Category: Destination4x4

Lake Manly

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Lake Manly is a rare and ephemeral lake that occasionally forms in Badwater Basin, the lowest point in North America at 282 feet (86 meters) below sea level, located in Death Valley National Park, California. This temporary body of water revives an ancient Pleistocene lake that existed during the Ice Age, when it reached depths of up to 700 feet and stretched nearly 100 miles long.

Looking into a perfect mirror image on Lake Many in January 2026. Photo by James L Rathbun
Looking into a perfect mirror image on Lake Many in January 2026. Photo by James L Rathbun

In recent years, including dramatic appearances after Hurricane Hilary in 2023, atmospheric rivers in 2024, and record-breaking fall rains in late 2025 (with more precipitation than an entire typical year), the basin has flooded to create a shallow lake — sometimes just inches deep, other times up to a few feet — allowing rare reflections and even temporary kayaking opportunities.

Badwater Basin itself is a surreal, otherworldly landscape dominated by expansive salt flats covering nearly 200 square miles. The surface is primarily sodium chloride (table salt), along with minerals like calcite, gypsum, and borax. The name “Badwater” comes from a small spring-fed pool near the road that’s extremely salty and undrinkable.

History of the lake

Lake Manly, gets its name from William Lewis Manly, a pioneer and hero of the 1849 California Gold Rush era.

In late 1849, a group of emigrants (known as the “Lost ’49ers”) took a risky shortcut to reach the gold fields and became stranded in the brutal heat and dryness of what would later be called Death Valley. William Lewis Manly, along with John Rogers, volunteered to walk out of the valley on foot to seek help. They trekked hundreds of miles across harsh desert terrain, eventually reaching safety, obtaining supplies, and returning to rescue the remaining group (including families like the Bennetts and Arcans) — saving their lives.

In honor of his bravery and lifesaving efforts, geologists named the prehistoric pluvial lake that once filled much of Death Valley after him. The name “Lake Manly” was formally coined in 1932 (sometimes misspelled as “Manley” in older sources, but Manly is correct). There’s even a proposed alternate name “Lake Rogers” for a potential northern section, after his companion, but “Manly” became the standard term used in scientific literature and by the National Park Service.

The lake itself is a remnant of wetter Ice Age periods (especially around 185,000–128,000 and 35,000–10,000 years ago), when glacial meltwater fed massive inland waters. Today, it only reappears briefly after extreme rainfall events — like the record storms in recent years that turned Badwater Basin into a shallow, reflective lake again.

It’s a fitting tribute: the name connects one of the valley’s most famous human survival stories to its deep geological past of water in a place infamous for being bone-dry!

Telescope Peak's reflection in the calm wates of Lake Manly, Death Valley National Park. Photo by James L Rathbun
Telescope Peak’s reflection in the calm wates of Lake Manly, Death Valley National Park. Photo by James L Rathbun

Conditions That Cause Lake Manly’s Formation

Death Valley is one of the driest and hottest places on Earth, averaging only about 2 inches of rain per year with evaporation rates exceeding 150 inches annually. This extreme aridity normally keeps Badwater Basin as a dry salt pan.

The lake forms only during rare, extreme rainfall events — such as remnants of tropical storms (e.g., Hurricane Hilary in 2023), powerful atmospheric rivers, or record-setting seasonal storms — that deliver several inches of rain in a short time. Runoff from surrounding mountains floods the endorheic (closed) basin, which has no outlet, creating a temporary lake. The water eventually evaporates rapidly under the intense heat and low humidity, returning the area to its characteristic salt flats — often within months.

This fleeting phenomenon highlights how even the harshest deserts can dramatically change with unusual weather patterns!

The hills next to Badwater turn green with the rains which cause Lake Manly. The sea sevel sign is visible high in the rocks on the the right. Photo by James L Rathbun
The hills next to Badwater turn green with the rains which cause Lake Manly. The sea sevel sign is visible high in the rocks on the the right. Photo by James L Rathbun

Winter 2026

Lake Manly is formed following several days of rain, so we opted to drive out to the park for a visit. Our first visit is cut short from a rain storm and flash floods which caused the road to be covered with flood levels. We made the drive from Vegas the next weekend, and were floored by the views of Lake Manly covering the salt flats of Badwater Basin. The walk out to the lake shore is about 1/4 of a mile from the Badwater parking lot.

On our visit, the lake surface is deathly still and the other visitors were silent giving us the feeling of isolation despite their being other travelers. This is my first visit to Lake Manly, and will certainly not be my last, if I am able to arrange the trip.

Simonsville, Nevada – Clark County Ghost Town

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Seal of Clark County Nevada
Seal of Clark County Nevada

Simonsville (occasionally referenced with variant spellings such as Simmonsville) was a short-lived Mormon farming settlement and milling site in Clark County, Nevada. It was situated on the east bank of the Muddy River in the Moapa Valley, west of the south end of the Overton Airport. Coordinates are 36°33′46″N 114°26′40″W, with an elevation of 1,325 feet (404 m). The settlement formed part of the broader network of 1860s Mormon colonies along the Muddy River, established to support agriculture in southern Nevada’s desert environment.

Early History/Founding

Simonsville originated as part of the Mormon Cotton Mission initiated by Brigham Young in the early 1860s. Seeking reliable water from the Muddy River and fertile soil for cotton production (to achieve economic independence for Utah Territory and secure southern trade routes), church leaders dispatched approximately 75–85 families to the Moapa Valley in 1865. The first major settlements were St. Thomas and St. Joseph.

The site was initially known as Mill Point after James Leithead constructed the valley’s first grist mill there. By December 1865, enough settlers had arrived for President Erastus Snow to establish a new colony under the leadership of Orrawell Simons (sometimes spelled Orawell). The settlement was renamed Simonsville in his honor. In spring 1866, Orrawell Simons oversaw construction of an additional grist mill, which quickly became operational.

Economic Activities

The economy of Simonsville centered on agriculture and milling, integrated with the larger Moapa Valley Cotton Mission. Settlers grew cotton, wheat, corn, oats, barley, and orchard crops, supported by irrigation canals drawn from the Muddy River. The grist mill at Simonsville (and its predecessor at Mill Point) ground wheat, corn, and salt for local use and regional supply.

A cotton gin, powered by the same mill infrastructure, processed the 1865 cotton crop; valley-wide production exceeded 5,000 pounds of lint that year, with individual acres yielding up to 695 pounds of first-class lint. By 1866–1867, cotton output grew significantly (e.g., 14,600 pounds of lint reported at nearby St. Joseph alone in 1867). The mill also supported defensive efforts, as a guard was maintained at Mill Point to protect the valuable infrastructure during Indian raids in 1866.

Decline/Abandonment

Simonsville’s decline mirrored that of the other Muddy River settlements. Harsh conditions—including remoteness (450 miles from Salt Lake City), desert climate, malaria, sandstorms, and Indian depredations—strained the colonies. A critical issue emerged when a boundary survey revealed the entire Moapa Valley lay in Nevada (specifically Lincoln County at the time), not Utah Territory or Arizona as initially assumed. This triggered disputes over taxation: settlers faced double levies (Nevada state taxes plus tithing to Utah’s Rio Virgin County) without corresponding representation or services.

In 1870–1871, Brigham Young described the area as a “God Forsaken place” and advised abandonment. Most residents, including those at Simonsville, voted to leave. By 1871, over 600 colonists abandoned their homes, farms, and mills, relocating eastward to Long Valley, Utah (founding communities such as Glendale and Mount Carmel). Simonsville was never reoccupied.

Legacy/Current Status

Simonsville exemplifies the ambitious but ultimately unsuccessful Mormon efforts to colonize southern Nevada’s river valleys in the 1860s. It highlights the challenges of territorial boundary ambiguities, taxation conflicts, and environmental hardships that doomed the Cotton Mission. The settlement contributed to early agricultural experimentation (cotton ginning and grain milling) in what became Clark County and paved the way for later, more permanent communities in the Moapa Valley (such as the revived Overton and Logandale).

Today, the physical site of Simonsville (and original Mill Point) is largely lost. It lies beneath or adjacent to modern Clark County flood-control infrastructure and realigned airport roads. No standing structures remain, and the area is not preserved as a public historic site, though it is documented in lists of Clark County ghost towns.

Sources/References

  • “The Settlements on the Muddy 1865–1871: ‘A God Forsaken Place’,” Utah Historical Quarterly, Vol. 35, No. 2 (1967), providing primary excerpts from church leaders and detailed colony records.
  • Historical Marker Database (HMDB): “Early Settlements in the Moapa Valley” (marker detailing the 1865–1871 Mormon colonies).
  • Additional context from Nevada ghost town compilations and Moapa Valley historical overviews (e.g., lists confirming Simonsville/Mill Point as a 1865–1870 site).

Bard, Nevada – Clark County Ghost Town

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Bard, Nevada, is an extinct ghost town and former railroad station located in Clark County in southern Nevada. It lies within the modern-day Enterprise census-designated place (CDP), approximately 14 miles southwest of downtown Las Vegas in the arid Mojave Desert terrain near the Eldorado Mountains. Its coordinates are approximately 35°59′16″N 115°14′15″W (elevation 2,572 feet / 784 meters).

Origins and Naming

Bard originated as a minor stop along the San Pedro, Los Angeles and Salt Lake Railroad (commonly called the “Salt Lake Route”), which later became part of the Union Pacific Railroad. The community took its name from the nearby Bard Mining District. Historical records attribute the name to D. C. Bard (sometimes referenced as a natural scientist, mining engineer, geologist, and prospector active in the American West). Some accounts also mention a possible link to U.S. Senator Thomas R. Bard of California, a mining investor, but primary sources from the Federal Writers’ Project (1941) and Nevada place-name studies consistently point to D. C. Bard.

The Bard Mining District, situated between Arden and Jean in Clark County, focused on industrial minerals such as limestone, gypsum, silica, and diatomite rather than high-value precious metals. It supported small-scale extraction operations in the early 20th century, with the railroad station serving as a logistical link for transporting these materials and supporting rail traffic through the remote desert.

Railroad Development and Role (1904–1905)

The San Pedro, Los Angeles and Salt Lake Railroad, promoted by Montana Senator William Andrews Clark (the namesake of Clark County), was a pivotal infrastructure project that opened southern Nevada to broader economic development in the early 1900s. Construction crews reached the Bard area in 1904. Because of challenging terrain—including the need to complete a grade over the summit between Las Vegas and Ivanpah Valleys—only a temporary “shoo-fly” (bypass) track was initially built. The permanent main line through Bard was completed in May 1905.

As a non-agency station (meaning it had no dedicated station agent or full passenger facilities), Bard functioned primarily as a siding or waypoint between Sloan (to the south) and Arden (to the north). It facilitated the movement of freight, passengers, and mining-related goods along the main line connecting Los Angeles to Salt Lake City. In the broader context of Clark County history, this railroad was instrumental in the founding and growth of Las Vegas (established 1905) and the agricultural and mining expansion that followed. Bard itself, however, remained a small, functional rail facility rather than a populated settlement.

Decline and Abandonment (1945)

Bard never developed into a substantial community with residents, schools, or businesses. Its entire purpose was tied to railroad operations. By the mid-20th century, shifts in transportation (including the rise of trucking and changes in rail routing and technology) reduced the need for minor sidings like Bard. The station was officially abandoned in 1945. No structures or population figures are recorded for Bard; it appears in historical lists simply as an “extinct town” or “populated place” absorbed into the Enterprise CDP for modern census purposes.

Legacy and Present Day

Today, Bard exists only as a historical footnote in Clark County’s railroad and mining heritage. No ruins, historical markers, or visible remnants are prominently documented at the site, which is now surrounded by the rapid suburban growth of the Las Vegas metropolitan area. It exemplifies the many short-lived railroad sidings and support points that dotted Nevada’s desert landscape during the boom years of rail expansion and early industrial mining. Bard is occasionally listed among Clark County ghost towns alongside more prominent sites such as Goodsprings or St. Thomas, though its story is far more modest.

In the wider narrative of southern Nevada, Bard highlights how the 1905 railroad—built by Senator Clark—transformed a remote region into a transportation corridor. While larger towns like Las Vegas thrived, smaller waystations like Bard quietly served their purpose and faded once economic conditions changed. Its legacy survives primarily in railroad histories, topographic maps, and Nevada place-name references.

Billie Mine

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The Billie Mine (also known as Billie I and Billie II) is a former underground borate mine located in the Furnace Creek Mining District of Death Valley National Park, Inyo County, California. Situated on the eastern slopes of the Black Mountains overlooking Death Valley, the mine’s surface structures—including the prominent steel headframe, shaft collar, support buildings, and waste rock dumps—are positioned just outside the park boundary along the paved Dante’s View Road, approximately 1.5 miles northwest of the historic ghost town of Ryan and 12 miles southeast of Furnace Creek. However, the rich borate ore body itself extends underground into park lands, with the mine portal offset about 1,500 feet west on Bureau of Land Management property to comply with environmental regulations under the Mining in the Parks Act of 1976.

The site sits in a stark, arid landscape typical of Death Valley: barren alluvial fans sloping down from rugged, basalt-capped ridges, dotted with creosote bush and sparse desert vegetation. The ore body, embedded in the Miocene-Pliocene Furnace Creek Formation, consists primarily of calcium borates such as colemanite, along with probertite and ulexite. Geologically, the deposit is lens-shaped, striking northeast with a southeast dip of 20–40 degrees, averaging 700 feet wide, 3,700 feet long down-dip, and 150 feet thick. Mining involved deep vertical shafts (reaching depths of around 1,200 feet) and long-hole stoping methods with backfilling to maintain stability, leaving tall, narrow pillars critical to the underground structure.

Today, the abandoned mine features a towering headframe silhouetted against the vast valley panorama, evoking the industrial intrusion into this remote wilderness. Visitors driving to Dante’s View often pause for photos, but the site is gated and off-limits—mines in the park are hazardous due to unstable shafts, toxic tailings, and potential collapses.

The Billie Mine’s history is intertwined with Death Valley’s long borax legacy, but it represents a modern chapter amid growing conservation efforts. Borate deposits in the Furnace Creek area were known since the late 19th century, exploited by the Pacific Coast Borax Company at nearby sites like the Lila C. and Widow mines near Ryan. However, after discovering richer sodium borates (kernite) at Boron in 1926–1927, operations in Death Valley largely ceased as companies shifted to more profitable locations.

Interest in the Billie deposit revived in the mid-20th century. In 1958, the Kern County Land Company staked claims and conducted drilling. Development accelerated in the 1970s: after the Mining in the Parks Act of 1976 restricted new claims and imposed strict environmental reviews, valid pre-existing operations like Billie were allowed to proceed with mitigation. Construction began in 1977 under a partnership that became the American Borate Company (initially involving Owens Corning Fiberglass and Texas United, later fully Owens Corning).

The mine reached ore in 1980 and became fully operational shortly after, extracting high-quality colemanite crystals (some large and collectible) alongside probertite and ulexite. Ore was trucked to processing plants in Dunn Siding, California, or Lathrop Wells, Nevada. For over a decade following the 1994 expansion of Death Valley to national park status, the Billie Mine was the only active mine within park boundaries, operating under rigorous National Park Service oversight to minimize surface disturbance.

Production continued into the early 2000s, but economic factors, declining demand, or resource depletion led to closure in 2005—marking the end of all mining in Death Valley National Park. In 2011, American Borate donated related patented claims (including parts of the Billie and nearby Boraxo sites) to the NPS, further securing the area’s protection.

The Billie Mine stands as a poignant reminder of Death Valley’s mining era: born from persistent exploration in a protected landscape, it bridged historic borax booms with modern environmental constraints, ultimately yielding to preservation in one of America’s most extreme and iconic wildernesses.

Byron, Nevada

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Byron is an extinct town, often classified as a ghost town, in Clark County, Nevada. It was located approximately 44 miles (71 km) north of Las Vegas, southwest of the community of Moapa. Its coordinates are 36°36′49″N 114°40′51″W, with an elevation of about 1,782 feet.

Unlike many Nevada settlements tied to mining booms, Byron developed solely as a minor railroad siding and depot. It never grew into a significant community and left behind little physical trace.

Establishment and Early History

Byron originated as a railroad siding on the Union Pacific Railroad (successor to the San Pedro, Los Angeles & Salt Lake Railroad, completed in the early 1900s through southern Nevada). It was established by at least 1914 and served as the first station southwest of Moapa.

Railroad sidings like Byron typically supported operations by providing stops for maintenance crews (section houses), water or fuel points, or passing tracks in remote desert terrain. The area’s arid, sparsely populated landscape made such facilities essential for the reliable operation of long-distance rail lines connecting Las Vegas northward.

No evidence exists of mining activity, agriculture, or other industries at the site. Byron appears to have been purely a functional railroad outpost rather than a planned settlement.

Peak Period (1940s)

In 1941, the Federal Writers’ Project documented Byron as a small depot on the Union Pacific Railroad with a population of about 10 residents. It was listed in official place-name records as “a town, pop. 10; alt. 1,782; first station southwest of Moapa on the Union Pacific Railroad.”

This modest size was typical for remote railroad sidings of the era—likely consisting of a few workers’ homes, a section house, and basic track infrastructure. The community existed during a period when rail transport remained vital to Nevada’s economy, especially for freight and passenger service across the state.

Decline and Abandonment

Byron was abandoned by 1949.

Post-World War II changes in the railroad industry— including dieselization, improved signaling, longer trains, and reduced need for frequent small stops—rendered many minor sidings obsolete. The growing dominance of automobiles and highways further diminished the importance of isolated rail depots. Byron, never having developed beyond its railroad function, simply ceased to exist as a populated place once its operational role ended.

Current Status

Today, Byron no longer appears as an active community or even a named stop on modern maps. It is catalogued among Clark County’s ghost towns and historical locales. The site lies in a remote desert area near the Moapa Valley. While one source suggests the location may fall within or adjacent to the Moapa River Indian Reservation, primary records emphasize only its historical railroad context.

No significant ruins, buildings, or interpretive markers are documented at the site, which is consistent with the transient nature of small railroad sidings.

Conclusion

Byron, Nevada, offers a brief but representative glimpse into the infrastructure that supported early 20th-century rail expansion in the American Southwest. Established to serve the Union Pacific Railroad and abandoned within a few decades as technology and transportation patterns evolved, it exemplifies the rise-and-fall cycle of countless minor outposts across Nevada. Though it left no lasting population or landmarks, Byron remains a footnote in Clark County’s transportation history and a reminder of the railroad’s pivotal role in opening the region.