Define in short (with respect to Earth):1. Crust 2. Mantle 3. Core .4. Biosphere 5. Asthenosphere
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The internal structure of Earth is layered in spherical shells: an outer silicate solid crust, a highly viscous asthenosphere and mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core.
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Crust:
- Upper most/ Outer most solid part
- Thinnest of all layers
- Oceanic crust is thinner & younger as compared to the continental crust
- Silicate matter + Aluminium (SIAL)
Mantle:
- Extends from Moho's discontinuity to a depth of 2900 km
- Moho's discontinuity: Boundary between the Earth's crust and mantle
- SIMA (Silica + Magnesium)
- Upper mantle & lower mantle
- Includes Asthenosphere
Asthenosphere:
- Upper portion of the mantle, extends up to 400 km
- Astheno means weak
- Main source of magma
Core:
- Gutenberg discontinuity: Between mantle & core
- Outer core is in liquid state and inner core is in solid state
- Mostly constituted by Nickel, iron (NIFE layer)
- V.high temperature & pressure
- Outer core & inner core
Biosphere:
- Biosphere is that sweet spot where atmosphere, lithosphere and hydrosphere interact and give rise to life
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