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Published byRebeca Perrett Modified over 9 years ago
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Rocks that are formed in flat layers called strata
Sedimentary Rocks Rocks that are formed in flat layers called strata
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Sedimentary Rocks Can Be Divided into Three Categories
CLASTIC CHEMICAL ORGANIC
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CLASTIC SEDIMENTARY ROCK
When sediments are deposited, they settle to the bottom based on particle size. This is called stratification. These layers are called strata.
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Classification of Clastic Rocks
Clastic sedimentary rocks are not classified by mineral composition They are classified by the SIZE and SHAPE of the particles of sediment
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Compaction and Cementation
As layers build up, the particles get pressed together. Water is squeezed out and the particles are cemented together by minerals
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Clastic Sedimentary Rocks Examples
Shale Made of mud and silt particles Often breaks off in flat sheets
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Clastic Sedimentary Rocks Examples
Sandstone Made of sand particles cemented together Different colors based on type sand particles
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Clastic Sedimentary Rocks Examples
Conglomerate Made of pebbles or rounded stones Looks like natural concrete
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Organic Sedimentary Rocks
Formed from the remains of living things Shells of sea creatures Dinosaur/ancient creature remains Decayed plant material
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Organic Sedimentary Rock Examples
Bituminous Coal Made from the remains of decayed plant material Used as a fossil fuel mostly for making electricity
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Fossiliferous Limestone
Formed from the remains of sea creatures cemented together Contains the mineral calcite (calcium carbonate)
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Organic Sedimentary Rock Examples
Chalk Made from the remains of microscopic organisms First used on chalkboards
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Chemical Sedimentary Rocks
Formed from dissolved minerals in water When water evaporates, the minerals are left behind and crystallize Most common places to find this: Where ancient seas evaporated Caves
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Chemical Sedimentary Rock Examples
Limestone Contains calcite Can form stalactites and stalagmites in caves
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Chemical Sedimentary Rock Examples
Halite also known as rock salt Forms when ocean water evaporates
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