But how did the Waimangu geyser form and become so powerful? The answer lies in the area’s geological history. In 1886, a volcanic eruption on Mount Tarawera created a series of volcanic vents that altered the plumbing of an existing hydrothermal system around Waimangu. The eruption was devastating, creating a landscape devoid of vegetation and killing many Maori people who lived in the area at the time. The subsequent evolution of the geyser and its pressure gradients created a deep boiling and fountaining system that erupted through an extensional fissure that formed a nozzle. Hence, the Waimangu geyser came to be.
Although the Waimangu geyser is no longer active, its evolution and existence remain an example of the awe-inspiring (and sometimes deadly) power of geothermal activity. What a world we live in!
Photo credits:
Top: S. Simmons, Waimangu-Tarawera aerial view
Bottom b&w: Waimangu Geyser, The Greatest Known Geyser, 1903, Rotorua, by A. Cromwell Shepherd, Muir & Moodie. Te Papa (C.016361)