Sedimentary Rocks
• Sedimentary Rocks - Those rocks that form from the aggregation of sediments that have been transported, deposited, and later lithified.
• Sediments are essentially fragments and particles of other rocks and/or minerals.
– The Sedimentation Process - producing sediments.
• Weathering and Erosion
• Transportation
• Deposition
– Lithification Process - How to convert sediments into rocks.
• Compaction
• Dehydration
• Cementation
Sedimentary Rocks
• Two types of sedimentary rocks based on the sources of their major components -
– 1. Detrital sedimentary rocks - composed of particles call detritus, which means rock particles and/or minerals from other rock types. Also known as Clastic !
– 2. Chemical sedimentary rocks - composed of precipitates or chemicals that were in solution within a liquid, usually water. Note Biochemical used by textbook.
Sedimentary Rocks
• Detrital Sedimentary Rocks -
– These rocks are composed of other rock types. Quartz is one of the most resistant rocks to weathering and is a dominate component of many sedimentary rocks.
• Gravel = Conglomerate or breccia 2-> 256 mm
• Sand = Sandstone 1/16-2 mm
• Mud = Mudstone to shale < 1/16 mm
Sedimentary Rocks
• Chemical Sedimentary Rocks
– These rocks are composed of materials carried in solution within lakes and oceans and/or of a biological origin.
• Limestone from dissolved CaCO
3
• Conquina is a coarse rock composed mostly of loosely cemented shells and shell fragments.
• Chert, flint, agate, etc. is from SiO
2
• Evaporites are salts - rock gypsum
• Coal - from organic material
Sedimentary Rocks
• The importance of these rocks is that they typically make-up 75 volume % of the upper most part of continental crust and are expressed as strata or beds or rock layers .
• Strata are the record of paleoenvironments .
Sedimentary Rocks
• The study of strata, beds, and their respected paleo-environments is the science of stratigraphy .
• Stratigraphic formation -sequence of strata distinctive enough to be traced across a large region.
• Special kinds of Bedding - Cross beds and graded beds.
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• Sedimentary Environments - these are environments where sediments were deposited.
– Glaciers, mountain streams, alluvial fans, sand-dunes, lake, ponds, rivers, etc.
– Reflective of a specific type of depositional energy.
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• What processes produce sediments?
– Weathering - disintegration and decomposition of rock at or near surface (Mechanical and chemical)
– Mass wasting - transfer of rock material down-slope under the influence of gravity.
– Erosion - incorporation and transportation of material by a mobile agent, usually water, wind, and/or ice.