Fossiliferous limestone has larger fossils in the rock and is of biochemical composition where as the oolitic limestone doesn't have any fossils and has a chemical composition. The Oolitic limestone has spherical grains that resemble miniature pearls (they are called ooliths or ooids). Both do effervesce in diluted HCL(acid)
No oolitic limestone is mostly calcium carbonate with some spar cement,but sandstone is mostly quartz but with all sorts of weathered products of other preexisting rocks with size within the range of 1/16mm to 4mm
Chemical
Sedimentary rocks formed by chemical precipitation from seawater include limestone, specifically in the form of travertine and oolitic limestone, as well as evaporites like halite and gypsum. These rocks result from the evaporation of seawater, which leads to the concentration and precipitation of minerals. As seawater evaporates, dissolved minerals crystallize out, forming solid deposits that can accumulate over time.
Clastic sedimentary rocks are formed by the weathering, erosion, deposition, compaction and cementation of other rocks. Chemical sedimentary rocks however may be precipitated directly from saturated solutions (examples incldue the evaporitic rocks and certain types of carbonates such as oolitic limestones). Some other sedimentary rocks may be biogenic in origin (such as the linmestones that are formed of coral reefs).
Igneous rocks are made from magma. Magma is made of melted rocks. (When it is underground it is called magma, when it erupts on the surface of the earth, it is called lava. It's the same material though.) When magma/lava cools, it forms igneous rocks. There are many types of igneous rocks and the specific type of igneous rock can vary according to which minerals are present in the melted rock, how fast it cools, and the presence of things like water. Sedimentary rocks are made out of tiny pieces of debris. This can include tiny rocks, sand, clay, silt, and organic material. (Organic materials can vary from rotted leaves to tiny, shelled ocean creatures, or many other types of organic material.) These bits of material collect in an area, then through compaction and cementation, they stick together to form sedimentary rocks. Sedimentary rocks can also be formed when minerals are dissolved in water and are then resolidified. This type of sedimentary rock is called a chemical sedimentary rock. Oolitic limestone is a good example of this type of sedimentary rock.
Limestone is primarily composed of the mineral calcite and may be very fine-grained, oolitic, or fossiliferous.
Chalk is a soft, porous rock composed of microscopic coccoliths, whereas limestone is a harder, more dense rock made up of larger calcium carbonate crystals. Chalk tends to form in marine environments with high biological productivity, while limestone forms in areas with high sedimentation rates and pressure.
The sedimentary rock described is likely to be oolitic limestone, which forms from the accumulation of small spherical grains called ooids. Oolitic limestone typically forms in shallow, warm marine environments with high rates of evaporation. Its distinctive concentric structure is due to the successive layers of mineral precipitation around a central nucleus.
Oolitic limestone is commonly used as a building material due to its durability and aesthetic appeal. It is often used in the construction of walls, flooring, and decorative elements such as columns and facades. Additionally, oolitic limestone can also be crushed and used in road construction, as a soil conditioner, and in the production of cement.
Limestone or dolostone forms marble. This encompasses all types, from Chalk to Oolitic Limestone.
Oolitic limestone is most likely to form in high-energy marine environments, such as shallow tropical seas with strong currents where the rapid agitation of water helps form small ooids (rounded sediment grains). These ooids accumulate and cement together to form oolitic limestone.
The two main types of limestone found in the Caribbean are coral limestone, formed from the skeletal remains of marine organisms like coral, and oolitic limestone, composed of small round grains called ooids. These limestone types are common in the region due to the prevalence of coral reefs and marine environments that have existed there over millions of years.
No oolitic limestone is mostly calcium carbonate with some spar cement,but sandstone is mostly quartz but with all sorts of weathered products of other preexisting rocks with size within the range of 1/16mm to 4mm
Oolitic refers to a sedimentary rock composed of small spherical grains called ooids, which are typically made of calcium carbonate. Oolitic rocks are formed in marine environments where currents cause the grains to accumulate and grow layer by layer.
Oolite is sometimes also known as 'Egg Stone'. It is a limestone formed from ooids, spherical grains found in concentric layers.
There are different types of limestone rock in the UK which differ in colour. Carboniferous limestone is greyish and hard and made from the remains of corals. Jurassic limestone is yellowish and softer. It is oolitic (made from little eggs of calcite). Cretaceous limestone is very white and chalky. It is made from the skeletal remains of planktonic organisms.
The Great Pyramid was the color of Oolitic limestone- a kind of honey color. When it was built, the outside was covered in a layer of polished white fine grained limestone, but had been removed later to build Cairo