Detrital Sedimentary Rocks • Detrital sedimentary rocks form from sediments that have been weathered and transported - Chief constituents of detrital rocks include clay minerals
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Particle Size Categories
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Detrital Sedimentary Rocks • Shale - Silt- and clay-sized (fine-grained) particles - Form from gradual settling of sediments in quiet
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Detrital Sedimentary Rocks • Sandstone - Sand-sized particles - Forms in a variety of environments - Second most abundant sedimentary rock - Quartz is the most abundant mineral
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Quartz Sandstone
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Detrital Sedimentary Rocks Conglomerate and Breccia - Conglomerate consists of rounded, gravel-sized (or larger)
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Biochemical Limestone
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Inorganic Limestone
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Chemical Sedimentary Rocks • Evaporites
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Salt Flats
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Coal: An Organic Sedimentary Rocks
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Turning Sediments into Sedimentary Rock: Diagenesis and Lithification
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Classification of Sedimentary Rocks
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Sedimentary Rocks Represent Past Environments
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Sedimentary Environments
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Sedimentary Structures . When present, they provide additional information for interpreting Earth's history • Types of sedimentary structures - The layers of the sedimentary rocks are called strata or
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Sedimentary Strata
Description:
Explore the formation, classification, and significance of sedimentary rocks in this comprehensive 38-minute lecture. Delve into the origins of sedimentary rocks, examining detrital, chemical, and organic types. Learn about particle size categories, shale, sandstone, conglomerate, and breccia. Investigate biochemical and inorganic limestones, evaporites, and coal. Understand the processes of diagenesis and lithification that transform sediments into rock. Discover how sedimentary rocks represent past environments and provide valuable information for interpreting Earth's history through various sedimentary structures and strata.