Step 1: Understand the setting. We need a deposit of volcanic origin that settles on the deep abyssal plain at about 3 km to 6 km depth.
Step 2: Recall how deep-sea deposits are grouped. They are mainly biogenic oozes (from organism shells) and inorganic clays.
Step 3: Remove the biogenic oozes. Calcareous ooze and radiolarian ooze come from tiny marine organisms, and calcareous shells even dissolve before reaching such great depths.
Step 4: Check pelagic deposits. Pelagic is a broad term for open-sea deposits, not specifically the volcanic clay we want.
Step 5: Identify the volcanic deposit. Red clay is an inorganic deposit rich in volcanic and wind-blown fine particles, found on the deepest abyssal floor.
Step 6: State the answer. So the volcanic-origin deep deposit is red clay. \[ \boxed{\text{Red clay}} \]
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