manganese nodules
No, manganese nodules are examples of hydrogenous sediment. They form through chemical precipitation in seawater, often around a nucleus like a shark tooth or a shell, rather than being produced by living organisms like biogenous sediment.
Two types of biogenous sediments are calcareous ooze and siliceous ooze.
Calcareous ooze is an example of a type of biogenic sediment made up of the skeletal remains of marine organisms like foraminifera, coccolithophores, and pteropods. It is a common component of deep-sea sediments in regions where these organisms are abundant.
The two types of biogenous sediments are siliceous oozes, which are made up of silica-based remains of diatoms and radiolarians, and calcareous oozes, which consist of calcium carbonate shells of organisms like foraminifera and coccolithophores.
The three types of ocean floor sediments are terrigenous (derived from land sources), biogenous (derived from biological organisms), and hydrogenous (derived from chemical processes in seawater).
biogenous sediment
Biogenous
Novanet answer: Biogenous.
Novanet answer: Biogenous.
No, manganese nodules are examples of hydrogenous sediment. They form through chemical precipitation in seawater, often around a nucleus like a shark tooth or a shell, rather than being produced by living organisms like biogenous sediment.
Biogenous are dominant on deep-ocean floors.
Two types of biogenous sediments are calcareous ooze and siliceous ooze.
penis
Calcareous ooze is an example of a type of biogenic sediment made up of the skeletal remains of marine organisms like foraminifera, coccolithophores, and pteropods. It is a common component of deep-sea sediments in regions where these organisms are abundant.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
The two types of biogenous sediments are siliceous oozes, which are made up of silica-based remains of diatoms and radiolarians, and calcareous oozes, which consist of calcium carbonate shells of organisms like foraminifera and coccolithophores.
Lithogenous sediment is the most common neritic deposit because it is primarily derived from the erosion and weathering of rocks on land. These sediments are transported to the ocean by rivers and wind, accumulating in shallow continental shelf areas where neritic deposits are found. This continuous process of erosion and transportation ensures a steady supply of lithogenous sediment to neritic environments.