Relative Dating Lecture Notes

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Relative Dating & Deforming the Earth’s Crust

Uniformitarianism

1.

Geologic processes that occurred in the past can be explained

___________________________________________________________________________________________ a.

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

Very slow, gradual, predictable process

Catastrophism

1.

_____________________________________________________________________________ a.

Mountains, canyons and oceans formed during rare events b.

These rare events are called catastrophes

2.

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

Relative Dating

1.

Relative Dating – a method used to determine whether an object or event ______________________________

_______________________________________________________________

Absolute Dating

1.

Absolute Dating – any method used to determine the _______________________________________________

 Certain molecules called Isotopes decay over time

Isotope – An atom that has the same number of protons, _________________________

________________________________________________________________________

 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 decay

Disturbances

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

1.

Unconformity – _______________________________________________________________________ a.

Missing rock layer(s) due to either Erosion or Non-deposition

2.

Deformations – Altering of rock layers after they are laid down, _________________________________

Deformations

 Tectonic plates move, causing stress to build up in the lithosphere a.

Stress = force (three types)

1.

Compression =

2.

Tension =

3.

Shearing =

 Stress from tectonic plates cause rock layers in the lithosphere to change

Folding

Definition: _____________________________________________________________ a) Older rock starts on bottom

Anticline =

Syncline =

 Folds can be large or small

 Some measured in kilometers or centimeters

Faults

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

 Can be seen on the earth’s surface

 Usually have a ___________________________________________________

 Faults, 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?

How do we find Relative Age?

 One way scientists calculate relative age is by using a set of rules

1.

Superposition – if undisturbed, rock layers will always be older as you go down (youngest on top)

2.

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

3.

Cross-Cutting Rule – _________________________________________________________________

__________________________________________________________________________________

4.

Deformation Rule – _________________________________________________________________

__________________________________________________________________________________

 Another way geologists can figure out disturbed layers of rock is with the Geologic Column

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

 Geologic Columns are used to find _____________________________

 When a layer of rock is missing from Erosion or Non-Deposition ________________

____________________________________________________________________

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