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Natural, solid earth materials made up of minerals |
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Igneous, Metamorphic and Sedimentary. Classified by how they are formed. |
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Molten rock inside the earth?
Molten rock on the earth's surface? |
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Forms when molten rock cools and solidifies. Has crystals, gas bubbles, no layers. Ex. basalt (Hawaiian Islands), obsidian |
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Cools INSIDE the earth (cools slower/larger crystals) |
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Cools OUTSIDE on the earth's surface (cools faster/smaller crystals) |
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Forms deep under the surface from heat and pressure (chemical change) inside the earth. Has layers (foliations) and crystals. Ex. gneiss, marble, slate |
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Forms on the surface when sediments (rock particles- sand, mud, pebbles, minerals) compact and cement. Has layers and can contain fossils. Ex. sandstone, limestone, coal |
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A natural process that slowly breaks apart or changes rock. Heat, water, wind, living things, and other natural forces cause weathering. |
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Fossils used to define geologic time periods (ammonites) |
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Rocks change from one type to another over millions of years. |
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Metamorphic->Melts->Magma->Cools->Igneous
Igneous->Melts->Magma->Cools->Igneous |
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Definition
Igneous->Weather/Erodes->Sediment
Metamorphic->Weather/Erodes->Sediment
Sedimentary->Weather/Erodes->Sediment |
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Sediment->Compacts/Cements->Sedimentary |
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Definition
Sedimentary->Heat/Pressure->Metamorphic
Igneous->Heat/Pressure->Metamorphic |
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Made of igneous rock--> carry metamorphic or sedimentary rock--> subducted back into earth |
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Within a sequence of layers of. sedimentary rock, the oldest layer is at the bottom and. each layer above gets progressively younger. |
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Water, wind, and other natural forces cause rocks and earth to wear away. These forces also move bits of rock and earth to new places. |
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