Chapter 21 - Geologic Time Scale Flashcards

1
Q

Record of earth’s history from its origin (4.6 bya) to present.

A

Geologic time scale

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2
Q

Longest time unit in the geologic time scale.

A

Eon

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3
Q

Informal unit of geological time consisting of the first 3 Eons, during which earth formed and became habitable

A

Precambrian

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4
Q

Second longest time unit in the Geologic Time Scale

A

Era

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5
Q

Third longest time unit in the Geologic time scale

A

Period

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6
Q

Time unit in the Geologic time scale, smaller than a period.

A

Epochs

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7
Q

The theory that geological processes occurring today have been occurring since the earth formed.

A

Uniformitarianism

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8
Q

The age of an object in relation to the ages of other objects

A

Relative age dating

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9
Q

The law that a sedimentary rock layer is older than the layers above it and younger than the layers below it if the layers are not disturbed

A

Superposition

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10
Q

A fault or body of rock is younger than any other body of rock that it cuts though

A

Cross cutting relationships

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11
Q

States that fragments, called inclusions, in a rock layer must be older than the rock layer that contains them

A

Principle of inclusions

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12
Q

A break in the geologic record due to rock layers weathering or sediment not depositing for a long period.

A

Unconformities

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13
Q

The matching of rock outcrops to fossils exposed in one geographic region to similar outcrops or fossils exposed in other geographic regions.

A

Correlation

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14
Q

A rock or sediment layer that serves as a time marker in the rock record.

A

Key-bed

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15
Q

States that sedimentary rocks left undisturbed will remain in horizontal layers

A

Original Horizontaliry

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16
Q

Method that enables scientists to determine the numeric age of certain rocks and other objects.

A

Absolute-age dating

17
Q

Emission of radioactive particles and its resulting change into isotopes over time.

A

Radioactive decay

18
Q

A method of determining the abolition age of an object by comparing the relative percentages of a radioactive (parent) isotope and a stable (daughter) isotope.

A

Radiometric dating

19
Q

The time required for half of a sample of a radioactive isotope to break down by radioactive decay to form a daughter isotope

A

Half-life

20
Q

Determines the age of relatively young organic objects.

A

Radio-carbon dating

21
Q

The science of using tree rings to determine absolute age.

A

Dendrochronoloy

22
Q

Bands of alternating light and dark colored sediments of sand, clay, and silt.

A

Varve