Tag Archives: Yellowstone National Park

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

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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 5. Grizzlies, coyotes and pronghorns – oh my!

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Note: this long posting is likely nicer to see on a laptop than a phone!

During my first spring visit to Yellowstone National Park in 2016, we encountered black bears (Ursus americanus) throughout the national reserve. When a mother bear with her little cubs was spotted, park visitors stopped often to watch the playful young, especially when they were practicing tree climbing.

During my 2022 visit, we did not see black bears but had the good fortune to see quite a few grizzly bears (Ursus arctos horribilis). Some were quite light in color, while others had dark fur. A mama grizzly and her cub were the first mammals we saw (due to my friend Joan’s sharp eyes!) and we must have seen at least one or two every day. (If not a live bear, there were plenty of them featured in artwork in Gardiner.)

Rangers were often present at our sightings or arrived shortly after we did. They mostly warned humans to keep considerable distance from the bears, but we also saw them shooing the bears away from roads when many people were passing by.

(The bears below were shooed back up the hill; the white spots on the photo are snowflakes.)

The “hump” on the grizzlies’ shoulders helped us identify them since black bears lack this feature. Also, when walking on all fours, the grizzly’s rump is lower than its shoulders. The impressive grizzly claws are also much longer than those of black bears.

Sometimes we spotted the grizzlies grazing far away in fields. A few times, we had the good fortune to spot a mother bear with her young cubs.

One mother in particular gave us wonderful views as she wandered about with her triplets. That was lucky for us as grizzlies have one of the lowest reproductive rates of North American terrestrial mammals.

They are not sexually mature before the age of 5 years. After mating in the summer, implantation of the embryo is delayed until the female hibernates. She could miscarry if she does not ingest sufficient calories and nutrients during the summer. She also will not mate again until her cubs have reached three years of age.

One of the most interesting foods that the grizzly bears eat is the adult form of the army cutworm, called the miller moth (Euxoa auxiliaris). This moth has the highest known percentage of body fat of any animal, comprising up to 72% of its body weight! The moths fly from low-lying farmlands to crevices in mountain slide rocks, where the bears go in late summer to dig them out. It’s estimated that a grizzly can eat up to 40,000 moths in a day, thereby ingesting up to 20,000 calories.

One of the grizzlies’ competitors for food, particularly carcasses, are the coyotes (Canis latrans). These beautiful canids are unfortunately detested by many people, as related by Dan Flores in his informative book Coyote America: A Natural and Supernatural History.

At one point, we saw numerous cars parked along a road and stopped to see what everyone was observing. There was a coyote feeding on a large carcass that had already been partly consumed.

The coyote was engrossed in getting some meat off the bone, which was apparently not an easy task. These canids usually eat deer and smaller prey such as little mammals (rabbits, hares, rodents), birds, reptiles and amphibians, and invertebrates. It was not entirely clear to me what this prey had been.

A fascinating coyote behavior is that they sometimes collaborate with badgers to dig up rodents. They even appear to like these fierce predators as people have seen coyotes licking a badger’s face or laying their heads on the badger’s body. A decorated jar found in Mexico dating back to the years 1250-13oo showed this relationship.

Unfortunately, although the coyote figures prominently in Native American/Indian folklore, the US government has initiated and supported efforts to eradicate the species altogether. From 1947 to 1956, about 6.5 million coyotes were killed in the American West. However, these intelligent animals have managed to survive and eventually spread to the eastern United States (where they are now again unfortunately detested by considerable numbers of people).

In Yellowstone, the larger ungulates on which the predators such as bears, coyotes and wolves feed include elk and moose. As mentioned in a prior blog, elk (Cervus canadensis) can be seen up close in Gardiner, the town at Yellowstone’s northern entrance, where they wander through the streets and rest in people’s yards. A more melodious name for them is wapiti, used by the Shawnee and Cree peoples. It refers to the animal’s white rump.

To me, the elk appeared quite large but they “only” measure about 4-5 feet in height. The males’ antlers can grow up another 4 feet, however, giving them a much taller appearance.

The males also have another interesting characteristic — their bugling, which is used to attract mates and mark their territories. This sound is the loudest call of any members of the deer family. The males produce it by roaring and whistling simultaneously!

Because elk prefer colder weather, they are more visible to Yellowstone visitors in the late autumn, winter and early spring. We saw females and young elk in town and spotted the males out in the valleys. They are very social animals and one of the largest herds (about 11,000 members in 2022) is known as the “Jackson Elk Herd”, which migrates between southern Yellowstone and the National Elk Refuge in Wyoming.

The other large, hoofed animal which we glimpsed one day was a moose (Alces alces). This ungulate is the largest member of the deer family, reaching a height of 6 feet (1.8 m) and a weight of up to 1,000 lb (450 kg).

We saw a male — identifiable by the antlers which were just beginning to grow — as he grazed in a marshy area beside the road.

Besides eating tree and shrub bark, leaves and twigs, they enjoy eating aquatic plants in ponds and streams. This can have a downside for them. Sometimes, they unknowingly eat snails while foraging and the snails can carry parasitic brain worms.

In Gardiner, we also often saw mule deer (Odocoileus hemionus). They can be distinguished from white-tailed deer by their large ears, which measure about 75% of the length of their heads!

They also have a white tail with a black tip, while white-tailed deer lack that feature.

I found them to have a sweet face.

The final ungulate that we had the pleasure to see at Yellowstone were the fast-footed pronghorn antelopes (Antilocarpa americana).

These small-hoofed creatures are not as fast as cheetahs but can sustain their speedy gait for a longer period of time, reaching speeds of up to 60 mph.

The pronghorns not only travel rapidly; they also may travel for long distances. During the winter of 2011, monitoring of a pronghorn herd showed that they had achieved the longest terrestrial migration in the continental USA (not counting Alaska).

While both sexes have horns, those of the female pronghorns are mere bumps, while the males display unique backward-pointing horns that grow up to 12 inches long. (The one grazing below had impressions in the fur on its back that looked like claw marks to me!)

According to the Natural Resources Conservation Service of Montana, “Pronghorns existed in North America at the same time as predators like the dire wolf, saber-toothed cat, and American cheetah, all of which are long extinct. Scientists believe the pronghorn’s excellent vision and extreme fleetness are adaptations to survive these super predators.”

It’s fascinating that so many of the animals living in Yellowstone National Park have been in this area for thousands of years. An upcoming blog will feature smaller mammals after taking another visit to thermal attractions in the park. Before that, I’ll post a couple blogs about some of the wildlife I’m seeing here at home. 😊

Yellowstone National Park: Part 4. An unplanned and unexpected encounter!

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As my friend Joan and I traveled through Yellowstone, we saw bison everywhere, in herds, small groups and sometimes in pairs or alone. Quite often this was on the road, so that we needed to be aware it might take us longer than planned to get to a particular place.

The many reports of human-bison encounters which I had seen and read about over the years made me quite aware of how dangerous it can be for a person to come close to a bison. They are huge animals – adults weighing between 1,200-2,000 pounds and standing 4-6 feet tall. If provoked or alarmed, they can be quite dangerous.

I was not above making derogatory comments about how thoughtless people took risks when they approached bison. For example, one day we stopped along a road and watched bison crossing the Yellowstone River, swimming with difficulty against the rapid currents.

Some park visitors had stopped down the road and a couple got out and descended into the valley, headed for the river. They apparently were hoping to get some close-up photos and I made some disparaging remarks about how they were taking unnecessary risks and should turn around.

A few days later, however, I discovered that not all encounters are the result of thoughtlessness.

Joan and I had stopped at a valley overlook where Park authorities had laid out a walking trail. It was a good distance from any hills and several people were out hiking the trail. As we both like to walk, we decided to go down to the trail as well.

As Joan walks faster than me and because I stop often to photograph, she went on ahead. I meandered along taking photos of plants, birds and what I thought were prairie dogs, but which were likely Uinta ground squirrels. There were some bison far down the valley, but they were mostly heading up into the hills, so we felt ok walking on the trail.

After a while, I was nearing the river and wanted to photograph some green-winged teal. As I approached their spot, Joan came walking back to my surprise. I’d thought she would go on for a while, but she said some people ahead of her were following the trail as it ascended a hill, and they were not that far from some bison. She didn’t want to be around any mammal-people encounters so she decided to return. I said I’d come back when I had photographed the ducks.

The sun was shining nicely and the teal were swimming back and forth. I checked my vicinity and saw no people or animals; the rodents had gone into their dens.

As I stood taking pictures, I suddenly heard a soft sound behind me, kind of like a grunt or snort. I slowly turned right with my camera still held up to my face and found myself facing a small group of bison with the lead male watching me from some yards away.

This is not the bison that faced me: I was not taking photos or making any noise at this point!

Joan had been watching from above the valley at the parking place along with a couple other people. She’d seen the bison come up over a hill and walk toward me, but she was too far away to let me know. I never heard them – or smelled them as the wind was blowing in their direction.

Not the bison who was examining me!

Joan considered calling 911 but phone coverage can be spotty. She also briefly thought about how to get medical help if something happened but hoped a ranger would come quickly as they did seem to magically appear all over the park when needed. We saw them often when groups of people stopped at roadsides.

Again – not the bison who was examining me!

In the meantime, I quickly considered my options. I can’t run; even if I could, it would be useless as bison have been clocked at 40-45 mph (65-70 km/h). I knew enough not to challenge the bison in any way, quickly looking away so I wasn’t gazing into the male leader’s eyes. I kept the camera with its long lens up in front of my face. Slowly, I pivoted back left towards the direction of the river, facing away from the bison. Then I stood completely motionless (camera still up in front of my face). I don’t know how long I stood there but at some point, I heard movement further away to my right and dared a look. The bison leader and his group had decided that I posed no threat and they had moved on down the valley.

I waited, still standing stock still, until they were a good distance away. I had to take a couple photos of the – now far off – group and then began walking as quickly as I could manage down the return path.

Photo heavily cropped; they were very distant!

My feelings were mixed: shock at what had happened, relief that I had known what to do in order not to provoke the bison, and elation that I had survived the close encounter unscathed. It also taught me that not all human-bison encounters are the result of complete stupidity – I was on a path laid out for visitors, there had been no bison nearby when we began walking, several other people had been on the trail and so I hadn’t suspected anything could happen. I likely won’t hike any paths at the park again if bison are in sight, even far away.

I continue to be in awe of the magnificent bison. I’m glad my love of wildlife and instincts helped me through a safe encounter and this will certainly be one of my most vivid travel memories. And I’ll continue to be as careful and watchful as I can when I go out into nature.

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

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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

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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!