Sedimentary Rocks: Formation, Types, Examples
Sedimentary rocks are a type of rock that formed through the accumulation and lithification of sediments, which are particles of rock, minerals, or organic matter that are transported and deposited by wind, water, or ice. These particles, over time, undergo compaction and cementation, transforming into solid rock.
Sedimentary rocks make up the majority of the rock exposed at Earth's surface, covering about 75% of the Earth's crust. However, they are only about 8 percent of the volume of the entire crust. This is because sedimentary rocks are typically thinner than igneous and metamorphic rocks, which form deeper within the Earth's crust.
How Are Sedimentary Rocks Formed
The formation of sedimentary rocks involves a series of distinct processes, each contributing to their unique characteristics.
Weathering and Erosion
The initial step in sedimentary rock formation is the breakdown of pre-existing rocks and the creation of sediments. This process, known as weathering, can be caused by physical, chemical, or biological agents. Physical weathering involves the disintegration of rocks due to mechanical forces like temperature fluctuations, freezing-thawing cycles, and abrasion by wind and water. Chemical weathering, on the other hand, involves the dissolution of rocks by water and acids, altering their chemical composition. Biological weathering, mediated by organisms like plants and microorganisms, contributes to the decomposition of organic matter, creating sediments as a byproduct.
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| What are Sedimentary Rocks? - Types, Formation, Uses, and Examples |
Transportation
Once sediments are formed, they are transported by various agents, primarily wind, water, and ice. Wind carries fine particles like silt and clay, while water moves heavier sediments like sand and gravel. Glaciers, with their immense ice masses, can transport a wide range of sediments, from boulders to fine clays. During transportation, sediments may undergo abrasion, sorting, and rounding, resulting in particles of similar size and shape.
Deposition
The final stage in sedimentary rock formation is the deposition of sediments at a particular location. Deposition occurs when the energy of the transporting agent decreases, causing the sediments to settle out of suspension. Calm water environments, like lakes and seas, promote the deposition of finer sediments, while more energetic environments, like rivers and coasts, favor the deposition of coarser sediments.
Lithification
After deposition, sediments undergo a process known as lithification, which transforms them into solid rock. Lithification involves several mechanisms, including compaction, cementation, and recrystallization. Compaction occurs as the weight of overlying sediments presses down on the deposited material, squeezing out water and reducing pore space. Cementation involves the precipitation of minerals between sediment grains, binding them together into a cohesive mass. Recrystallization involves the dissolution and rearrangement of existing minerals, creating a more tightly interlocking structure.
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| Sedimentary Rocks |
Types of Sedimentary Rocks
Sedimentary rocks can be classified into three main types based on their origin:
- Clastic Sedimentary Rocks
- Chemical Sedimentary Rocks
- Bioclastic Sedimentary Rocks
Clastic Sedimentary Rocks
Clastic sedimentary rocks formed from the accumulation and lithification of clasts, which are fragments of pre-existing rocks or minerals. These clasts are transported by wind, water, or ice and eventually deposited in a variety of environments, such as rivers, lakes, and oceans. Over time, these clasts are compacted and cemented together, forming solid rock. Clastic sedimentary rocks are the most common type of sedimentary rock. Also called Detrital Sedimentary Rocks, Mechanical Sedimentary Rocks.
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| Clastic Sedimentary Rocks examples |
Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.
Sandstone
Sandstone is a clastic sedimentary rock composed of sand-sized (0.0625 to 2 mm) grains, typically quartz or feldspar. It is formed by the lithification of sand, which is a loose sediment that is transported by wind, water, or ice. Sandstone is a common building material and is also used in a variety of other applications, such as glassmaking and electronics.
Shale
Shale is a clastic laminated sedimentary rock composed of clay-sized (less than 0.004 mm) particles. It is formed by the lithification of clay, which is a fine-grained sediment that is transported by water. Shale is a soft, flaky rock that is used in a variety of applications, such as making bricks, ceramics, and roofing tiles.
Conglomerate
Conglomerate is a clastic sedimentary rock composed of rounded gravel-sized (2 millimetres (0.08 inch) in diameter) clasts. It is formed by the lithification of gravel, which is a coarse-grained sediment that is transported by water. Conglomerate is a durable rock that is used in a variety of applications, such as construction, landscaping, and road building.
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| Chemogenic sedimentary rock |
Chemical Sedimentary Rocks
Chemical sedimentary rocks are formed from the precipitation of minerals from solution.
There are ways that chemical sedimentary rocks can form:
Evaporation: When water evaporates, the minerals that were dissolved in it become concentrated.
Inorganic precipitation: Chemical sedimentary rocks can also form when minerals precipitate out of solution due to changes in temperature or pressure. For example, chert is a type of chemical sedimentary rock that is composed of silicon dioxide that has precipitated from solution.
Examples of chemical sedimentary rocks include limestone, dolostone, and gypsum.
Limestone
Limestone is a chemical sedimentary rock composed of calcium carbonate(CaCO₃). Limestone is formed by the precipitation of calcium carbonate from seawater or from freshwater lakes and ponds. Limestone is a common building material and is also used in a variety of other applications, such as making cement, fertilizer, and paper.
Dolostone
Dolostone is a chemical sedimentary rock composed of calcium magnesium carbonate CaMg(CO₃)₂. Dolostone is similar in appearance to limestone, but it is harder and denser. Dolostone is formed by the alteration of limestone or by the precipitation of calcium magnesium carbonate from seawater. Dolostone is a common building material and is also used in a variety of other applications, such as making fertilizer and glass.
Gypsum
Gypsum is a chemical sedimentary rock composed of calcium sulfate CaSO₄·2H₂O. Gypsum is a soft, white rock that is easily carved and molded. Gypsum is formed evaporates, leaving behind calcium sulfate minerals. Gypsum rock can be found in a variety of environments, including deserts, caves, and salt domes. Gypsum is used in a variety of applications, such as making plaster, fertilizer, and wallboard.
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| Chemical and Bioclastic Sedimentary Rocks Examples. Dolostone, Gypsum and Limestone are examples of chemical Sedimentary Rocks, While Chalk, Fossilferous limestone and Coquina are examples of Bioclastic Sedimentary Rocks. |
Bioclastic Sedimentary Rocks
Bioclastic sedimentary rocks are a type of sedimentary rock formed from the accumulation and lithification of the remains of dead organisms. These organisms can be plants, animals, or microorganisms. Bioclastic sedimentary rocks are often composed of a variety of different types of fossils, including shells, bones, and teeth.
Examples of bioclastic sedimentary rocks include chalk, limestone, and coquina.
Chalk
Chalk is a bioclastic sedimentary rock composed of microscopic skeletons of marine organisms, such as plankton and algae. It is formed by the accumulation of these skeletons on the seafloor. Chalk is used in a variety of applications, such as making blackboard chalk, cosmetics, and paint.
Limestone
Limestone can also be a bioclastic sedimentary rock if it is formed from the accumulation of the shells or skeletons of marine organisms. Bioclastic limestone is a common building material and is also used in a variety of other applications, such as making cement, fertilizer, and paper.
Coquina
Coquina is a bioclastic sedimentary rock composed of fragments of shells or skeletons of marine organisms. It is formed by the accumulation of these fragments on beaches or in shallow water environments. Coquina is a common building material and is also used in a variety of other applications, such as making jewelry and decorative items.
Diatomite
Diatomite is a bioclastic sedimentary rock composed primarily of the microscopic skeletons of diatoms, which are single-celled algae. It is formed from the accumulation of diatoms in freshwater or marine environments.
Characteristics Distinguish Sedimentary Rocks
Stratified: Sedimentary rocks typically exhibit a layered or stratified structure, meaning they comprise thin layers of different types of sediment.
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| Sandstone, shale and limestone layers Photo: Gailhampshire |
Fossiliferous: Sedimentary rocks often contain fossils, the preserved remains of organisms that lived when the sediments were deposited, providing valuable clues about past environments.
Variable Composition and Texture: Sedimentary rocks exhibit a wide range of compositions, textures, and colors, reflecting the diverse origins and depositional environments of their constituent particles.
Sedimentary Rocks Importance
Sedimentary rocks are important because they provide a record of Earth's history. Fossils, which are the preserved remains of organisms that lived in the past, are often found in sedimentary rocks. These fossils can be used to date the rocks and to learn about the environment in which they were formed.
Sedimentary rocks act like a giant history book of our planet. These rocks are formed in layers, with the oldest layers on the bottom and the youngest on top. By studying these layers, scientists can learn about the Earth's past climate, geography, and life forms. Fossils, which are the preserved remains of ancient plants and animals, are most commonly found in sedimentary rocks.
Source of Natural Resources: Sedimentary rocks are a vital source of many natural resources that we use every day. Fossil fuels like coal and oil are formed from the buried remains of organic matter. Limestone, a common sedimentary rock, is used in construction materials, fertilizer, and even medicine. Sandstone is another important sedimentary rock used in construction as well as in the production of glass.
Freshwater Sources: Many aquifers, which are underground layers of rock or sediment that contain water, are formed from sedimentary rocks. These aquifers provide fresh water for drinking, irrigation, and industrial uses.
Construction Materials: Sedimentary rocks are widely used in construction projects. Sandstone, shale, limestone, and granite are all popular choices for building materials due to their durability and ease of working with.
See also: The Differences Between Sedimentary Rocks and Igneous Rocks