Rock salt, rock gypsum, and some forms of limestone.
Limestone is roasted to make lime (calcium oxide) or slaked lime (calcium hydroxide).Other materials and rocks added during roasting are clay, shale, sand, iron ore, bauxite, fly ash, and slag which provide alumino-silicates.
It depends on what kind of rock they are made of. Cliffs formed of igneous rock generally do not contain carbonates. Cliffs that have some limestone, marble, or dolomite do contain carbonates.
Fossils are nearly always found in some type of sedimentary rock. Limestone is a sedimentary rock which very commonly contains fossils, as is coal.
No. If a sedimentary rock has undergone even a low grade metamorphism, it is considered a metamorphic rock.
soem examples of chemical sedimantery rock are limestone, and gypsum.
Some examples of chemical sedimentary rocks include limestone, dolostone, and rock salt. These rocks form when minerals precipitate out of a solution, such as when water evaporates or through processes like precipitation.
What are some uses of chemical limestone
It can be. Some limestone is formed from the precipitation of calcite from saturated solutions, and is considered a chemical sedimentary rock. Other limestone that consists largely of the skeletal remains of marine organisms is considered bio-clastic, a cross between an organic and a detrital sedimentary rock. Typical detrital sedimentary rocks are those composed mostly of particles of pre-existing rock, although organic matter may be included; examples would be sandstone, shale, and conglomerate.
how are the origins of rock salt and some limestone similar
The acid precipitation will react with the calcium carbonate in the limestone, forming soluble calcium salts that will be carried away by the water runoff. This chemical weathering process will gradually erode the limestone rock, causing it to lose mass and potentially leading to the formation of limestone caves or sinkholes over time.
Limestone is considered the parent rock of marble because marble forms from the metamorphism of limestone. Under heat and pressure, the mineral composition of limestone changes, resulting in the formation of marble. This transformation gives marble its distinct crystalline structure and unique appearance while retaining some of the original characteristics of limestone.
Some landforms created by chemical weathering include caves, sinkholes, and limestone pavements. Over time, chemical reactions between rock and water or air can dissolve or alter the composition of the rock, leading to the formation of these distinct landforms.
Some examples of sedimentary rocks formed by chemical precipitation from seawater are limestone, dolomite, and evaporites such as rock salt and gypsum. These rocks form when minerals in seawater precipitate out and accumulate over time to create solid rock formations.
Rock salt, rock gypsum, and some forms of limestone.
Limestone is not generally referred to as an organic rock. It is primarily composed of calcium carbonate, which is a mineral. However, in some cases, limestone can contain remnants of organic matter such as shells, coral, or other marine organisms, which can give it a slightly organic origin. This is why some people may refer to limestone as an organic rock.
Limestone is a sedimentary rock that is primarily composed of the mineral calcite. It is a valuable resource used in construction, agriculture, and manufacturing industries for materials such as cement, concrete, and steel production.