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Is limestone a sedimentary rock?
Yes, limestone is a sedimentary rock primarily composed of calcite or aragonite minerals that are deposited from the remains of marine organisms. It is formed through the process of lithification, where loose sediment is compacted and cemented together over time.
Type of sedimentary rock that forms when sediments stick together?
A type of sedimentary rock that forms when sediments stick together is called a clastic sedimentary rock. This process occurs when loose grains of sediment, such as sand or clay, are compacted and cemented together over time to create a solid rock. Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.
What occurs when substances harden crystallize in the spaces between loose sediments?
When substances harden and crystallize in the spaces between loose sediments, they form a type of rock called a crystalline sedimentary rock. This process involves the filling of pore spaces with mineral crystals, which bind the sediments together to create a solid rock matrix. Common examples of crystalline sedimentary rocks include limestone and dolomite.
Forms as pieces of loose material get pressed or cemented together?
Sedimentary rocks form as pieces of loose material get pressed or cemented together. The process of forming sedimentary rocks is lithification.
What type of rock is formed when layers of loose materials and compacted?
Sedimentary rock is formed when layers of loose materials, such as sand or sediment, are compacted and cemented together over time.
Is limestone a sedimentary rock?
Yes, limestone is a sedimentary rock primarily composed of calcite or aragonite minerals that are deposited from the remains of marine organisms. It is formed through the process of lithification, where loose sediment is compacted and cemented together over time.
What kind of rock is formed when sediment and loose material bind together?
Sedimentary rock is formed when sediment and loose material such as sand, silt, and clay bind together over time through the process of compaction and cementation. Examples of sedimentary rocks include sandstone, shale, and limestone.
What kind of rock is formed loose rocks and dirt are transported and re-deposited.?
Sedimentary rock is formed when loose rocks and dirt are transported and re-deposited. This process can happen through erosion, transportation by wind or water, and eventual deposition in layers that solidify over time to form sedimentary rock. Examples include sandstone, shale, and limestone.
Are all sedimentary rocks hardened by natural cement?
No, not all sedimentary rocks are hardened by natural cement. Some sedimentary rocks are formed by the compaction of loose sediment particles without cementation, such as shale. Others may be composed of organic matter, like coal or some types of limestone, which do not require cementation to harden.
Type of sedimentary rock that forms when sediments stick together?
A type of sedimentary rock that forms when sediments stick together is called a clastic sedimentary rock. This process occurs when loose grains of sediment, such as sand or clay, are compacted and cemented together over time to create a solid rock. Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.
Which types of rock can weather and wear away to form sediment?
Sedimentary rocks such as sandstone, shale, and limestone can weather and wear away to form sediment. These rocks are often composed of loose grains that can be eroded by wind, water, or ice, leading to the formation of sediment.
Rocks formed from sediments deposits?
Sedimentary rocks are formed from sediment deposits (gravel, sand, silt, clay) over long periods of time either on land or in water (lakes, oceans). As more and more sedimentary layers are deposited, the newer layers exert pressure on the older layers, which compacts the loose particles and cements them together - forming sedimentary rocks. Sedimentary rocks can also be formed through the precipitation of dissolved minerals to form limestone or dolomite.
What occurs when substances harden crystallize in the spaces between loose sediments?
When substances harden and crystallize in the spaces between loose sediments, they form a type of rock called a crystalline sedimentary rock. This process involves the filling of pore spaces with mineral crystals, which bind the sediments together to create a solid rock matrix. Common examples of crystalline sedimentary rocks include limestone and dolomite.
Which does not belong shale basalt sand stone or limestone?
In the question "which does not belong; shale, basalt, sandstone, or limestone?" the answer is Basalt. Shale, Sandstone, and Limestone are all sedimentary rocks. Basalt is an Igneous rock. Shale and Sandstone are both clastic sedimentary rocks which means they come from the "pieces" or remains of rocks after weathering. Limestone is a chemical sedimentary rock which means it is deposited as a result of a chemical reaction, or a collection of material made by organisms, such as coral. volcanic basalt dykes are molten basalt that rose through existing sedimentary rock, and crystallized when it rose to the surface about 32 million years ago. The magma cools and hardens which creats a basalt stack, resistant to weather. Basalt is a common extrusive volcanic rock.It color is usually gray or close to black.
Forms as pieces of loose material get pressed or cemented together?
Sedimentary rocks form as pieces of loose material get pressed or cemented together. The process of forming sedimentary rocks is lithification.
Are sedimentary rocks easily eroded?
YES! Sedimentary rocks, like sandstone, limestone and chalk can easily be eroded. This is because the grains in them (different to particles) are further apart to the grains in rocks like igneous rocks. This means that the grains can easily be crumbled off, and you get left with sand.
What type of rock is formed when layers of loose materials and compacted?
Sedimentary rock is formed when layers of loose materials, such as sand or sediment, are compacted and cemented together over time.
