Folding and Faulting Flashcards

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1
Q

Tectonic forces that change the rock structure on the earth

A

TENSION, COMPRESSION, SHEARING

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2
Q

Tension

A

Plates separate and lengthen or stretch and break apart

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3
Q

Compression

A

Plates collide, rocks are squeezed and shortened causing them to fold or fracture

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4
Q

Shearing

A

Plates slide past eachother

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5
Q

Process of folded structures

A

Continental plate is compressed by forces acting on both sides, flat body of rock buckles, doesn’t fracture due to flexibility of plates and time scale (long time)

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6
Q

Anticline

A

Layers of rock that fold upwards

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7
Q

Syncline

A

Layers of rock that fold downwards

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8
Q

Limb

A

Sides of the fold that join anticline and syncline

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9
Q

Symmetrical fold

A

Limbs on each side are the same in length and steepness

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10
Q

Asymmetrical fold

A

Limbs on either side are different in length/steepness

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11
Q

Overfold

A

One limb pushes over the top of the other

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12
Q

Recumbent fold

A

When both limbs are moving in same direction causing large overhang

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13
Q

Orogeny

A

Mountain building period caused by folding and faulting e.g Caledonian

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14
Q

Trend

A

General direction in which something is developing

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15
Q

Denudation

A

The breakdown of rock by weathering or erosion

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16
Q

Caledonian folding

A
  • 400M years ago
  • Ocean floor subducted and sea floor buckled up
  • Magma intruded into gaps in unfolds to form igneous rocks and metamorphic rocks
  • Large crystals formed
  • ORIGINALLY higher than any other
17
Q

Armorican Folding

A
  • 250 million yrs ago
  • East to west directional trend
  • Never reached the height of Caledonian folding
  • Caha Mountains or Comeraghs
18
Q

Alpine folding

A
  • Reached peak 30M years ago
  • Subduction didn’t occur
  • Current highest mountains
19
Q

Faulted Structures

A

Compression, tension leads to fractures and weakness, strata displaced at fault line

20
Q

Case study: East African Rift Valley

A
  • 20M yrs ago
  • 4,800km from Syria to Zambezi river
  • Magma plume caused continent to bulge
  • Rift valley formed
  • Subsided land is 153m below sea level
  • Widens at 4mm per year
  • Eventual split of plate
  • Mt. Kilimanjaro formed due to Magma rising through weakness in rock
21
Q

Faults resulting from compression
- Reverse Fault

A

Forms at convergent plate boundaries when compression in the earth’s crust causes fractures.

22
Q

Compression: Thrust Fault

A

Found in areas where one plate is being subducted under another, fault at 45° or less

23
Q

Compression: Block Mountain or Horst

A

Compression creates two parallel faults and a large block of land between faults gets pushed upwards.

24
Q

Shearing: Tear Fault

A

Occurs at transform boundaries where rocks at edge of plate can lock. Earthquakes can occur

25
Q

Others: Dome structures

A

Layers of rock arch upwards to form a circular structure called a dome. This happens when a compressional force is exerted on a plate, or when rising magma raises rock upwards. E.g Slieve Blooms

26
Q

Other: Horizontal Structures

A

Uplifted without any tilting, folding or faulting. Can be easily seen in sedimentary rocks e.g loop head

27
Q

Other: Uniclinal Structures

A

Uplifted on one side and not the other e.g Ben Bulben