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Relative Time:

Date post: 31-Dec-2015
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Relative Time:. Ages of events are placed in order of occurrence. No exact date is identified. Ex. WWI and WWII I am the second child in my family. Absolute Time:. identifies the exact date of an event. Ex. 65 Million Years Ago 1990. Finding age with relative time:. - PowerPoint PPT Presentation
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Relative Time: Ages of events are placed in order of occurrence. No exact date is identified. Ex. WWI and WWII I am the second child in my family.
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Page 1: Relative Time:

Relative Time:

Ages of events are placed in order of occurrence.

No exact date is identified. Ex. WWI and WWII I am the second child in my family.

Page 2: Relative Time:

Absolute Time:

identifies the exact date of an event. Ex. 65 Million Years Ago 1990

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Finding age with relative time:1. The Law of Superposition - in a

sequence of undisturbed sedimentary rocks, the oldest rocks will be at the bottom.

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2. The law of cross-cutting relationships – anything that cuts across layers of rock is younger than the rocks that it has intruded into. This applies to faults and igneous intrusions.

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3. The law of included fragments - the fragments that make up a rock are older than the entire sample.

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4. The Law of Folds or Tilts: tilts in rocks are younger than the rocks themselves.

5. Original Horizontality- Rocks are usually deposited flat and level.

6. Cole’s Law-

Thinly sliced cabbage.

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Other Guidelines for figuring out a sequence:

Sedimentary rocks are usually formed under water.

Weathering and erosion usually happen above water (on dry land).

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Contact metamorphism shows that the rock that was changed was there first when the intrusion happened.

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Time for a worksheet

Sequence 1 & 2

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Sequence 1: Uplift & Erosion

1. Limestone deposited

2. Sandstone deposited

3. Shale Deposited

4. Uplift

5. Erosion

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Sequence 2: Faulting

1. Limestone deposited

2. Sandstone deposited

3. Shale deposited

4. Faulting

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Time for another worksheet

Sequence 3 & 4

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Sequence 3: Folding

1. Limestone deposited

2. Sandstone deposited

3. Shale deposited

4. Folding

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By the way…

How can you tell if folding has gone so far as to flip the layers over?

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Sequence 4: Igneous Intrusion

1. Limestone deposited

2. Sandstone deposited

3. Shale deposited4. Igneous Intrusion

Note: contact metamorphism is the same event as the intrusion.

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Formation of an unconformity

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Layers are formed according to superposition.

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Something happens to uplift the areafoldingfaulting, etc.

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Erosion wears away the uppermost layers

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Area submerges and deposition begins again.

Here’s the unconformity


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