GEOLOGIC TIME SCALE
Absolute Dating
Relative Dating
Geologic change over time
Vocab
100

About how old is Earth?

4.6 billions years 

100

What kind of isotopes do parent isotopes break down into?

Daughter isotopes.

100

 Define relative dating.

 Relative dating is used to find if one object or event is older or younger than another.

100

 Define fossils.

Fossils are the traces or remains of organisms that lived long ago.

100

Climate

The weather conditions in an area over a long period of time.

200

What epoch do we currently live in?

Holocene

200

Define absolute dating

Absolute dating is a measure of the age of an event or object in years.

200

Explain the law of superposition. 

The law of superposition states that an undisturbed sedimentary rock layer is older than the layers above it and younger than the layers below it.

200

Describe the ways organisms can be preserved as fossils.

 Organisms become fossilized by being buried in rock, frozen, trapped in amber or asphalt, or petrified.

200

Ice core

A long cylinder of ice obtained from drilling through ice caps or ice sheets; used to study past climates.

300

What is uniformitarianism?

The same geologic processes have occurred in a uniform manner throughout geologic time, and the rate of change was relatively slow and constant.

300

Define index fossil.

An index fossil is a fossil that is distinct, abundant, and widespread for only a short period of geologic time.

300

Define unconformity.

 An unconformity is a gap in the geologic record caused by erosion or a pause in deposition.

300

 List examples of trace fossils

Trace fossils include tracks, burrows, and coprolites.

300

Geology

The scientific study of the origin, history and structure of the Earth and the processes that shape Earth.

400

What is catastrophism?

Sudden, rapid, and devastating geologic processes brought about geologic change.

400

 Explain radiometric dating

Radiometric dating is used to determine an object’s age by comparing the percentages of parent and daughter isotopes.

400

Explain how scientists can use fossils to determine the relative age of rock layers. 

A rock layer that contains a fossil of an earlier life form is relatively older than a rock layer that contains a fossil of a more recent life form.

400

Describe and give evidence for the movement of continents over time.

The continents have been moving throughout Earth’s history. At one time, they formed a single landmass, which is evident by the shapes of continents and the distribution of rock types, mountains, and fossils.

400

Unconformity 

A break in the geologic record created when rock layers are eroded or when sediment is not deposited for a long time. 

500

What is the geologic time scale?

The method used to divide Earth's History into parts.

500

How can we determine how old Earth is?

Earth’s age has been determined by using radiometric dating techniques on rocks from the moon and from other parts of the solar system, such as meteorites, that were formed when the solar system was forming. 

500

Define geologic column.

A geologic column is an ordered arrangement of rock layers based on their relative ages that is used to identify the relative ages of rock layers that are located in different regions.

500

List types of evidence that support that Earth’s climate has changed over time.

 Ice cores, sea-floor sediments, and tree rings provide evidence that Earth’s climate has changed over time.

500

Geologic column

An ordered arrangement of rock layers that is based on the relative ages of the rocks- older at the bottom, younger at the top.