16-22 June 2016

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The U.S. National Park Service has launched a successful campaign this year called #FindYourPark to celebrate the 100th birthday of the park service. The idea is to find a national park to visit and appreciate. I think the better slogan would be #FindTheOutside. Find that place where you can sit and observe. Find that place where you can listen and smell. Find that place in nature where you can learn. For 12 students from Mitchell Community College, that place just happened to be our nation’s first national park, Yellowstone. However, it wasn’t so much the typical attractions that made this trip special. It was the remote areas that gave us the opportunity to get away and experience wildness.

16 June
From Charlotte to Bozeman–> through Paradise Valley–> Gardiner–> Mammoth

We arrived in Bozeman a little after lunch and slowly started our journey towards the north entrance. As we rode through the remnants of the Pinedale glacial period (70,000 – 13,000 years ago), we searched for osprey and eagles in the cottonwoods that line the banks of the Yellowstone River. The Yellowstone River is the longest, undammed river in the U.S. and one of the few that flows northward.

It is strange that Lewis and Clark made it to about where Livingston, Montana is today, but did not explore the source of the river. If they would have chosen to travel a little further south, they would have certainly seen the many geological wonders. Clark wrote the following in 1809:

“At the head of this river the natives give an account that there is frequently heard a loud noise, like thunder, which makes the earth tremble. They state that they seldom go there because their children cannot sleep.”

After arriving in Gardiner and checking into our lodge, we went off to explore some of these geological features at Mammoth, the main headquarters of the park. Bob gave us a wonderful talk on the terraces as we walked the upper boardwalk. These terraces are made of travertine, which is a type of freshwater limestone. The terrace rock consists of calcium carbonate. The addition of carbon dioxide lowers the pH of the water and makes it more acidic. Bob mentioned that the vents frequently change locations. Old, “extinct” springs were evident in every direction. The cool thing about these springs is that they are home to species of bacteria, flies, wasps, spiders, beetles, birds, and other animals. We even came across a white-tailed jackrabbit enjoying a snack. These rabbits have found a good niche in the Mammoth area. Much of the rest of the park receives too much snow, but since Mammoth gets the least precipitation per year in the park, there is enough vegetation to support this species.

17 June
Mammoth–>Norris–>Grand Prismatic–>Old Faithful–>Yellowstone Lake      –>Hayden Valley–> Lamar Valley

“The park is just a howling wilderness of three thousand square miles, full of all imaginable freaks of a fiery nature.”

-Rudyard Kipling

As we drove from Gardiner through Mammoth towards Norris, we were entertained by swans, cranes, and yellow-headed blackbirds. We stopped and walked around Norris Geyser Basin, which is the hottest basin in the park with pools around 190°F and a pH of 5.

Sitting above the basin gave us the perfect opportunity to make a connection to what Mitchell CC students are currently doing in our science labs. In 1969, Thomas Brock and his graduate student isolated a bacteria from Mushroom Spring (not far from Norris) that was thriving at 160°F. The bacteria that they isolated was Thermus aquaticus. An enzyme from the bacteria, known as Taq polymerase, allows researchers and students to perform DNA analyses. Mitchell CC students are using a technique called DNA Barcoding to determine insect biodiversity on campus. This bacterium has served as the basis for a $300 million industry per year.

We then drove to Grand Prismatic and then on to Old Faithful for a lunch break. After the big geyser erupted and the huge crowd began to file out, the ravens took advantage of the opportunity by swooping in and eating whatever food had been dropped. These intelligent birds know an opportunity when they see one.

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Grand Prismatic

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Norris Geyser Basin

 

Yellowstone Lake was our next stop. Mr. Parks Davidson taught us about the ecosystem of this lake, which is actually the largest high elevation lake in North America. Lynn led an exciting discussion about the lodgepole pine trees that surrounded us. She even tried to get one of the cones to burst open in her hand, but it wasn’t quite hot enough.

As we got out of the car at Mud Volcano, our next stop, we immediately smelled rotten eggs. Members of the Washburn expedition named “Mud Volcano” in 1870 for the cone-shaped mud that covered it. However, by 1872, an explosion had blown away the mud. The smell comes from hydrosulfide gas, which is converted to sulfuric acid by microbes. Sulfuric acid breaks down the rock, and the bubbling is the release of the gases. The thermal features here are mostly mud pots and fumaroles simply because the area does not have enough ground water to make geysers or hot springs.

Elizabeth led the discussion at our next stop, the beautiful Hayden Valley. This valley was named for Ferdinand Hayden, a geologist and surveyor, who led a geological expedition in 1871. His findings played an integral part into Yellowstone becoming a national park in 1872. Elizabeth taught us about the formation of the valley and how it differs from the Lamar Valley. As we sat and listened, we watched a bald eagle land along the river.

After supper at Roosevelt, we traveled through the Lamar Valley to Cooke City. On our way, we stopped at Slough Creek and watched some of the Junction Butte wolf pack at their den site. The pups were in and out of view, as were several of the yearlings. We even turned our scopes around and were able to see a grizzly sow with two cubs across the road. To cap off an exciting day, we heard the pack howl several times.

18 June
Slough Creek–> Mt. Washburn–> Grand Canyon of the Yellowstone–> Cooke City 

Our first alpine hike of the trip was scheduled this morning, a steady climb up Mt. Washburn. What scheduled was having a cinnamon-colored black bear cross the road right in front of us on our way to the valley. We pulled into Slough Creek and watched the den site for about 30 minutes. The pups were again in and out of view. After eating breakfast at Roosevelt, we headed for Washburn.

In 1870, General Henry Dana Washburn led a military expedition into this territory along with Nathanial Langford, Cheyney Doane and others. At the end of August 1870, while scouting a direct route to the Grand Canyon of the Yellowstone, the group reached the summit of mountain. They named it after their leader. Doane’s description of the summit is as follows:

“The view from the summit is beyond all description…A single glance at the interior slopes of the ranges shows that a former complete connection existed, and that the great basin has been formerly one vast crater of a now extinct volcano.”

Half of our group started at the Chittenden road lot with the other half starting from Dunraven Pass. This trail from the south is actually an old cut road that visitors could once drive up. It’s short, but sneaky. You must gain around 1400 feet in elevation in just over 3 miles. Golden-mantled chipmunks scurried along the rocks, yellow-bellied marmots ducked in and out of crevices, Clark’s nutcrackers controlled the skies, and Douglas firs and white-bark pines held their ground, even at the high elevations. This really excited Laura, since she was our white-bark pine expert. The wind was really strong towards the top, so it was nice to catch a break inside the fire tower to rest and eat lunch.

Before heading back through the Lamar valley for the evening, we made a stop at Artist Point to take in a beautiful view of the Lower Falls. It’s not surprising that on that same 1870 expedition, Nathaniel Langford said, “A grander scene than the lower cataract of the Yellowstone was never witnessed by mortal eyes.” Even with the heavy crowds of people, this is a must stop.

Lower Falls

Lower Falls

19 June
Lamar Valley–> Tower Junction–> Pebble Creek–> Cooke City–> Trout Lake

“There is something in the wild romantic scenery of this valley which I cannot nor will I attempt to describe; but the impressions made upon my mind while gazing from a high eminence on the surrounding landscape one evening as the sun was gently gliding behind the western mountain and casting its gigantic shadows across the vale were such as time can never efface from my memory.”

—Osborne Russell describing the Lamar Valley in 1835

Our day started at 0430 this morning so that we could meet Dr. Nathan Varley in the valley by 0500. We started off observing a bald eagle just beside the river and a couple of coyotes and sandhill cranes on further down. Several pronghorn and 4 bull elk were grazing just up the slopes from our next pullout. We soon arrived at an osprey nest, and the male and female were both there. We watched the male leave and bring several sticks back to repair some spots in the nest. As we arrived at Slough creek, it soon became apparent that others had the same idea. We found a spot on a hill that would give us a great view of the den. For the next hour, we watched both the wolves as well as two grizzlies wandering around the opposite slopes. There were also bighorn rams just above the wolf den. It seems bold that they are that close.

After leaving Slough Creek, we drove to Tower Falls where we watched a bighorn ewe with a lamb on the opposite side of the canyon. There was also a peregrine falcon circling overhead. Our last stop of the day with Nathan was at the Pebble Creek Campground where we watched a family of mountain goats walk up the cliffs with ease.

After a midday break, we hiked around Trout Lake and enjoyed the beauty of the area. It was here that Kathy taught us about the caldera that we viewed yesterday, and Michael led a discussion on cutthroat trout. After the hike, Diana discussed raven biology. She even had a raven-fact foldable for everyone! On the way back to Cooke City, we stopped at Warm Creek (misleading) for a foot-soak challenge.

20 June
Yellowstone–> Beartooths–> Hartman Gallery

We were all excited about meeting Dan Hartman this morning for a hike up to an owl nest. Dan is a wildlife photographer and naturalist, but also a good friend who has always been generous with his time. When we got to the nest, we had a hard time finding the female great gray until a raven flew close. She appeared for a while then disappeared in the woods. We waited for a couple of hours, but never did see the chicks.

Dan offered to take us to a different nest so we agreed to follow him (without hesitation). We were about 500 ft. past the tree line when we heard the calling, or begging, from the owl chicks. When we came upon them, the chicks were all 3 sitting on the same branch. The mother had just flown away after feeding them. We stood still and watched the chicks for the next 30 minutes, and even were able to find the mother sitting close by. What an exciting time to be able to see this bird that most people who visit Yellowstone never get to see!

After leaving the area, we checked out an aspen grove with Dan that was filled with red-naped sapsuckers, hairy woodpeckers, bluebirds, and flickers. We then headed into the Beartooths to have our minds blown from the scenery. After making several stops, we ate lunch at the “Top of the World”. It was here where we discussed trophic cascades and also where Holly taught us about grizzly bears.

On the way back, we found a great-horned owl nest that was occupied. We also stopped at an aspen grove so that Jim could talk to us about aspen trees and their importance in the ecosystem.

When we got back, we stopped in at the Hartman house and gallery for a visit. After supper, some of us spent one last night in the valley observing.

21 June
Cooke City–>Yellowstone Picnic Area–> Mammoth–> Gardiner

After breakfast at the Bear Claw Café, we packed up and headed through the Lamar for the last time. Our plan for the day was to hike the Yellowstone Picnic Trail. On our way to the parking lot and trailhead we came across a black bear. He already had quite the audience so we didn’t stay long.

The first part of the trail was filled with excitement and anticipation because we all knew that we would soon learn all about bison and pronghorn behavior from Will and Bedford, respectfully. Bedford even had a pronghorn show up for his talk. The hike was great with many wonderful views of the Yellowstone River. We were even entertained by several marmots trying to seek shelter from the strong winds.

We spent the rest of the evening at Mammoth before supper in Gardiner.

22 June
Gardiner–> Bozeman to Charlotte–> Back home

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Another year of the program is complete. This year included lots of wonderful hikes, beautiful scenery, and rare wildlife sightings. We saw lots of old friends and made new ones. Hopefully, using places like Yellowstone as a classroom improves our understanding of biology as well as helps us to better appreciate nature. Go forth and find your “park”, whether that’s a national park, state park, refuge area, the woods behind your house, or a tree in your backyard. Take time to be still and observe.

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10-17 June 2015

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10 June

From Charlotte to Bozeman–> through Paradise Valley–>Roosevelt Arch–> Roosevelt Lodge

Ten of us drove in from Bozeman, two from Jackson Hole, and two from Vancouver. As we sat in the valley between the enormous Gallatin range to our west and the Absaroka range to our east, we discussed how glaciers carved the valley during part of the last ice age, specifically the Pinedale glacial period.

The glacier discussion gave us a chance to apply concepts to home and think about when ice locked up the northern Appalachian mountains. We talked about how the southern Appalachians are much more diverse than the northern mountains. So, is it possible that the spread of glaciers throughout North America limited biodiversity in some areas?

Hello, old friend.

Hello, old friend.

The area around the Roosevelt Arch was undergoing major construction as part of the Gardiner Gateway Project so it was difficult to take good pictures. We drove to the self-guiding “Forces of the Northern Range” trail to discuss the dynamic nature of the northern part of the park. Some of the questions we asked included the following:

1. If elk and bison increase on the northern range, how is vegetation impacted?
2. How does one best manage land in a national park if the whole idea is built around the land being “free from direct human manipulation?”
3. How many bison and elk can the northern range of Yellowstone support?

On our way to Roosevelt Lodge, we passed two mule deer (notice the mule-like ears) along the road to the Petrified tree. These two males were not startled at all by our presence.

We finally reached our destination for the night.


11 June
OVT (Optional Valley Time in Lamar)–> Canyon–> Norris–> Grand Prismatic–> Old Faithful–> Yellowstone Lake–> Mud Volcano–> Hayden Valley–> Roosevelt

There were lots of bison and calves in the valley this morning. Wolves were hanging near Hitching Post, but never came into view. After breakfast, we left for our geothermal drive. Just past Norris, Jim enlightened us  on the geological history of Yellowstone as well as the caldera. We watched an osprey on the cliff above.

Between Norris and Midway Geyser Basin, we watched a mother coyote hunt off the road. She must have had young pups somewhere close by.

After hiking the Fairy Falls trail and turning left to head straight up the hill, we were rewarded with the beauty of Grand Prismatic, the largest hot spring in the United States. Osborne Russel, a trapper, described it like this in 1839:

“The steam which arose from it was of three distinct colors. From the West side for one third of the diameter it was white, in the middle it was pale red, and the remaining third on the East light sky blue. Whether it was something peculiar in the state of the atmosphere.. or whether it was some chemical properties contained in the water… I am unable to say and shall leave the explanation to some scientific tourist who may…visit this place in the future.”

Old Faithful and Yellowstone Lake were next on the agenda. Barb led a discussion on Yellowstone Lake. This lake is the largest lake at an elevation above 7,000 ft. in the North America. The geology of the bottom of the lake is very similar to the terrestrial features in Yellowstone with hot springs, fumaroles, and geysers. We crossed the road into a lodgepole pine forest where Hutch gave us a lesson on pine tree reproduction and how the lodgepole relies on fire.

We stopped at Mud Volcano on our way through the Hayden Valley. What, geologically, makes this valley different from the Lamar Valley to the north? See here. During the Washburn expedition in 1870, Gustavus Cheyney Doane described the Hayden valley while standing on top of Mt. Washburn:

“A grassy valley, branching between low ridges, running from the river toward the center of the basin. A small stream rose in this valley, breaking through the ridges to the west in a deep cañon, and falling into the channel of the Yellowstone, which here bears in a northeast course, flowing in view as far as the confluence of the small stream, thence plunged into the Grand Cañon, and hidden from sight. No falls can be seen, but their location is readily detected by the sudden disappearance of the river; beyond this open valley the basin appears to be filled with a succession of low, converging ridges, heavily timbered, and all of about an equal altitude. To the south appears a broad sheet of water — the Yellowstone Lake.”

In Hayden, we spotted bison, elk, mallards, trumpeter swans, an American widgeon, and a bald eagle.


12 June
OVT–> Mt. Washburn ascent–> OVT

“The view from the summit is beyond all description”
–Cheyney Doane

In 1870, General Henry Dana Washburn led an exploration party into Yellowstone. The army provided a military escort, which was led by 2nd Lieutenant Cheyney Doane. Fifty-four year old Truman Everts also joined the group. You can read about his adventures here. At the end of August 1870, they climbed up a mountain through stands of timber and across meadows of late-blooming wildflowers where grizzlies foraged for berries and whitebark pine nuts. The terrain was rough and steep. At the summit, they began to take measurements with a barometer. There arose a dispute about the altitude. One member, a former civil engineer, estimated their altitude at 10,700 ft. Another said 9800ft. Doane said 9966ft (Actual altitude- 10,243ft). However, there was no dispute about this name. They decided to name the mountain after their leader and general, who had reached the summit alone the previous day. It would be known as Mount Washburn.

This morning after OVT (we did see a grizzly sow with a cub just north of Fisherman’s pullout) we met Dr. Nathan Varley for a discussion on grizzly bear ecology as well as a hike up to the summit of Mt. Washburn. We knew it was going to be tough, but the potential view kept everyone motivated. After discussing bear management in the park, we started up from Dunraven Pass. We had several more mini-discussions along the way as we traveled over snow patches. We saw mountain bluebirds, Clark’s nutcrackers, golden-mantled ground squirrels, yellow-bellied marmots, and bighorn sheep. Saheba channeled her knowledge of the whitebark pine through Nathan and led a very good discussion about how integral it is to the grizzly’s diet.


13 June
OVT–> Hike with Dan Hartman–> Thunderer–> Beds and Buns–> Beartooths–> OVT

This morning’s OVT was filled with excitement as we pulled into Fisherman’s pullout. Rick M. was parked there so we knew he must have been getting a signal. After several minutes, we had the scope on a black wolf just as the fog lifted. For many in the group, this was the first time seeing a wild wolf. Unfortunately, our wolf sighting was cut short because we had an appointment. Fortunately, that appointment was with renowned photographer, naturalist, and friend Dan Hartman.

While hiking with Dan, we saw a bear bed and a lone bison. We also heard western tanagers and three-toed woodpeckers. As we crested a hill, Dan glassed a nearby snag for any movement. Just as we set up the scope and camera we heard several deep hoots. These hoots were followed by a male great grey owl flying into the nest to transfer food to the female. She then proceeded to feed the chicks. Dan knew of this nest and wanted to get a chick count. From the pictures he took, we counted 2 babies.

After the hike with Dan, we stopped at Thunderer to scan for mountain goats.  Just like always, they were there on the steep cliffs. Since we were near the creek, we took the opportunity to soak our feet. On the way to Cooke City, MT for lunch at Buns N Beds, we stopped at Dan’s House/Gallery and were entertained by a red squirrel and her babies.

We drove into the Beartooth Mountains after lunch where Joei led a talk about bison and Carlos discussed pine martens.

This evening in the valley, we watched a grizzly sow and cub from Hitching Post as well as lots of bison and pronghorn.


14 June
Canyon–> Hike around South Rim–> Trout Lake–> Cooke City–> OVT

We loaded up and drove around the slopes of Mt. Washburn to Canyon for breakfast. After eating, we parked at the trailhead along the south rim of the canyon. The 3.5 mile loop provided great scenery as well as a few mosquitoes. We hiked around lakes, through geothermal features, through lodgepole forests, and finally along the rim of the canyon.  Aspen and Jane talked about mountain goats and wolves, respectively.

After a short break at Roosevelt, we drove to Trout Lake. Thanh delivered a lecture on the cutthroat trout and some of the issues conservationists face when trying to preserve them.


15 June
OVT–> Specimen Ridge–> Yellowstone Picnic Area–> Blacktail Pond

We drove through the valley this morning to Hitching Post. As we made our way back through, we saw the grizzly sow with a cub again.

After breakfast, we started our hike from the Specimen Ridge trail head. Our plan was to loop around and end at the Yellowstone Picnic Area after walking along the ridge. It was not long before we were entertained by the acrobatic tree swallows as well as flashes of yellow and blue.

John led a discussion about the pronghorn and Bill talked about coyote behavior during a rest break. American Pronghorn really are fascinating creatures. Reaching speeds close to 55-60 mph, they are easily the fastest animal in North America. But, why are they so fast? Why spend all that energy when there is no need? This article highlights the hypothesis of one researcher. Here’s the book. On the west side of the loop we came across six bighorn sheep who were trying to cross the trail as well as several marmots.

Several days ago Hutch received some inside intelligence about a grizzly with a carcass near Blacktail Pond, so we decided to check it out after lunch. Soon after spotting the grizzly, we knew we were in for a long wait (several hours, in fact). He seemed to be enjoying his nap. He occasionally rolled over and glanced in our direction, but never really managed to get to his feet. A wandering coyote was not even enough to get this big boy up and moving.

It is typical behavior for single bears to be resting at or near carcasses. The researchers in this study observed that, during the summer, single grizzlies rested longer and more frequently while near carcasses than those not near carcasses. This makes sense, especially in a place like Yellowstone where grizzlies are not easily chased away by top predators, such as wolves. This video from last year clearly shows the hierarchy in Yellowstone. The Blacktail Pond grizzly looked plenty full.

Quick glance

Quick glance


16 June
OVT–> Tower Falls–> Petrified Tree–> Blacktail Pond–> Mammoth–> Gardiner, MT

During OVT this morning we spotted wolf-watchers at the Slough Creek Campground road. Wolf signals were coming in loud and clear, but the fog was not cooperating. We decided to ride into the Lamar one last time to enjoy the sights and smells. On our way back past Slough Creek, Bill spotted a black wolf (890M) on the south side of the rode. Soon after, a grey (911M) crossed the road behind us. 911M stopped and howled. 890M responded with his own howl. They then met up and ran off into the fog. It was very cool seeing and hearing wild wolves so close. These two are members of the Junction Butte pack, which claims this territory around Slough as their own.

After breakfast, we visited Tower Falls and the Petrified Tree. On our way to Mammoth Hot Springs we stopped by Blacktail Pond to check on the grizzly. Soon after arriving, he stood up and began walking from his napping spot to the carcass. We watched him as he fed on what was left for about an hour and a half.

After walking around the Upper Terraces at Mammoth Hot Springs and discussing the geology of the area, We headed towards Gardiner, MT, our destination for the night.


17 June
Breakfast–> Gardiner to Bozeman–> Bozeman to Charlotte


Thanks to Mitchell Community College for supporting this program. Thanks to Dan Hartman and Dr. Nathan Varley for being so generous with their time and sharing their knowledge. Thanks to Bill Day for continuing to assist year after year. It must be hard to drive the #1 car. Finally, thanks to each and every participant for making this year’s trip so special.

Here are some good books that I have found to be very helpful and entertaining:

Mind of the Raven
When the Wolves Returned
Empire of Shadows
Adventures in Yellowstone
In the Temple of Wolves
Decade of the Wolf
Yellowstone Wildlife
Windows into the Earth
The Yellowstone Story Volume 1
The Yellowstone Story Volume 2

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Influence of Glaciers

Glaciers form when more snow falls in winter than melts in summer. Over time, the bottom layers melt, and the top layers slide due to gravity. The last Ice Age, which was characterized by massive glaciers, ended about 12,000 years ago.

As we drive away from the Bozeman airport and pass through the town of Livingston, MT, we will turn south and enter into what is known as Paradise Valley. This valley was carved out by glaciers during the last Ice Age. We will see lots of evidence of this “glacial carving,” from the sediment that is deposited to the random boulders that are sitting in the northern part of Yellowstone National Park (seen in second photo below)

Paradise Valley in Montana

Paradise Valley in Montana

Running off together

Running off together

Glaciers can also cause an abnormal distribution of plant and animal species, limiting biodiversity in some areas and causing biodiversity to explode in other areas. The Appalachian Mountains, which were also impacted by glaciers, display a great range of biodiversity. The southern range is a lot more diverse than the northern range. The Great Smokey Mountain National Park has 130 different tree species. This is almost as many tree species that can be found in all of Europe! How do you explain that? What limited biodiversity in the northern range the Appalachian mountains, and what promoted it in the south?

Greatvalley-map.png

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Ash in Nebraska?

“…a howling wilderness of three thousand square miles, full of all imaginable freaks of a fiery nature.”
Rudyard Kipling

In the summer of 1971, a young geologist made a startling discovery at the edge of a cornfield in eastern Nebraska. Mike Voorhies was exploring some land close to where he grew up in Orchard, Nebraska. As he passed through a steep gully, a shiny object caught his attention. After climbing up for a closer look, Voorhies discovered that the object was the skull of a young rhinoceros.

Just a few yards away was one of the weirdest fossil beds ever discovered in the United States. It was a dried up water hole and served as a mass grave for not only rhinoceroses, but also camels, turtles, saber-toothed deer, zebra-like horses, and other animals. It was discovered that these animals had died from an event just under 12 million years ago during the Miocene geologic epoch. The animals had been buried under volcanic ash up to ten feet deep in some areas. The only problem was there had never been any volcanoes in Nebraska.

How do you explain that?

Mike Voorhies at Ashfall Fossil Beds
Mike Voorhies at Ashfall Fossil Beds, from the NET Television documentary “Mysteries in the Dust,” produced in 1992.

Ashfall rhino

 

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Geology Introduction

Why are ancient clamshells and other marine fossils so often found on mountaintops?

By the late 18th century, scientists knew very precisely the dimensions of the Earth and its distance from the sun and planets. You might think that determining the age of the Earth would be relatively straightforward. However, humans would split the atom and invent television, nylon, and instant coffee before they could figure out the age of their own planet. Why? One reason is simply because no one was interested in geology. James Hutton, who is given credit for creating the science of geology in 1795, wrote about the slow processes that shaped Earth. His landmark writing did little good in advancing geology because it was so boring no one could understand it. Hutton did, in fact, ask one important question (see above).

The video below gives a 1.5 minute overview of the geologic processes that have shaped and continue to shape Yellowstone. What are those processes?

Geology Animation

http://www.nps.gov/grte/learn/photosmultimedia/geo_film.htm (dead link)

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12-18 June 2014

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12 June

From Charlotte to Bozeman–> through Paradise Valley to Roosevelt Arch–> Roosevelt Lodge

Most of the group left Statesville for an early departure from Charlotte. After arriving in Bozeman, MT, we picked up “Famous Dave’s” barbeque to take to the best rest area west of the Mississippi R. The female osprey was sitting on her nest at the rest area. As we stood by the Yellowstone River, we talked about how glaciers were influential in the geology of Yellowstone and in carving out the valley in which we sat. We observed elk and bison as soon as we entered the park. During our hike at Wraith Falls, we saw Uinta ground squirrels, ravens, magpies, and a yellow-bellied marmot.


13 June

OVT (Optional Valley Time) in Lamar–> Specimen Ridge–> Thunderer–> Chedder Bombs–> OVT

0515- Some of the group woke up and left Roosevelt for the Lamar Valley. We decided to call early morning and evening Lamar Valley observations “OVT” (optional valley time). Around the Little America pullout in the valley, we spotted a bison carcass with no predators around. Suddenly, while we were watching, two coyotes showed up and ate for a while.

After breakfast, we hiked the Specimen Ridge trail to the Yellowstone picnic area. Linda and Bill gave their expert presentations on sage and pronghorns, respectively. Linda wins the virtual trophy (VT) for engaging the audience so much that several tasted the sage. Bill wins the VT for timing. After talking about pronghorn having twins, we observed a pronghorn and her twins. I am sure he made a call and somehow made that happen. We saw mountain bluebirds, flickers, bison, bighorn sheep, osprey, a peregrine falcon, and ravens along the trail. The winds got up to around 40 mph near the top.

After filling up our water bottles, we drove to Thunderer to observe mountain goats high up on the cliff. This also gave us the chance to soak (or freeze) our feet in Soda Butte Creek (reading 45 degrees C). Bill spotted a moose cow and calf in the river, but they both soon scampered away. We had a good discussion of the wolf reintroduction controversy (see this case study). Trophic cascades were discussed. Dr. Cooper brought up the benefits of eco-tourism and increased visitation to the park. Most felt strongly that wolves belonged in the park. Some could understand the views and opposition of the surrounding ranchers and farmers. All agreed that top predators are needed for an ecosystem to function efficiently and properly

We drove into Cooke City, MT to have supper with our friends from “Buns N Beds.” Chedder Bombs and milkshakes all around.


14 June
Canyon–> Hayden Valley–> Mud Volcano–> Yellowstone Lake–> Old Faithful–> Grand Prismatic–> Gibbon Falls–> OVT in Lamar

0630- We left the cabins and headed towards the Canyon area. About 1.5 miles down the road, we spotted our first black bear. Another 0.5 mile and we spotted a second bear. This one was much larger. They were both foraging nonstop.

After breakfast, we headed towards Hayden Valley. With the help of some “wolf-watchers,” we spotted a black wolf in Hayden that was bedded down. Andy, an old friend from years past, and his wife were also there watching. Jim spotted a bald eagle sitting on the ground. Expert Bob explained to us what makes Hayden Valley different from the Lamar Valley (see here).

We stopped at Mud Volcano and Dragon’s Mouth to get a sense of some of the geothermal features the park has to offer. Then, on to Yellowstone Lake where Diana told us it is the largest sub-alpine lake in North America. We walked into a lodgepole pine forest where Will explained to us how lodgepoles are well adapted to forest fires and actually use the fires as a means of propagation (see here).

We watched Old Faithful as it erupted. Then, we made our way to Grand Prismatic. However, we did not get to observe the entire hot spring because of a trail closure. We saw Gibbon Falls on the way back to Roosevelt.


1930- OVT- There is a badger den near Slough Creek Campground. We spotted a grizzly walking away from the bison carcass near Little America pullout. There are lots of bison with calves in the valley.

15 June
Calcite Springs–> Silvergate–> Trout Lake–> OVT

0715- We started out the morning with coffee and breakfast at the cabins. We drove to meet wildlife photographer, naturalist, and friend Dan Hartman at the Calcite Springs overlook. We hiked on the west side of the road through numerous meadows (aka black bear territory). We saw lots of bear sign as well as bluebirds, flickers, robins, Cassin’s finches, Audubon’s warblers, hairy woodpeckers, a western tanager, and a female Williamson sapsucker. Dan shared lots of stories from photographing and guiding for wildlife shows.

After hiking, we ate lunch in Silvergate at the “Log Cabin Café.” We then went back to Dan’s house and gallery to look at some wildlife productions that he has been involved with. While there, a pine martin showed up in the front yard.

The Trout Lake trail was next on our agenda. There were lots of swallows zipping around the lake. Allison told us the story of the American Bison. After a brisk hike around the lake, we headed back to Roosevelt.

1930- OVT- Wolf 911M had pulled a drowned bison calf to the bank of the Lamar River. When we got there, two coyotes were feeding. A bison cow had died earlier in the day near the Picnic pullout. We had observed its calf still prodding the cow and trying to nurse. It was very sad. When we went back to this carcass, approximately 15 bison had huddled around it in sort of a bison “funeral” (see excellent video below). Wolves 755M and 689F were nearby, but did not go near the carcass. They did, however, chase several calves to no avail.

16 June 2014
OVT–> Canyon–> Yellowstone Falls–> Dunraven Pass–> Roosevelt–> OVT

0515- OVT- There were 3 grizzlies on the bison carcass at Little America. When we drove to the Old Picnic pullout, wolf 911M and a black yearling from the Junction Butte pack were near the carcass. Soon, the black yearling ran off the remaining bison and started feeding while 911M napped nearby.

We traveled to Canyon for breakfast and saw a black bear on the way. Still no sign of the sow with 3 cubs near Calcite. After breakfast, we went to view the lower falls. We spotted a coyote with a large ground squirrel in its mouth at Inspiration Point. Jane explained to us about the intelligence of the raven. Jane wins the VT for best prop. I am glad she did not get arrested for messing with the wildlife. We had planned on hiking to the fire tower on Mt. Washburn, but heavy snow and high winds changed our mind. However, we did pull out at Dunraven pass for Aspen to share with us the importance of the whitebark pine tree. We saw another coyote crossing the road near the slopes of Washburn.

1530- We headed off for an off-trail hike near the cabins. We saw lots of bear scat. It rained on and off, looking scary at times. Jim talked a little about elk ecology and the history of elk in the park.


1930- OVT- We drove to the Old Picnic pullout to check out the carcass there. Scarface, a grizzly and somewhat of a Yellowstone celebrity, had complete control of the carcass. Scarface, a collared grizzly, is 24 years old (see more info. about Scarface here). The old bear ate a little and napped a lot.

17 June 2014
OVT–> Roosevelt–> Petrified tree–> Forces of the Northern Range–> Mammoth

0515- Final OVT- Most of the group decided to exercise their option of getting up in the gloom to see what was in the valley. We had no idea that this would be the best morning of the trip. On arrival at the Old Picnic carcass, we observed two grizzlies (Scarface and a larger bear), 3 wolves (911M, the black yearling, and another), and even several bald eagles (2 mature eagles and 1 juvenile) in the area. The larger bear controlled the carcass most of the time, even chasing the wolves off from time to time. The wolves did get chances to feed when the bear took breaks. It is no surprise that in 1835, trapper Osborne Russell said the following about the Lamar Valley:

“There is something in the wild romantic scenery of this valley which I cannot nor will  I attempt to describe; but the impressions made upon my mind while gazing from a high eminence on the surrounding landscape one evening as the sun was gently gliding behind the western mountain and casting its gigantic shadows across the vale were such as time can never efface from my memory.”

During breakfast at Roosevelt, we noticed a black bear sow and three cubs had wandered near the lodge. The sow sat down as the cubs played around a tree about 75 yards from where we were eating. This was the sow we had failed to see until this point. The cubs took turns climbing the tree, then quickly falling off. In an instant, the sow caught and killed a deer fawn that had been hidden in the tall grass by her mother. As the bear took off with the fawn, the mother deer hopped around, frantically looking for her young. It was sad to watch, but then you realize the sow had 3 mouths to feed. Nature is not always comfortable. The rangers in the area did a great job setting up a perimeter and keeping everyone safe while the bear fed.

We stopped at the petrified tree and the “Forces of the Northern Range” self-guiding trail on our way to Mammoth. At Mammoth, Joei taught us about the hot springs and how they are different than the other thermal features in the park. NPS ranger Grant Marx then took us on a guided walk around the terraces. After eating at K-Bar Pizza, we spent the night in Gardiner, MT.


18 June 2014
Through Paradise Valley to Bozeman–> to Charlotte–> home

-Thanks to all the participants for signing up for this trip. The expert topics were great. Getting to know all of you was the best part.
-Thanks to Mitchell Community College, especially Continuing Education, for offering the trip.
-Thanks to Dan and Cindy Hartman for being so kind and having us into their house
-Thanks to Rick Lamplugh for writing In the Temple of the Wolves

-Nature was observed and appreciated, topics were discussed, facts were learned, memories were etched, and friendships were made.

 

 

 

 

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