4 Geography · 4.1.2 Interior of the Earth and plate tectonics
4.1.2.1 Interior of the Earth: crust, mantle, core and discontinuities
The Earth is layered like an onion: a thin rocky crust, a thick solid but slowly flowing mantle, and an iron–nickel core whose outer part is liquid and inner part solid; we know this mostly from indirect evidence, above all seismic waves.
- APPSC Group 1
- Advanced level
- 8 min read
- Full course
Key terms
- crust
- mantle
- core
- lithosphere
- asthenosphere
- Moho
- Gutenberg
- Lehmann
- Conrad
- sial
- sima
- nife
- gravity anomaly
- Kola borehole
- direct and indirect sources
What this note covers
- Core factsFoundation
- ExplainedStandard
- DeeperAdvanced
- Mains writingMains writing
- Common trapsFoundation
- Quick revisionFoundation
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