Today,Peggy and I are continuing our exploration of Yellowstone National Park, which we visited as part of our four month, 12,000 mile exploration of the US between September and December this past year. All photos in this post were taken by either Peggy or me unless otherwise noted.
If you are visiting Yellowstone National Park, be sure to visit the colorful travertine terraces of Mammoth Hot Springs.
Located 50 miles north of Old Faithful, the travertine terraces of Mammoth Hot Springs are one of the most unique and beautiful of Yellowstone’s hydrothermal created landscapes. The terracing is a result of underlying limestone. Hot water dissolves the limestone and deposits it on the surface. The bright colors, like the colors of the hot springs in the Yellowstone Caldera to the south, are created by thermophiles, tiny microorganisms that thrive in the hot springs. Different types of thermophiles have different tolerance for the heat and come in different colors based upon their exposure to sunlight. Those that can tolerate the most heat live deep in the pools and tend toward blue and green. The ones living on the cooler outer edges are more in the brown and yellow range.
Peggy and I took a day to drive up from where we were camped in the town of West Yellowstone to visit Mammoth Hot Springs. On the way up we saw a lot of great scenery that I will feature in another post and two hydrothermal features I haven’t covered in this series yet: mud pots and fumaroles.
Mud pots occur when hot thermal water is flowing under a layer of clay that blocks the water from escaping to the surface. Steam from the water, however, is able to make its way through the clay. Certain microorganisms convert the sulfur dioxide in the steam to sulfuric acid which turns the clay into a gooey, sticky consistency. Bubbles are created as a result of the steam bubbling up through the goo. It sound like plop, plop, plop. I included this exploding bubble in an earlier post. I liked it so much you get to see it again.A fumarole is similar to a geyser but lacks the water to create eruptions. Instead, the heat from the volcanic rocks turns what water is available into incredibly hot steam that escapes from vents and ranges in temperatures up to 280°F (138°C). It can be noisy. This is a shot of Roaring Mountain that received its name from the noise created by the escaping steam. It could be heard from miles away in the 90s. It’s quieter today.
And now it’s time to visit the terraces of Mammoth Hot Springs. A convenient road takes you around the terraces. Walkways off the road take you to the lower terraces. The following photos were taken from the walkways.
Canary Springs is one of the most popular sites along the lower terrace trail at Mammoth Hot Springs.A broader, softer perspective of Canary Springs.A view of the travertine terrace just above Canary Springs.Another perspective of the terrace just before the water flows over the edge.Cupid Springs. I don’t have a clue on how it got its name.Umpteen shades of grey.
The road snakes around the upper terrace. There are several pullouts that allow close up views of the various formations.
This section is known as Angel’s Terrace. I’m assuming it’s because of the white travertine, which is how the dissolved lime comes out of the ground.Another perspective. Like stair steps.We really liked the contrast of colors here.It was the colors, shape and tree that caught our attention that had us pull out our cameras.This unique dome is known as Elephants Back.We were driving back to West Yellowstone when we came across this very colorful small dome. The steam coming from the back suggests a fumarole. We simply had to stop and photograph it. That does it for today. Our next post will be on Heidelberg Castle. After that, it will be back to Yellowstone and its scenic beauty.
Wandering through Time and Place 