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RELATIVE AGES OF ROCKS Chapter 7-1
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James Hutton
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Uniformitarianism states that process that are at work today are the same as the processes in Earth’s past
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What are the three types of rocks?
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Igneous
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Metamorphic
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Sedimentary
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The physical and chemical breakdown of rocks into smaller pieces
Weathering The physical and chemical breakdown of rocks into smaller pieces
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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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Physical and Chemical Weathering
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Physical and Chemical Weathering
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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.
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What are the ways that sediments can move?
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Different-sized pieces of rock
Clast Different-sized pieces of rock
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A B C
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A B C
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A B C
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Deposition Sediments being transported by water, wind, or a glacier slows down and deposits in low lying areas
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process of changing sediment into rock
Lithification process of changing sediment into rock
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What are the four processes involved in the formation of sedimentary rock?
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What is the Law of Superposition?
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How would a scientist use the Law of Superposition to determine Relative Age?
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What do these pictures tell you ?
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