The Local Flock

The Great Salt Lake Bird Festival has been captivating bird watchers and nature enthusiasts since 1999, a demographic that has grown exponentially since the festival’s inception. The event includes about 50 field trips each year, yet these typically sell out in less than 10 minutes. For instance, in 2023 all tickets were claimed in about seven minutes. Why so popular, and why so popular with us?

The Great Salt Lake is critical to migratory birds attracting 8-10 million each year. This flying influx is comprised of 338 species. The bird festival is an excellent way to appreciate and learn about those species and the unique ecosystem that attracts them alongside avian and ecology experts. We love attending, but every year we have the same debate. Namely, how many early-morning field trips do we sign up for? In these sleep versus scholarship battles, scholarship usually wins. This time, we predictably decided getting up at ungodly hours three days in a row was worth it.

mist netting
Mist nets are a safe way to capture birds in order to study behavior and population health.

Why ungodly hours? Birds get up early. If you want to see them, you must also. We had to wake between 4:15 and 5:30 AM for all our field trips. After three days of that, we were exhausted. Somehow, we squeezed in afternoons of snowboarding on two of those days though. You’ve got to admit, our craziness is persistent.

The first field trip we attended, joined by a niece, was Mist Netting and Bird Banding. This took place in Farmington at the Eccles Wildlife Education Center headed by staff from the Department of the Interior who normally spend a morning catching birds every week at Hill Air Force Base. The information they collect is used for a national avian monitoring system. The bands are not electronic or WIFI, just old-school numbered metal circles. Banded birds are rarely recaptured, but it does happen.

a feisty flicker
This flicker was intent on doing harm to its handler, which is understandable.

During our session, we caught song sparrows, a robin, and a flicker. The bigger birds were feistier. Apparently, the little species are more accustomed to being picked on by other birds and are therefore more accepting of being handled. In contrast, the flicker had no intention of accepting anything and made that known with a lot of biting attempts. The robin also dabbled in snapping.

Our second outing was Birding by Electric Bike, which Jason’s parents joined us on. During this adventure, we peddled along the Jordan River. This was my first time ebiking, and I thought the optional power made the job way too easy. I want a workout when I bike. Hence, I turned my bike off half the time, and the rest of the time I set it to eco, the lowest setting. It didn’t seem right to pawn off my muscles’ job. While on this relaxing and pleasant excursion, we observed American kestrels, an osprey, and a cormorant along with a plethora of more common birds.

birding by bike
Birding by bike is both relaxing and productive.

Our last field trip was Bountiful Pond. Bountiful Pond was created when clay was removed from an area for a nearby landfill. Although its origins may be less than elegant, it now attracts many waterfowls and songbirds. We birded around the water for 2.5 hours finding sandhill cranes, Canadian geese, a domestic duck with peculiarly poofy hair, a cinnamon teal, a double-crested cormorant, and a yellow warbler just to name a few. Two of our nieces came with us. They seemed minimally eager at first but got more and more excited as we began finding species. I was surprised how many birds were all around us as soon as we started paying attention.

Bountiful Pond
Songbirds, waterfowls, and gulls are all commonly spotted at Bountiful Pond.

I’ve never understood why people don’t take advantage of their local events, natural wonders, and attractions. Jason and I do our best to get as much out of our whereabouts as possible. That’s why a week last May found us birding in the morning and boarding in the afternoon. Were we tired? Yes. Were we regretful? No… at least not eventually after we got some sleep.

Eureka! Let’s Dig!

Jason and I are all about experiencing life and sharing experiences with others. This ideology led to us giving our family members their choice of one of four activities in lieu of birthday presents in 2023. One of these options was a trip into Utah’s unconventional and under populated West Desert for some world-famous rock excavating. Eight of our family members chose this as their birthday activity and three others tagged along. The primary objective was trilobite fossils, but we found many other solid masses of significance. Here’s the scoop on our scooping.

We started this stone excursion with a stop in Eureka and nearby Silver City. Eureka was once Utah’s 9th-largest city. It’s story of boom and bust is typical of any mining mecca, except the boom lasted for over a century. Once home to nearly 4,000 people, Eureka is now an interesting and colorful settlement of 650 hardy residents and many relics of the past. If you are passing through, I’d recommend checking out the historic brick buildings, Porter Rockwell’s cabin, and the Star Theater’s projection equipment from 1935. (The theater itself closed in 1958.) We also stopped at Crazy Mary’s Rock Shop in the Gatley Building, which was constructed in 1898. Mary kindly gave us a tour of the old structure including its 20-foot indoor well used for cooling purposes during the prohibition days.

Silver City
Intriguing concrete foundations are what remains of Silver City.

From Eureka, we traveled to neighboring Silver City, a true ghost town. At one time, Silver City was home to a population of 1,500. From 1869 to 1915, it went from being a mining town to an ore sampling mill and smelter. After 1915, the mill closed, and by 1930 Silver City was mostly deserted. Massive concrete foundations with compartments, tunnels, arches, and towers are the principal remains at the location. We explored these and then headed up the road to the mouth of Dragon Canyon where the Dragon Mine still operates. Outside the gates of Dragon Canyon, we found a promising patch of dirt and started digging. There, we believe we found samples of hematite but plan on further analysis to confirm.

Gunnison Bend Reservoir
Our rented home was right on Gunnison Bend Reservoir, which meant the kids were instantly into fishing, kayaking, and forcing the adults to swim.

Long before the brief influx of miners, the West Desert was home to lasting residents, trilobites. Trilobites, one of Earth’s most successful lifeforms, evolved over 300 million years into more than 25,000 species. These sea-dwelling creatures flourished about 1,000 times longer than the entire span of current human existence.

It's the pits!
The fossils buried thousands of feet underground elsewhere are exposed at U-Dig.

Roughly an hour past Delta, an outcropping of Wheeler Shale containing some of the highest concentrations of trilobite fossils in North America was forced to the surface from thousands of feet below by warping and weathering. This remarkable layer is open to curious enthusiasts for personal excavation and fossil removal at U-Dig Fossils: Quarry. That was our destination the next day.

muscle and metal
Breaking up rocks sometimes requires more than just meager muscles.

While trilobites survived for hundreds of millions of years, the trilobites at U-Dig are from just the Cambrian Period, 500-550 million years ago. A lot of fossils can develop over 50 million years though. They are prolific at the site, and no one walked away empty-handed.

U-Dig dampness
A little dampness never hurt anyone… much.

We chipped and pried through rock in one of the quarry’s prehistoric pits from noon to a little after 5:30, almost closing time. At least, some of us did. You see, there was no rain in the forecast that day, but that didn’t stop it from raining. The showers started about 3:00 and continued the rest of the afternoon. The less resilient members of our group left early because they didn’t appreciate the soaking. Jason and I, along with a few others, kept at it and found some great specimens while chilled and water-logged.

Elrathia kingii
Elrathia kingii is the most common species of trilobite, but its fossils still thrill.

The following day, we headed to Obsidian Hill in search of Apache Tears, which are rounded obsidian pebbles. We found them and a whole lot of jasper. Unfortunately, the gnats found us. I obtained at least thirty gnat bites that afternoon. Jason didn’t get nearly as many, but he got one inside his ear and couldn’t sleep that night because he was in so much pain. The origins of these gnats were a mystery as there didn’t seem to be any water or anything else of gnatty interest nearby.

Utah’s West Desert is a fantastic place to travel back in time 150 years or 550 million years. The oddities are plentiful in that parched expanse. If you have a curiosity about rocks or just an inquisitive mind, it might be time to take your own family on a West Desert, dirt-sleuthing experience.

Spires, Slots, and Folds Part II: Folds

As I mentioned in my last post, food and footpaths are primary attractions in Torrey. We couldn’t jump right onto a trail the instant we arrived, but we didn’t waste any time getting to the eating. That evening we dined at my favorite section of Hell. Hell’s Backbone Grill & Farm has been a beloved out-of-the-way dining location for us since we first discovered it about 15 years ago. The required 50-minute drive up Boulder Mountain is quickly forgotten when the Jenchiladas, Blue Ribbon Black-Powder Biscuits, blueberry bread pudding, and seasonal favorites hit the tongue. This time, those seasonal offerings included asparagus and peas from the Hell’s Backbone Farm. Delish! We loaded up past our max fill lines and then dodged black free-range cattle on the dark trip back to Torrey.

The next day, we hiked in Capitol Reef National Park on the Navajo Knobs Trail. The Navajo Knobs are a cluster of bumpy outcroppings at the tippy top of one of the park’s many plateaus. Hikers can bail halfway up this path to complete just the Rim Overlook or continue another 2.4 miles to reach the top. We weren’t sure how 2,400 feet of elevation change would go over with my testy, recovering knee. Hence, we’d settled on ending at that halfway point and only 1,110 feet of altitude variation. However, once we reached the Rim Overlook, I could tell we would decide to go all the way, 9.4 miles RT, knee aside. Why waste all the already-exerted effort?

The Castle
The Castle, one of Capitol Reef’s many impressive geological features, towers 800 feet above the park’s visitor center.

Past the Rim Overlook, the route to the Navajo Knobs keeps mostly to cliff edges but rarely close enough to make the typical person nervous. (That includes me in this case!) Although the trail is almost exclusively uphill, the grade stays below 30% except during a short, final scramble up one of the knobs. While some guidebooks claim there are two knobs, that’s not true as there are a whole cluster of bulbous bulges of varying sizes protruding from the plateau top. The trail leads you up the westernmost one.

The views along this path were spectacular and alien even to us, Utah natives. The plateau traversed is not straight but noticeably angled, giving a greater appreciation for the wrinkled nature of the Waterpocket Fold, Capitol Reef’s defining geological feature. This lovely setting must be too strenuous for most as we saw just two people in total once we passed the Rim Overlook. I was okay with that.

Navajo Knobs
Up close, the Navajo Knobs are more intimidating but still knobby.

It took us five hours and 40 minutes to complete the Navajo Knobs, which apparently is in the “normal” window. Also in our normal window is not making it back before dark. We were typical in that regard as well. We only needed flashlights for the last third of a mile though, and that’s better than our average.

For our last day in Capitol Reef, we decided to hike another route classified as strenuous, the Freemont Gorge Overlook, even though we’d pushed my knee and our legs in general the day before. (For the record, my knee handled the challenge with dignity and only a little swelling.) The path to the Fremont Gorge Overlook, according to the park’s trail guide, is identical in length and almost equivalent in elevation change to the Rim Overlook. Therefore, we were expecting another enduring uphill workout. Instead, we got ups on either end of a long section of level.

Johnson Mesa
Johnson Mesa is topped with black boulders and abundant grasses.

The route climbs one steep 300-foot hill and then kicks back for an extensive, nearly flat traverse across the meadow topping Johnson Mesa. Johnson Mesa’s crown is strewn with desert grasses and lava rocks spewed from Boulder Mountain 20-30 million years ago. Glaciers brought those giant stones to Capitol Reef at the end of the last ice age where they now look completely out of place. That curious meadow is followed by another long climb, about 700 feet in elevation.

The Fremont Gorge Overlook is about 4.5 miles RT. It took us a bit under three hours and required less energy than the Rim Overlook portion of the Navajo Knobs Trail, despite their supposed similarities in length and elevation change.

Fremont Gorge
The Fremont River has dug a trench 800 feet deep over eons, and it’s all on display from the overlook at trail’s end.

Please note, the Fremont Gorge Overlook has absolutely no shade on it. If you hike it in the summer, I’d highly recommend going early or late in the day. The other thing it had absolutely none of? People. We saw exactly no one on it, which made it all the better.

That sums up the Torrey piece of our desert extravaganza. The entire holiday pie was magnificent and memorable from its smallest corridors to its vastest vistas! I’ll end with one final comment on luck. Spring weather in Utah can be temperamental, but it was nearly ideal during our entire trip. It oscillated from the low 70s to the mid-80s and was almost always windy. It never got uncomfortably hot, but we did make use of jackets on occasion. The day we left, temperatures dropped down into the 50s, and it started raining. The luck of the slickrock was on our side!