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Download Structure of the Earth
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Structure of the Earth What are the layers of the Earth Crust Thin layer of rock Surrounds Earth like a shell surrounds an egg Two types of crust Continental crust Makes up the continents and some major islands Oceanic crust Makes up the ocean floor Between 6-70 km thick (about 3.7 – 43.5 miles) Furthest we have ever been in 12.3 Km (7.6 miles) – This is 0.2% of the way there Two Kinds of Crust Continental Crust Thicker of the two Less Dense Composed mostly of Granite Avg. of 20 – 40 Km thick (12 – 24.9 Miles) Oceanic Crust Thinner of the two More Dense Composed mostly of Basalt Avg. of 6 – 11 Km thick (3.7 – 6.8 Miles) Mantle Thickest Layer of Earth Made mostly of Hot Molten Rock Very, Very top is cool ridged rock About 2900 Km (1802 miles) 870 – 4400 C (1598 – 7952 F) Outer Core Layer of liquid metal Iron & Nickel 2300 Km (1429 Miles) 4400 – 6100 C (7952 – 11,012 F) There is more pressure than the mantle but less pressure than the inner core Inner Core Solid ball of metal Iron & Nickel 2400 Km in diameter (1491 Miles) 7000 – 8000 C (12,632 – 14,432 F) Extreme pressure keeps it solid Densest layer of the Earth Lithosphere Made up of the crust and very top rigid part of the mantle This is what the tectonic plates are made of Most plates have both continental and oceanic crust On continents it is believed to be an average of 150 Km (93 miles) In ocean it is believe 50-100 Km (31 – 62 miles) Asthenosphere The hot soft layer of molten rock in the middle mantle on which the lithosphere rests Flows slowly like hot tar Estimated to be 85- several hundred Km thick (50 – several hundred miles)