Relative and Absolute Dating 2013
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Transcript Relative and Absolute Dating 2013
Relative and Absolute Dating
What is Dating?
When geologists date rocks, they are
determining how long ago they formed.
Two ways to do this:
Relative Dating
Absolute Dating
Relative Dating
Determining how old something is
compared to something else
Use words like “older” or “younger” instead
of exact numbers
Rules of Dating
two rules for dating rocks:
1. Stuff on the bottom is oldest and the stuff on
the top is youngest
This is called the
Law of Superposition
This only works for sedimentary rocks
(sometimes lava flows)
Order these layers from oldest to
youngest
Youngest layer
Oldest layer
Rules of Dating
two rules for dating rocks:
2. If a fault or another rock cuts through a layer it
happened after (and is younger than) the layer
This is called the
Law of Cross-Cutting Relations
Order the events from oldest to youngest
YOUNGEST LAYER/EVENT
Fault
Gray Layer
Multicolored layer
Tan Layer
OLDEST LAYER/EVENT
Absolute Dating
Determining how old something is
Use numbers (in millions of years, mya)
Only works for Igneous Rocks
How Absolute Dating Works
When magma/lava cools, radioactive elements
are incorporated into the minerals
Examples:
-- Potassium 40
-- Uranium 235
How Absolute Dating Works
These elements begin to decay at a known rate
starting when the rock cools
We can measure how much of the element is
left
Tells us how much time has passed since the
rock formed.
What can we learn from this?
Geologist
Basalt, dated to 80
mya
T-Rex Fossil
Sandstone
Basalt flow, dated
to 100 mya
So when did this T-Rex live?
Between 100 and 80 mya
This may not seem very accurate, but compared to
the 4,500 million years the earth has been around it
gives us a lot more information than we had before
What can we learn from this?
Absolute Dating
Helps us determine the age of the earth
Helps us determine when specific events in the
history of the earth happened (ex. Extinction of
the dinosaurs)
Relative Dating
Can help us estimate the time span between
major earthquakes, storms, tsunamis etc
Can help us determine the order that life forms
developed on earth