| Last lecture we looked at how the rock record was subdivided into the relative time units of the Geologic Time scale. |
| Today we will look at how absolute dates were added to the Geologic Time scale |
| There has been a long debate over the age of the Earth. |
| The age of the earth is key to evalutating geologic and biologic processes. |
| Uniformitarianism and Evolution require a large age of the Earth. |
Measuring the age of the Earth |
| extrapolating age by using generations listed in Genesis |
| Bishop Jame Ussher (1665) |
| El Moro Nation Monument, New Mexico |
| Canyon De Chelly, Arizona |
| Salt concentration in the oceans |
| John Joly (1899), 90 million years |
| John Phillips (1860), 96 Million years |
| C.D Walcott (1893), 27.6 Million years |
| Lord Kelvin (1862), 20 to 40 million years |
| Radioactive Dating Methods |
| Radioactivity discovered in 1890s |
| Radioactive elements decay to non-radioactive forms at a constant rate |
| Use uniformitarianism (present is key to past) |
| Measure ratio of parent to daughter |
| Half-lifes and Applicable Range |
|
Parent
|
Daughter
|
Half-life
|
Applicable Range
|
Rubidium-87
|
Strontium
|
47,000 million years
|
> 10 million years
|
Thorium-232
|
Lead-208
|
13,900 million years
|
> 5 million years
|
Uranium-238
|
Lead-206
|
4,500 million years
|
> 1 million years
|
Uranium-235
|
Lead-207
|
713 million years
|
> 1 million years
|
Potassium
|
Argon
|
1,300 million years
|
>50,000 years
|
Carbon-14
|
Nitrogen-14
|
5,568 years
|
< 50,000 years
|
|
| Oldest Earth rocks are 3.8 billion years old |
| Meteorites on earth are generally around 4.6 billion years old |
| Moon rocks are between 4.6 and 3 billion years old |
| Age of the Earth is thought to be 4.6 billion years old |
|