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Relative Dating  &  Deforming the Earth’s Crust Relative Dating  &  Deforming the Earth’s Crust

Relative Dating & Deforming the Earth’s Crust - PowerPoint Presentation

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Uploaded On 2018-11-06

Relative Dating & Deforming the Earth’s Crust - PPT Presentation

Folds Faults and Deformities OH MY Uniformitarianism Geologic processes that occurred in the past can be explained by current geologic processes Erosion and weathering that happens today must have been the same millions of years ago ID: 718170

layers rock stress relative rock layers relative stress geologic older erosion disturbed causing age wall missing mountains column time

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Slide1

Relative Dating & Deforming the Earth’s Crust

Folds, Faults and Deformities…

OH MY!!Slide2

UniformitarianismGeologic processes that occurred in the past can be explained by current geologic processes

Erosion and weathering that happens today must have been the same millions of years ago

Very slow, gradual, predictable process

Is this the correct principle?Slide3

CatastrophismGeologic change happens suddenly

Mountains, canyons and oceans formed during rare events

These rare events are called catastrophes

Up until the mid-1800’s, this was the accepted principle

Why was this the accepted principle?Slide4

Modern Geology

Uniformitarianism

Catastrophism

Can

geologic processes take a very long time? (think Tectonic Plates, mountains growing)

YES!

Mountains

forming/growing

Grand Canyon forming from erosion

Moving of

the continents

Can events happen very quickly?

(Think meteor causing dinosaur extinction)

YES!

Large Volcanic eruptions forming islands and causing extinctions

Meteor strikes creating craters and causing extinctions

Earthquakes, Tsunamis,

etc

…Slide5

Relative DatingRelative Dating – a method used to determine whether an object or event is older or younger than another object or event

Who is Older or Younger?Slide6

Absolute DatingAbsolute Dating – any method used to determine the age of an event or object in numbersCertain molecules called

Isotopes

decay over time

Isotope

– An atom that has the same number of protons, but a different number of

neutrons

We can use this decay to measure how old something is (rocks, fossils,

etc

…)

Half-life

– the amount of time it takes for half of a radioactive substance to decaySlide7

DisturbancesUnfortunately not all rock layers are laid out perfectly. Some things that can make things more difficult are…

Unconformity –

missing part of a geologic column

Missing rock layer(s) due to either

Erosion

or

Non-deposition

Deformations

– Altering of rock layers after they are laid down, but not removing themSlide8

DeformationsSlide9

DeformationsTectonic plates move, causing stress to build up in the lithosphere

Stress = force (three types)

Compression = squeeze together

Tension = stretch apart

Shearing = sliding past

Stress from tectonic plates cause rock layers in the lithosphere to changeSlide10

Folding

Definition: bending rock layers due to stress

Older rock starts on bottom

Anticline = upward arch (looks like an

A

)

Syncline = downward, U shaped (think sink)Slide11

SYNCLINE

ANTICLINESlide12

Folding

Folds can be large or small

Some measured in kilometers or centimetersSlide13

MONOCLINESlide14
Slide15
Slide16
Slide17

Faults Definition: surface along which rocks break and slide past each other

Can be seen on the earth’s surface

Usually have a

Hanging wall

and

FootwallSlide18

Type of Stress?Which wall falls down?

Are rock layers disturbed?Slide19

Type of Stress?

Which wall falls down?

Are rock layers disturbed?Slide20

Type of Stress?

Which wall falls down?

Are rock layers disturbed?Slide21

Relative DatingFaults, Unconformities and Deformations raise a very important problem…Rock layers aren’t always perfect

So what do we do when rock layers aren’t perfect?

What happens when they look more like…Slide22

This. How do we find Relative Age?Slide23

Relative DatingOne way scientists calculate relative age is by using a set of rulesSuperposition – if undisturbed, rock layers will always be older as you go down (youngest on top)

Original Horizontality

– Layers of rock are always formed in relatively even horizontal layers

Cross-Cutting Rule

– if there is a fault cutting through layers of rock, the rock must be

older

Deformation Rule

– if there is a deformation (fold, tilt, intrusion) the rock that is deformed must be

olderSlide24

How do we find Relative Age?Slide25

Relative DatingAnother way geologists can figure out disturbed layers of rock is with the Geologic ColumnGeologic Column

– a complete set of the rock layers with all known fossils and layers in their proper order

Geologic Columns are used to find

Unconformities

When a layer of rock is missing from

Erosion

or

Non-Deposition

the geologic column can tell geologists what SHOULD be thereSlide26
Slide27

Which layers are missing from the second outcropping?