Midterm & Glaciers Flashcards
(138 cards)
Relative Time
Determines the sequence of events
Absolute Time
Determines the date/age of events
Geologic Principles
- Original Horizontality
- Superposition
- Inclusions
- Cross-cutting relations
- Contact margins
- Faunal succession
Original Horizontality
Rock is initially laid down horizontally; any change in angle has been cause afterwards
Superposition
Rocks that are closer to the surface are younger
Inclusions
Young rock can contain pieces of older rock
Cross-cutting relations
Young rock or features can cut across older rock or features
Contact Margins
A young rock/feature can cause changes along the contact line with an older rock/feature
Faunal succession
Fossil assemblages can be correlated to specific deposits/time periods
Unconformities
Periods of time that are missing from the geologic record
Still help us determine what happened during that time; we know that there was uplift, erosion, etc.
Three types:
- Angular unconformity
- Nonconformity
- Disconformity
Angular unconformity
rock is uplifted, eroded, then new sediment is laid horizontally on top
Nonconformity
Sedimentary rocks overlie intrusive igneous rocks and/or metamorphic rocks
Disconformity
Contact between two beds represents a period during which no deposition occurred - i.e. there is a large gap in the age of the two sediments
So basically they’re like that 51-year-old and 16-year-old getting together
Radiometric dating
Radioactive isotopes decay randomly but at a set rat, meaning we can predict how long it takes for them to decay to a certain ratio of daughter and parent isotopes
Assumes that there has been no loss or gain of parent or daughter isotopes, and the rock is below closure temperature (and has been since it was formed)
Body fossils
The actual physical remains of an organism (i.e. skeleton) has been left behind and mineralized
Trace fossils
Evidence of an organism’s existence in an area has been preserved in the rock (i.e. footprints, coprolite)
Concordia Curve
Plotting two things against each other (ex. two half-lifes) to form a curve, then plotting experimental data along the same plot to see if they come up with a similar answer
Fission tracks
Disintegration of the nucleus of 238U create sausage-shaped tracks within a mineral
You can determine age by counting tracks
Rhythmic processes
Can be used as absolute dating methods, e.g:
- Varves (yearly patterns in lake sediment deposition)
- Corals (daily growth marks)
- Magnetostratigraphy (reversals of earth’s magnetic field)
Geologic Timescale
Division of earth’s history into eons, eras, periods, and epochs
Eons
Largest division of time on the geologic timescale:
- Hadean
- Archean
- Proterozoic
- Phanerozoic
Eras
- Palaeozoic
- Mesozoic
- Cenozoic
Oldest Rock
Acasta gneiss from the Northwest Territories
4,025 +/- 15 Ma
Age of the Earth
4.567 Ga
Determined from the age of meteorites believed to be from the same time the solar system was formed