Only about a thousand geysers are known to exist, and roughly half of them are found in Yellowstone National Park in the western US. Given a suitable—and rare—geology, underground liquid and vapor are heated and pressurized until turbulently vented to the atmosphere. To study an eruption jet’s dynamics, a multi-institutional team of geophysicists spent four days monitoring Yellowstone’s Lone Star Geyser, which has erupted reliably every three hours for many decades. Similar to other geysers, Lone Star had four distinct event stages. The main eruption stage has a notably unsteady flow with maximum velocities of 16–28 m/s, near the sound speed of the erupting bubbly mixture, and forms a fountain up to 13 m high, as seen in this IR image. The image also reveals some of the conduits within the 3-m-tall mineral-crusted cone. The other stages are relaxation to ambient conditions; recharging during which the plumbing refills; and...
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1 September 2013
September 01 2013
Citation
Stephen G. Benka; Dynamics of a geyser. Physics Today 1 September 2013; 66 (9): 17. https://doi.org/10.1063/PT.3.2106
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