Geologic Time Flashcards
Relative dating
Putting everything in order without knowing the exact date on which they happened
Principle of Superposition
Sediments get stacked over time. Because of gravity, the oldest sediments are usually on the bottom
Principle of Original Horizontality
Sediments that have been deposited in horizontal layers can be deformed into folds or broken faults
Principle of Original Lateral Continuity
Because sediments are deposited in horizontal layers, you can trace undeformed layers from one rock outcrop to another, even when some of the layer has been eroded
Principle of Cross-Cutting Relationships
A geologic feature that cuts across another is younger than the feature it cuts across
Principle of Inclusions
A rock inclusion is older than its host (The inclusion had to exist first in order to be incorporated into another unit)
Principle of Unconformities
Rocks above unconformity (an erosional surface) are younger than the rocks below. Unconformities mean that there is something missing from the rock record
Principle of Faunal Succession (Evolution)
- Animals evolve and go extinct, never to return again
- An extinct organism will only appear in rocks that formed when it was alive
- Fossils of different animals will succeed each other vertically in a specific, predictable order
Absolute dating
Calculating a numerical date
Atom
Smallest component of nature with the properties of a given substance
Isotopes
Atoms with differing numbers of neurons (different mass numbers) but same number of protons
Difference between stable isotopes and radioactive isotopes
Stable isotopes do not spontaneously break down, radioactive isotopes do. Radioactive isotopes (parent isotopes) are not stable and break down into daughter isotopes over time.
What is the rate of decay and how is it measured?
The rate of decay is how quickly a radioactive isotope breaks down, it is measured using half-life.
Half-time
The amount of time it takes for half the sample to break down
Radiometric dating
Used to calculate the age of a sample (you need to know the half-life & measure the ratio of parent to daughter isotope)