Widtsoe – Garfield County Ghost Town

Widtsoe (pronounced /ˈwɪtsoʊ/) is a ghost town in Garfield County, southern Utah, located in Johns Valley along the East Fork of the Sevier River at the mouth of Sweetwater Creek. It sits at an elevation of about 7,605 feet (2,318 m), roughly 15–16 miles northeast of Bryce Canyon National Park. The town existed primarily from about 1908 to 1936 (with earlier seasonal use of the valley) and stands as a classic example of an ambitious early-20th-century dry-farming settlement that flourished briefly before collapsing under environmental and economic pressures during the drought years and the Great Depression.

Emery Valley Mercantile Co. store in Widtsoe, 1936
Emery Valley Mercantile Co. store in Widtsoe, 1936

Early Settlement and Ranching Era (1870s–early 1900s)

Johns Valley was used mainly as seasonal open range for cattle by local ranchers in the late 19th century. Permanent settlement began around 1876, when Isaac Riddle and others (including a wife of John D. Lee) established a presence. Riddle’s ranch became a key regrouping point for the San Juan (Hole-in-the-Rock) Expedition in 1879. James Houston, a Mormon stake president from Panguitch, ran cattle in the area as early as 1872. Through the end of the century, the high, cold valley supported few permanent residents; it remained primarily stock country.

Founding and Rapid Growth (1902–1920)

In the early 1900s, Jedediah Adair purchased land and successfully grew oats, wheat, and barley using dry-farming techniques suited to the arid high country. His results drew other settlers. By 1908 the community was known as Adairville. In 1910, Adair’s wife Julia Ann donated 40 acres for an official townsite, laid out in the typical Mormon “Zion” pattern: a central park and church/school meetinghouse surrounded by one-acre family lots, with streets 5 rods wide and blocks 20 rods square. Additional land was later donated (including 160 acres in 1914 by the Mangums and Quince K. Kimball).

The settlement went through several name changes reflecting prominent local Latter-day Saint leaders:

  • Briefly Houston (after John/James Houston, Panguitch stake president).
  • Winder (after John R. Winder of the LDS First Presidency) when a post office was granted in 1912.
  • In 1917 the post office required another change because of duplicate “Winder” names in Utah; the community chose Widtsoe in honor of John A. Widtsoe (1872–1952), then president of the University of Utah, an agricultural scientist, dry-farming expert, and later LDS apostle. His work on dry farming and irrigation had directly aided local farmers.

Nearby settlements (including Henderson a few miles north) gradually consolidated into Widtsoe. Infrastructure developed quickly: sawmills supplied lumber; a combination church and school (later a three-room schoolhouse); two hotels; four stores; a confectionery; a post office; and, by 1915, piped running water from a local spring. In 1919 the U.S. Forest Service moved its district office (and the area’s first telephone) from Panguitch to Widtsoe. There was serious discussion of relocating the Garfield County seat there.

Population estimates vary. Some accounts place the peak at around 1,100 in 1920 (when the town was described as one of the principal communities in the county and its grain production reportedly exceeded that of the rest of Garfield County combined). The 1920 census figure cited in detailed local research is closer to 365. Regardless of the exact number, the town was prosperous enough that residents enlarged nearby Pine Lake and built an embankment dam in anticipation of further growth.

Decline (1920–1935)

A severe drought began in the summer of 1920, threatening crops. Rain arrived late that season and produced a decent grain harvest, but dry conditions continued. The high elevation and cold limited vegetable production; soil quality was marginal; floods and erosion compounded problems. An apparent multi-year cycle of drought versus better water years worked against the settlers. By the mid-1920s the only consistently successful crop was a high-altitude variety of iceberg lettuce.

In 1923–1924, California developer and Imperial Valley irrigation pioneer W.F. Holt invested heavily (reports of nearly $300,000) at the urging of Utah state senator Quince Kimball. Holt bought the Widtsoe Hotel, built more than ten homes, founded the nearby settlement of Osiris, constructed irrigation works (storage pond and flume bringing water about 7 miles from Pine Lake), installed telephone lines, established a creamery, and promoted high-altitude lettuce seed. The efforts failed against persistent drought, erosion, rodents, and climate extremes. The Forest Service office left in 1925. Population fell to 210 by 1930 and to only 17 families (or about 40 families in some accounts) by 1934–1935. The area was described as among the most destitute in Utah during the early Depression years.

Post office and postmistress, Widtsoe, Utah.
Post office and postmistress, Widtsoe, Utah.

Federal Resettlement and Abandonment (1935–1938)

In spring 1934 residents petitioned for federal help. Officials of the Resettlement Administration (a New Deal agency) concluded the land was sub-marginal and could no longer support agriculture. On February 8, 1935, residents voted to accept resettlement assistance. The government purchased roughly 30,000 acres for about $81,300, resettled 29 families to more productive land elsewhere in Utah, and used the Widtsoe Project as a model for similar programs in other western states. Administrative costs exceeded the purchase price, and the process was slow.

In 1936 the Resettlement Administration bought out remaining landowners. Most buildings were demolished; more than 26,000 acres were placed under the Taylor Grazing Act for public grazing. Photographer Dorothea Lange documented the nearly empty town for the agency in April 1936, producing well-known images of the post office and postmistress, the Emery Valley Mercantile Co. grocery store, approaching views of the settlement, and families preparing to leave. The last federally assisted families departed by March 1938. The name was removed from highway signs and maps.

Legacy and Present Condition

A few structures survived: remnants of a schoolhouse (sometimes described as the original one-room building), the Woodard house (with an assay-office extension), a barn, a few private residences or summer cabins, sheds, and root cellars. Foundations, debris, and a weathered stop sign have also been noted. Ownership is mixed (private, State of Utah School and Institutional Trust Lands Administration, and federal). An active pioneer cemetery remains nearby and continues to see occasional burials. Visitors are cautioned not to remove artifacts, as both federal and state laws protect the site.

Widtsoe illustrates the limits of dry-farming optimism in Utah’s high valleys, the influence of LDS agricultural experts such as John A. Widtsoe, the boom-and-bust pattern of early-20th-century rural settlement, and the New Deal’s role in managing environmental failure. Annual gatherings of former residents and descendants have helped preserve memory of the community long after the physical town disappeared. Today the quiet site in Johns Valley serves as a tangible reminder of the challenges of making a living on the Colorado Plateau’s arid highlands.

Grand Staircase – Escalante National Monument

Escalante Canyon, Utah
Escalante Canyon, Utah

Grand Staircase-Escalante National Monument in southern Utah represents a profound intersection of geological time and human endeavor. Spanning approximately 1.87 million acres, the monument preserves over 270 million years of Earth’s history through its iconic “Grand Staircase”—a series of stepped cliffs and plateaus that reveal ancient environments from deserts and shallow seas to lush floodplains. Geologically, it is renowned for its continuous stratigraphic record and abundant fossils, including dinosaur remains and petrified forests. Historically, the area has been inhabited by Indigenous peoples for millennia and later traversed by Mormon pioneers, culminating in its controversial establishment as a national monument in 1996. Managed by the Bureau of Land Management (BLM), GSENM faces ongoing debates over resource use and preservation.

Introduction

Established on September 18, 1996, by President Bill Clinton under the Antiquities Act, GSENM initially encompassed 1.7 million acres to protect its unparalleled scientific and cultural resources. The monument’s name derives from the Escalante River, named after Spanish explorer Silvestre Vélez de Escalante, and the Grand Staircase, a geological feature conceptualized by Clarence Dutton in 1880. Divided into three sections—the rugged Grand Staircase in the west, the high Kaiparowits Plateau in the center, and the dissected Escalante Canyons in the east—GSENM spans diverse landscapes of slot canyons, buttes, and badlands. Its boundaries were reduced by nearly 47% in 2017 under President Donald Trump but restored to their original extent in 2021 by President Joe Biden, a decision upheld by federal courts in 2023 with appeals ongoing as of late 2024. Today, it serves as a critical site for paleontological research, cultural heritage, and recreation, attracting over 1 million visitors annually while balancing conservation with traditional uses like grazing and off-road access.

Geological History

The geology of GSENM is a testament to the dynamic forces that have shaped the Colorado Plateau, recording environmental shifts from arid deserts to marine incursions over nearly 300 million years. The monument’s strata, gently dipping northward, form the “Grand Staircase”—a 100-mile-long, 6,000-foot-high sequence of cliffs (risers) and plateaus (treads) that ascends from the Grand Canyon northward to Bryce Canyon National Park. This staircase, first described by geologist Clarence Dutton in 1870, preserves a near-continuous record from the Permian Period (about 275 million years ago) to the Eocene (about 50 million years ago), with only minor unconformities representing erosion gaps.

Major Rock Formations and Depositional Environments

The stratigraphic column is divided among the monument’s three sections, with thicknesses varying due to local tectonics. From oldest to youngest:

  • Permian Formations (275–251 Ma): Basal layers include the Kaibab Limestone (marine shelf deposits with crinoids and brachiopods) and underlying units like the Toroweap Formation (gypsiferous sandstones from tidal flats) and Coconino Sandstone (eolian dunes). These form the Chocolate Cliffs in the southern Grand Staircase, recording a marginal marine lowland with periodic sea advances.
  • Triassic Formations (251–201 Ma): The Moenkopi Formation (red beds, limestones, and gypsum from tidal flats and mudflats, 440–1,150 feet thick) and Chinle Formation (fluvial-lacustrine mudstones with bentonite, 425–930 feet thick) dominate the Chocolate Cliffs. Volcanic ash in the Chinle preserved vast petrified forests of conifers and ferns.
  • Jurassic Formations (201–145 Ma): Eolian and fluvial dominance defines this era. The Wingate Sandstone (dune sands, 100–350 feet) and Navajo Sandstone (massive cross-bedded dunes, 1,300–1,500 feet thick, forming the White Cliffs) represent vast deserts. The Kayenta Formation (fluvial sandstones, 150–350 feet) creates the Vermilion Cliffs, stained red by iron oxide. Middle Jurassic units like the Carmel Formation (shallow marine limestones with mollusks) and Entrada Sandstone (dunes) transition to the Morrison Formation (floodplain mudstones with dinosaur bones, up to 950 feet thick). These layers form the Gray Cliffs in the north.
  • Cretaceous Formations (145–66 Ma): The Western Interior Seaway’s advance deposited marine shales (Tropic Shale, 500–750 feet) and coastal sands (Dakota Formation, 3–370 feet). Continental units like the Straight Cliffs Formation (deltaic sandstones with coal, 900–1,800 feet), Wahweap Formation (piedmont gravels, 1,000–1,500 feet), and Kaiparowits Formation (alluvial mudstones, 2,000–3,000 feet thick) record a retreating sea and lush coastal plains teeming with life.
  • Tertiary Formations (66–23 Ma): Post-dinosaur extinction, the Claron Formation (lacustrine limestones, up to 1,400 feet) formed the Pink Cliffs through lake sedimentation, later sculpted into hoodoos by freeze-thaw cycles.

Unconformities, such as a 20-million-year gap between Permian and Triassic rocks, indicate erosion during tectonic quiescence.

Structural Features and Landscape Evolution

Tectonic events shaped the monument’s architecture. The Sevier Orogeny (Late Jurassic–Early Cretaceous) folded strata into north-south anticlines, synclines, and monoclines, including the dramatic East Kaibab Monocline (Cockscomb thrust, with 5,000 feet of displacement) and Escalante Monocline. The Laramide Orogeny (Late Cretaceous–Eocene) uplifted the Colorado Plateau by up to two miles, while Miocene Basin-and-Range extension created normal faults like the Paunsaugunt and Johnson Canyon faults, forming grabens and tilted blocks. Quaternary erosion by the Escalante and Paria Rivers, exacerbated by monsoons and flash floods, incised deep canyons and exposed the staircase. Volcanic activity in the middle Tertiary added ash flows in the Aquarius Plateau, but the dominant process remains differential erosion: resistant sandstones cap cliffs, while softer shales form slopes.

Paleontological Significance

GSENM is a global hotspot for Mesozoic fossils, offering insights into ancient ecosystems. Triassic Chinle layers yield petrified wood (up to 90 feet long), dinosaur tracks, and reptiles. Jurassic Navajo and Morrison formations preserve theropod and sauropod tracks, plus rare bones. The Cretaceous Kaiparowits Formation is exceptionally rich, with hadrosaurs, ankylosaurs, crocodiles, turtles, and plants from a subtropical floodplain—over 1,000 specimens collected since 1996. Marine fossils in Tropic Shale include ammonites and mosasaurs. These finds, protected under the Paleontological Resources Preservation Act, underscore the monument’s role in understanding the dinosaur era’s end.

Historical Significance

Indigenous and Early Human Occupation

Human presence dates to the Paleo-Indian period (ca. 10,000 BCE), but permanent settlements emerged during the Basketmaker III Era (ca. AD 500). Ancestral Puebloans (Anasazi) and Fremont peoples farmed corn, beans, and squash in canyons, constructing pithouses, granaries, and rock art panels depicting hunters and abstract symbols. Ruins like those in the Escalante Canyons reveal a sophisticated adaptation to arid environments, with trade networks extending to Mesoamerica. By AD 1300, climate change and overuse led to abandonment, leaving over 5,000 archaeological sites—20% of Utah’s total.

Euro-American Exploration and Settlement

Spanish explorers, including the 1776 Domínguez–Escalante expedition, first mapped the region but did not settle. Mormon pioneers arrived in 1866, with Captain James Andrus leading the first recorded Euro-American party to the Escalante River headwaters. In 1871, Jacob Hamblin traversed the river, aiding John Wesley Powell’s surveys. The 1879 Hole-in-the-Rock Expedition, involving 250 Mormons, blasted a perilous trail through Glen Canyon to establish a southeastern Utah colony, taking six weeks and symbolizing pioneer resilience. By the early 20th century, ranching and mining boomed, with uranium and coal prospects on the Kaiparowits Plateau threatening resources.

Establishment and Modern Controversies

Conservation efforts began in the 1930s, but momentum built in the 1990s amid coal mining threats. Clinton’s 1996 proclamation, announced during his reelection campaign, bypassed Utah’s congressional delegation, sparking lawsuits and accusations of federal overreach. The 1998 Utah Schools and Lands Exchange Act swapped state inholdings for $50 million and alternative lands. Trump’s 2017 reduction enabled coal and logging leases, reversed by Biden in 2021 amid lawsuits from counties and states. As of 2025, the monument remains intact, though disputes over Revised Statute 2477 “right-of-way” roads persist, with BLM closing some routes while locals maintain others. Culturally, GSENM honors Indigenous heritage through co-management discussions with tribes like the Kaibab Paiute and Navajo Nation.

Conclusion and Recommendations

GSENM embodies the interplay of geological grandeur and human legacy, from Permian seas to Mormon trails. Its preservation safeguards irreplaceable fossils and sites, but challenges like climate-driven erosion and visitation impacts loom. Recommendations include enhanced paleontological monitoring, Indigenous-led interpretation programs, and sustainable tourism policies. As a cornerstone of the National Conservation Lands, GSENM continues to inspire scientific inquiry and reflection on our shared past. For further reading, consult BLM visitor centers in Escalante or Kanab.

Grand Staircase – Escalante National Monument Points of Interest

Devils Garden off the Hole in the Rock Trail, Lake Powell, Utah

Devils Garden

In the sun-scorched heart of Utah's Grand Staircase-Escalante National Monument, where the Hole-in-the-Rock Trail claws its way through a labyrinth of crimson canyons like the…
Hole in the wall trail in Escalante, Utah

Hole in the Rock

Recognized on the National Register of Historic Places, the Hole in the Rock trail is an old Mormon trail in Utah that was used to establish colonies…

Camgrounds

Bureau of Land Management Campground

Calf Creek Recreation Area Campground

Bureau of Land Management Campground Calf Creek Recreation Area Campground is a serene desert oasis nestled along Calf Creek in the Grand Staircase-Escalante National Monument…

White House Campground

Nestled in the rugged southwestern expanse of Utah's Grand Staircase-Escalante National Monument (GSENM), White House Campground offers a serene, primitive escape for adventurers seeking solitude…

Wide Hollow Campground

Nestled within the stunning Escalante Petrified Forest State Park in southern Utah, Wide Hollow Campground beckons adventurers, families, and nature enthusiasts to an idyllic retreat…

Wide Hollow Campground

Nestled within the stunning Escalante Petrified Forest State Park in southern Utah, Wide Hollow Campground beckons adventurers, families, and nature enthusiasts to an idyllic retreat where ancient geology meets serene waters. Perched at approximately 5,900 feet elevation along the shores of the 130-acre Wide Hollow Reservoir—just a short drive west of the charming town of Escalante off Scenic Byway 12—this campground offers a perfect base for exploring the dramatic landscapes of Grand Staircase-Escalante National Monument. Imagine awakening to the golden hues of sunrise reflecting off the reservoir’s clear blue waters, with the rugged silhouettes of distant canyons and the Kaiparowits Plateau framing your view. The area, part of Utah’s “Swell” region, is a geologic treasure trove shaped by millions of years of erosion, where slot canyons, natural arches, and expansive vistas create a playground for outdoor pursuits. Here, the air is crisp and invigorating, the nights starlit and quiet, and the days filled with the symphony of birdsong from raptors, songbirds, and waterfowl that frequent the shores.

Natural Features and the Surrounding Area

Wide Hollow Campground is enveloped by the park’s signature attractions, blending aquatic serenity with terrestrial marvels. The reservoir itself is a highlight, stocked year-round with rainbow trout, largemouth bass, and bluegill, making it a prime spot for shore fishing or casting from a rented canoe, kayak, or paddleboard—rentals available on-site during warmer months (March to November). Its calm, swimmable waters invite lazy afternoons lounging on the sandy beach, while the adjacent petrified forest showcases nature’s artistry: colorful, mineralized logs in kaleidoscopic shades of red, orange, yellow, and purple, remnants of ancient trees fossilized over 150 million years ago. Easy-access hiking trails, like the 1-mile Petrified Forest Loop, wind through these formations, offering interpretive signs that reveal the area’s rich paleontological history amid blooming wildflowers in spring or golden cottonwoods in fall. Beyond the park, the broader Escalante region unfolds into endless adventures—hike slot canyons, horseback ride through desert washes, or stargaze in one of the darkest skies in the U.S. The elevation provides cooler summers and mild winters, though visitors should prepare for high-desert conditions with plenty of sun and minimal rainfall.

Available Facilities

Designed for comfort without sacrificing the rustic charm of camping, Wide Hollow Campground features modern amenities to enhance your stay. The park offers 29 full-hookup sites across its loops (including the adjacent Lake View Campground), accommodating tents, RVs, and trailers up to 40 feet. Each site includes a shaded shelter, picnic table, fire pit with grate, paved parking, and ample space for privacy—many boast premium reservoir views toward Escalante’s iconic canyons and Powell Point. Electrical hookups range from 20 to 50 amps, with potable water and sewer connections at every site; additional frost-free water spigots are scattered throughout for convenience.

Supporting facilities keep things clean and convenient:

  • Restrooms and Showers: Modern, well-maintained buildings with hot, free showers—spacious and family-friendly, though occasional upkeep notes from visitors highlight their general cleanliness.
  • Group Areas: A dedicated group pavilion and lakeside overflow spots for larger gatherings (up to 8 people per standard site).
  • Water Recreation: Boat ramp for easy launches, plus canoe/kayak/paddleboard rentals.
  • Day-Use Amenities: Picnic areas with shelters, a swimming beach, and an RV dump station (additional fee applies).
  • Essentials: Drinking water fill-ups, firewood sales (harvested locally to prevent invasive species), and a small camp store for basics. Generators are not permitted in the campground to preserve the peaceful ambiance, but quiet hours are strictly enforced.

Reservations are recommended year-round via Utah State Parks’ online system, with fees starting at $16 per night for basic sites (including park entry). Pets are welcome on leashes, and the campground remains open all year, though services like rentals may vary seasonally. Whether you’re toasting marshmallows by the fire ring or embarking on a dawn paddle, Wide Hollow Campground delivers an unforgettable blend of comfort, recreation, and raw natural beauty—your ideal launchpad for Utah’s red-rock wonders.

Hole in the Rock

Recognized on the National Register of Historic Places, the Hole in the Rock trail is an old Mormon trail in Utah that was used to establish colonies on the east side of the Colorado River in 1879. The Hole in the Rock from which the trail is named, is a narrow canyon from the rim of the canyon down into the Colorado River Valley. This canyon provided access to the Colorado River and the much needed water require to survive in these remote locations. Months were spent widening the narrow canyon to allow “safe” passage of all the wagons and cattle.

Hole in the wall trail in Escalante, Utah
Hole in the wall trail in Escalante, Utah

The original trail was bisected when the Glen Canyon damn bottled the Colorado River and started to fill up Lake Powell in 1966. However, thE road continues to exist and allows access to the Escalante Canyon system, along with access to the Devils Garden, numerous slot canyons and lots of back country hiking and camping opportunities.

Devils Garden off the Hole in the Rock Trail, Lake Powell, Utah
Devils Garden off the Hole in the Rock Trail, Lake Powell, Utah

The road passes between the Kaiparowits Plateau and the Escalante River. This area is a labyrinth of roads and trails.  The trail leaves the small town of Escalante and travels 44 miles south along a sandy road.

Camping at Dance Hall Rock, Hole in the Rock trail
Camping at Dance Hall Rock, Hole in the Rock trail

Do not underestimate how cool this area is to visit. The rock formations, remote locations and sunsets are beyond comprehension. One can get the feeling of isolation on just a short visit.

Escalante Canyon, Utah
Escalante Canyon, Utah

Hole in the Rock Trail Map