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