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Relative and Absolute Dating . By: Mr. Meringolo. Before We Begin… Write down the following questions, answer them throughout the powerpoint. What is relative dating? How can scientist use relative dating based on the formation of sedimentary rock? What is superposition?

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before we begin write down the following questions answer them throughout the powerpoint
Before We Begin… Write down the following questions, answer them throughout the powerpoint
  • What is relative dating?
  • How can scientist use relative dating based on the formation of sedimentary rock?
  • What is superposition?
  • What are three ways in which rock layers can be disturbed?
  • How can relative dating be used to date rocks containing fossils?
  • What is a geological column?
  • Howis a geological column constructed?
relative dating
Relative Dating

Relative Dating is the process of determining whether an object or event is older or younger than other objects or events.

Scientists most commonly use relative dating for fossils and rocks.

This method does not give the age of a rock or fossil in years, it only allows scientists to find out what rock/fossil is older or younger compared to another rock/fossil.

how are undisturbed rock layers dated
How are undisturbed rock layers dated?
  • To find the relative ages of rocks, scientists study the layers in sedimentary form when new sediments are deposited on top of older rock.
  • Over time, different layers of sediment pile up on Earth’s surface. Younger layers pile up on top of older ones. Scientists can use the order of these layers to date the rock of each layer.
superposition
Superposition
  • Superposition is the principle that states that younger rocks lie above older rocks if the layers have not been disturbed.
how are sedimentary rock layers disturbed
How are sedimentary rock layers disturbed?
  • Forces in Earth can disturb rock layers so much that older layers end up on top of younger layers. Some of the ways that rock layers can be disturbed are as follows:
  • Tilting- Earth’s forces move rock layers up and down unevenly
  • Folding- The bending of rocks that can happen when rock layers are squeezed together.
  • Fault- A break or crack in Earth’s crust where rocks can move.
  • Intrusion- An igneous rock that forms when magma is injected into rock and solidifies.
  • Unconformity- A break in the geologic record that is made when rock layers are eroded or when sediment is not deposited for a long period of time.
how are rock layers ordered
How are rock layers ordered?
  • Finding out what happened to form a group of rock layers is similar to piecing together a jigsaw puzzle.
  • The law of superposition and the idea that layers of rock have to be in place before anything can disturb them helps scientists to find out
how are fossils used to determine the relative ages of rocks
How are fossils used to determine the relative ages of rocks?
  • Fossils are the traces or remains of an organism that lived long ago, most commonly preserved in sedimentary rock.
  • Fossil forms of plants and animals show change over time as they evolve. Scientists can classify fossilized organisms based on these changes and as a result can then classify the relative age of rocks in which the fossils are found.
  • Rock that contains fossils of organisms similar to those that live today is most likely younger than rock that contains fossils of ancient organisms.
how are geologic columns used to compare relative ages of rocks
How are geologic columns used to compare relative ages of rocks?
  • Relative dating can also be done by comparing the relative ages of rock layers in different areas. The comparison is done by using a geologic column.
  • A geologic column is an ordered arrangement of rock layers that is based on the relative ages of rocks, with the oldest rocks at the bottom of the column.
  • A geologic column is made by piecing together different rock sequences from different areas to form an ideal image of a rock layer sequence that does not actually exist in any one place on earth.
  • Scientists can compare a rock layer with a similar layer in a geological column that has the same fossils or that has the same relative position.