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Calcareous ooze is an example of .?

biogenous sediment


Which type of ocean floor sediment is biological in origin?

Biogenous


What type of ocean-floor sediment is biological in origin?

Novanet answer: Biogenous.


What type of ocean floor sediment is biological in origin?

Novanet answer: Biogenous.


Are manganese nodules examples of biogenous sediment?

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.


What sediment covers most of the North Pacific?

Biogenous are dominant on deep-ocean floors.


Which type of material does biogenous sediment form?

Two types of biogenous sediments are calcareous ooze and siliceous ooze.


Which group of living things contributes the most to biogenous sediment?

penis


What is calcareous ooze an example of?

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.


What are the three types of the ocean floor sediments?

The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.


What are the two types of biogenous 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.


Why is lithogenous sediment the most common neritic deposit?

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.