The main types of sedimentary rocks are clastic (formed from fragments of other rocks), chemical (formed from minerals precipitated from water), and organic (formed from the remains of once-living organisms). Examples include sandstone, limestone, and shale.
Clastic and nonclastic
Mechanically formed sedimentary rock is composed of particles that are eroded, transported, and deposited by wind, water, or ice. These particles are compacted and cemented together to form rocks such as sandstone, conglomerate, and shale. This type of sedimentary rock is characterized by its clastic composition, meaning it is made up of broken fragments of pre-existing rocks.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
No, sedimentary rocks formed from fragments of other rocks are called clastic sedimentary rocks. Chemical sedimentary rocks form from minerals that are dissolved in water and precipitate out to form rocks like limestone or halite.
Mechanically formed sedimentary rock , Chemically formed sedimentary rock and Organically formed sedimentary rock.
The main types of sedimentary rocks are clastic (formed from fragments of other rocks), chemical (formed from minerals precipitated from water), and organic (formed from the remains of once-living organisms). Examples include sandstone, limestone, and shale.
Clastic sedimentary rocks: Formed from the accumulation of mineral and rock fragments that are cemented together. Chemical sedimentary rocks: Formed from precipitation of minerals dissolved in water. Organic sedimentary rocks: Formed from the accumulation of organic material, such as plants or animals.
Clastic and nonclastic
Sedimentary rocks are formed through the accumulation and compression of sediments over time. Processes like weathering, erosion, transportation, deposition, and lithification contribute to their formation.
Sedimentary rocks are formed through the accumulation and compression of sediments, such as sand, mud, and organic matter, over time. The short answer explanation for their formation is that sediments are deposited, compacted, and cemented together to create sedimentary rocks.
"Sedimentary" is an adjective used to describe a type of rock formed from the deposition of sediment.
Mechanically formed sedimentary rock is composed of particles that are eroded, transported, and deposited by wind, water, or ice. These particles are compacted and cemented together to form rocks such as sandstone, conglomerate, and shale. This type of sedimentary rock is characterized by its clastic composition, meaning it is made up of broken fragments of pre-existing rocks.
Cementing is not a process involved in the formation of sedimentary rock.
SEDIMENTARY ROCK FORMATION, begins with igneous, metamorphic, or other sedimentary rocks. When these rocks are exposed at the earth's surface they begin the long but relentless process of becoming sedimentary rock.
Some examples of clastic sedimentary rocks include sandstone, conglomerate, shale, and breccia. These rocks are formed from the accumulation of fragments of pre-existing rocks and minerals, which are then compacted and cemented together over time.
Clastic sedimentary rocks are formed from the accumulation of rock and mineral fragments, while chemical sedimentary rocks are formed from the precipitation of minerals out of solution. Organic sedimentary rocks are formed from the remains of plants and animals. They differ in their composition, formation process, and appearance.