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14 Cards in this Set

  • Front
  • Back
The four principle eras of the geologic time scale (from the earliest to the most recent)
1. Precambrian
2. Paleozoic
3. Mesozoic
4. Cenzoic
Precambrian Life Characteristics
Spans from the formation of the earth to the evolution of macroscopic hard shelled animals
Paleozoic Life Characteristics
Spans from the appearance of soft shelled animals to the start of the age of the reptiles and modern plants
Paleozoic Land Characteristics
Started shortly after the breakup of a supercontinent at the end of an ice age, ended as the continents formed Pangea
Mesozoic Life Characteristics
The age of the reptiles
Mesozoic Land Characteristics
Continents shifted from their current state through continental drift, allowing speciation and other evolutionary developments to take place
Cenozoic Life Characteristics
Began with the demise of the last non-avian dinosaurs, and is currently ongoing
Cenozoic Land Characteristics
The continents moved into their current positions
Disconformity
The contact representing missing rock strata separates beds that are parallel to one another
Angular Unconformity
A contact in which younger strata overlie an erosion surface on tilted or folded layered bedrock
Nonconformity
A contact in which an erosion surface on plutonic or metamorphic rock has been covered by younger sedimentary or volcanic rock
Requirements for Radiometric Dating
1) Igneous or metamorphic rock
2) Decay rate of isotope
3) Accurate measurement of % parent within the mineral
Steps for Radiometric Dating
1) Determine the ratio of parent isotopes to daughter isotopes
2) Using the ratio, determine the number of half lives elapsed
3) For the Parent-Daughter pair, find the time for each half life
4) Multiple the number of half lives elapsed by the time for each half life
Rules of Geologic Time
1) Superposition - newest on top
2) Cross cutting relations - faults, folds, or intrusions are younger than the rocks, faults, folds, or intrusions they cut
3) Inclusions - are older than their host rocks