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Welcome!!!! Mr. Sandomenico Today you will be able to: Today we will begin a new unit! The Earth’s History!!!!! Utilize the SEVEN rules of rock age identification to describe the geologic age of this rock sequence!

Mr. Sandomenico Welcome!!!!95science.weebly.com/uploads/2/8/0/0/2800658/earth... · Welcome!!!! Mr. Sandomenico Today you will be able to: Today we will begin a new unit! The Earth’s

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Page 1: Mr. Sandomenico Welcome!!!!95science.weebly.com/uploads/2/8/0/0/2800658/earth... · Welcome!!!! Mr. Sandomenico Today you will be able to: Today we will begin a new unit! The Earth’s

Welcome!!!!Mr. Sandomenico

Today you will be able to:

Today we will begin a new unit! The Earth’s History!!!!!

Utilize the SEVEN rules of rock age identification to describe the geologic age of this rock sequence!

Page 2: Mr. Sandomenico Welcome!!!!95science.weebly.com/uploads/2/8/0/0/2800658/earth... · Welcome!!!! Mr. Sandomenico Today you will be able to: Today we will begin a new unit! The Earth’s

Let’s Begin With a Review:How are Sedimentary Rocks formed?How are Sedimentary Rocks formed?

1. Large rocks are ____________ to form smaller rocks.

2 The smaller rocks are downstream by the process of2. The smaller rocks are ________ downstream by the process of ________.

3. As large and angular rocks are carried downstream they become ________ and _________.

4. The higher the river’s __________ the large and more sediment it can carry.

5 O th i h l b d f t th l it f th i5. Once the river reaches a larger body of water the velocity of the river _________.

6. When river velocity decreases, the sediments it was carrying are _________ onto the bottom of the larger body of water.

7 d t th di t t f S di t R k !7. __________ and __________ cement the sediments to form Sedimentary Rocks!

8. Sedimentary rocks are formed in ____________ environments.

Page 3: Mr. Sandomenico Welcome!!!!95science.weebly.com/uploads/2/8/0/0/2800658/earth... · Welcome!!!! Mr. Sandomenico Today you will be able to: Today we will begin a new unit! The Earth’s

Police use clues to help piece h htogether the past.

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Now we are goingNow we are going to be detectives!!!!!to be detectives!!!!!

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #1: Uniformitarianism

- The process we see occurring today most likely occurred in the past

- “The Present is the Key to the Past!”

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Example of UniformitarianismExample of Uniformitarianism

• Continental DriftContinental Drift

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #2: Superposition

Originally sedimentary rocks at the-Originally, sedimentary rocks at the bottom are the oldest and deposited

first

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Example of SuperpositionExample of Superposition

• Deposition ofDeposition of sediments and creation of Sedimentary Rocks

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #3: Original Horizontality

- A rock is always older than the process that changes it.

R b S di t k hi h h- Remember, a Sedimentary rock which has been eroded, folded, faulted or intruded must

h b h i t ll t d fi t!have been horizontally created first!

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Example of Original HorizontalityExample of Original Horizontality

• FoldingFolding

• Faulting

• Intrusions/Extrusions• Intrusions/Extrusions

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #4: Erosion, Folds, Faults, Intrusions and Extrusions areIntrusions and Extrusions are

always younger than the rock it ff teffects.

- Again, a rock is always older than the process that changes itthe process that changes it.

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Example of Younger Folding, F l i d I i /E iFaulting and Intrusion/Extrusions

• FoldingFolding

• Faulting

• Intrusions/Extrusions• Intrusions/Extrusions

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #5: Contact Metamorphism

- If Contact Metamorphism forms on the bedrock around the intrusion, the intrusion is younger than , y g

the rock (the rock is older).

- If Contact Metamorphism does not form on the bedrock around the intrusion, the intrusion is older

than the rock (the rock is younger).

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Example of Contact MetamorphismExample of Contact Metamorphism• The intrusion has a red zone

d i Thi iaround it. This is contact Metamorphism. (The rock is older, the intrusion is younger.)

• The intrusion continued to the surface creating an extrusion.

• Sediment was then deposited on top of the extrusion and does not have contact metamorphism. p(The rock is younger and the extrusion is older.)

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #6: Unconformities

- When erosion occurs, a part of the rock record h b l thas been lost.

- A surface which has been eroded and then buriedburied.

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Example of Contact UnconformitiesExample of Contact Unconformities

• Sediments are deposited and pform Sedimentary Rock.

• Uplift occurs exposing the bottom of the water body.

• Wind and flowing water erode the rock.

• A body of water forms over the area and more depositionthe area and more deposition.

• The erosion which occurred is buried and some of the old deposition is lostdeposition is lost.

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What rules can we follow in order to fi t th f k ?figure out the sequence of rocks?

RULE #7: Unable to tell

- In the ‘real world’ sometimes we just can’t tell which rock is older by these rules (we can use y (

other methods which we will learn later)!

- You will be able to tell the age of the rock sequences I give you for assignments so don’t

t t thi l !even try to use this rule!

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Group WorkGroup WorkSo what is the sequence of the of the rock record in the q

Grand Canyon?

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Group WorkGroup WorkTo help, fill out the order of events for this sequence!p, q