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Relative Dating in Geology

Explore the principles of relative dating used to determine the chronological order of geological events.

Grade 10 Science Earth & Space ScienceRelative Dating
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Multiple ChoiceFill in the BlanksShort AnswerTrue / False

Standards

HS-ESS1-6

Topics

Relative DatingGeologyEarth ScienceStratigraphy
6 sections · Free to use · Printable
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Relative Dating in Geology

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Read each question carefully and answer to the best of your ability. Refer to the provided diagrams where applicable.

1. Which principle states that in an undisturbed sequence of sedimentary strata, the oldest layer is at the bottom and the youngest is at the top?

a

Principle of Cross-Cutting Relationships

b

Principle of Superposition

c

Principle of Original Horizontality

d

Principle of Faunal Succession

2. An igneous intrusion cuts through existing sedimentary layers. According to the Principle of Cross-Cutting Relationships, which is older?

a

The igneous intrusion

b

The sedimentary layers

c

They are the same age

d

Cannot be determined

3. The Principle of   states that sedimentary layers are originally deposited in horizontal or nearly horizontal layers.

4. An unconformity represents a gap in the geologic record, often due to erosion or a period of non- .

5. Observe the image below of sedimentary layers. Based on the Principle of Superposition, identify the oldest and youngest layers.

Sedimentary Layers

Oldest layer:  

Youngest layer:  

6. Explain how index fossils are used in relative dating.

7. The Principle of Original Horizontality can be used to infer that tilted sedimentary layers have been disturbed after their deposition.

T

True

F

False

8. Relative dating provides a numerical age for geological events.

T

True

F

False