Limestones are sedimentary rocks made of skeletal remains. Limestones are recognizable because they react with Acid.
Crystalline limestone are micro skeletons with large visible crystals.
Micritic limestone is lithographic limestone and it is basically fine grained mud with micro-skeletons.
Fossiliferous limestone is made with whole fossils in my experience mostly shells.
Coquina is parts of skeletons pressed together. The difference between coquina and fossiliferous is that coquina doesn't have whole fossils.
Lastly there is chalk. This is a lot of microorganisms remains pressed together.
No, chalk is not made of diatoms. Chalk is primarily composed of calcite, a mineral form of calcium carbonate, which originates from the skeletal remains of marine organisms like coccolithophores and foraminifera. Diatoms, on the other hand, are a type of algae with silica-based cell walls, and they contribute to different types of sedimentary rocks. While both chalk and diatomaceous earth are formed from the remains of microscopic organisms, their compositions and origins differ significantly.
No, chalk is primarily composed of calcium carbonate, a mineral made up of the skeletal remains of plankton and other marine organisms. Microplankton are tiny organisms found in the ocean, but they are not the main component of chalk.
A sedimentary rock made from the shells of dead sea creatures is called limestone. This rock forms primarily from the accumulation of calcium carbonate, which is derived from the shells and skeletal remains of marine organisms. Over time, these materials are compacted and cemented together, leading to the formation of limestone. Other types of sedimentary rocks can also include similar organic materials, but limestone is the most common associated with marine shells.
All fossils are found in sedimentary rocks. Some sedimentary rocks are made of nothing but fossils such as chalk. A creature ( microscopic or larger) skeleton is deposited after death usually on the ocean floor. Sediments cover it, and over time turns into a fossil.
Chemical sedimentary rocks form from dissolved minerals in water, such as limestone made from calcium carbonate. On the other hand, organic sedimentary rocks, like coal or limestone made from the remains of dead organisms, are created from the accumulation and compaction of organic material over time.
Clastic sedimentary rocks, like conglomerate and sandstone.
Organic sedimentary rocks, such as limestone and coal, are formed from the remains of once-living things. Limestone is primarily made of calcium carbonate from the shells and skeletal remains of marine organisms, while coal forms from the buildup of plant material in swampy environments over millions of years.
Limestone is a sedimentary rock that is often formed from the remains of dead marine organisms such as shells and coral. This type of rock is composed mainly of calcium carbonate.
This type of sedimentary rock is called organic sedimentary rock. It forms from the accumulation and compaction of plant and animal remains, such as shells, skeletons, and plant materials. Common examples include limestone, coal, and chalk.
My kitchen counter is made from limestone.
No. Limestone is formed from precipitated calcite or from the shells or skeletal remains of marine organisms.
No, chalk is not made of diatoms. Chalk is primarily composed of calcite, a mineral form of calcium carbonate, which originates from the skeletal remains of marine organisms like coccolithophores and foraminifera. Diatoms, on the other hand, are a type of algae with silica-based cell walls, and they contribute to different types of sedimentary rocks. While both chalk and diatomaceous earth are formed from the remains of microscopic organisms, their compositions and origins differ significantly.
The mountain is likely made of sedimentary rock, such as limestone or sandstone, that formed from the accumulation and compaction of the remains of ancient ocean organisms over millions of years.
Like most other sedimentary rocks, limestone is composed of grains; however, most grains in limestone are skeletal fragments of marine organisms such as coral or foraminifera.
No, chalk is primarily composed of calcium carbonate, a mineral made up of the skeletal remains of plankton and other marine organisms. Microplankton are tiny organisms found in the ocean, but they are not the main component of chalk.
Limestone is composed of the skeletal remains of minute sea creatures. The layers are then subjected to compression and, over a very long time, hardened into a sedimentary rock.
sedimentary rock