The Oceanic Deposits of the Ocean Floor

Materials eroded from the earth which are not deposited by rivers or at the coast are eventually dropped on the ocean floor. The dominant process is slow sedimentation where the eroded particles very slowly filter through the ocean water and settle upon one another in layers. The thickness of the layer of sediments is still unknown. Its rate of accumulation is equally uncertain. Generally speaking, we may classify all the oceanic deposits as either muds, oozes or clays.

• The muds - These are terrigenous deposits because they are derived from land and are mainly deposited on the continental shelves. the muds are referred to as blue, green or red muds; their colouring depends upon their chemical content.
• The oozes - These are pelagic deposits because they are derived from the oceans. They are made of the shelly and skeletal remains of the marine micro-organisms with calcareous or siliceous parts. Oozes have a very fine, flour-like texture and either occur as accumulated deposits or float about in suspension.
• The clays - These occur mainly as red clays in the deeper parts of the ocean basins, and are particularly abundant in the Pacific ocean. Red clay is believed to be an accumulation of volcanic dust blown out from volcanoes during volcanic eruptions.

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