Seismic Waves & Earth's Interior
Distinguish between P-waves (compression, travel through solids and liquids) and S-waves (shear, cannot pass through liquids); explain why a seismic shadow zone exists on the far side of an earthquake; describe how seismologists use wave refraction and reflection to infer that Earth has a solid inner core, liquid outer core, mantle, and crust
Lesson
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Practise the bounded task in Seismic Waves & Earth's Interior; see exact limits before inferring broader coverage.
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Distinguish compression from sideways motion and evidence from inference.
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Practise the bounded task in Seismic Waves & Earth's Interior; see exact limits before inferring broader coverage.
Practise the bounded task in Seismic Waves & Earth's Interior; see exact limits before inferring broader coverage.
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Learning resources
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USGS · Practice link — not the full lesson
Earthquake Hazards Program
Before you open · source notes
Earthquake Hazards Program supports Seismic Waves & Earth's Interior. An adult previews and guides; this is a learning page, not a scored quiz.
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Before you openAsk the learner one fact they learned and one question they still have.
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Public USGS page. An anonymous GET on 2026-11-12 returned HTTP 200 with no login or payment prompt for this URL. Opening the link does not save practice or assess mastery. An adult should preview and guide the learner.
USGS. “Earthquake Hazards Program.” External page; Gakuva does not copy, host, embed, or redistribute materials.
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Check understanding
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“Can your child explain how scientists know Earth has a liquid outer core if nobody has ever drilled that deep — what clues do earthquake waves give us about Earth's hidden interior?”
Curriculum record
- Type
- Conceptual
- Subject
- Science
- Domain
- Volcanoes & Earthquakes
- Age range
- Ages 11–13