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Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

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Page 1: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Earth’s Geologic History

Aim: How do we determine the chronology of earth’s

events?

Page 2: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Vocabulary

Uniformitarianism Relative Age Horizontality Superposition Chronology Intrusions Extrusions Inclusions

Correlation Unconformity Index fossils

Page 3: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Uniformitarianism Processes going on today also took

place in the past Ex. - Weathering, erosion, deposition,

earthquakes, volcanoes The processes layering sedimentary

rocks today also occurred in the past

Page 4: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Relative Age of Layers Original

Horizontality – sediments are deposited in parallel, horizontal layers.

Superposition- undisturbed layers will have the oldest on the bottom and youngest on top

Page 5: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

How can the older layers end up on top? Faulting Folding Crustal Uplift

Page 6: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Intrusions

Magma forcing its way into cracks and solidifying into igneous rock

The surrounding rock is older than he intrusion.

Page 7: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

What is the sequence of events?1. Formation of sedimentary rock layers

3. Intrusion of igneous magma into the sedimentary rock

4. Contact metamorphism where magma meets sedimentary rock layers

2. Movement / uplift along the fault

Page 8: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Extrusions

Magma that surfaces and solidifies The rock layers below the extrusion are older than the extrusion.

Another layer of deposition can lay more sedimentary rock above the extrusions… which would then be younger than the extrusion

Page 9: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Order of events:

Page 10: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Name them oldest to youngest:

Page 11: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

1 Shale is older than basalt intrusion

2 Shale is older than sandstone

3 An unconformity exists directly under the shale.

Page 12: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Sediments and cracks Sediments have been weathered,

eroded and deposited before they became part of a larger rock.

The sediments must be older than the rock.

Cracks, joints and veins form after the rock

Page 13: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Inclusions If a sediment falls into lava, it may

become included if it does not melt. The inclusion is older than the lava.

Page 14: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Correlation ( co-relation)

Matching rocks in one area with rocks in another area helps determine history of events on Earth.– Comparison of rocks –walking the outcrop– Matching up layers of rock separated over

time

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Page 17: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Correlation

Index fossils– Similar fossils that existed for a brief period of time

but appear in layers of rock (strata) all over the world .

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Page 21: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Matching up index fossils helps correlate layers of rock and age them.

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Which layers are the same age?How old are they? (ESRT pg 8/9)

Page 23: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Correlation

Volcanic Ash or Meteorite Debris– A thin layer of fine

sediment spread over the Earth that settles and is trapped between layers of rock

Page 24: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Volcanic Ash layer

Page 25: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Layer of Meteorite Debris

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VOLCANIC ASH LAYER AT THE SAME TIME AS THE DINOSAURS BECAME EXTINCT LEAD SCIENTISTS TO LOOK FOR METEORITE CRATER Chicxulub Crater 65 mya 170 km. Wide

Page 27: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Unconformities – something is missing

Layers of exposed rock get eroded and leave gaps in the geologic record

Four steps to unconformity:– Uplift– Erosion– Subsidence (submergence)– Deposition

Page 28: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Four steps to unconformity

Page 29: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Missing info in the rock layer

Page 30: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Types of unconformities

Angular – tilted or folded layers that have been eroded and recovered

Parallel – also called disconformities, parallel layers separated by an erosional surface

Nonconformities – sedimentary layers deposited on top of eroded igneous layers

Page 31: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?
Page 32: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Grand Canyon Geology

Page 33: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

HW: Youtube review

Relative Dating of the Earth http://www.youtube.com/watch?v=gFtd

O7woJ3I&feature=related

Page 34: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

What is the correct order of development from oldest to youngest?

Do Now:

Page 35: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Bedrock outcrops A and B are located at two different locations along the Genesee River in western New York State. Rock layers 1, 2, and 4 are the same in both outcrops.

Which statement best explains why rock layer 3 is missing from outcrop B?(1) A fault exists between outcrops A and B.(2) Erosion created an unconformity between rock layers 2 and 4 in outcrop B.(3) A volcanic eruption destroyed rock layer 3 in outcrop B.(4) Metamorphism of outcrop A created rock layer 3.

Page 36: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Earth’s Geological History

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Page 38: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Arrange the order of the following time measurements from biggest to smallest: Year Second Epoch Era Minute Hour Month Eon Period Century Decade Day

Page 39: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

ESRT: page 8/9

How old is the Earth? 2 eons….which one are we in now? Identify the era, period and epoch we

are currently living in. How many eras ago did our current

epoch begin?

Page 40: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Eurypterus… a NY State Index Fossil

Find me on the ESRT pg 8-9.

Page 41: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Using index fossils on the ESRT

What period did Eurypterus live? What era? What eon? How many years ago? What was happening with life on earth? What was happening in NY State?

Page 42: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Index fossils – Page 8-9 ESRT

Index fossils –any animal or plant that is characteristic of a particular span of geologic time or environment.

2 criteria to be an index fossil: Life form lived over a wide geographic

area – horizontal distribution Life form existed for a short period of

time – short vertical distribution

Page 43: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Location A

Location B

Location C

Rock layer 1

W W W Z

Rock layer 2

W Z

Y Z

Rock layer 3

W X X X Z

Which letter would make a good index fossil?

Page 44: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Which graph shows the relative duration of geologic time for the Precambrian, Paleozoic, Mesozoic, and Cenozoic time intervals?

Page 45: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

What is the geologic age of layer B?(1) Cambrian (3)

Devonian(2) Ordovician (4)

Permian

Page 46: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

Evolution of life of Earth

http://www.johnkyrk.com/evolution.html

Page 47: Earth’s Geologic History Aim: How do we determine the chronology of earth’s events?

HW: Youtube review

Age and events of the earth – pg. 8http://www.youtube.com/watch?v=dmUpOYvxiZw&feature=related

Index fossils – pg. 9http://www.youtube.com/watch?v=5fbx4TBIZPE&feature=related

Linking pgs. 2,3,8,9http://www.youtube.com/watch?v=dmUpOYvxiZw&feature=related