My family history in the Eastern Sierra and Yosemite dates back almost eighty years. In 1938, while on a hiatus from living in prewar Los Angeles, my fraternal grandmother, Dorothy met her second husband John A. McCollum there. At that time, he was helping construct U.S. Highway 395 near Bridgeport, California. They fell in love, were married and for the next fifty years returned to fish for trout in Gardisky Lake and Saddlebag Lake near the Tioga Road. In 1944, my mother, Phyllis married my father, Loron N. McGillis. For their honeymoon, in December of that year, they chose Yosemite Valley.

In 1959, I got my first taste of Yosemite National Park and nearby Mono County. For several nights, our family of five camped in Yosemite Valley. When we naively set out one morning to climb the Yosemite Falls Trail, we took no water or food. By the time we reached the base of the main falls, we were hot, tired and dehydrated. When my father wisely made the decision to turn back, at infamous Columbia Rock, I refused to move. The lure of the giant waterfall was too strong for me to admit defeat and return to our campsite.

At night, bears would roam the campgrounds, silently looking for food. On our final morning in Yosemite Valley, a neighboring camper showed me where a bear had licked the side window of his old truck. There had been a melon sitting on the front seat, but bears and people were more naïve in those days. Instead of smashing the window and taking the melon, the California Black Bear walked around our sleeping bags and headed back to his or her domain.

When we left Yosemite Valley, we drove up Highway 120, heading for Tioga Pass and the town of Lee Vining, California on the far side. Although it was late June, there was still snow in the high country. Two years later, in 1961, construction crews completed the modern version of the Tioga Road, all the way to the eastern entrance of Yosemite Park, at the top of Tioga Pass.

Because the construction season was so short and there was no alternate route, traffic stopped for up to one hour at a time. Traffic would alternate at the construction sites and then everything would close down for an hour or more blasting and grading around Tanaya Lake. As a ten year old, the experience seemed to last forever. Even after the arduous trip over the Tioga Road of old, we motored on. In late afternoon, we arrived in the City of Bishop, California. There, we spent the night at a motel with a swimming pool. To me, it seemed the height of luxury.

From Bishop to our home in Burbank, California was about a three hundred mile trip, featuring desert heat and Sierra Nevada views much of the way. In the late 1950s, most of U.S. Highway 395 was a two-lane road, with only occasional passing lanes or other safe places to pass slower vehicles. To this day, one treacherous stretch of road between Olancha and Cartago remains as it was back in the day. With completion of a four-lane bypass scheduled for 2022, I guarantee every day, some fool will pull out to pass, even though there are twenty vehicles ahead of him.

Since my first visit to Yosemite National Park, it has held a place in my heart, as it did for my parents and grandparents before me. Over the decades, I would often visit Yosemite, driving north on U.S. Highway 99 to Fresno and then northeast on Highway 41. Once inside the national park, the highway becomes the Wawona Road. From Los Angeles to Yosemite Valley was a three hundred mile trip, with lots of San Joaquin Valley heat to endure. From Yosemite Valley to Tuolumne Meadows was only sixty miles, but that took another two hours via the Tioga Road. In recent years, I realized it was eight miles shorter to drive from Los Angeles to Tuolumne Meadows via Highway 395 and then over Tioga Pass. In addition, once you leave Bishop, heading north, you ascend almost immediately into the high country, with its cooler temperatures and scenic views.

After a decade of drought in California, the winter of 2016-2017 brought record-setting snowfall in the Sierra Nevada. With a cool springtime and a late start to summer heat, many Sierra trails and secondary roads remained blocked well into July. After seeing a complete lack of snow atop Mammoth Mountain in August 2016, I wanted to see the Sierra snowpack that remained this summer. In order to avoid July 4th weekend crowds, I planned my trip to end on July 1, 2017.

When I left Los Angeles on June 28, my initial destination was the Mammoth Mountain RV Park. I planned to road test my New Titan XD truck, towing our travel trailer to that location. From there I could venture to Lee Vining and then over the Tioga Road to Tuolumne Meadows. Over the winter, the meadows had received up to thirty feet of snowpack. In Mammoth Lakes, at an elevation of 7,500 feet, there was no trace of snow. At an elevation of 8966 feet, nearby Lake Mary was still frozen. As is often the case in July, the days were warm and the nights were cool.

After arriving at Mammoth Lakes, I remembered that it takes almost a week to acclimate to the altitude. On Thursday morning, I slept late and did not venture away from my campsite until late afternoon. Wanting to test my four-wheel drive system, I drove my new truck to Obsidian Dome, just fifteen miles away. One of five volcanic craters in the Mono-Inyo Craters group, I knew that the Obsidian Dome forest trail was challenging but not too daunting for such a big truck.

Looking more like a huge pile of volcanic rocks than a crater, I decided not to hike to the top of the dome. Instead, I drove to a turnout in the woods and enjoyed the solitude of the place. Soon, two other vehicles pulled up to my secluded spot and idled for several minutes before moving on. One might think my spot was the only place to stop in the Eastern Sierra. After the interlopers departed, I noticed that there was still snow a few hundred feet above my location.

Upon returning to the RV Park, I confirmed that the Tioga Road had indeed opened to traffic on that very day. The next morning, I started out for the historic town of Lee Vining and then up the Tioga Road to Yosemite National Park. While talking on my mobile telephone, I became distracted and missed the Tioga Road turnoff. That was a lucky break, because a trip through Lee Vining on Highway 395 is always a treat. Just north of the town, there are spectacular views of ancient Mono Lake, so I stopped to take pictures.

In all my years of visiting Mono County, I had not seen the lake level so high. This summer, there was more water available to the City of Los Angeles than it could divert. As a result, Lee Vining Creek and other streams in the Mono Lake watershed appeared to disgorge directly into the lake.

After researching historic water levels at Mono Lake, I determined that the July 7, 2017 elevation of 6380.4 ft. was up 2.1 ft. from the same date the previous year. Even at that, the lake level was forty-seven feet lower than it was in 1919. Today, the City of Los Angeles and the Mono Lake Committee have an agreement regarding diversion and partial refilling of Mono Lake. With its gently sloping shores and shallow depth, even a small rise in water level covers a vast expanse of the original lakebed.

After gazing at Mono Lake, I realized that I had driven right past the Tioga Road Junction. Soon, I turned around and headed back toward Highway 120, also known as the Tioga Road. When I stopped at the service station just off Highway 395, I could see that it was busy. Inside the store and deli, several hundred people milled around and blocked every aisle. Luckily, I had brought my own snacks and did not need to wait in line for food.

Back on the Tioga Road, I used the torque of the Titan XD’s turbo-diesel engine to glide up the steep grade. I was passing slower vehicles and appeared hell-bent to get to the high country. Then, I saw the first of two large lakes visible from the highway. It was full to the brim and the spillway was open. I stopped to see a cascade of water plunging down the rocky slope into Lee Vining Creek. At each subsequent stop, I positioned the truck off-road, so I could and take pictures through the open side window. On the return trip, I would photograph points of interest on the other side of the road. One place I stopped, the Tioga Pass Resort, founded in 1914 was flooded and partially destroyed. That was my first taste of infrastructure destruction in the area. Later, I learned that the resort would not open for the season in 2017.

By the time I reached Tuolumne Meadows, I realized that I had missed the sign for the Tuolumne Meadows Lodge, which is located in the woods, to the east of the actual meadows. Strange… I thought. Did they cover or remove the signage? Before long, I arrived at the Tuolumne Meadows Store. I should say… what was left of the store. In the late fall, the store is stripped of its canvas roof. As winter snows fall, they drift and accumulate inside the skeleton of the wooden structure.

This year, over thirty feet of snow accumulated on the concrete floor of the store. We perceive that snow melts vertically, disappearing into the earth without a trace. The reality is that deep, wet Sierra Nevada snow-pack behaves like a slow-motion glacier. As the snow-pack accumulated in the store, it could not melt through the concrete floor, so it pushed sideways, contorted by both wind and gravity. The result was about ten-years of weathering in only one season. The ends of rafters snapped under the load. Anything left standing looked decrepit and derelict.

Compared to the summer drought of 2016, this year Tuolumne Meadows looked green and lush. There was no remaining snow in the upper meadow, but high water flowed down the Tuolumne River. When I headed west another mile along the Tioga Road, I came to the lower meadow that gives the place its plural name. There, the river had backed up at the entrance of a small canyon, creating a seasonal lake. A later check of Google Maps showed no lake in that location, only a wide spot in the river.

Traveling back to the east, toward Tioga Pass, I turned right on to the Tuolumne Meadows Lodge Road. At a fork in that road, temporary barriers blocked blocked vehicle access. Parking in the adjacent parking lot, I began a short hike up the closed road. My goal was the Tuolumne Meadows Lodge, with its famed tent-cabins, dining hall and general store. With no one else in sight, my hike alternated between hot sun and gentle shade from the pine and fir trees. When I arrived at the lodge parking lot, I saw the first signs of destruction.

During the spring melt, the Dana Fork of the Tuolumne River had breached its natural banks and an errant stream had cut through grounds of the lodge. Below, mud, rocks and gravel lay fanned out across the parking lot. Closer to the wood-framed lodge, the new stream had cut a v-shaped channel in the pathway. Although a dozen of the tent cabins had their canvas tops and sides installed, there was no sign of any additional work or work parties.

On August 25, 2016, I had visited the Tuolumne Meadows Lodge. By chance, it was the centennial of the U.S. National Parks Service. On that date, the lodge was bustling with activity. Some people sat in the shade, reading, while others had lunch in the dining hall. Hikers and visitors crowded the little store, buying backcountry supplies. Unless one had a prior reservation, no lodging was available. After ten years of drought and insignificant snowfall, the lodge had opened early in 2016.

On the Friday before the July 4th weekend of 2017, the scene was quite different. No other humans were in sight. Almost nothing of the old wooden lodge had received attention. The white-painted structure looked like the bleached bones of a beached whale. The shed roof in front was broken and falling down. Many of the hand-made trusses that supported the dining hall roof were broken. One dangled over the concrete floor, hanging by a length of old electrical conduit. No one had yet taken a broom to the floor, let alone repaired any of the extensive damage. It appeared that the many layers of flaking white paint were all that held the structure together.

Out back, I had the cascading falls of the Tuolumne River’s Dana Fork all to myself. I could see where the river had jumped its banks and toppled an enormous old tree. Steel lunch tables, where campers had sat reading the previous year lay crumpled and broken by the weight of the winter snow-pack.

With no one working and the road so recently opened, repair of both the Tuolumne Meadows Store and Lodge appeared to be an overwhelming task. With California experiencing the lowest unemployment figures in a decade, I wondered who would endure the hardship of living in a tent cabin in order to rebuild derelict buildings that might not be repairable. With meager federal government funding for the National Park Service, where would the money come from to repair structures that my parents had first visited seventy-five years ago?

At the old Tuolumne Meadows Service Station, I noted that there were no gas pumps. Where once had been a concrete pad and a service island was a large patch of gravel. Nearby, I photographed an old roadside sign. For motorists heading west to Yosemite Valley, it read, “No Services Next 39 Miles”. The irony was that there were no motorist services for the seventy-five mile stretch between Lee Vining and Yosemite Valley. As I departed Yosemite National Park, I realized that high country visitors would find no food, fuel, campsites, wilderness permits or lodging any time soon. As with everything else in Yosemite and Mono County this year, unprepared travelers could be in for a rude shock and a very long wait.

Email James McGillis

You Won't Need a Furnace at Furnace Creek in Death Valley

In November 2016, on my first trip to Death Valley National Park, I started with a sundown visit to Zabriskie Point. As darkness gathered on the floor of Death Valley, I located my campsite at the Furnace Creek Campground. The temperature felt warm, but after sunset, it no longer felt amazingly hot. With the doors and windows open on my coach, I was able to move indoors as the evening progressed.

The campground itself will look familiar to anyone who has camped in a National Park. You will recognize the layout as a series of loop-roads. Each loop has fifteen or twenty campsites. At Furnace Creek Campground, a recent change in management resulted in the repaving of all its roads and refurbishment of water and restroom facilities. The setting is ancient, yet the campground feels new again. Unobstructed views of both the Amargosa Range and the Panamint Range add drama to the scene.

Since the few full-hookup RV-sites were long since reserved, I settled for two nights of dry camping in a dry desert. Luckily, the water supply at Furnace Creek is sufficient for cooking and bathing. The first Anglos to visit Furnace Creek in 1849 barely found sufficient water to survive until their rescue in 1850. By the early twentieth century, residents and tourists at the village of Furnace Creek could enjoy potable water piped to the town from artesian springs in the nearby Amargosa Range. Today, groundwater withdrawal and storage tanks support what looks like a thriving oasis, but is actually doomed to return to its dry state at a time uncertain. With such paltry rainfall in Death Valley, groundwater pumping is ultimately unsustainable. Except for rare seasonal flow, what once was a true oasis along Furnace Creek is now mostly a dry wash.

Although there is a wide range of tourist services at Furnace Creek, the 2010 U.S. Census pegged the fulltime population as only twenty-four hardy souls. Admittedly, most of the public and private facilities in Furnace Creek are air-conditioned, making life easier for heat-weary visitors and workers. One exception to that is the Native Americans known as the Timbisha Shoshone Tribe. As a federally recognized tribe, their small, private enclave adjacent to Furnace Creek appeared to be hot, dusty and dry. What few trees and shrubs that survive the harsh climate provide scant shade or relief from the sweeping winds. Recent data suggest that the Timbisha tribal population in Death Valley is around forty individuals.

During my November 2016 visit, there was not a trace of water on the vast salt pan, including the Upper Basin, Middle Basin and Badwater, which lays almost 280-feet below sea level. Furnace Creek, on the other hand, is only 190-feet below sea level. This difference in elevation means that in wet years, water will overflow the Upper Basin, pass through the Middle Basin and form a large, shallow lake at Badwater Basin. Salt, borax and alkali, which dries in the connecting channels suggests a short-lived, landlocked stream that may flow through Death Valley in the springtime. Upon my return in February 2017, all three basins contained surface water. By April 2017, almost all of the surface water had evaporated or settled into the graben, leaving the salt flats dry and susceptible to wind erosion and vandalism.

While visiting Furnace Creek in February 2017, water seemed to be everywhere. The dry lakes were wet. Furnace Creek flowed down its traditional course and water fell from the sky, in the form of rain. Upon arrival, the evidence of flood damage to roads and trails was evident. Orange traffic cones stood guard at many small washouts along Highway 190, leading to Furnace Creek. Nearby Artists Drive, a one-way formerly paved road through spectacular canyon scenery remained washed out. After historic winter rains had swept that road away in many places, workers used heavy machinery to make repairs. During our February visit, only gentle showers passed through Furnace Creek. The showers cleared the air, leaving the scent of moist creosote in an otherwise desolate place.

Why was the winter of 2017 so wet in Death Valley? My personal observations may or may not be scientifically correct, but here is my theory. North of Furnace Creek the Panamint Range to the west and the Amargosa Range to the east form a sort of wind tunnel. Between Tin Mountain (8,953 ft. elev.) and Grapevine Peak (8,743 ft. elev.), a cyclonic effect can arise. If little moisture is available, a whirlwind or “dust devil” will rise and sweep toward Furnace Creek and Badwater to the south. If the counter-clockwise wind is strong enough, it can pull moisture from the Eastern Sierra Nevada Range and feed it toward the salt flats of Death Valley.

Another contributing factor in rainfall is dust particles. In February, I watched a tall, thin strand of wind shear traveling along the course I already described. As it reached the Middle Basin, it had enough strength to kick up untold amounts of dust from the periphery of the standing water. Soon, we could see a large cloud of dust and rain forming against the eastern slopes of the Panamint Range. Upon our return to the campground, another shower swept from North to South. With the minimal moisture we experienced, only the rock strewn landscape hinted at floodwaters issuing forth from every canyon and wash in Death Valley. The recent winter rains must have been a dangerous, yet remarkable sight.

By April 12, 2017, when I again visited Furnace Creek, it was hot and dusty. Again, I dry camped, but this time it was warmer, approaching 100 °F (37.8 °C). With the wind and sand looking to sandblast my truck, I decided to hunker down inside the trailer until the wind abated. Using my cordless vacuum to keep up with the dust in my coach was almost a full time job. If I had opened the door, it might have blown off its hinges, but would surely fill my coach with even more dust. With my afternoon spent inside a hot coach, I began to understand how the original pioneers of 1849 must have felt. Trying to allay both wind and dust, they had nothing more than brush lean-tos to protect them against the onslaught.

For me, temperatures above 100 °F (37.8 °C) are uncomfortable. In the heat of summer, many Norwegians visit Death Valley. Considering the cool air in their home country, Norwegians come to Death Valley in the summer just to feel outdoor heat for the first time in their lives. Whether my Norwegian story is true or not, German, Dutch other Northern Europeans find Death Valley to their liking. No matter what time of year, it is common to hear people speaking various European languages in and around Death Valley National Park. Since older members of the Timbisha Shoshone Tribe still speak their native language, you might have the rare opportunity to hear that language spoken at Furnace Creek, as well.

Email James McGillis

Zabriskie Point in Death Valley - It's not a gap...it's an abyss!

- “How you get there depends on where you're at.”

For most of my life, I avoided Death Valley like the plague. The stories about an ill-fated attempt to reach California by wagon train in 1849 - 1850 created a daunting image. The graben of Death Valley holds the record as the hottest place on Earth, with five consecutive days in 1913 registering 129 °F (54 °C), or above. Annual precipitation at Death Valley averages less than 2.5-inches. Further, its existence as the lowest point of elevation in the United States added to the negative connotations in my mind.

Then, in November 2016, I traveled from Las Vegas, through Pahrump, Nevada and on to Death Valley National Park, California. Other than photos and video I had viewed of the area, I had no idea what to expect. What I found upon arrival was reminiscent of a Martian landscape, rather than Earth. Volcanism, erosion and rocky or sandy soil abounded. As distinguished from the face of Mars, there were a few hardy plants and animals, but otherwise, normal life-support seemed unlikely.

Before arriving at my campsite in Furnace Creek, I visited Zabriskie Point. Relatively unknown until the latter 20th century, Zabriskie Point became the prime location and namesake of Michelangelo Antonioni’s 1970 counterculture flick. Filmed in 1969, with music by Pink Floyd and Jerry Garcia, the movie features an incoherent plot, as if the cast and crew were not only blazing in the sun, but also blazing on lysergic acid (LSD). In fact, the often-panned, but

of fame or infamy.

On Oct. 12, 1969, at Barker Ranch, in Death Valley, just north of the San Bernardino County town of Trona, the murder spree of the Charles Manson “family” ended with his arrest. In September 1973, members of the rock band, The Eagles accompanied singer and songwriter Gram Parsons to the place and time of his death in Joshua Tree, California. According to public records, between October 2003 and November 2013, twenty people of lesser fame died in or around Death Valley. On July 6, 2014, hikers in the badlands near Zabriskie Point discovered the body of British actor Dave Legeno, known for his role as werewolf Fenrir Greyback in three of the ‘Harry Potter’ films. Temperatures at the time of Legeno’s death were as much as 123 °F (50.5 °C).

In the film Zabriskie Point, I remember a scene with the male and female stars standing on a tiny pinnacle of land. Filmed at sunset, one can see the Panamint Range looming and glooming in the west. As the stars embrace, the camera revolves around them. Amid clouds of dust, we see lots of skin and writhing bodies. Amidst the whipping wind and the grand vistas at sundown, we see dozens of couples apparently copulating on the hillocks below. After almost fifty years, both film acolytes and the curious continue to trek up the hill to see that famous spot. That tiny pinnacle of film-fame has eroded into dust. Oh, that the faithful shall not trample His grave, too.

In 2004, a flash flood swept across the highway, uprooting and destroying the substantial concrete pit-toilets previously installed in the parking area. After extensive repairs, both then and in 2014, there is now a paved pathway, leading up to a viewing plaza. With its low stone wall, the plaza is about the size of a baseball diamond. Although the once remote place called Zabriskie Point is no longer so remote, the views at sundown are every bit as exciting or sublime, depending on one’s energies at the time.

heritage.

On an April 2017 visit to Zabriskie Point, I noticed a curious recurring phenomenon. Once again, the sun set through the abysmal gap, framed by the Panamint Range, which is visible west of Zabriskie Point. At sunset, the place darkened like a theater when the lights go down. After staring toward the sun for the final fifteen minutes of daylight, my eyes could not readily adjust to the twilight and approaching darkness. Although the sun still shone for a time on the Amargosa Range to the east, the Zabriskie Point plaza looked like there had been a solar eclipse.

After gazing around the plaza, I snapped a few photos of the sunlight as it receded from the Amargosa Range. As darkness rapidly approached, all visible landforms were in shadow. Since there was nothing more to see, I sauntered down the sinuous pathway that led to the parking lot below. Here is

the curious part. At the end of each visit, I spotted several photographers carrying long-lens cameras. Each was hoofing it up the pathway to the viewing area. I wanted to say, “It is all over. Don’t even bother going up there. There is nothing more to see”.

If you plan to visit Zabriskie Point and view that famous sunset, do not refer to the official sunset times listed in your almanac or on a weather website. They will list the time of day when the sun slips below the Earth’s horizon, not when it disappears behind the Panamint Range, which may be ten or fifteen minutes earlier.

Each time that I observed a Zabriskie Point sunset, several photographers ran toward the ancient plaza. With the sun already set, one can only hope that they arrived in time to take pictures of the

Email James McGillis

Let's Go Places and Find New Roads to Crescent Junction, Utah

Recently, I received an email message from Ms. Bobbe Wimmer Kidrick. She wrote, “I read your articles about Crescent Junction, Utah with a great deal of pleasure. My grandfather, Thomas G. Wimmer initiated the homesteading of Crescent Junction. I have pictures of family members, some of the buildings and additional history.”

Bobbe went on, “The history of Crescent Junction really began with the homestead. My grandfather, Thomas G. Wimmer was a diversified businessman (sheepman, river runner and freight hauler) who lived in Green River in the early 1900's. In 1916, he contracted to haul equipment from the railroad to build the copper mine at Big Indian, some fifty miles south of Crescent, in the Lisbon Valley, Utah.”

“At the time (1915/16), the road didn't go directly from Moab to Crescent. It went north as far as the place then called Valley City. From that central point, the road veered west to Floy (AKA Little Grand) and east to Thompson (now Thompson Springs). Because there was a railroad siding at Crescent (Brendel), he decided it would be easier on his team to go directly north to Crescent. A short time into the operation, he persuaded his two daughters, Laura and Marg to file for a homestead at what is now Crescent Junction.”

“Laura and Marg filed for 160-acres each, and my dad, Ed Wimmer, being too young to file, lived there with them. Ed fell in love with the desert and no matter where he was, he was always ‘going home’. For the required five years, Laura, Marg and Ed lived at the railroad siding known as Brendel, with no road access closer than Thompson, which is six miles to the east. In 1923, after living there for the required five years, the two young women received the patents for 160-acres each. They later divided the 320-acres into three parcels of 106 acres each, and deeded the middle parcel to their Dad (Thomas Wimmer). This then was the beginning of Crescent.”

Bobbe said, “I am telling you all this to put it in perspective. Although I was born in Moab, I now live in the Salt Lake area. Here, I will tell my father, Ed Wimmer’s story.”

“Ed Wimmer was born in Salt Lake City in 1900, but spent much of his formative years in Green River, Utah. He grew to love the desert, to the point that no matter where he went throughout his life, he always returned. After graduating from East High in SLC, he married Erma Snyder and they moved to Helper, Utah, where he worked as a Railroad Express Messenger. As such, he was required to carry a gun because he took the mine payroll from Helper to Sunnyside, a distance of thirty-three miles. Their oldest child, Bette was born in Helper.”

“The family moved to Los Angeles shortly after Bette was born and Ed worked for Crescent Creamery. Their second child, Bud was born at this time. From there, the growing family moved back to Utah, living in the town of Cliff. At that time, son Duane was born in nearby Fruita, Colorado. Soon thereafter, the family moved again to Los Angeles, where Ed worked in the petroleum industry. Their fourth child, Pat was born at this time.”

“In March of 1932, an earthquake shook Southern California and the country was in the middle of the Depression. After arranging with his brother, Andy to buy calves and start a dairy heard in Utah, the whole family traveled by automobile back to Utah. Even in early April, it was hot in the desert, so they traveled at night for the first two days. Bette remembers Las Vegas as being little more than a small oasis, and certainly no casinos.”

“Their journey took them through Mesquite, Nevada, and on to St. George and Cedar City, Utah. They turned east at Cove Fort and then through Price, and eventually to Green River. When a hoped-for ranch in Green River was unavailable, Ed moved the family to Moab in 1934, where he continued to try to make a go of the dairy business. The last child, Bobbe was born there in 1934. Even after moving the family to Roosevelt, the dairy business did not thrive.”

“When the Second World War broke out in 1941, Ed secured a job as a welder in Salt Lake at the Remington Arms plant. Also during that time, he worked in Hawaii as a welder, repairing damage sustained during the Japanese attack on Pearl Harbor.  As the War ended, he then returned to Salt Lake, where he started a service station. In 1947, Ed Wimmer headed back to Crescent for what would be the last time. There he established the Crescent Junction Service and Café, which he and Erma owned jointly until his death in 1951. Erma retained ownership of both businesses until 1969, when she turned the service station over to son Pat and the Café over to daughter Bette and her husband, Al Lange.”

“After the War ended, Dad headed back to Crescent. He had very little money but owned a redwood livery barn in the backyard of the house in Salt Lake. After dismantling the barn, Dad, Bud and Duane left Salt Lake with a load of wood and high hopes to begin the building at Crescent Jct. They laid the foundation of Crescent in July of 1947. It was on July 24, that they poured the cement floor. At the time, Dad marked the date in the wet cement writing, ‘Just 100 years after Brigham (Young)’.”

“Mom and Dad gave their all to Crescent and in many respects; they expected the same from the rest of us. Money was always hard to come by, so we made do with what was available. Mom sold the house in Salt Lake. The proceeds went to pay debts incurred by an employee at Dad’s service station on Main Street, Salt Lake. Dad felt honor-bound to clear up everything even though he was not legally responsible. I also found out, years later, that he had cashed savings bonds belonging to me to buy materials for the first building. No matter… it was a family project and we all did what we could. Some of the proceeds from a small curio business I handled during the early 1950s also went into the business.”

“Providence has a way of looking out for those who can't or don't look out for themselves. In Crescent, we had been using a Koehler Light Plant for power. Then, just a few months before Dad died, Utah Power & Light built a small sub-station to provide electricity to Crescent. By that time, all the debts from Salt Lake had been paid and there was a growing business with comfortable living quarters. Dad (Ed Wimmer) died in October 1951, but in his fifty-one years, he had done what he set out to do. He made it home to Crescent, and in doing so, took some of us ‘home’ with him.”

“Mom (Erma Wimmer), was often seen as strong willed and opinionated, but over the next eighteen years, those traits would serve her well. Upon dad’s death in 1951, she became sole owner of the business. From 1947 through 1966, Crescent’s water problem was solved by hauling water from Thompson, six-miles east. At first, we used a fifty-gallon barrel on the back of a pickup. Later, as need dictated, we graduated to a 1000-gallon tank on a larger truck. A cistern was built and the water dumped into it, to be pumped out as needed.”

“The cistern was in place until 1966, when mom obtained a loan from Utoco (Utah Oil Refining Company), to buy the necessary supplies to build a waterline from Thompson. Pat, with the help of family and friend Tony Pene, walked a Ditch Witch from Thompson to Crescent during 1966 and ‘67. In the resulting trench, they installed the waterline. The loan was paid back through gas sales for the next several years.”

“In the early 1970s, there was a move underway to build Interstate Highway I-70 between Colorado and I-15 in Western Utah. Mom became aware of the fact that the new highway was proposed to go through Grand County. When she discovered that its route would bypass Crescent Junction, about four miles south of the existing highway between Thompson and Green River, she took action. She approached Archie Hamilton, the project manager, and offered to trade acreage at Crescent for the new project. He accepted her offer and I-70 now runs parallel to the old highway. If built as originally planned, I-70 would have bypassed Crescent Junction, leaving the Wimmer family business high and dry.”

“When Aunt Marg died in 1949, she left her original portion of the Homestead to Dad (Ed Wimmer). Upon his death, under Utah law, the property was intestate. As such, one-third went to Mom (Erma Wimmer) and the remaining two-thirds to his five children. By 1955, Bud, Duane, Pat and I were all married. Bud lived in California, Duane in Moab, teaching school, Pat at Crescent, managing the station and my husband Ralph and I lived in various places throughout the country, due to his work. We always kept our mailing address at Crescent and Mom would forward it each week.”

“In 1969 mom got in touch with, Bud, Duane and me, saying that she was considering signing the business over to Pat and Al, in joint tenancy with rights of survivorship. She asked what we all thought about that idea. We all three agreed that it was her right to make the decision. She explained in the letter that she was feeling a certain amount of pressure to make sure the business remained, as it then existed. She did just that and the business remained that way until recent years.”

“Thomas Wolfe once said ‘You can't go home again’ and largely, he was right. It just all depends on how or what you define as home, I guess. I will never ‘go home again’ physically but I know ‘home’ is there at Crescent Junction.”

Here, I will express my appreciation to Bobbe Wimmer Kidrick. She is one of a few individuals who have both lived and worked at Crescent Junction, Utah. By sharing stories about her extended family and their home in the desert, she has made her “home” come alive.

In 2009, I first mention Crescent Junction in an article titled, “Rediscovering the Old Spanish Trail - Now it's a Freeway”. In 2010, I returned to the area and wrote “Green River to Floy, Utah, via Old Hwy. U.S. 6 & 50”. Later that year, I wrote, “Crescent Junction, Utah - It isn't Brendel Anymore”. In 2011, I wrote about the transfer of uranium mine tailings from Moab to a disposal site near Crescent Junction in, “The ‘Train of Pain’ Travels Thirty Miles from Moab to Crescent Junction”. In 2012, I wrote, “Interstate I-70 from Cove Fort to Crescent Junction, Utah”.

Also in 2012, I wrote, “Brendel, Utah - Still Moving Around on the Map”. When Bobbe Wimmer Kidrick’s niece, Lani (Lee Anne Lange Asay) wrote to me with some pictures of Crescent Junction, I published, “A Resident of Crescent Junction, Utah Tells the History of the Place”. In 2014, when the Grand County Council made plans to defile the Sego Canyon Indian Rockart site near Thompson Springs, I wrote “Grand County Council Plans to Desecrate Sego Canyon’s Ancient Indian Heritage Site”.

If you find yourself traveling past Crescent Junction, Utah on I-70, be sure to stop at Papa Joe's Stop & Go for gas and refreshments. If you do, you will see firsthand the place homesteaded by the Wimmer family a century ago. You may also notice that in Crescent Junction, the more things change, the more they stay the same.

Email James McGillis