eruption was vertical; but when they missed connection, there were side shots. One of these killed four New Zealanders, two being women, a few weeks before the geyser ceased playing. This ill-fated party had gone near the pit to take photographs. Suddenly Waimangu shot sideways, directly at them. All were knocked into the creek down which the geyser always poured its flood, and their scalded bodies were carried a considerable distance.
Waimangu's basin is still slightly active. In its alum-sprinkled, sulphur-dyed surface are simmering holes and small spouters and a large muddy pool. These evidences of activity, and a belief that the sand is the main, if not the sole, cause of Waimangu's cessation, have persuaded many theorists that, with assistance, the geyser can be enabled to play again. Acting on this theory the New Zealand Government dynamited the hollow, but without encouraging result.
Adjoining Waimangu Basin was the Inferno, a large pool of hot, blue water at the base of the high cliff on which the abandoned Waimangu shelter shed stood. It was covered with steam, and occasionally muffled "torpedo" explosions disturbed it. When Waimangu was active, the Inferno never failed to rise about fourteen seconds before each outburst of the geyser, but no furious turmoil accompanied the elevations. The Inferno's overflow formed a hot creek, which flowed into Lake Rotomahana, about two miles distant. The channel through which it ran is a dismal place, a rain-
