Yellowstone National Park —located partially in Idaho, Montana and Wyoming—puts modern volcanic activity on full display. Near boiling, ominous pools of water in the form of geysers, mud pots, fumaroles (vents that release steam) and hot springs are all present and active in the park and visitors flock to the park to view a handful of thermal features every year during the peak summer visitor season. Coincidentally, this is when a large portion of scientific research also takes place at the park. Combining both the boardwalk paths that are open to all who visit the park and the expansive backcountry, Yellowstone is host to over 10,000 thermal features. These thermal features are fed by superheated water that travels through a complex groundwater system—think the pipes under your kitchen sink—where subsurface water collects gases and chemical compounds en route to the surface. As a result, near-boiling water that bubbles through to the surface is often rife with chemicals like sulfur, iron or magnesium. Early scientists thought of hot springs as uninhabitable, but as it turns out, these conditions are just the right environment for thermophilic (or “heat-loving”) bacteria to thrive.
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The Volcano Beneath our Feet
This summer my family and I vacationed on one of the world’s largest active volcanoes. We weren’t alone. Every year over three million people visit this super volcano.
Yellowstone National Park covers almost 3,500 square miles in the northwest corner of Wyoming (3% of the park is in Montana and 1% in Idaho). The park is famous for its hydrothermal features, including the Old Faithful Geyser and vivid hot springs such as the Grand Prismatic Spring.
The park’s hydrothermal system is the visible expression of the immense Yellowstone volcano; they would not exist without the underlying partially molten magma body that releases tremendous heat. National Park Service website
These features are all visible reminders of the immense volcano that exists beneath the surface. Recently, a team of seismologists discovered a reservoir of partly molten rock 12–28 miles beneath Yellowstone National Park. This video from Science 360 describes the discovery and why scientists are interested in it. It is important to note that this discovery does not mean that there is new activity or that the volcano under the park is closer to erupting. It does mean that scientist now have a better picture of the underground “plumbing”.