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How and why do we collect sediment cores in Yellowstone Lake?

How and why do we collect sediment cores in Yellowstone Lake?

In August 2021, YVO scientists collected sediment cores from the floor of Yellowstone Lake. Analysis of the sediment composition, as well as the...

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Taking Yellowstone seismology to the classroom for some “deep learning”

Taking Yellowstone seismology to the classroom for some “deep learning”

Locating earthquakes in Yellowstone is a time-intensive process that requires the trained eye and extensive experience of a human analyst. But...

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Scientists can now “sniff” Yellowstone gases in real time

Scientists can now “sniff” Yellowstone gases in real time

Much is known about how the chemical compositions of gases vary across the Yellowstone volcanic system, but how they vary in time has remained largely...

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Silver Gate—the Mammoth Terraces of yesteryear!

Silver Gate—the Mammoth Terraces of yesteryear!

Just south of Mammoth Hot Springs, near the north entrance of Yellowstone National Park, lies a jumble of white/gray rock known as the Hoodoos or...

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Locating earthquakes in the Yellowstone region

Locating earthquakes in the Yellowstone region

Ever wonder how seismologists determine the location of an earthquake in Yellowstone?  It’s an intricate process, but thanks to experienced scientists...

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Volcano deformation: What and why?

Volcano deformation: What and why?

The ground surface at Yellowstone goes up and down.  Since 2015 the caldera has been going down at a rate of about 2–3 cm—about 1 inch—per year, but...

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Borehole instruments: The hidden component of geophysical monitoring in Yellowstone

Borehole instruments: The hidden component of geophysical monitoring in Yellowstone

When it comes to data, Yellowstone is a geophysicist’s dream. There is continuous activity from earthquakes, geysers, and of course, the volcano...

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Where is the volcano?

Where is the volcano?

Visitors to Yellowstone ask a lot of questions! So how do park rangers answer when they are asked, “where is the volcano?”

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Relics of past earthquakes: How the 1959 Hebgen Lake M7.3 earthquake may continue to influence Yellowstone seismicity today

Relics of past earthquakes: How the 1959 Hebgen Lake M7.3 earthquake may continue to influence Yellowstone seismicity today

The M7.3 Hebgen Lake earthquake in 1959 is one of the two the largest recorded earthquakes in the entire Intermountain West of the United States.  We...

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“Land of the burning ground”: The history and traditions of Indigenous people in Yellowstone

“Land of the burning ground”: The history and traditions of Indigenous people in Yellowstone

We sometimes think of Yellowstone as an untouched landscape, but humans have been present in the area for over ten thousand years!  The history and...

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Yellowstone’s sibling in the southern hemisphere: Taupō, New Zealand

Yellowstone’s sibling in the southern hemisphere: Taupō, New Zealand

Yellowstone is not the only large caldera system in the world.  Indeed, caldera systems can be found all over the planet!  In New Zealand, the Taupō...

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An outlier of Yellowstone's thermal areas: the travertine of Mammoth Hot Springs

An outlier of Yellowstone's thermal areas: the travertine of Mammoth Hot Springs

Early explorers during the separate Washburn, Hayden, and Hague expeditions of the 1870s were astonished by the massive terraces and pools of hot...

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