New geyser appears in Kamchatka
Its not every day that a new geyser appears out of the blue, but that is exactly what appears to have happens in Kamchatka, as the Prikolny ("Peculiar") Geyser has appears near Uzon caldera.
I write the Eruptions blog on Big Think. I've been mesmerized with volcanoes (and geology) all my life. It helps that part of my family comes from the shadow of Nevado del Ruiz in Colombia, where I could see first hand the deadly effects of volcanic eruptions. Since then, I've taken a bit of a winding path to become a volcanologist. I started as a history major at Williams College, almost went into radio, but ended up migrating to geology, including an undergraduate thesis on Vinalhaven Island, Maine. I followed this up by changing coast to get my Ph.D. from Oregon State University. Then I ran a MC-ICP-MS lab at University of Washington for a spell (and wrote for an indie rock website). I spent three years as a postdoctoral scholar at University of California - Davis studying the inner workings of magmatic systems. I am now an assistant professor at Denison University and have projects in New Zealand, Chile and Oregon.
I am fascinated by volcanoes, their eruptions and how those eruptions interact with the people who live around the volcanoes. I started this blog after getting frustrated with the news reports of volcanic eruptions. Most of them get the information wrong and/or are just sensationalistic. I will try to summarize eruptions as they occur, translate some of the volcanic processes that are happening and comment on the reports themselves.
And no matter what people tell you, I definitely do not have a cat named Tephra. (OK, I do).
You can find out more about my research by visiting my website. If you have any comments, questions or information, feel free to contact me at eruptionsblog at gmail dot com.
Hydrothermal fields are tricky beasts. They can wax and wane as the magmatic system heats and cools, as the water table rises and falls and as other events such as earthquakes or explosions might change the conduit systems. Changes are relatively common, as we've seen in recent events in the Yellowstone Basin and with the changes within the Waimangu Valley in New Zealand. Understanding the cause-and-effect relationships in these fields can be a challenge even to the most seasoned volcanologist.
Prikolny Geyser near Uzon Caldera in Kamchatka. Image taken in July 2009.
Case in point is the new geyser that has appears on the Kamchatka Peninsula in Russia. Dubbed the "Prikolny Geyser" (more or less "Peculiar"), it was first noticed in the spring of 2009. The geyser is located 14 kilometers' from
Eurasia's only geyser field,** the "Valley of Geysers" - the valley was inundated by a landslide in 2007 that covered almost half the geysers. The Prikolny Geyser appears to have a periodicity of ~6-20 minutes between eruptions, but oddly it seems that the geyser recycles the water it erupts (video link). It is unclear from the article exactly how we know that all the water is being recycled - you might expect that there should be some net loss during the eruption - but the geyser spouts the water 5 meters / ~15 feet, and then it all trickles back into the geyser to do it over again.
The Valley of Geysers and Prikolny Geyser are both located near the Uzon caldera (below), and this is likely the source of heat for the hydrothermal features. This caldera (along with the Geyzernaya Caldera) form a fairly sizeable one at 7x18 km depression and last erupted ~7700 years ago. This eruption wasn't the caldera-forming eruption but rather some silicic domes and maars (volcanic crater formed by a phreatomagmatic - water-related - eruption). The caldera-forming eruption, however, was a big one, ejecting 20-25 km3 of pyroclastic material from the caldera. This eruption likely occurred somewhere around 39,000 years ago (or more recent). Periodic hydrothermal explosions occur in the depression as well, most recently in 1986.
Uzon Caldera, Russia
Concerning the new geyser, Valery Droznin of the Kronotsky Nature Reserve speculates that the geyser might be the result of an overactive hot spring, but why the hot spring might be pulsating to form the geyser is unknown. The geyser is being monitored by rangers in the Nature Reserve for temperature, periodicity and any changes that might occur. If you want to take a peek at the area, there is even a webcam for
Prikolny GeyserValley of the Geysers. It will be interesting to see how long the geyser might last in this location and what it might say about any regional changes to the hydrothermal fields of the Uzon caldera.
**Note (July 10, 2009): Dr. Aldo Piombino pointed out to me that the Valley of Geysers is not the only geysers in Eurasia:
In Tuscany, there were geysers that now are used for geothermal power plants at Larderello, Tuscany (with others artificial holes). In some zones of the area (Sasso Pisano) there are still volcanic steams and hot waters with little geysers near the Etruscan termal area. Beneath Larderello there is a granodioritic pluton 3.5 MY old, wich is still hot because a thick shales level has not allowed thermal water-driven heat.
Thanks for the correction, Aldo!
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