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Geologic Time - Geology - Lecture Slides | GS 106, Study notes of School management&administration

Material Type: Notes; Class: Physical Science (Geology); Subject: General Science; University: Portland Community College; Term: Spring 2007;

Typology: Study notes

Pre 2010

Uploaded on 08/18/2009

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GEOLOGIC TIME
RELATIVE DATING
ABSOLUTE DATING AND RADIOACTIVITY
DIVISIONS OF THE TIME SCALE
RELATIVE DATING
1) Law of Superposition =
Oldest rocks on the bottom,
Younger rocks on the top
RELATIVE DATING
2) Principle of Horizontality = Layers are generally
deposited horizontally. Flat rock layers have not
been disturbed
RELATIVE DATING
3) Principle of Cross-cutting Relationships = A
Younger feature cuts through an older feature
RELATIVE DATING
4) Inclusions =
One rock unit is enclosed within another.
The rock containing the inclusions is
younger than the inclusions.
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GEOLOGIC TIME

RELATIVE DATING

ABSOLUTE DATING AND RADIOACTIVITY

DIVISIONS OF THE TIME SCALE

RELATIVE DATING

  1. Law of Superposition =

Oldest rocks on the bottom, Younger rocks on the top

RELATIVE DATING

  1. Principle of Horizontality = Layers are generally deposited horizontally. Flat rock layers have not been disturbed

RELATIVE DATING

  1. Principle of Cross-cutting Relationships = A Younger feature cuts through an older feature

RELATIVE DATING

  1. Inclusions =

One rock unit is enclosed within another.

The rock containing the inclusions is younger than the inclusions.

RELATIVE DATING

FOSSIL SUCCESSION

Fossils = the remains or traces of prehistoric life Fossil Types Relatively recent organisms Entire animals, flesh included Petrified (turned to stone) Molds and Casts Carbonization Others (tracks, burrows, coprolites, gastroliths)

RELATIVE DATING

FOSSIL SUCCESSION

Conditions favoring preservation Rapid burial and possession of hard parts

CORRELATION OF ROCK LAYERS Matching rocks of similar age Fossils succeed one another in a definite order Index Fossils (widespread and short-lived) Fossils are environmental indicators (land or sea)

ABSOLUTE DATING

BASIC ATOMIC STRUCTURE

Protons, Neutrons and Electrons

Atomic number (# of protons)

Mass number (# of protons + # of neutrons)

Isotope (same # of p’s, different # of n’s)

ABSOLUTE DATING

RADIOACTIVITY

Spontaneous breaking apart (decay) of atomic nuclei

TYPES OF RADIOACTIVITY

Alpha Emission, Beta Emission, Electron Capture

GEOLOGIC TIME SCALE GEOLOGIC TIME SCALE

GEOLOGIC TIME SCALE

EONS = Precambrian and Phanerozoic

Precambrian Eon

ERAS = Hadean, Archaen, Proterozoic

Phanerozoic Eon

ERAS = Paleozoic, Mesozoic, Cenozoic

GEOLOGIC TIME SCALE

ERAS OF THE PHANEROZOIC ARE SPLIT

INTO PERIODS

Paleozoic Era (“ancient life”) Periods = Cambrian, Ordivician, Silurian, Devonian, Mississippian, Pennsylvanian, Permian Mesozoic Era (“middle life”) Periods = Triassic, jurassic, Cretaceous Cenozoic Era (“recent life”) Periods = Tertiary, Quaternary

GEOLOGIC TIME SCALE

TERTIARY ANDQUATERNARY

PERIODS ARE SPLIT INTO EPOCHS

Tertiary Period (Paleocene, eocene, Oligocene, Miocene, Pliocene) EPOCHS

Quaternary Period (Holocene and Pleistocene) EPOCHS

GEOLOGIC TIME SCALE

PNEUMONICS

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