Interior of the Earth
ICSE · Class 11 · Geography
Quick revision notes for Interior of the Earth — ICSE Class 11 Geography. Key concepts, formulas, and definitions for last-minute revision.
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Sources of Information About Earth's Interior
- Direct sources: mines, boreholes, and volcanic eruptions provide limited surface-level data
- The deepest mine (Robinson Deep, South Africa) is only 4 km deep; deepest oil drill is about 6 km
- Earth's radius is 6,370 km — making direct observations negligibly small in comparison
Internal Properties: Density, Temperature, and Pressure
- DENSITY: Earth's average density is 5.5 g/cm³ as per Newton's laws of gravity
- Surface sedimentary rocks have density of 2.7; igneous rocks below have 3.0–3.5 density
- Core density is estimated at 11–12, rising to 13–14 at Earth's centre
Earthquake Waves: Types and Characteristics
- Three main types of earthquake waves: P-waves, S-waves, and L-waves
- P-WAVES (Primary waves): Longitudinal waves; particles move in direction of wave propagation
- P-waves velocity: ~8 km/second — FASTEST of all earthquake waves
Behaviour of Earthquake Waves and the Shadow Zone
- Earthquake waves change their course and velocity at boundaries between different internal zones
- Waves suffer REFLECTION and REFRACTION when travelling through different media
- Curved path of waves proves that density increases with depth inside Earth
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