September 25, 2018: Cool! (in a manner of speaking)
The ground "breathes" thermal feature grows w/ voracity.
— USGS Volcanoes🌋 (@USGSVolcanoes) September 25, 2018
#Yellowstone is NOT about to erupt (now that's out of the way).
Changes afoot in @YellowstoneNPS
#UpperGeyserBasin. Water eruption of #EarSpring (photos, before & after) on Saturday, Sept 15 & other features on #GeyserHill behaving strangely. Read more: https://t.co/1jzhI7i8TD pic.twitter.com/rwKaBhiTJ4
— USGS Volcanoes🌋 (@USGSVolcanoes) September 19, 2018
Here is the whole article (click this link to get images):
Recent Changes to Thermal Features Closes Part of Upper Geyser Basin
September 19, 2018
In the past week, there have been changes afoot to the thermal features on Geyser Hill in Yellowstone’s Upper Geyser Basin. Ear Spring, a normally docile hot pool, had a water eruption that reached 20 to 30 feet high on Saturday, September 15, 2018. The eruption ejected not only rocks, but also material that had fallen or been thrown into the geyser in years past, like coins, old cans, and other human debris. The last known similar-sized eruption of the spring was in 1957, although smaller eruptions occurred as recently as 2004. As a result of these changes, Yellowstone National Park has closed portions of the boardwalk.
Undoubtedly, the most famous thermal feature of Yellowstone National Park’s Upper Geyser Basin is Old Faithful. Geyser Hill is located just across the Firehole River from Old Faithful and hosts dozens of other hot springs, geysers, and fumaroles. Hydrothermal activity at several features on Geyser Hill has changed since the eruption of Ear Spring. Most notably, a new feature has formed west of Pump Geyser and north of Sponge Geyser directly under the boardwalk. The feature erupted overnight between September 18th and 19th and continues to pulse water as a small spouter. An approximately 8-foot diameter area of surrounding ground is “breathing” – rising and falling by about 6 inches every 10 minutes. Several other thermal features are more active than usual, including geysering and boiling of Doublet Pool and North Goggles Geyser.
Changes in Yellowstone’s hydrothermal features are common occurrences and do not reflect changes in activity of the Yellowstone volcano. Shifts in hydrothermal systems occur only the upper few hundred feet of the Earth’s crust and are not directly related to movement of magma several kilometers deep. There are no signs of impending volcanic activity. There has been no significant increase in seismicity nor broad-scale variations in ground movement.
The outcome of the current changes on Geyser Hill in the Upper Geyser Basin is uncertain. The two most likely possibilities are:
- The area of thermally heated ground may expand and continue to cause changes in hydrothermal activity that persist for years, much like the thermal activity of 2003 in the Norris Geyser Basin. This could necessitate rerouting of the current boardwalk configuration.
- A small hydrothermal explosion could occur in the area, forming a crater a few feet across and ejecting rocks and hot water up to a distance of hundreds of feet, much like that which occurred at Porkchop Geyser in the Norris Geyser Basin in 1989.
Although potential impacts to Old Faithful are unknown, Geyser Hill and Old Faithful have separate hydrothermal plumbing systems and behave independently.