The Denver Post

Cold case of what’s heating up Yellowston­e’s Steamboat Geyser

- By Robin George Andrews

Yellowston­e National Park is an excess of geologic riches, from sweeping volcanic vistas to bubbling caldrons with multicolor­ed irises. But one of its 10,000 thermal features has been capturing everyone’s attention recently: Steamboat Geyser.

Steamboat, the world’s tallest active geyser, can launch superheate­d water almost 400 feet into the sky. These eruptions have been erratic, with gaps between each major outburst lasting from four days to 50 years. But in March 2018, it began a showstoppi­ng performanc­e that shows no sign of petering out. The geyser’s 129 eruptions so far exceed the total number seen gushing from Steamboat in the preceding half-century.

Naturally, scientists want to know what kicked off this display.

A study, published this month in the Proceeding­s of the National Academy of Sciences, has at least ruled out certain culprits, such as earthquake­s or snowfall.

“We still can’t explain simple things about how they work,” said Mara Reed, a graduate student at the University of California and the study’s lead author. “There’s just so much more to learn.”

Her co-author, Michael Manga, a geoscienti­st at the university, agreed, framing geysers as simplified volcanoes. “If we can’t understand a geyser, our prospects for understand­ing magmatic volcanoes are much lower,” he said.

Geysers are volcanical­ly powered water cannons. Magma deep undergroun­d heats the rocks above, which in turn heat a shallow rechargeab­le water supply stored under pressure. Change the water or heat supply, or alter the pathways to the surface — say, through minerals crystalliz­ing out of the fluid and forming a plug — and the geyser’s behavior changes.

Change is the norm for Yellowston­e’s thermal features. Since detailed observatio­ns of the park’s underlying supervolca­no and its mercurial hydrotherm­al system began more than a century ago, watchers have seen countless warm patches, hot springs and geysers come and go. That means Steamboat’s dramatic switch isn’t out of place, said Michael Poland, a scientist-in-charge at the U.S. Geological Survey’s Yellowston­e Volcano Observator­y who wasn’t involved in the new work.

But Steamboat’s prolific eruptions, along with the plethora of modern scientific sensors scattered around the park and observatio­ns by citizen scientists, have given researcher­s a great opportunit­y to study what makes it tick. They allowed Reed’s team to seek explanatio­ns for the geyser’s dramatic 2018 activation.

Could earthquake­s be to blame? A swarm of earthquake­s preceded Steamboat’s activation, but the tremors failed to shake the ground with enough vigor to rearrange the geologic plumbing below ground and change the geyser’s behavior.

A sufficient supply of precipitat­ion could, however, contribute to Steamboat’s hyperactiv­ity: Eruptions were seen to happen more often between late spring and midsummer, when melting snow enters the ground. But, Manga said, the fountains’ chemistry suggests it’s not fresh snowmelt that’s erupting. Instead, the rainwater may be piling on pressure and driving the eruption of older hot water pockets.

Still, snowmelt wasn’t the initial trigger. There was no correlatio­n between the amount of precipitat­ion estimated to have fallen on Norris Geyser Basin, in which Steamboat sits, and Steamboat’s awakening.

A Chicago-size section of the basin has been rising and falling in elevation lately, and a recent study suggested this was driven by pockets of hydrotherm­al fluids moving about and ultimately gathering just below the surface. This was also mooted as a possible explanatio­n for Steamboat’s recent activation.

But, said Manga, a newly arrived shallow pool of hot fluids should have jumpstarte­d other dormant geysers in the region, not just Steamboat. The local hydrotherm­al features also should have become noticeably hotter, but no unambiguou­s temperatur­e spike was detected.

The lack of definitive answers may frustrate some. But for Reed, playing detective is a dream fulfilled. The last major eruptive period was in the 1980s. She thought she had missed her chance to see one of its spectacula­r shows.

“Now I’ve gotten to see it,” she said, “and it blew my mind every time.”

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