Lady Knox Geyser
Facts and practical information
Nestled within the geothermal wonderland of Wai-O-Tapu, near Rotorua on New Zealand's North Island, the Lady Knox Geyser presents a spectacle that draws tourists from around the world. This natural geyser, named after a daughter of a 19th-century New Zealand Governor, has been a crowd-pleaser for over a century, showcasing the volatile volcanic forces that shape this region.
Unlike many of its unpredictable counterparts, Lady Knox Geyser has a unique feature: it erupts almost on schedule, daily around 10:15 AM, thanks to a little human intervention. A soap-like substance is introduced into the geyser's opening to break the surface tension of the cold water layer above the hot water within its vent. This process triggers the geyser's eruption, sending a jet of steam and water up to 20 meters into the air, much to the delight of onlookers.
The geyser sits within a sinter basin created from silica deposition over thousands of years, a testament to the long-standing geothermal activity in the area. The surrounding landscape is dotted with other geothermal features, including bubbling mud pools, steaming vents, and colorful mineral terraces, making it a prime destination for those interested in the Earth's volcanic phenomena.
Lady Knox Geyser – popular in the area (distance from the attraction)
Nearby attractions include: Waimangu Volcanic Rift Valley, Champagne Pool, Waiotapu, Reporoa Caldera.