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Fossil Dating Worksheet

Explore the methods used to determine the age of fossils, including relative and absolute dating techniques, for Grade 10 Science students.

Grade 10 Science BiologyFossil Dating
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Includes

Multiple ChoiceFill in the BlanksShort AnswerTrue / FalseMatching

Standards

HS-LS4-1HS-ESS1-6

Topics

Fossil DatingBiologyScienceGrade 10Relative DatingAbsolute Dating
7 sections · Free to use · Printable
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Fossil Dating: Uncovering Earth's History

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Read each question carefully and answer to the best of your ability. This worksheet covers various aspects of fossil dating, including relative and absolute dating techniques.

1. Which dating method estimates the age of a fossil by comparing its position in rock layers to other fossils?

a

Radiometric dating

b

Carbon-14 dating

c

Relative dating

d

Absolute dating

2. The half-life of a radioactive isotope refers to the time it takes for:

a

All of the parent isotope to decay

b

Half of the parent isotope to decay

c

Half of the daughter isotope to form

d

The fossil to become radioactive

3. The principle of   states that in an undisturbed rock sequence, the oldest layers are at the bottom and the youngest layers are at the top.

4. Carbon-14 dating is effective for dating fossils up to approximately   years old.

5. Fossils that are geographically widespread and existed for a relatively short period are known as   fossils.

6. Explain the difference between relative dating and absolute dating.

7. Describe how the principle of superposition is used in relative dating.

Sedimentary rock layers

8. Absolute dating methods provide an exact numerical age for a fossil.

T

True

F

False

9. Index fossils are useful for relative dating because they lived for a very long time.

T

True

F

False

Match each term on the left with its definition on the right.

10. Half-life

 

a. The process of using radioactive decay to determine a fossil's age

11. Radiometric dating

 

b. The time it takes for half of a radioactive isotope to decay

12. Superposition

 

c. Principle stating that oldest rock layers are at the bottom