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8.4 Earth’s Layered Structure I. Layers Defined by Composition A) Earth’s interior consists of 3 major zones (chemical composition). 8.4 Earth’s Layered Structure Defined by Composition 1)Crust • a) Continental crust - Upper crust composed of granitic rocks 8.4 Earth’s Layered Structure 1)Crust • b) Oceanic crust - 1) Basaltic composition - 2) Younger than the continental crust 8.4 Earth’s Layered Structure 2) Mantle • a) Below crust. 3) Core • a) Below mantle • b) Composed of an iron-nickel alloy • c) Really dense 8.4 Earth’s Layered Structure II. Defined by physical properties 1) Lithosphere • a) Crust and uppermost mantle (about 100 km thick) • b) Cool, rigid, solid 8.4 Earth’s Layered Structure 2) Asthenosphere • a)Beneath the lithosphere • b) Upper mantle • c) Soft, weak layer that is easily deformed 8.4 Earth’s Layered Structure 3) Lower Mantle • a) More rigid layer • b) Rocks are very hot and flow like a milkshake. 8.4 Earth’s Layered Structure 8.4 Earth’s Layered Structure 4) Inner Core • a) Behaves like a solid Fe & Ni 5) Outer Core • a) Liquid layer • b) Convective flow of metallic iron within generates Earth’s magnetic field Earth’s Layered Structure 8.4 Earth’s Layered Structure Discovering Earth’s Layers ˇ´ Moho- boundary • Separates crust from underlying mantle Earth’s Interior Showing P and S Wave Paths 8.4 Earth’s Layered Structure Discovering Earth’s Composition Crust • Early seismic data and drilling technology indicate that the continental crust is mostly made of lighter, granitic rocks. Mantle • Composition is more speculative. • Some of the lava that reaches Earth’s surface comes from asthenosphere within.