Yellowstone

Yellowstone Volcano receives ample attention for being a large, active, caldera-forming volcanic system. Given the massive eruptions over the last 2.1 million years, our focus on Yellowstone is understandable. However, hidden in its metaphorical shadow is another volcanic complex – the Absaroka Volcanoes.

The interactive Geology of Yellowstone Map has been updated with new data. Check out recently added map layers that highlight Yellowstone’s monitoring instrumentation, hydrothermal features, and more!

The Yellowstone hotspot—the source of heat that powers Yellowstone’s vast volcanic system—has long been thought to have initiated about 17 million years ago.  A growing volume of evidence, however, suggests that it has been around much longer.

Results from laboratory experiments have provided significant insights on many fundamental physical and chemical processes on Earth. They also add insights into the Yellowstone hydrothermal system that could not be obtained otherwise.

Yellowstone hosts thousands of thermal features which have diverse chemistries and origins. The most iconic features, like Old Faithful, have neutral to alkaline pH. Some Yellowstone features, however, can be acidic enough to break down the very rock that hosts them!

The tallest active geyser in the world has been erupting at a record pace since March 2018. Why are eruptions so energetic, what influences the intervals between eruptions, and why did Steamboat reactivate in the first place?

Although 2020 may not have been a great year for many of us, it was a pretty interesting year in Yellowstone.  With this first Yellowstone Caldera Chronicles article of the new year, let’s take the traditional look back at what happened in Yellowstone during the previous 12 months,

Although Yellowstone Lake itself may seem calm, the floor of the lake is littered with hydrothermal explosion craters.  Detailed studies are beginning to reveal the details of these explosions, like the one that formed Elliott’s Crater about 8000 years ago.

Geology is inherently a three-dimensional science—it’s not just about what is at the surface, but what is beneath the surface as well. This is especially true at Yellowstone, where complex geology controls subsurface geyser plumbing systems. Fortunately, a long history of scientific drilling has pulled back the curtain on this hidden world!

Yellowstone National Park is known for its unique hydrothermal features and array of animals and plants, but what about its fossils? From tiny invertebrates to large marine reptiles, Yellowstone’s boundaries include a wide range of paleontological resources that date back over 500 million years.

Have you noticed that there has been an increase in the number of earthquakes happening in Yellowstone over the last week?  This is because there is an active earthquake swarm occurring beneath Yellowstone Lake!  Although it looks impressive, it pales in comparison to past sequences, including the 2008–2009 Yellowstone Lake swarm.