Subduction Flashcards

1
Q

What is the cause of the Subduction Mountains?

A

Compressional stress

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2
Q

Where are the Subduction Mountains located?

A

Oceanic subduction zones (Japan)

Continental Subduction zones (Andes)

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3
Q

Forms where ocean crust goes down a trench

A

Accretionary Wedge

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4
Q

Thrust slices pile up over time with the youngest slice added at the ___

A

Base

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5
Q

Are fold and thrust zones unique to subduction?

A

No, it also occurs in a collision

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6
Q

Where the rocks are hotter and can slide a long distance, you get:

A

A fold and thrust belt

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7
Q

A mix of strong and weak rocks make:

A

Both folds and faults

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8
Q

Unique to continental subduction

A

Suspect Terranes

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9
Q

Smaller continents get dragged toward the trench

A

Suspect Terranes

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10
Q

They can’t subduct so they get added on instead

A

Suspect Terranes

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11
Q

When two large continents collide, they make wide and very complicated mountain belts.

A

Collision Mountains

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12
Q

Different compressional folds and faults form at different locations and depths

A

Collision Mountains

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13
Q

Bring ocean rocks to mountain tops

A

Thrust faults

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14
Q

Form deep underground

A

Large recumbent folds

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15
Q

To remove the ocean between two continents what do you need on at least one side

A

Subduction

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16
Q

Volcanic mountains deform rocks before the continents collide

A

Active Margin

17
Q

Quiet and undisturbed until it tries to go down the trench

A

Passive Margin

18
Q

Unique to collision

A

Suture Zone

19
Q

Ultramafic rocks end up smashed between the two continents, marking the former ocean

A

Suture Zone

20
Q

Folds and thrusts form on both sides of the:

A

Suture

21
Q

Deformation is worse on the side that tried to subduct =

A

The former passive margin

22
Q

Result of being under the two plates of collision

A

A much wider and deeper fold and thrust best than in subduction zones

23
Q

Fault blocks appear to rise up as mountains, but they are really sinking

A

Rift valleys

Rifting Mountains

24
Q

Can occur over a narrow or wide region

A

Rifting Mountains

25
Q

Allow valleys to sink along facing foot walls

A

Normal faults

26
Q

Ranges made from basin and range terrain

A

Horsts

27
Q

Basins made by basin and range terrain

A

Grabens

28
Q

One valley breaks through the crust forming a new ocean

A

Typical Rift

29
Q

Hundreds of valleys form but none break through the crust

A

Soft Rifting