Answer: Pyroclastic material is more likely to form in high-viscosity lava than low-viscosity lava.
Explanation: This is because as magma rises, it decreases in pressure, causing the fluid trapped in the magma to form gas bubbles. However, because the magma has a high viscosity, these bubbles cannot escape easily. As the bubbles expand, the solidified lava pieces, volcanic ash, and hot gases (pyroclastic material), rise faster.