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Published byDale Carr Modified over 8 years ago
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Most sedimentary rock forms this way Sediment is material that settles out of water or air Sand at the beach Mud in the bottom of a lake Pebbles in a river Dirt in your yard Dust on furniture Rock develops when layers of sediment build up on land or water and get cemented together
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Rain Washes away rock particles as it runs down slopes Water Streams can move sediment that ends up in lakes or the ocean Wind Strong wind can pick up sand and rock dust and carry it to distant places As this sediment is transported it gets laid down in layers
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As layers of sediment layer on top of each other the pressure causes the layers to form into rock Silt and clay Other times minerals need to crystallize between sediment acting as cement.
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Made mainly of sand-size weathered debris (1/16 – 2 millimeters in diameter) Forms mostly where large amounts of sand accumulate Beaches Deserts Flood plains Deltas
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Fine-grained Formed from silt and clay-size minerals Otherwise known as mud Made of thin layers
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Does not contain any minerals Made from the remains of plants and animals Takes millions of year to form Conditions must be right Forms from ancient swamps
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Made of carbonate minerals like calcite Shells and skeletons of ocean organisms have these minerals Ocean organisms die and their remains go to the bottom of the ocean Over time the shells/skeletons get cemented together because their minerals dissolve and re- form Coral reefs also consist of limestone As the coral grows its old shells die
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Minerals are dissolved in water When water evaporates it leaves the minerals behind These minerals then recrystalize to form rock Rock salt or halite is an example Detroit has a huge deposit of this under the city
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The only type of rock that fossils can be found in Tell us about plants and animals that lived in the past Crossbeds Show the direction wind was blowing over sand dunes Ripples Show the direction water was traveling over the sand Mud Cracks Show periods of wet followed by dry periods Floods Shown when sediment size is layered large up to small
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