Yellowstone National Park. Part 6: “Fire burn and cauldron bubble”!

When my friend Joan and I visited Yellowstone National Park in May 2022, we were interested in seeing other thermal features in addition to the Mammoth Hot Springs. A major part of the Park is actually a super-volcano, with a caldera measuring 43 by 28 miles (70 x 45 km). It has half of all the world’s geysers, as well as other hydrothermal features (i.e., more than 10,000)!

A visit to the Old Faithful geyser was rewarding for Joan, but perhaps less so for me and others who decided to stand outside nearby. (Joan watched from inside a building with viewing windows.)

I’d seen it from afar before but now thought it would be interesting to be closer. When the awaited eruption occurred (happening about every 69 minutes or so in 2022), I hadn’t realized that I would just get soaked and see only spume and clouds! You readers can see an eruption online without getting wet!

    

Information about Yellowstone often reiterates that the geysers and other hotspots are always changing because of the geothermal dynamics propelling them. Earthquakes can affect them, and human vandalism can also end a geyser’s “life”. For example, in the 19th century, visitors would throw coins into geysers, which eventually plugged up the vents. (No one claims that the visitors pictured here did this; these parents must have been preoccupied keeping watch over their large brood!)


Photo on display in the Park Museum

When I was in high school, our assigned reading included older English texts, including work by Shakespeare. I found the stories interesting, but the language used did not appeal to me, except for an occasional phrase. The line “Fire burn and cauldron bubble” from Macbeth has a nice rhythm and it came to mind when we stopped to watch the mud pots.

The mud pots are hot springs which are so acidic that they dissolve the rock around them. Microorganisms help convert the emerging hydrogen sulfide gas into sulfuric acid; that breaks the nearby rock into a porridge-like clay which bubbles as gases gurgle through them.

Waiting for shapes to emerge from the thick moving masses was not at all boring. Instead, it made for a nice quiet, contemplative time — and judging by how many people were standing quietly and waiting for shapes to pop up, this was a shared experience. A video of one mud pot can be seen by clicking this link.

The area known as the Artists’ Paintpots was more colorful, even though we didn’t have sunny weather to highlight their hues.

There was vegetation here and there, making for some interesting scenes.

  

The Norris Geyser Basin is Yellowstone’s oldest, hottest and most changeable area. The National Park Service notes: “Norris has the greatest water chemistry diversity among Yellowstone’s hydrothermal areas. Multiple underground hot water reservoirs exist here and as their water levels fluctuate, concentrations of chloride, sulfate, iron, and arsenic change. Although Norris is known for its acid features, it also has alkaline hot springs and geysers.”

Norris has two main areas. The Porcelain Basin is bare of trees and vegetation. The Porcelain Springs, named for the milky colors of the deposited minerals, are the fastest changing area in the Norris Geyser Basin.

Fumaroles, the hottest hydrothermal features (up to 280°F/138°C) dotted the landscape in the Porcelain Basin. Where the steam and gases spewing from the holes are rich in sulfur, the feature is called a solfatara. Where the gases are mostly carbon dioxide, the fumarole is called a mofette. The sound of the fumarole can be quite loud, as in this video, sometimes sounding like hissing or whistling.

The Back Basin area has more wooded scenery. It was fascinating to see that there were mounds of bison dung in various places near fumaroles. I asked a park ranger how the bison could travel in those areas and whether they were ever injured.

 

She said that groups of bison will rest around the vents in winter. Their heavy fur apparently insulates them well and they can withstand the heat. She did note, however, that bison have been seen with burns on their legs, so they can be somewhat hurt by the heated clay ground.

 

Visitors should stay alert even when remaining on boardwalks. In 1989, the Porkchop Geyser threw rocks into the air; fortunately, no one was hurt.

In the early Park days, visitors were invited to bathe in the hot pools but that is fortunately no longer the case.

  

Where thermal colors are green, chlorophyll-containing algae predominate.

Where yellow is the dominant color, sulfur abounds and heat-loving and -tolerant creatures (thermophiles) use it to create energy.

The Cistern Spring is a beautiful pool that shows blue, green and brown colors with sunlight. These colors are produced by thermophilic algae and bacteria. They, in turn, are accompanied by tiny insects, such as ephidrid fly larvae that feed on bacteria. Spiders and dragonflies then feed on the flies.

We returned a couple times to see some of the famous features because the first day we visited them, it was rainy and then snowed with lots of cold wind. There was so much steam we could scarcely see the colored pools of water; only some features close to boardwalks were clearly visible.

Signs warned that it was a windy area, and the warning was certainly warranted! (Even so, some visitors were perturbed and complained about being subjected to sleet and flurries during their outing!)

The Excelsior Geyser used to erupt regularly in the 1880s and then stopped. In September 1985, it erupted again for 47 hours and again stopped. It was dormant and not very visible during our visit.

At Grand Prismatic Spring, which has stunning blue, green, yellow and rusty orange coloring, we saw mostly gray steam and mud-like rivulets on one visit.

I spoke with a man in a group of people including grandma, who was heavily bundled up in a wheelchair. He remarked that they had been there the previous day, when it was warm, sunny and scarcely windy at all. (Spring weather is extremely changeable at Yellowstone, not only day to day but within a day as well.) Their group had seen the beautiful colors of the Grand Prismatic and it made for a perfect outing since they had come to celebrate a wedding held on the spot. That was really an auspicious start to the married life of the lucky couple!

All in all, we didn’t get many spectacular views of the colorful thermals, but we did learn a lot. A future visit with warmer and sunnier periods would be something nice to anticipate. Nevertheless, the cold, windy, and partly wet days certainly did not dampen our overall enthusiasm. The visions of bubbling mud pots will last a long time, too.

Next up: a few blogs with some of my springtime sightings and then a visit back to Yellowstone to see some small mammals and Western birds.

Yellowstone National Park: Part 2B.  The living creatures of Mammoth Hot Springs

Continuing our tour through the Mammoth Hot Springs. It was a surprise for me to learn that the hot spring colors are produced by living creatures! Thermophiles are microorganisms that thrive in heat. Those living in the hottest water are colorless or yellow.

The people of the Shoshone and Bannock tribes came to Mammoth to collect minerals to make white paint.

Cooler waters contain orange, brown and green thermophiles. Sunlight also influences which colors you may see.

 

 

When hot springs rise up through limestone, they dissolve calcium carbonate. The resulting calcite is then deposited, creating travertine terraces.

These are the Palette Spring terraces coming down from the thermal pool above them.

.To my surprise, there were quite a few birds hopping about, including a chipping sparrow (Spizella passerina) and very colorful yellow-rumped warblers (Setophaga coronata).

 

Mountain bluebirds (Sialia currucoides) were a delight to see.

 

The trail through the Hot Springs complex winds around for more than 2 miles. As I was walking along one area at the bottom of a steep hill, some fellow tourists approaching me said there was a coyote going up the hill further on. I hurried on and caught sight of him as he neared the top.

You reach the Upper Terraces by climbing steep stairs.

There were more trees along the upper pathway with fumaroles (venting steam) nearby.

I did catch sight of some eagles soaring over the large flat springs expanse, but I was happy to go back down to the lower terraces. (Unfortunately, sliding my gloved hand down a wooden railing on the descent gave me a splinter in my palm that I did not manage to get out completely. I had a very sore hand for quite some time: unwanted souvenir!)

I lost track of exactly which places had which names — looking them up on the Internet is not always helpful because the Mammoth features have changed considerably over time. When a hot spring remains dormant for a long time, it will eventually be covered by soil and again create an environment for trees and flowers. To complicate matters, the names of sites have changed over time.

The name Cleopatra Spring has been given to at least three different sites over the years. The original Cleopatra Spring eventually came to be called Minerva Spring. This was, I believe, the current Cleopatra Terrace.

 

When trees are flooded by hot water, they absorb calcium carbonate. This hardens their veins so they cannot absorb “normal” water and nutrients and they harden into what look like petrified trees which may stand for decades.

The hot springs were an early commercialized attraction for those seeking relief from ailments in the mineral waters.

Today, to preserve these unique and fragile features, soaking in the hot springs is prohibited.

Next stop in Yellowstone: The adorable red dogs!

Yellowstone National Park: Part 2A. Mammoth Hot Springs and women in the park

On 19 May 2022, Joan and I had our first full day in Yellowstone National Park (YNP).  This two-part blog covers what we did in the morning: an excursion to the Mammoth Hot Springs, only 5 miles from the Gardiner/Roosevelt Arch entrance. Shortly after passing through the gate, we caught sight of a river running alongside the road. We had no idea that within 20 days, this river would rise and take out part of the road on which we traveled! The recovery effort has also been phenomenal and the National Park Service has done a great job opening up the park again.

About 10 minutes into the park, Joan called out that she had seen a bear! She pointed to my side of the road and, looking up, I saw the bear on a hillside beside some rocks — she was enormous (perhaps the biggest we saw). She was also accompanied by offspring so I began scrambling to get my camera. By the time we got to a pull-off, they had disappeared behind big boulders and did not reappear. She looked somewhat like the (blurry) bear below that we saw another day when we couldn’t stop (rangers were present and moved everyone along). This spotting was certainly an exciting beginning to our YNP adventure.

This sighting taught me that Joan would be an excellent wildlife spotter even when guiding the car along winding roads with sometimes steep drop-offs at the side! It was cold our first day and we dressed warmly – long pants, sturdy shoes, sweaters, warm jackets and caps.

I was glad that we didn’t have to gallivant around in the long dresses and headgear worn by the first women who visited the park. However, the early female visitors to YNP were no “delicate flowers” as I learned from a book of their writings (Sidesaddles and Geysers: Women’s Adventures in Old Yellowstone. 1874 to 1903. Edited by M. Mark Miller).

Carrie Strayhorn wrote, after her 1882 visit to YNP, that both men and women clambered all over the mineral deposits. She and her party traveled about 400 miles on horseback through the park, leaving her with memories of “the charms of nature which go with the wilderness and wonders in all their primal glory.” Strayhorn visited Mammoth Hot Springs and we made that our first stop. (Photo from “Fifteen Thousand Miles by Stage (1911) by Carrie Adell Strahorn)

At the entrance to the Mammoth site, we were met by brown-headed cowbirds (which we have in North Carolina) and black-billed magpies (Pica hudsonia).

The first thermal feature we neared is called the Hymen Terrace. Old records kept at the University of Wyoming Libraries contained an enthusiastic description of this site.

As our day had started off quite overcast, this thermal did not look very colorful or terribly fascinating, so we moved on to walk along the trail.

Off to the side was a structure of some 37 feet in height (11 m) known as the Liberty Cap.

It received this name in 1871 from people who thought it resembled the caps worn by French revolutionaries who fought for freedom and liberty. It looked a bit more interesting when the skies cleared and the sun appeared.

The Mammoth site’s thermals mainly include hot springs and travertine terraces. Joan generally walks much faster than me and I stop often to photograph, so we split up to see the sights.

As Joan took off down a boardwalk, I stopped to photograph my first view of a Clark’s nutcracker (Nucifraga columbiana). I hadn’t expected to see many birds around the thermals so it was a welcome surprise.

 

Hot springs are Yellowstone’s most common thermal features. They comprise pools, sometimes quite deep, of heated water that may be calm and clear or froth like boiling water.

Rain and snow bring water that seeps into the earth where it is heated. It is still not certain which volcanic heat source is responsible for this.

It might be the magma chamber underlying the Yellowstone Caldera or another smaller place nearby. According to researchers, only 10% of the water in the Mammoth area is above ground at any one time.

What looks like steam arises from the hot springs and this seemed to be especially the case when we were viewing them in colder temperatures. Here you can see how our view of the Palette Spring changed as the day started warming up.

 

Read on to find out what causes the colors in the hot springs!