The Hawaiian Islands sit smack in the middle of the Pacific Plate—~3,000 km (1,860 miles) from the nearest plate boundary (the Pacific–Antarctic Ridge to the south, the Pacific–North American boundary off California/Alaska to the northeast, and the Pacific–Philippine boundary to the west).
This intraplate location explains Hawaii's hotspot volcanism: a stationary mantle plume burns through the plate as it drifts northwest (~7–9 cm/yr), creating the island chain. The islands are not on a subduction zone or spreading ridge—hence no massive earthquakes or explosive subduction volcanoes like the Ring of Fire.