how can she
determine if the sill is an intrusion or an
extrusion?
12(No Transcript)
13 Is H an intrusion or extrusion?How can you
tell?
14 H is an intrusion.Contact metamorphism on top
15On to the next question...
16What is an unconformity? How does it complicate
the relative dating of rock layers?
- a buried erosional surface
- a part of the rock record
- is missing
17Using the diagram to the left, identify where the
unconformity is located by drawing an arrow and
writing the word unconformity next to it.
18What are
Index fossils?
19What characteristics must fossils have in order
to be good index fossils?
- lived over a large geographic area (large
horizontal distribution) - lived for a short period of time (small vertical
distribution)
20In the diagram below, a geologist has matched up
rock layers based on index fossils.
In geology, this is referred to as CORRELATION
21On to the next question...
22Absolute Age
Why are radioactive isotopes useful in
determining the absolute age of a rock?
their half-lives are constant
23Absolute Age
- What can be done to change the
- half-life of a radioactive isotope?
- Why is this important?
NOTHING!
it is reliable to calculate age
24Draw the generic graph for the half-life of a
radioactive isotope.
stable atoms
unstable atoms
25Absolute Age
- What radioactive isotope could be
- used to determine the absolute
- age of material that was recently living?
- carbon-14
26Please answer the two questions on page 7 of
your Notes
What is the half life of uranium-238? 4.5 x
109 4,500,000,000 4.5 billion years choice (c)
27If there is a 100g sample of C14, how many grams
of C14 would remain after three half-lives?
How long would this take? Show all work.
?
?
?
100g
50g
25g
12.5g
3 half-lives x (5.7 x 103) 1.71 x 104
17,100 years