Limestone is mostly made up of fossilized coral piled and compressed by the weight of the ocean over millions of years. Coral require sunlight for photosynthesis so cannont grow in deep water. Also, coral does better in warm regions.
Limestone is found where coral is successful. Warm, shallow water.
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.
Limestone is formed from particles derived from organic processes, usually in a marine environment. Sandstone particles are derived from the weathering and erosion of silicate bearing rocks, normally.
Limestone deposits can indicate the past presence of shallow tropical seas or marine environments. Fossils found within limestone can provide insights into the organisms that lived in these environments and help reconstruct the paleoclimate of the area. Additionally, the composition and structure of limestone can reveal information about the sedimentary processes and tectonic history of the region.
Oil (petroleum) was formed from the remains of small animals, algae, and other organisms that lived in oceans and shallow inland seas. Over millions of years, the organic matter decomposed and was compressed within the Earth's crust to form oil deposits.
Limestone forms in the Earth's crust through the accumulation and lithification of calcium carbonate sediment, often from the remains of marine organisms like coral and shells. It commonly occurs in environments such as shallow seas, lagoons, and coral reefs where these organisms flourish and deposit their calcareous material.
White limestone is formed from the accumulation of calcium carbonate from the remains of marine organisms like coral and shells. This accumulation often occurs in shallow seas and is deposited from the water onto the sea floor over time, eventually forming limestone rock.
No, we don't. Limestone is a sedimentary rock laid down in ancient seas. It is formed from the skeletal remains of countless marine creatures.
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.
Limestone often contains fossils of marine animals, indicating that it was formed in shallow, warm seas. Common sea animals found in limestone include corals, mollusks like clams and snails, and echinoderms such as sea urchins and starfish. These organisms contribute to the sediment that eventually compacts into limestone rock. Additionally, the porous nature of limestone can host various marine life in its crevices and cavities.
...In Shallow Seas We Sail was created in 2020-09.
Limestone is formed from particles derived from organic processes, usually in a marine environment. Sandstone particles are derived from the weathering and erosion of silicate bearing rocks, normally.
Limestone is formed on the floor of ancient seas from the skeletal remains of marine organisms such as coral, forams and molluscs, etc.
deposits of volcanic ash in the shallow seas during the deposition of the chalk
Limestone is the skeletal remains of small marine shelled creatures. Their remains sank to the floor of the seas, and the layers became rock over a very long time.
Most Dolphins are found in all oceans, they are found in the shallow seas.
Limestone deposits can indicate the past presence of shallow tropical seas or marine environments. Fossils found within limestone can provide insights into the organisms that lived in these environments and help reconstruct the paleoclimate of the area. Additionally, the composition and structure of limestone can reveal information about the sedimentary processes and tectonic history of the region.
Many geologists believe that limestone deposits on land exist where ancient seas used to be. The moisture, over many centuries, created limestone.