Section 1- Geological Time Flashcards
Define catastrophism
Geological theory from 18th century, points to disasters (floods, earthquakes)to explain features of the earths surface such as mountains and valleys
Define uniformitarianism
Suggests past geological events can be explained by the forces observable today because The same geological processes happening now must have happened in the same way throughout time
Principle of original horizontality
Due to gravity sedimentary rocks are deposited as horizontal layers
If sedimentary rocks are folded(or faulted) this occurred after deposition
Principle of superposition
In a sequence of bedded rock, the rock above is younger than the ones below
Igneous intrusions/cross cutting relationships
Igneous intrusions are younger than the rock that they intrude or break
Principle of lateral continuity
Rock units with similar characteristics can be correlated across different exposures over large distances
Rocks that are similar but now separated by a valley or other feature can be assumed to be originally continuous.
Define unconformities
Represent breaks in the geological record(ie. erosional surfaces and missing rock in the expected sequence)
Principle of biotic succession
Since organisms have evolved and gone extinct through time, specific groups of fossils succeed one another in the rock record in a definite order, so fossil content can be used to determine the age of rock units
2 methods of geological time
Relative time:
Observed contact relationships between rock units, fossil records
Absolute time: specific age of a unit in years
Explain radiometric/absolute dating
Radioisotopes(parents-unstable radioactive isotope) are trapped in minerals when the crystallize and then decay through time. The ratio of parent to daughter(stable isotope resulting from decay of parent) reveals the number of half lives that have elapsed
Geological time scale major divisions
Hadean Eon (4-4.5 Ga)
Archean Eon(2.5-4Ga)
Proterozoic Eon(2.5Ga-545Ma)
Phanerozoic Eon <545Ma
Hadean Eon
4-4.5 Ga
Earths cooling period
Widespread volcanism
Archean Eon
2.5-4Ga
First unicellular life for s(age of bacteria)
Oldest rocks found on the planet
Final stage of earths cooling and formation of the crust
Proterozoic eon
2.5Ga-545Ma
Most diamonds formed
Oldest sedimentary rocks
Formation of ozone layer
First multicellular organisms(jellyfish)
Phanerozoic Eon
<545 Ma
Abundant animal and plant life
Age of marine life, age of dinosaurs and age of mammals
(Paleozoic, Mesozoic,Cenozoic eras)