The type of fossils
The rock formed when dissolved minerals cement sediments together is called sedimentary rock. This process occurs over time through the compaction and cementation of particles such as sand, silt, and clay. Examples of sedimentary rocks include sandstone, limestone, and shale.
Petroleum is found in the ocean floor beneath the seafloor sediments. It accumulates in underground reservoirs formed by porous rocks such as sandstone or limestone. These reservoirs are typically located in offshore areas where sedimentary rocks have been deposited over millions of years.
Deep ocean deposition is the norm for the bulk of limestone formation, although seepage in caves also creates limestone structures, as well as shallow water coral reefs, and hydrothermal surface structures.
Chemical sediments are sedimentary rocks that form from the precipitation of minerals dissolved in water. These minerals accumulate on the ocean floor or in lakes through processes like evaporation or chemical reactions. Common examples of chemical sediments include limestone, gypsum, and halite.
Limestone deposits suggest that they were formed in a marine environment, typically in shallow, warm, and calm waters where the accumulation of calcium carbonate skeletons and shells of marine organisms was prevalent. The presence of fossils within limestone can indicate the past biodiversity and environmental conditions of the area where the deposits formed. Additionally, the purity and composition of the limestone can provide clues about the depositional processes and the source of the materials.
Chalk formed from sediments made of skeletions of microscopic living things in the ocean must be a(n) organic rock.
over a very long time layers of these sediments hardened into a sedimentary rock called limestone
Hydrogenous sediments are formed when minerals precipitate from the ocean, or they can be formed when minerals in the water react with older sediments.
The sediments are called silt or alluvium. The land formed from these sedimants where the river meets the ocean is a delta.
The rock formed when dissolved minerals cement sediments together is called sedimentary rock. This process occurs over time through the compaction and cementation of particles such as sand, silt, and clay. Examples of sedimentary rocks include sandstone, limestone, and shale.
the ocean
Pure white limestone often forms in areas where the limestone has experienced very little exposure to impurities or contaminants during its formation process. This can happen in environments such as deep ocean basins, where the limestone can accumulate without being mixed with other sediments or minerals.
Limestone is often sedimentary, formed of calcite in the form of shells and coral. So it's found where there used to be an ocean.
Skeletal remains of many sea creatures settle on the ocean floor. Here they mix with sediments and eventually become sedimentary rock.
Petroleum is found in the ocean floor beneath the seafloor sediments. It accumulates in underground reservoirs formed by porous rocks such as sandstone or limestone. These reservoirs are typically located in offshore areas where sedimentary rocks have been deposited over millions of years.
Hydrogenous sediments form when minerals precipitate directly from seawater as a result of chemical reactions or biological processes. For example, manganese nodules and phosphorite deposits are examples of hydrogenous sediments that form in this way in the deep sea. These sediments accumulate slowly over time on the ocean floor.
Deep ocean deposition is the norm for the bulk of limestone formation, although seepage in caves also creates limestone structures, as well as shallow water coral reefs, and hydrothermal surface structures.