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Comparing the Layers of Earth S6E5.a. Earth’s layers are compared by: • Temperature • Density – (the thickness or depth of the layer) • Composition – What each layer is made of or how it is described Which is the outermost layer? THE CRUST Temperature: Temp of the air outside to 1600 °F Density: 5km – 70km thick The Crust: What’s it made of? • 2 types of crust: – Oceanic – mostly basalt rocks The thinnest crust – Continental – mostly granite rocks The thicker crust What do you find on Earth’s crust? • • • • Rocks Mountains Soil Water • What else??? Where the Crust ends and the Mantle begins is an area called the MOHO Discontinuity. 1909: Andrija Mohorovicic discovers the moho discontinuity, which is the boundary between Earth’s crust and mantle. Next is the Mantle… • Mantle Temperature range: From 1600 °F to 6700 °F • Density of the WHOLE Mantle = 2867 km! –Let’s break it apart! The Mantle • Made of 3 distinct areas: –Lithosphere –Asthenosphere –Lower Mantle Mantle’s Lithosphere • Density = approx 100 km • Composition: –Rigid layer –Rocky like Crust –“Lithos” means “Stone” • Unique? Made up by part of the Crust! Mantle’s Asthenosphere • Density = 300 km • Composition: – Plastic-like – Solid, but softer – “Asthenes” means “weak” – Unique? Makes the plates move! Because it’s slowly flowing. Lower Mantle • Density = 2467 km • Composition: – Solid Unique? Semi-rigid Gutenberg Discontinuity Where the Mantle ends and the Outer Core begins is an area called the GUTENBERG DISCONTINUITY Outer Core • Temperature = 6700 °F to 7800 °F • Density = 2266 km • Composition: – Liquid, Molten Metal (Fe & Ni) What makes the Outer Core unique? • Creates Earth’s magnetic field • High temps from the formation of the planet keep the Iron (Fe) & Nickel (Ni) liquid Inner Core • Temperature = 7800 °F to 13000 °F HOTTEST LAYER!!! • Density = 1216 km • Composition: – Dense, solid metal ball of Fe & Ni! What’s unique about the Inner Core? • Extreme pressure squeezes the atoms of the Fe & Ni so much, they cannot spread out! • Stays solid!