Plate Boundaries and Interactions

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Questions and Answers

What type of fault occurs when a block of Earth's crust pushes upward along the dip angle?

  • Strike-slip Fault
  • Oblique-slip Fault
  • Reverse Fault (correct)
  • Normal Fault

What is the term used to describe the point within the Earth where the rocks break and seismic energy is first released?

  • Epicenter
  • Seismic Center
  • Focus (correct)
  • Hypocenter

Which type of fault involves horizontal movement where two blocks slide past each other in opposite directions?

  • Normal Fault
  • Reverse Fault
  • Strike-slip Fault (correct)
  • Thrust Fault

Which of the following focuses on earthquake preparedness information?

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

What is the depth range of shallow focus earthquakes?

<p>10 to 100 km (A)</p> Signup and view all the answers

What occurs at a divergent plate boundary?

<p>Plates move away from each other (A)</p> Signup and view all the answers

Which geological feature is likely to form as a result of oceanic-continental convergence?

<p>Chain of volcanoes (C)</p> Signup and view all the answers

What type of plate boundary is characterized by plates sliding against each other in opposite directions?

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

Which geological process occurs most commonly along convergent plate boundaries?

<p>Creation of mountain ranges (B)</p> Signup and view all the answers

What is a common consequence for communities living along the Ring of Fire?

<p>High risk of earthquakes and volcanic eruptions (C)</p> Signup and view all the answers

What is formed when two continental plates converge?

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

Which of the following is NOT a feature formed by divergent plate boundaries?

<p>Oceanic trenches (D)</p> Signup and view all the answers

At what average rate do tectonic plates move on top of the asthenosphere?

<p>1 to 10 cm per year (A)</p> Signup and view all the answers

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Study Notes

Plate Boundaries

  • Tectonic plates move on the asthenosphere at rates of 1 to 10 cm per year.
  • Interactions between plates occur through three main types of movement: converging, diverging, or sliding past each other.
  • Plate boundaries are associated with geological features such as faults, rifts, and trenches.

Divergent Plate Boundary

  • Forms when two plates move apart, creating gaps or rifts.
  • Can lead to mid-oceanic ridges, volcanic islands, and rift valleys.
  • Example: Great East African Rift Valley.

Convergent Plate Boundary

  • Occurs when two plates collide, forming subduction zones or orogenic belts.
  • Types of convergence:
    • Oceanic-oceanic
    • Oceanic-continental
    • Continental-continental
  • Results in chains of volcanoes, island volcanoes, oceanic trenches, and mountain ranges.
  • Examples:
    • Mariana Trench (oceanic-oceanic)
    • Andes Mountains (oceanic-continental)
    • Alps and Himalayas (continental-continental)

Transform Plate Boundary

  • Plates slide against each other in opposite directions.
  • Commonly results in earthquakes due to the shifting of rocks.
  • Types of faults associated:
    • Normal Fault: Hanging wall slips downward.
    • Reverse Fault: Earth's crust block pushes upward.
    • Strike-slip Fault: Vertical planes slide parallel in opposite directions. Example: San Andreas Fault.
    • Oblique-slip Fault: Combination of strike-slip and dip-slip motions.

Earthquakes

  • Energy travels through the Earth as seismic waves.
  • Focus (hypocenter) is the initial point of rock breakage within the Earth.
  • Epicenter is located directly above the focus on the Earth's crust.
  • Focus depths can vary:
    • Shallow: 10 to 100 km (causes most damage)
    • Intermediate: 70 to 300 km
    • Deep: 300 km or deeper

Earthquake Preparedness

  • Shallow epicenters lead to concentrated seismic energy and greater damage.
  • Important to have disaster preparedness plans in place, especially for communities along the Ring of Fire.
  • Recommended to develop earthquake response strategies based on local guidelines and resources.

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