Yellowstone National Park is home to some 10,000 thermal features, over 500 hundred of which are geysers. In fact, Yellowstone contains the majority of the worlds geysers. Within Yellowstone's thermal features can be seen the product of millions of years of geology at work. Much of Yellowstone sits inside an ancient volcanic caldera (the exploded crater of a volcano). The last major caldera forming eruption occurred 600,000 years ago. For hundreds of thousands of years following that, subsequent lava flows slowly filled in most of the caldera. Even now, in some places, nearly molten rock resides as little as 2-5 miles below the surface. Heat from the volcanic activity makes its presence known by heating ground water and creating the thermal features we now see. The four basic types of thermal features present in the Park are geysers, hot springs, fumaroles, and mudpots. Many of these are concentrated in Yellowstone's major geyser basins: Upper, Midway, Lower, Norris, West Thumb, Shoshone and Heart Lake. |
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Yellowstone's Thermal Features
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Upper
Geyser Basin
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The Upper Geyser Basin has the largest concentration of geysers in the world. Learn more about the basin by following this link. |
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Lower
Geyser Basin
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Located in the Lower Geyser Basin are some very interesting and easy to see thermal features including some very nice mud pots. Learn more about the basin by following this link. |
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Norris
Geyser Basin
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Norris Geyser Basin is the hottest and most changeable of Yellowstone's geyser basins. Learn more about the basin by following this link. |
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Mammoth Hot Springs
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The formations at Mammoth Hot Springs are formed differently than the formations in the geyser basins. The sinter formations of the geyser basins are formed when silica dissolved from rock deep underground, by extremely hot water, is deposited at the surface when the water cools. The travertine terraces at Mammoth are formed from limestone deposited when carbon dioxide gas is released from the warm limestone impregnated water that reaches the surface at Mammoth. The carbon dioxide makes the water slightly acidic allowing it to dissolve and carry large amounts of limestone in solution as it flows underground to Mammoth. Once the water reaches the surface, the carbon dioxide is released and the limestone falls out of solution and is deposited as travertine terraces. This deposition can be quite rapid, sometimes being measured in feet per year. By comparison, sinter deposits in the Upper Geyser Basin are measured in inches per hundred years. As might be expect from such rapid deposition, water flows at Mammoth are constantly being redirected. Water is the life blood of the terraces. When the water stops, they dry up and disintegrate. Thus, the activity at Mammoth changes quickly. There are few places that geologic changes occur so quickly. As of July 1997, the best activity at Mammoth was at Minerva Terrace and at Canary Spring. Both of these must-see attractions are located on the Main Terrace. It is easiest to explore the Main Terrace in two parts. First, park your car at the bottom, preferably at the eastern most parking area. (It is the highest in elevation of the parking areas at the bottom and the one most distant from the town site). From there walk the loop trail of the lower portion of the Main Terrace. Be sure to pass by Minerva Terrace. Once you've done this, then, return to your car and drive to the one way, Upper Terrace Drive. In this way you will avoid the steep stairs to the top of the Main terrace. On the Upper Terrace Drive be sure to stop at the Main Terrace Overlook and take the trail on the far right to Canary Spring. For the past few years, Canary Spring has been truly spectacular. |
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Mud Volcano Area
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The activity at the Mud Volcano area is interesting and worth exploring. The temperatures here are lower than at the geyser basins. In most cases, what looks like boiling is actually just the evolution of gasses, especially carbon dioxide. |
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Some Other Geyser
Basins
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Yellowstone
Travel Guide | Yellowstone's Geysers
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