Relative Dating

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Relative Dating

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Relative Dating. Relative Dating. Relative Age : the age of something compared to something else. Absolute Age : the actual age of a rock or an event . The Principal of Superposition. In undisturbed sedimentary rock layers (strata), the oldest rock is at the bottom. . - PowerPoint PPT Presentation

Transcript of Relative Dating

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Relative Dating• Relative Age: the age of something compared to

something else.

• Absolute Age: the actual age of a rock or an event

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The Principal of Superposition• In undisturbed sedimentary rock layers (strata),

the oldest rock is at the bottom.

YOUNGEST rock layer

OLDEST rock layer

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Dating Intrusions, Extrusions, & Inclusions

• Intrusion: when magma squeezes into preexisting rocks and cools.– YOUNGER than any rock it cuts through

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Dating Intrusions, Extrusions, & Inclusions

• Extrusion: when lava flows on the SURFACE and cools.– YOUNGER than rocks beneath it– OLDER than rocks above it.

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Dating Intrusions, Extrusions, & Inclusions

• Inclusion: a piece of older rock within igneous rock.

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Cross-Cutting Relationships• Types of Cross-cutting relationships: Intrusions,

faults, veins, etc. – These features are YOUNGER than the rocks they cut

across.

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Cross-Cutting Relationships A fault is younger than

the rock layers it cuts across

An igneous intrusion is younger than the rockit penetrates

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The folding and tilting of rock layers are events that are younger than the rock layers

they effect.

Dating Rock Features

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Unconformity – A surface of erosion between rock layers that represents a missing gap in Earth’s history.

Deposition Uplifting and folding

Erosion SubsidenceUnconformity

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Correlation• The process of showing that rock layers, or

geologic events, from different places are the same, or similar in age.

• Types of Correlation:1. Exposed bedrock2. Similarities in Rocks3. Use of Index Fossils4. Volcanic Ash or Meteorite Deposits

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1. Correlation by Exposed Bedrock• Bedrock is usually

covered with soil, but can occasionally be exposed.– Correlation can be

accomplished by directly following the rock layers.

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2. Correlation by Similarities in Rocks• Rocks can be correlated by having similar

appearance, color, mineral composition, and rock sequence.

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3. Correlation by Index Fossils• Index Fossil: a fossil that is used to date the rock

layers in which it is found.1. An organism that lived during a relatively short,

well-defined time span.2. Have a wide distribution geographically.

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Which of these is an INDEX FOSSIL?

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4. Correlation by Volcanic Ash and Meteorite Deposits• Volcanic Ash: ash from each volcanic eruption has

unique composition– Ash deposits are widely distributed, and represent a

small period of time.

• Meteorite Deposits: rock particles and debris produced by an asteroid, comet, or meteorite impact can cover large areas of Earth.

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“SEQUENCE OF EVENTS”PRACTICE WORKSHEETS

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Sequence 1: Uplift & Erosion

1. Limestone deposited2. Sandstone deposited3. Shale Deposited4. Uplift5. Erosion

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1. Limestone deposited

2. Sandstone deposited

3. Shale deposited4. Faulting

Sequence 2: Faulting

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Sequence 3: Folding

1. Limestone deposited2. Sandstone deposited3. Shale deposited4. Folding

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Oldest- Limestone

Youngest- Igneous Intrusion

Oldest- Shale

Youngest- Siltstone

Oldest- Sandstone

Youngest- Shale

Oldest- Sandstone

Youngest- Igneous Intrusion

Oldest- Shale

Youngest- Folding

Oldest- Shale

Youngest- Fault

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3

456

Folding

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6(erosion)7

1

23

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1

2

34

5 1

2

34

5

6 12

3

4

5

6

5(tilting)

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