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RELATIVE AGES OF ROCKS Chapter 7-1.

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Presentation on theme: "RELATIVE AGES OF ROCKS Chapter 7-1."— Presentation transcript:

1 RELATIVE AGES OF ROCKS Chapter 7-1

2 James Hutton

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5 Uniformitarianism states that process that are at work today are the same as the processes in Earth’s past

6 What are the three types of rocks?

7 Igneous

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9 Metamorphic

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11 Sedimentary

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14 The physical and chemical breakdown of rocks into smaller pieces
Weathering The physical and chemical breakdown of rocks into smaller pieces

15 Physical Weathering Chemical Weathering
breaks down the rock without changing the mineral (atomic) composition Chemical Weathering changes the mineral (atomic) composition

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20 Physical and Chemical Weathering

21 Physical and Chemical Weathering

22 Sediments that move downhill to lower level where they come to rest.
Transportation Sediments that move downhill to lower level where they come to rest.

23 What are the ways that sediments can move?

24 Different-sized pieces of rock
Clast Different-sized pieces of rock

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27 A B C

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29 A B C

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31 A B C

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33 Deposition Sediments being transported by water, wind, or a glacier slows down and deposits in low lying areas

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35 process of changing sediment into rock
Lithification process of changing sediment into rock

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37 What are the four processes involved in the formation of sedimentary rock?

38 What is the Law of Superposition?

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49 How would a scientist use the Law of Superposition to determine Relative Age?

50 What do these pictures tell you ?

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