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Geologic Time Review

Geologic Time Review

Assessment

Presentation

Science

12th Grade

Practice Problem

Medium

NGSS
HS-PS1-8, MS-ESS1-4, MS-LS4-1

+4

Standards-aligned

Created by

Schivonne John

Used 10+ times

FREE Resource

20 Slides • 21 Questions

1

media

Geologic Time Review

by Schivonne John

2

Objectives - ​Discovering Earth's History

  • ​Explain the principle of Uniformitarianism

  • ​Describe how geologists use relative dating principles, inclusions and unconformities to help then understand Earth's history.

  • Describe how geologists use correlation of rock layers to interpret the rock record.

3

​Historical Notes ...

Catastrophism

Landscape developed by catastrophes e.g. tornadoes, hurricanes, earthquakes, meteoritic impacts.

Modern geology

Uniformitarianism

Fundamental principle of geology

"The present is the key to the past." Meaning that to be able to determine the different types of geological processes that have occurred in the past, we can observe the geological processes that are occurring in the present.

Geological processes associated with uniformitarianism include weathering, erosion, continental drift, seafloor spreading.​

4

Multiple Choice

Identify the name of the belief system that supported the idea that Earth's landscapes were formed by a series of sudden, powerful events.

1

Uniformitarianism

2

Catastrophism

5

Multiple Choice

Identify the principle of modern geology that is underpinned by the statement "The Present is The Key to The Past."

1

Catastrophism

2

Uniformitarianism

6

Open Ended

What did James Hutton mean by his statement "The Present is The Key to The Past."

7

Open Ended

Identify 3 examples for what could be described as a catastrophic event.

8

Open Ended

Identify 3 examples of different types of geological processes for events that could be described as processes associated with uniformitarianism.

9

Relative Dating

Placing rocks and events in sequence

Principles and rules of relative dating

Law of superposition Oldest rocks are on the bottom

principle of original horizontalitysediment is deposited horizontally

principle of cross cutting relationshipsyounger feature cuts through an older feature

10

​Relative Dating

Principles and rules of Relative Dating

Inclusions – one rock contained within another (rock containing the inclusions is younger)

Unconformities

An unconformity is a break in the rock record

Types of unconformities

Angular unconformity – tilted rocks are overlain by flat-lying rocks

Disconformity – strata on either side are parallel

11

​Relative Dating

Principles and rules of Relative Dating

Unconformities: Types of unconformity

Nonconformity

Metamorphic or igneous rocks below

Younger sedimentary rocks above 

12

Correlation of Rock Layers

Matching rocks of similar age in different regions

Often relies upon fossils

13

Multiple Select

Identify the principles of relative dating

1

Principle of Superposition

2

Law of Original Horizontality

3

Protrusions

4

Principle of Cross-Cutting Relationships

5

Unconformities

14

Multiple Choice

The law that states "in a column of rock, older samples are found further down than younger samples"

1

Law of Cross-Cutting Relationships

2

Law of Superposition

3

Law of Horizontality

4

Law of Absolute Dating

15

Open Ended

Identify the difference between an inclusion and a cross cutting relationship.

16

Open Ended

Define and identify the different types of unconformity (3)

17

​Fossils: Evidence of Past Life

fossils are the ​Remains or traces of prehistoric life   

Types of fossils

• Petrified – cavities and pores are filled with precipitated mineral matter

Formed by replacement – cell material is removed and replaced with mineral matter

• Mold – shell or other structure is buried and then dissolved by underground water

• Cast – hollow space of a mold is filled with mineral matter

18

​Fossils: Evidence of Past Life

Types of fossils

• Carbonization – organic matter becomes a thin residue of carbon

• Impression – replica of the fossil's surface preserved in fine-grained sediment

• Preservation in amber – hardened resin of ancient trees surrounds an organism

19

​Fossils: Evidence of Past Life

Types of fossils

Indirect evidence includes:

• Tracks

• Burrows

• Coprolites – fossil dung and stomach contents

• Gastroliths – stomach stones used to grind food by some extinct reptiles

20

Fossils: Evidence of Past Life

Conditions favoring preservation

Rapid burial

Possession of hard parts

fossils and correlation

• Principle of fossil succession

Fossils succeed one another in a definite and determinable order

Proposed by William Smith – late 1700s and early 1800s   

21

​Fossils: Evidence of Past Life

Fossils and correlation

• Index fossils

Widespread geographically

Existed for a short range of geologic time

22

Multiple Choice

Which type of fossil is formed when water deposits minerals to fill in a space. This fossil has the exact same shape as the original organism?

1

Petrified

2

Imprint

3

Cast

4

Mold

23

Multiple Choice

What type of fossil is formed when mud fills in the hollow spaces around something hard, such as a shell, and then hardens. This results in a hollow space shaped exactly like the original object?

1

Amber

2

Mold

3

Petrified

4

Cast

24

Multiple Choice

This is a fossil in which minerals replace part or all of an organism. making it rock like.

1

Imprint

2

Cast

3

Petrified

4

Amber

25

Multiple Select

Select 2 answers. What does the fossil records tell us?

1

Earth's History

2

Changing Life Forms

3

Age of Earth

26

Multiple Choice

The remains or traces of prehistoric life found in sediment and sedimentary rocks.

1

Fossils

2

Unaltered Remains

3

Altered Remains

4

Carbonization

27

Multiple Choice

A widespread geographically, are limited to a short span of geologicc time, and occur in large numbers.

1

Index Fossils

2

Fossils

3

Fossil Succession

28

Multiple Choice

A fossil that shows the activity of organisms

1

Index Fossil

2

Cast and Mold

3

Preserved Fossil

4

Trace Fossil

29

Radioactivity and Radiometric Dating

Atomic structure reviewed 

Nucleus 

• Protons – positively charged

• Neutrons - Neutral charge

Protons and electrons combined

Orbiting the nucleus are electrons – negative electrical charges

30

Radioactivity and Radiometric Dating

Atomic structure reviewed 

Atomic number

An element's identifying number

Number of protons in the atom's nucleus

Mass number

Number of protons plus (added to) the number of neutrons in an atom's nucleus

Isotope

Variant of the same parent atom

Different number of neutrons and mass number

31

Radioactivity and Radiometric Dating

Radioactivity

Spontaneous breaking apart (decay) of atomic nuclei

Radioactive decay

• Parent – an unstable isotope

• Daughter products – isotopes formed from the decay of a parent

32

Radioactivity and Radiometric Dating

Radioactivity

Radioactive decay

Types of radioactive decay

• Alpha emission

• Beta emission

• Electron capture

33

Types Radioactive Decay

media

34

Radioactivity and Radiometric Dating

Radiometric dating

Half-life – the time for one-half of the radioactive nuclei to decay

Requires a closed system

Cross-checks are used for accuracy

Complex procedure

Yields numerical dates

35

The Radioactive Decay Curve

media

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​Radioactivity and Radiometric Dating

Carbon-14 dating

Half-life of only 5730 years

Used to date very recent events

Carbon-14 produced in upper atmosphere

Incorporated into carbon dioxide

Absorbed by living matter

Useful tool for anthropologists, archeologists, historians, and geologists who study very recent Earth history

37

Multiple Choice

If a sample starts with 100 atoms of an unstable atom, how much will be left after 2 half-lives?

1

75

2

50

3

25

4

20

38

Multiple Choice

 

If there are 25 atoms left from a 100 atom sample of an isotope with a half life of 100 years, how old is the sample?

1

500 years

2

200 years

3

100 years

4

50 years

5

25 years

39

Multiple Choice

A radioactive element has a half-life of 2 days.

What percentage would remain radioactive after 6 days?

1

100%

2

75%

3

50%

4

25%

5

12.5%

40

Multiple Choice

A radioactive element has a half-life of 2 days. If the original mass was 120 grams, how much would have decayed after 6 days?

1

240 grams

2

120 grams

3

60 grams

4

30 grams

5

15 grams

41

Multiple Choice

A radioactive element has a half-life of 2 days. How many half-lives would it experience at 6 days?

1

5

2

4

3

3

4

2

5

1

media

Geologic Time Review

by Schivonne John

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