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Sedimentary Rocks. What is a sedimentary rock?. Sedimentary rocks are products of mechanical and chemical weathering They account for about 5 percent (by volume) of Earth’s outer 10 kilometers Contain evidence of past environments Provide information about sediment transport
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What is a sedimentary rock? • Sedimentary rocks are products of mechanical and chemical weathering • They account for about 5 percent (by volume) of Earth’s outer 10 kilometers • Contain evidence of past environments • Provide information about sediment transport • Often contain fossils
What is a sedimentary rock? • Sedimentary rocks are important for economic considerations because they may contain • Coal • Petroleum and natural gas • Sources of iron, aluminum, and manganese
Fossil Fish - 50 Million Year Old Lakes in southern Wyoming These fish tell us the Wyoming climate 50 million years ago. Sedimentary Rock made of fine-grained mudstone.
Sedimentary Rocks • Sedimentary – form in water • Generally formed by the deposition, burial, compaction, and cementation of sediments (pieces of other rocks) • 3 Types • Clastic • Chemical (crystalline) • Organic (Bioclastic)
3 Types of Sedimentary Rocks: • Clastic (also called Detrial)—made of broken pieces of other rocks
3 Types of Sedimentary Rocks: Organic—remains of plants and animals are deposited in thick layers • Examples • Fossil rich limestone is made from the shells of ocean animals; used to make chalk
3 Types of Sedimentary Rocks: • Chemical—minerals dissolved in lakes, seas, or underground water Mineral crystals are made as the shallow water that has flooded the bottom of Death Valley evaporates. Click on image for full size (66K JPG)Courtesy of Martin Miller, University of Oregon
Detrital sedimentary rocks • The chief constituents of detrital rocks include • Clay minerals • Quartz • Feldspars • Micas • Particle size is used to distinguish among the various types of detrital rocks
Classification of sedimentary rocks • Two major textures are used in the classification of sedimentary rocks • Clastic • Discrete fragments and particles • All detrital rocks have a clastic texture • Nonclastic • Pattern of interlocking crystals • May resemble an igneous rock
Detrital sedimentary rocks • Common detrital sedimentary rocks (in order of increasing particle size) • Shale • Mud-sized particles in thin layers that are commonly referred to as laminea • Most common sedimentary rock
Detrital sedimentary rocks • Sandstone • Composed of sand-sized particles • Forms in a variety of environments • Sorting, shape, and composition of the grains can be used to interpret the rock’s history • Quartz is the predominant mineral
B. Descriptions of individual clastic rocks Arkose Graywacke Quartz Sandstone
World’s Biggest Rock • The Ayers Rock is made up of arkose, a course-grained sandstone rich in feldspar at least 2.5 km thick. Uplifting and folding between 400-300 mya turned the sedimentary layers nearly 90 degrees to their present position. The surface has then been eroded.
Detrital sedimentary rocks • Alternating sequences of shale and sandstone exposed in the Grand Canyon. Shale cannot support steep cliffs or form erosion
Detrital sedimentary rocks • Conglomerate and breccia • Both are composed of particles greater than 2mm in diameter • Conglomerate consists largely of rounded gravels • Breccia is composed mainly of large angular particles
B. Descriptions of individual clastic rocks Breccia Conglomerate
Characteristics of sedimentary rocks • Sorting – the distribution of grain sizes in a rock Sorting depends on properties of the depositing agent
Sorting Glacier deposit – poorly sorted Sand dune – well sorted