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Page 1: Geological faults  student copy

Geological Faults

Page 2: Geological faults  student copy

Objective: By the end of this session you should be able to use

diagrams and examples to describe and explain the different

types of geological faults

Page 3: Geological faults  student copy

Types of Geological Faults

Vertical Movement (Dip-Slip)• Normal (East African Rift Valley)• Reverse (Salt Lake City)Horizontal Movement (Strike-Slip)• Tear Faults (The Great Glen Scotland)• Transform Faults (San Andreas Fault)Thrust Faults• Overfold or Nappe (cliffs Broadhaven

Dyfed)

Page 4: Geological faults  student copy

You have one minute to draw and label a normal fault

Page 5: Geological faults  student copy

Normal FaultsTENSION / Pulling motion = LENGTHENING

Throw = Vertical DisplacementHeave = Horizontal Displacement

H

T

Fault Plane

Fault Scarp

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Upthrow and Downthrow

A UPTHROW

B DOWNTHROW

1. A moved up while B moved down2.3.4.5.

Throw is therefore a RELATIVE position

Give five ways that the blocks could have moved?

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Reverse Faults

Fault Plane

T

H

COMPRESSION / Pushing motion = SHORTENING

Page 8: Geological faults  student copy

Rift Valleys

Graben or Rift Valleys are the result of subsidence between Normal Faults (i.e. TENSION/pulling) Horsts are left upstanding after subsidence on either side.

Fault Scarp

Name a famous rift valley:________________________________________

Page 9: Geological faults  student copy

Strike-slip faults (horizontal faults)

• Tear Faults - the result of shearing forces applied to rocks this can be famously seen at the Great Glen Fault where there is SINISTRAL movement (to the left) of a Granite Intrusion split in two. The opposite of sinistral movement is DEXTRAL movement (to the r_____).

Page 10: Geological faults  student copy

Strike-slip faults (horizontal faults)

• Transform Faults - associated with plate margins. Famously seen at the S___ A____ Fault. These faults are also common at right angles to a mid-ocean ridge. Plate motion can also be seen at transform faults.

Page 11: Geological faults  student copy

Thrust Faults• Intense c__________•Beds so contorted movement can only occur through fracture•Overfold or Nappe moves up and over lower part•A type of reverse fault with an almost horizontal fault plane•Crustal s_________ takes place•Associated with mountain building•Older rocks can be pushed over y_____ rocks•At the Moine Thrust Fault in NW Scotland Pre-Cambrian rocks are found above Cambrian rocks

Nappe

Page 12: Geological faults  student copy

Other Fault Features• Fault Breccia: crushed and broken fragments along

fault planes• Slickenslides: deep grooves along fault planes showing

direction of movement• Gaps along fault planes: often filled with fluids such as

magma giving rise to dykes or hydrothermal solutions carrying minerals (such as veins of galena and fluorite found in the Pennines)

• Erosion: valleys can form along weak fault lines; upthrow can be eroded to the same level as downthrow which can leave misleading geological patterns

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1. Draw and label a Dip-Slip Fault2. Name a specific example of a Normal

Fault3. Is dextral movement to the left or right?4. What types of faults involve Nappes?

What have you remembered?(Blank paper, two minutes!!!)

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What have you remembered?

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Exam Question from Summer 2007

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Mark Scheme for Exam Question

• Specific type of fold/fault e.g. "reverse fault", "anticline" (1)

• Quality of diagram/description (2)• Reference to appropriate scale (1)• Specific location of feature (1)

• Correct name of stress involved (1) R• e.g. Extension/Tension for normal fault, • Compression for reverse/thrust fault or fold• Shear for tear fault