Faults: Active, Inactive, and Dip-Slip

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Questions and Answers

What distinguishes an active fault from an inactive fault?

  • Active faults are located deeper within the Earth's crust.
  • Active faults are characterized by horizontal displacement, while inactive faults are characterized by vertical displacement.
  • Active faults have generated an earthquake within the last 10,000 years, while inactive faults have not. (correct)
  • Active faults only experience strike-slip movement, while inactive faults only experience dip-slip movement.

In a normal fault, the hanging wall moves upward relative to the footwall due to compressional forces.

False (B)

What type of force is primarily responsible for the creation of a reverse fault?

Compressional forces

The term used to describe the steepness of a fault surface is known as ______.

<p>dip</p> Signup and view all the answers

Match the fault types with their primary direction of movement:

<p>Dip-Slip Fault = Vertical Strike-Slip Fault = Horizontal Oblique-Slip Fault = Combination of Vertical and Horizontal</p> Signup and view all the answers

Which type of fault is characterized by horizontal movement where the opposite side appears to have moved to the left?

<p>Left-lateral fault (A)</p> Signup and view all the answers

Strike is measured counter-clockwise from north.

<p>False (B)</p> Signup and view all the answers

Besides dip and strike, what are terms of rock that are above and below the fault plane?

<p>Hanging wall and footwall</p> Signup and view all the answers

Movement along a fault is vertical, that is up or down, is know as ______ fault

<p>Dip-slip</p> Signup and view all the answers

Which statement best describes an oblique-slip fault?

<p>A fault that exhibits a combination of both dip-slip and strike-slip movement. (A)</p> Signup and view all the answers

Flashcards

Fault

A fracture in the Earth's crust where movement has occurred.

Active Fault

A fault that has produced an earthquake within the last 10,000 years and may continue to generate earthquakes.

Inactive Fault

A fault showing no signs of earthquake activity in the last 10,000 years, but could potentially generate earthquakes in the future.

Hanging Wall

The rock above the fault plane.

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Footwall

The rock below the fault plane.

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Dip

Describes the steepness of the fault surface.

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Strike

Measurement taken clockwise from north that describes the orientation of the fault line.

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Dip-Slip Fault

Fault where movement is vertical (up or down) along the dip of the fault plane, caused by compressional or tensional forces.

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Normal Fault

Hanging wall moves down relative to the footwall due to tensional forces.

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Strike-Slip Fault

Movement is horizontal (side to side) along the strike of the fault plane caused by shear forces.

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Study Notes

  • Faults are fractures in the Earth's crust.

Active Faults

  • Active faults have generated earthquakes within the last 10,000 years.
  • These faults might still generate earthquakes.

Inactive Faults

  • Inactive faults show no signs of earthquake activity in the last 10,000 years.
  • These faults could still possibly generate earthquakes in the future.

Fault Components

  • The hanging wall refers to the rock above the fault plane.
  • The footwall refers to the rock below the fault plane.
  • Dip describes the steepness of the fault surface.
  • Strike is measured clockwise from north.

Dip-Slip Faults

  • Movement is vertical along the dip of the fault plane.
  • Compressional or tensional forces cause them.

Normal Faults

  • The hanging wall moves down relative to the footwall.
  • Due to tensional forces.

Reverse Faults

  • The hanging wall moves up relative to the footwall.
  • Compressional forces cause them.

Strike-Slip Faults

  • Movement is horizontal along the strike of the fault plane.
  • Shear forces cause them.

Left-Lateral Faults

  • The opposite side appears to have moved to the left.

Right-Lateral Faults

  • The opposite side appears to have moved to the right.

Oblique-Slip Faults

  • These are a combination of dip-slip and strike-slip faults.

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