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Earth’s Systems . Layers, Rock cycle, Plate tectonics . Earth’s Layers. 4 layers 3 solid and 1 liquid Crust Mantle Outer Core Inner Core. Crust. Not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle. Mantle. Outer Core. Inner Core.
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Earth’s Systems Layers, Rock cycle, Plate tectonics
Earth’s Layers • 4 layers • 3 solid and 1 liquid Crust Mantle Outer Core Inner Core
Crust Not a solid shell; it is broken up into huge, thick plates that drift atop the soft, underlying mantle.
Other important info • Magma: molten beneath the earth’s surface • Lava: Magma on the surface • Magma is a mixture of many minerals
Sea Floor Spreading • Mid Ocean Ridges – underwater mountain chains that run through the Earth’s Basins • Magma rises to the surface and solidifies and new crust forms • Older Crust is pushed farther away from the ridge
Rocks • A rock is a naturally occurring solid mixture of one or more minerals, or organic matter • Rocks are classified by how they are formed, their composition, and texture • Rocks change over time through the rock cycle
Igneous Rocks “Fire Rocks” Coarse-Grained Fine-Grained Felsic Granite Rhyolite Mafic Gabbro Basalt
Sedimentary Rocks “Sandwich Rocks” • Sedimentary rock is formed by erosion • Sediments are moved from one place to another • Sediments are deposited in layers, with the older ones on the bottom • The layers become compacted and cemented together
Metamorphic Rocks “Changing Rocks” • Meaning to change shape • Changes with temperature and pressure, but remains solid • Usually takes place deep in the Earth