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Earth’s Structure. Ryan B., Emmett H., and Coleman S. Earth’s Core . Outer Core and inner core Inner core is solid iron and nickel Outer core is liquid iron surrounding inner Inner core is 9,000 degrees Fahrenheit Outer core is 4,000 to 9,000 degrees . Earth’s Mantle. Hot dense rock
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Earth’sStructure Ryan B., Emmett H., and Coleman S.
Earth’s Core • Outer Core and inner core • Inner core is solid iron and nickel • Outer core is liquid iron surrounding inner • Inner core is 9,000 degrees Fahrenheit • Outer core is 4,000 to 9,000 degrees
Earth’sMantle • Hot dense rock • 1,800 miles • 2 parts • Hot dense rock that flows • Convection currents deal with plate tectonics
Earth’s Crust • 3-5 miles under the ocean • 25 miles under the continents • 1,600 degrees Fahrenheit • Broken into plates above the hot mantle • Subducting and layering rock
Landforms • Types of landforms: valleys, mountains, plateaus, plains • Other types: hills, and glaciers • Mountains rise when crust collides • Plateaus form as magma pushes toward surface • Magma fails to reach surface, building rock • How valleys formed • Plains result from eroded and elevated terrain
Atmosphere • More than the air we breathe • Ozone layer absorbs ultraviolet light • Communication radio waves bounce off • Incinerates meteorites coming towards Earth • Layers: tropos, stratos, mesos, ionos, and exosphere
Earth’s Water • Seal level rising1 to 2 millimeters • Average North American uses 400 liters/ day • About 768 million people don’t have access • 2.5 billion cant access adequate sanitation
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