Sedimentary Rock
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Transcript of Sedimentary Rock
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Sedimentary RockSection 3.3
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Sedimentary RocksAll sedimentary rocks begin to form when
existing rocks are broken down into sediments through a process called weathering
Weathering is the process in which rocks are physically and chemically broken down by water, air, ice and gravity
Sediments are transported, by water, gravity, glaciers or wind, and eventually become compacted and cemented together, forming sedimentary rocks
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Formation of Sedimentary RocksSedimentary comes from the Latin word sedimentum, which means settling
There are several major processes that contribute to the formation of sedimentary rocks:Weathering, Erosion and DepositionCompaction and Cementation
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Weathering, Erosion and DepositionWeathering is any process that breaks
rocks into sedimentsChemical weathering takes place when the
minerals in rocks change into new substancesErosion involves weathering and the
transportation of sedimentsDeposition is the process when water, wind,
ice or gravity loses energy causing sediments to dropLarger sediments are deposited first,
smaller sediments are dropped later
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Compaction and CementationOnce sediments are deposited, they
become lithified or turned into rockCompaction is a process that squeezes,
or compacts, sediments, pushing water outCompaction is caused by the weight of
sedimentsCementation takes place when dissolved
minerals are deposited in the tiny spaces among the sediments
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Classification of Sedimentary RocksSedimentary Rocks can be classified into
two main groups according to the way they formClastic – rocks that are made of
weathered bits of rocks and mineralsChemical – forms when dissolved minerals
precipitate from water solutions
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Clastic Sedimentary RocksClastic sedimentary rocks are made of
weathered bits of rocks and mineralsClastic sedimentary rocks can be grouped
according to the size of the sediments in the rocksConglomerate rocks are made up of
rounded, gravel-size or larger particlesBreccia rocks have angular particlesSandstone rocks have sediments that are
sand-sized grains
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Clastic Sedimentary RocksConglomerat
e
Sandstone
Breccia
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Chemical and Biochemical Sedimentary RocksChemical sedimentary rocks forms when
dissolved minerals precipitate from water solutions
The precipitation generally occurs when water evaporates or boils off leaving a solid productExamples include limestones, rock salt,
chert, flint and rock gypsumBiochemical sedimentary rocks contain
shells and skeletal remains of organisms that settle to the ocean floor
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Chemical Sedimentary Rocks
Rock Salt
Limestone
Chert
Flint
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Biochemical Sedimentary Rocks
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Features of some Sedimentary RocksSedimentary rocks give clues to how,
when and where the rocks formedLayers of sedimentary rock records a period
of sediment deposition. The oldest layers are found at the bottom
Ripple marks may indicate that the rock was formed along a beach or stream bed
Mud cracks are formed when wet mud or clay dried and shrank, leaving a record of a dry environment
Fossils found in sedimentary rocks can help answer questions about the rock
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Ripple marks
Fossils
Layers of sedimentary rock
Mud cracks
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Summary of Sedimentary RocksSedimentary rocks form as the result of
four major processWeathering produces particles called
sedimentsWind, water, ice and gravity erode and deposit sediments
Sediments are compacted and cemented to form sedimentary rocks
Sedimentary rocks can be classified according to how they form, by using rock formation, texture and composition
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(Table 2 on page 79)