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Geological Time The Present is the Key to the Past

Geological Time The Present is the Key to the Past

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Page 1: Geological Time The Present is the Key to the Past

Geological TimeThe Present is the Key to the Past

Page 2: Geological Time The Present is the Key to the Past

Interpreting Geologic History

• The Earth was thought to have formed about 4.6 billion years ago.

• Geologists try to put the pieces of the Geologic past back together using several methods.

Page 3: Geological Time The Present is the Key to the Past

Interpreting Geologic History

• Uniformitarianism• Original

Horizontality• Law of

Superposition• Intrusions and

Extrusions• Folds and Faults• Unconformities

Page 4: Geological Time The Present is the Key to the Past

Interpreting Geologic History

• Uniformitarianism – The processes we see today are similar to those that have been taking place throughout geologic time.

“The present is the key to the past.”• Original Horizontality – Rock is

always older than the process that changed it. Ex. Tilting, folding, faulting. Layers were always flat first.

Page 5: Geological Time The Present is the Key to the Past

Law of Superposition

• Rocks found at the bottom of an undisturbed exposure are usually the oldest.

D, K, A, G

Page 6: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

• Melted Rock can often rise and cut through sedimentary layers.

• If the magma solidifies in the earth it will form an igneous intrusion surrounded by contact metamorphism.

• If the magma reaches the surface (Lava) It can form an igneous extrusion.

Page 7: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

Intrusion

Page 8: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

R, Y, C, Z, J

An Intrusion is probably going to be Granite or Gabbro

Page 9: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

Extrusion

Page 10: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

R, Y, C, Z, J

An Extrusion is probably going to be Basalt or Rhyolite

Page 11: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

R, Y, C, Z, J, M

A Buried Extrusion Is Still An Extrusion

Page 12: Geological Time The Present is the Key to the Past

Intrusions and Extrusions

Page 13: Geological Time The Present is the Key to the Past

Faults and Folds

• Faults and Folds are a result of the Earth’s shifting tectonic plates.

• Folds are Bends in the rock layers.• Folds are the EXCEPTION to the law

of superposition.• Faults are cracks where layers are

offset from each other.• REMEMBER: rocks must be older then

the process that alters them.

Page 14: Geological Time The Present is the Key to the Past

Folds

Lets add some heat and pressure

Page 15: Geological Time The Present is the Key to the Past

Folds

Lets Convert the colors to Symbols

Page 16: Geological Time The Present is the Key to the Past

Folds

Lets add some more heat and pressure

Page 17: Geological Time The Present is the Key to the Past

Folds

If a Fold is so extreme that it bends back over itself it is called an Overturn

Lets take a closer look

Page 18: Geological Time The Present is the Key to the Past

Folds

Young

old

Young

Page 19: Geological Time The Present is the Key to the Past

Folds

Page 20: Geological Time The Present is the Key to the Past

Folds

Page 21: Geological Time The Present is the Key to the Past

Faults

R, Y, C, Z, J, M, K

Page 22: Geological Time The Present is the Key to the Past

Faults

Page 23: Geological Time The Present is the Key to the Past

Faults

Page 24: Geological Time The Present is the Key to the Past

Unconformities

• An Unconformity is a buried erosional surface.

• They happen when an area of bedrock is weathered and eroded and then buried again by another layer of sedimentary rock.

• This can happen to any kind of rock; sedimentary, igneous, metamorphic, folded, tilted or faulted.

Page 25: Geological Time The Present is the Key to the Past

Unconformities

Erosional Agent

Page 26: Geological Time The Present is the Key to the Past

Unconformities

Unconformity

Remember!! An unconformity is not an unconformity until it is buried!!

R, Y, C, Z, J, H, P

Page 27: Geological Time The Present is the Key to the Past

Let’s Try Some Relative Age Dating

____ Young____________________________________________________ Old

Page 28: Geological Time The Present is the Key to the Past

Geologic History

• The Geologic Timeline is divided up into different units of time.

• The largest unit is the Eon, often made up of billions of years.

• Each Eon is divided up into Eras.• Each Era is made up of Periods.• Each Period is made up of Epochs.

Page 29: Geological Time The Present is the Key to the Past

Geologic History

• In your ESRT you have a chart that has a timeline of geologic history.

• This chart primarily focuses on New York State.

• It is very important that we understand how to read this chart.

• It includes information about rock type, life-forms, fossils, geologic events and continental layouts throughout geologic history.

Page 30: Geological Time The Present is the Key to the Past

Geologic History

Page 31: Geological Time The Present is the Key to the Past

Geologic History

Let’s try a sample question

During what Period did the earliest birds appear?

Page 32: Geological Time The Present is the Key to the Past

Geologic History

Jurassic

Page 33: Geological Time The Present is the Key to the Past

Radioactive Decay

Page 34: Geological Time The Present is the Key to the Past

Radioactive Decay

• Radioactive Decay refers to the breakdown of unstable elements into stable elements.

Unstable element

Stable Element

Page 35: Geological Time The Present is the Key to the Past

Radioactive Decay

• The rate at which these unstable (radioactive) elements decay is predictable and constant.

• This rate can enable us to perform Absolute Dating.

Page 36: Geological Time The Present is the Key to the Past

Absolute Dating

• Where Relative Age Dating can only give us the age of material as it relates to other material… (which came first, last, before etc…)

• Absolute Dating can give us a measurable value for the age of material.

• This is because of that predictable decay rate called Half-Life.

Page 37: Geological Time The Present is the Key to the Past

Half-Life

• Half-Life is defined as the amount of time it takes for ½ of an unstable (radioactive) element to decay into a stable (daughter/decay) element.

• Only half of the radioactive material will decay per each Half-Life.

• This means that there can never be 0% radioactive material remaining or 100% decay material created.

Page 38: Geological Time The Present is the Key to the Past

Half-Life

Radioactive

Stable

Here we start with 100% Radioactive Material

Page 39: Geological Time The Present is the Key to the Past

Half-Life

Radioactive

Stable

After 1 half-life 50% of the radioactive material has decayed into stable material

Let’s see what happens after the second Half-Life

50% 50%

Page 40: Geological Time The Present is the Key to the Past

Half-Life

Radioactive

Stable

After 2 Half-Life’s the remaining radioactive material has now decayed half way. Only 25% of

the original is remaining.

25%

75%

…and a third

Page 41: Geological Time The Present is the Key to the Past

Half-Life

Radioactive

Stable

After a 3rd Half-Life there is only 12.5% of the original radioactive material remaining.

12.5%

87.5%

Page 42: Geological Time The Present is the Key to the Past

Half-Life

The chart for any Radioactive Material will look like this.