Seismic Waves

Page 1: Earthquake Basics

  • Earthquake: A natural phenomenon caused by the movement of the Earth's crust at a fault or crack.

  • Seismic Waves: Energy waves generated by earthquakes that travel through the Earth and can be detected around the world.

Page 2: Seismic Waves Travel Paths

  • Earthquake Epicenter: The point on the Earth's surface directly above where the earthquake occurs.

  • P-Waves and S-Waves:

    • P-Waves (Primary waves) and S-Waves (Secondary waves) exhibit different travel patterns:

      • P-Waves: Travel through both solids and liquids.

      • S-Waves: Only travel through solids.

  • Shadow Zone: Areas (e.g., 102° and 143°) where no waves are detected due to the presence of the Earth's inner composition.

Page 3: Characteristics of P-Waves

  • P-Waves:

    • Characteristics:

      • Primary waves and the first to arrive at a seismic station.

      • Exhibit a push-pull motion (compression).

      • Can travel through solid and liquid mediums.

    • Observation Activity: Make predictions on the appearance and motion of P-waves.

Page 4: Observation of P-Wave Motion

  • Activity: Draw a slinky in your notebook to visualize P-wave motion.

  • Description of Motion: Discuss your observation, enhance, and clarify your description of the motion.

Page 5: Characteristics of S-Waves

  • S-Waves:

    • Characteristics:

      • Secondary waves that follow P-waves.

      • Involve shaking or shearing motion.

      • Travel exclusively through solids.

    • Observation Activity: Make predictions on the appearance and motion of S-waves.

Page 6: Observation of S-Wave Motion

  • Activity: Draw a slinky in your notebook to visualize S-wave motion.

  • Description of Motion: Discuss your observations and improve upon your original descriptions of motion.

Page 7: Comparison of P and S Waves

  • Comparison Activity:

    • Create a Venn diagram or T-chart comparing P-waves and S-waves.

    • Identify which wave travels faster and discuss methods to determine speed.

    • Explore potential damage these waves may cause to the Earth's crust.

Page 8: Wave Medium and Refraction

  • Medium: The material through which a wave travels (liquid, solid, gas).

  • Refraction:

    • The bending of waves as they enter different mediums.

    • Pose the question: Can sound waves bend? Provide evidence for your answer.

Page 9: Energy Transfer in Waves

  • Energy Transfer: Waves transfer energy without transporting matter.

    • Matter: Defined as anything that has mass and occupies space.

    • Stadium Wave Activity:

      • Reflect on whether you moved with the wave or if the wave passed through you while remaining seated.

      • Identify the medium involved in the stadium wave.

Page 10: Exploring Slinkies and Energy Transfer

  • Slinky and String Activity: Discuss how these tools illustrate wave behavior and the concept of energy versus matter.

  • Observation Discussion: Evaluate and explain observations, utilizing evidence to support claims regarding wave behavior.

Page 11: Reflection Questions on Matter and Waves

  • Matter Interaction with Waves:

    • Contemplate how matter reacts when waves pass through it.

    • Develop a new test to demonstrate that waves do not transport matter.

    • Outline methods to collect data and evidence.

Page 12: Speeds of Sound in Different Materials

  • Speed of Sound:

    • Rubber: 60 m/s

    • Air (40°C): 355 m/s

    • Air (20°C): 343 m/s

    • Lead: 1210 m/s

    • Gold: 3240 m/s

    • Glass: 4540 m/s

    • Copper: 4600 m/s

    • Aluminum: 6320 m/s

Layers on the Earth

  • Crust

    • Earths skin

    • Solid layer of rock

    • Dry land and ocean floor

    • Between 5-70 km thick

  • Outer Mantle

    • Molten iron and nickel

  • Inner Mantle

  • Outer Core

  • Inner Core

    • Molten Iron and nickel