Chapter 3 – 3 Sedimentary Rocks

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Chapter 3 – 3 Sedimentary Rocks How do sedimentary rocks form?

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Chapter 3 – 3 Sedimentary Rocks. How do sedimentary rocks form?. Sandstone is the most common form of sedimentary rock. Arches Park!. Sediment – small solid pieces of material from rocks or living things. - PowerPoint PPT Presentation

Transcript of Chapter 3 – 3 Sedimentary Rocks

Page 1: Chapter 3 – 3 Sedimentary Rocks

Chapter 3 – 3 Sedimentary Rocks

How do sedimentary rocks form?

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Sandstone is the most common form of sedimentary rock. Arches Park!

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Sediment – small solid pieces of material from rocks or living things.

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Erosion helps to create sediment. Water or wind loosens and carries away fragments

of rock.

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Deposition re-deposits sediment at the bottom of a lake or ocean where it

compacts and cements and changes to sedimentary rock!

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Compaction is that process that presses sediments together. Year after year, the weight

of the layers becomes greater and greater.

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Cementation is the process in which dissolved minerals crystallize and glue particles of the sediment together into

sedimentary rock.

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Types of Sedimentary Rocks include Clastic and Organic Rocks.

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Clastic rock forms when rock fragments are squeezed together. From tiny microscopic

particles to huge boulders.

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Shale is formed from tiny particles of clay. No cementation is needed to hold shale together.

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Sandstone is a clastic rock that forms from the sand on beaches, riverbeds and sand

dunes.

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Compaction and cementation of quartz material often leaves spaces for water to

seep in.

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Conglomerate and Breccia are sedimentary rocks containing a mixture of rock

fragments of different sizes.

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Conglomerate rocks have fragments of rock stuck in that have rounded edges.

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Breccia are sedimentary rocks that contain large fragments with sharp edges.

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Organic rock forms where the remains of plants and animals are deposited in thick layers. Coal & Limestone.

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Coal forms from the remains of layers and layers of swamp plants. Buried for millions

of years, they slowly change to coal.

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Limestone includes the remains of marine life. Coral, clams, oyster and snail shells contain

calcite, a mineral that with pressure and over time, forms limestone.

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Chalk is a very common form of limestone. Chalk is made from the skeletons of living

things.

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Chemical rocks form in nature when minerals dissolved in solution crystalize.

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Dry lake beds often have deposits of halite (salt), gypsum & tufa.

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Uses of sedimentary rock include building materials, cement, and iron ore

production.