Lesson 9) Statigraphy and Geologic Time Flashcards
Statisgraphic concepts and the scale of Earth History
Principle of Superposition
Tendency or rock layers to be chronologically stacked.
- Sediments deposited -> gradual build up
- How things normally work, but can be exceptions:.
Unconformity
Flat surface caused by partially melted igneous intrusions that are uplifted and eroded
Statigraphy
Science of using arrangement and composition of rock layers to interpret geological history
Formation
Large uninterrupted sequence of rock that is made of multiple layers that all share similar properties (eg- composition + grain size) all formed under similar conditions
What is indicated when a rock changes formations?
Large scale change occurred in the environment where the rocks were deposited.
Principle of Superposition
Allows stratigraphies to infer relative age of rock layers (layer age vs other layer age)
- DOES NOT determine absolute age
Radiometric dating
Technique to determine rocks age.
As rock ages, isotopes decay and ratio of isotopes : decay product decreases.
Mass spectrometers can measure the isotope ratio of rock, which can tell how old it is.
Isotope
Variant of a chemicalelement that has unusual number of neutrons.
- some are unstable and undergo radioactive decay: energy release, resulting in atoms w/ different compositions (decay products)
What rock can’t be radiometrically dated?
Sedimentary
They are not new: they are made of sediments that have already formed and are undergoing radioactive decay already probably.
However: can use volvanic ash layers (within sedimentaries to estimate nearby fossil ages)
What can usually be radiometrically dated?
Igneous
Formed anew
- When igneous rock solidifies, it starts out w/ isotope ratio equal to that found in its environment
How can we measure fossils age, if they’re usually found in sedimentary rocks?
Radiometric dating + principle of superstition
IF found between two horizontally deposited igneous rock layers— can bracket age
Geologic Time Scale
Standardized series of chronological divisions that parses Earth’s history into discrete named units.
Eons > Eras > Periods > Epochs
Hadean eon
4.4-4 billions yrs ago
Formation and earl Earth years.
- Surface partially molten and hella volcanoes
- Planet collision which formed moon
By then end, Earth had cooled and hella oceans
- organic molecules form
Archean Eon
2-2.5 billion yrs ago
- Oldest fossils (single-celled organisms)
- Cynanobacteria made oxygen and stromatolites
Stromatolites
Structures formed by cyanobacteria from the Archean Eon
- Lump stones that when cut in half, show layers of secreted sticky limbs trapping sediment particles.