STRESS, FAULTS, AND FOLDS Flashcards

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1
Q

is the bending, tilting, and breaking of the Earth’s crust. Plate tectonics is the major cause of crustal deformation.

A

Deformation

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2
Q

Thicker and heavier crust sink deeper into the mantle where thinner and lighter crust will rise higher on the mantle.

A
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3
Q

Isostasy is the rising or settling of a portion of the Earth’s lithosphere that occurs when weight is removed or added in order to maintain equilibrium between buoyancy forces that push the lithosphere upward and gravity forces that pull the lithosphere downward.
Equal stand still

A

Isostasy

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4
Q

The up and down movement of the crust to reach isostasy. During this adjustment the rocks in the crust are bent causing deformation.

A

Isostatic adjustment

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5
Q

There are 3 basic kinds of stress that the isostatic adjustment causes

A

Compression, Tension, Shearing

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6
Q

occurs when crustal rocks are squeezed together.

A

Compression

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7
Q

occurs when crustal rocks are squeezed together.

A

Compression

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8
Q

the force that pulls rocks apart. Here rocks tend to become thinner.

A

Tension

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9
Q

pushes rocks in opposite directions. rocks bend, twist and break.

A

Shearing

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10
Q

The result of stress are

A

Folding and faulting.

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11
Q

When a rock has stress put on it and does not break it is called. appear as wave-like structures in rock layers. Some are small and can be seen in individual rocks and some folds are huge and can only be seen from the air.

A

Folding

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12
Q

The 3 general types of folds

A

Anticlines
Synclines
Monocline

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13
Q

Rocks don’t always bend, sometimes they break. When the rock moves and breaks it is called

A

Fault

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14
Q

The side that is above the fault plane is called the

A

Hanging wall

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15
Q

When the hanging wall moves down it is called. occur in places where there is tension or the rocks are being pulled apart.

A

Normal fault

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16
Q

When the hanging wall moves up it is called. are caused by compressional forces.

A

Reverse fault

17
Q

A low angle reverse fault is called a because one side is being thrust onto the other.

A

Thrust fault

18
Q

faults slide horizontally past one another.

A

Strike-slip fault

19
Q

If you are looking across to the other side of a strike-slip fault and that side moves to the left of you it is called a left lateral strike-slip fault. Strike-slip faults occur in and around transform plate boundaries like where we live near the San Andreas fault. This is also where shearing takes place.

A