Interior of the Earth
Himachal Pradesh Board · Class 11 · Geography
Complete topic list for Interior of the Earth in Himachal Pradesh Board Class 11 Geography. Key concepts, sub-topics, and what to focus on for board exams.
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Topics in Interior of the Earth
Sources of Information about Earth's Interior
- Earth's radius is approximately 6,378 km, making direct observation of the interior impossible
- Direct sources include: mining operations (deepest mines reach 3-4 km), deep drilling projects (Kola project reached 12 km), volcanic eruptions providing magma samples, and meteorite analysis
- Deep Ocean Drilling Project and Integrated Ocean Drilling Project provide valuable data about crustal composition
Earthquakes and Seismic Waves
- Earthquake is the shaking of Earth caused by sudden release of energy along fault lines
- Focus (hypocenter) is the point where energy is released; epicenter is the surface point directly above focus
- All natural earthquakes occur within the lithosphere (up to 200 km depth)
Types of Earthquakes and Measurement
- Tectonic earthquakes: most common, caused by sliding along fault planes
- Volcanic earthquakes: associated with active volcanic areas
- Collapse earthquakes: due to underground mine roof collapse
Structure of Earth's Interior
- Crust: outermost solid layer, brittle nature. Oceanic crust (5 km average), Continental crust (30 km average, up to 70 km in Himalayas)
- Mantle: extends from Moho discontinuity to 2,900 km depth. Upper mantle includes asthenosphere (weak zone, source of magma)
- Lithosphere: crust + uppermost mantle, thickness 10-200 km
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