· 370-372. 2, I. A. .tor., Nev- BIBLIOGRAVíA Math. soc. (1920), Created Date: 12/11/2009 2:16:50 PM
The Earth’s Interior Glencoe Ch. 12-3 Pages 370-372.
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Transcript of The Earth’s Interior Glencoe Ch. 12-3 Pages 370-372.
The Earth’s InteriorThe Earth’s Interior
Glencoe Ch. 12-3 Glencoe Ch. 12-3
Pages 370-372Pages 370-372
A look inside the EarthA look inside the Earth
EEaarrtth’h’ss CCrroossss--sseeccttiioonn
Layers of the EarthLayers of the Earth- Crust –________________ and
__________________ layer
2 types
of crust
Layers of the EarthLayers of the Earth
1. Oceanic crust – under ______________, 4-7 km thick (high density)
2. _____________________ crust – under
continents, ___-____ km (lighter in density)
EEaarrtth’h’ss CCrroossss--sseeccttiioonn
Layers of the EarthLayers of the Earth
- Mantle – _____________ km thick - rock
- Upper mantle – ________________ rock (closer to surface)
- ________________ mantle – plastic rock (___________ magma)
Layers of the EarthLayers of the Earth
Lithosphere – _____ and solid upper mantle
solid and rocky
• Asthenosphere – soft and plastic __________mantle
_______, _______, ________ rock and magma
Layers of the EarthLayers of the Earth
Layers of the EarthLayers of the Earth
- _______________ – the innermost / center of the Earth
- thought to be made of ___________ and ______________
1. Outer core – _______________ metal
2. Inner core – _______________ metal
EEaarrtth’h’ss CCrroossss--sseeccttiioonn
Layers of the EarthLayers of the Earth
- As you go toward the Earth’s core the temperature steadily ______________- Evidence –1. Radioactive decay of unstable _______2. Heated liquid rock in mantle3. Heated solid and liquid metal in core
heat is radiated outward toward the surface