7.4.c Students know that the rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally.

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How to tell how old the layers of rock are.
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Presentation transcript:

7.4.c Students know that the rock cycle includes the formation of new sediment and rocks and that rocks are often found in layers, with the oldest generally on the bottom.

Relative age- the age of a rock compared to the age of other rocks Absolute age- the number of years since the rock was formed Sedimentary rocks form when sediment is deposited in layers The Position of Rock Layers

Key Concept: According to the law of superposition, in horizontal sedimentary rock layers the oldest layer is at the bottom. Each higher layer is younger than the layers below it. Scientists can’t determine absolute age using the law of superposition but they can get relate age The Position of Rock Layers

Extrusion- lava that hardens on the surface Intrusion- when magma cools and hardens beneath the surface Formation of Igneous Rock Fault- a break in the Earth’s crust Determining Relative Age

Key concept: To determine relative age, geologists also study extrusions and intrusions of igneous rock, faults, and gaps in the geologic record, and inclusions.

Geologists use extrusions, intrusions, or faults to date rocks using the principle of cross-cutting Principle of cross-cutting states that when something cuts across a body of rock, it is younger than the rock it cuts across Geological record of sedimentary rock is not complete Deposition slowly builds layers but some layer erode away exposing older layers, deposition forms new on top of those older layers Determining Relative Age

Unconformity- the surface where new rock layers meet a much older rock surface

Determining Relative Age Unconformity shows a gap in the geologic record because of erosion

Determining Relative Age An unconformity occurs where erosion wears away layers of sedimentary rock

Determining Relative Age Other rock layers then form on top.

Helps date rocks when there is an unconformity Definition- a piece of rock that is contained in another rock Starts as a solid rock piece that breaks off an existing rock and becomes part of another rock The rock containing an inclusion is younger than the rock the inclusion came from Inclusions

Using Fossils to Date Rocks Index fossils- a fossil that is widely distributed and represents a type of organism that existed briefly Key concept: Index fossils are useful because they tell the relative ages of the rock layers in which they occur. Index fossils are used to match up rock layers at locations that may be far apart Ammonites in layer C are index fossils because they: 1.only occur in one layer (existed briefly) 2.are in different locations (widely distributed)