Concept:
Deep-sea sediments on the ocean floor are classified by their origin into calcareous oozes, siliceous oozes and inorganic clays.
Step 1:
Calcareous and radiolarian oozes are biogenic, formed from the shells of tiny marine organisms. At very great depths these carbonate and silica shells dissolve and cannot accumulate.
Step 2:
In the deep abyssal plains at depths of about 3 km to 6 km, the dominant deposit is red clay, made largely of fine inorganic particles including volcanic and wind-blown dust that settle slowly. Hence the volcanic-origin deep abyssal deposit is red clay.
Answer: Option (4) — Red clay.