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Earth Science
Geologic Time Scale
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The method of reading the order of rocks is called
stratigraphy
Biostratigraphy
is the study of the order in which fossils appeared and disappeared through time and rocks
Fossils can help to match rocks of the same age through
correlation
Most radiometric dating measure the amount of isotopes in rocks using a
mass spectrometer
Index Fossil
: lived in one period, easy to identify, abundant, found in many places
Index fossils must be
Distinctive
or
easily recognizable
Abundant
Wide geographic distribution
Short range through time