Desert Dandelion ( Malocothryx glabrata )

The Desert Dandelion, also commonly known as Smooth Desertdandelion, is a striking annual wildflower native to the arid regions of western North America. It belongs to the sunflower family and is renowned for forming vibrant carpets of yellow blooms in sandy desert landscapes following wet winters. This report details its scientific taxonomy, plant and flower morphology, habitat, range, distribution, and ecological characteristics, drawing from botanical sources such as regional floras and field guides.

Desert Dandelion ( Malocothryx glabrata ) Photo by James L Rathbun
Desert Dandelion ( Malocothryx glabrata ) Photo by James L Rathbun

Scientific Taxonomy and Categorization

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Aster or Sunflower Family) – characterized by composite flower heads and milky sap in many genera
  • Genus: Malacothrix (Greek: “soft hair,” referring to the pappus on seeds)
  • Species: Malacothrix glabrata (A. Gray ex D.C. Eaton) A. Gray
  • Binomial Authority: Named by Asa Gray; the epithet “glabrata” refers to the nearly hairless (glabrous) leaves and stems.
  • Synonyms: Malacothrix californica var. glabrata
  • Common Names: Smooth Desertdandelion, Desert Dandelion

This dicotyledonous annual herb is categorized within the tribe Cichorieae (chicory tribe) of Asteraceae, featuring ligulate (strap-shaped ray) florets only, with no disk florets—distinguishing it from true dandelions (Taraxacum spp.).

Detailed Plant Description

Malacothrix glabrata is a low-growing to erect annual forb arising from a taproot. Plants reach 10–40 cm (4–16 inches) tall, with stems that are mostly glabrous (smooth), occasionally sparsely puberulent near the base, and branched proximally and distally. The stems may appear ascending or upright and contain milky latex sap, a hallmark of the Asteraceae family.

Leaves are primarily basal in a rosette, green, linear, and pinnately lobed with narrow, filiform (thread-like) or stringy segments (6.5–12.5 cm long). Cauline (stem) leaves are alternate, reduced upward, and similarly lobed. The foliage is nearly hairless, contributing to its “smooth” common name.

Detailed Flower Description

The inflorescences are solitary or 1–3 per stem, daisy-like composite heads measuring 2.5–6.5 cm (1–2.5 inches) wide (up to 4.5 cm or more). Each head consists of 31–139 ligulate ray florets (strap-shaped, 5-lobed at the tip) that are pale yellow to white, often with purple-tinged undersides. The receptacle is bristly, and the involucre (base) is campanulate to hemispheric, with 20–25+ phyllaries in 2–3 series and 12–20+ lanceolate bractlets with translucent margins at the base.

Immature or young flower heads often display a distinctive orange-to-red “button” or spot in the center (composed of developing structures). The flowers are fragrant and open primarily in the morning, closing by early afternoon. In mass blooms, they create showy yellow displays across the desert floor.

Desert Dandelion ( Malocothryx glabrata ) - Photo by James L Rathbun
Desert Dandelion ( Malocothryx glabrata ) – Photo by James L Rathbun

Fruit and Seeds

The fruit is a single-seeded cypsela (often called an achene), cylindro-fusiform (cylindrical and tapered at both ends), sometimes weakly 5-angled. It bears a pappus of soft hairs for wind dispersal. Seeds mature from March to June.

Habitat

This species thrives in coarse, fast-draining soils (gravel, loam, sand, silt) in open areas, among shrubs, or in vegetation gaps. Preferred habitats include sandy deserts, plains, mesas, rocky hillsides, washes, and flats, often associated with creosote bush (Larrea tridentata) communities. It also occurs in foothill woodlands and desert shrublands. Elevation range: below 2,000 m (6,500 ft). It is highly responsive to winter rainfall, becoming abundant in “good wildflower years.”

Range and Distribution

Malacothrix glabrata is native to the southwestern United States and northwestern Mexico. It occurs across the Mojave, Sonoran, and Great Basin Deserts.

U.S. States: Arizona (AZ), California (CA), Idaho (ID), Nevada (NV), New Mexico (NM), Oregon (OR), Utah (UT). Broader Range: Southwestern Idaho and eastern Oregon south to southern California, much of Arizona, and into Baja California and northwestern Mexico.

It is particularly common in the Mojave Desert (including areas near Las Vegas, Nevada) and intermountain regions. Sporadic records exist in the Colorado Plateau and Chihuahuan Desert fringes.

Ecology and Biology

As an annual, Malacothrix glabrata germinates in response to cool-season precipitation and completes its life cycle rapidly. Blooming occurs February–July (peak March–June), with fruits maturing soon after. It is primarily insect-pollinated (e.g., by solitary bees such as Nomadopsis spp.) but may be self-compatible. Seeds are wind-dispersed.

Ecologically, it serves as an important nectar source for butterflies, moths, bees, and other insects, and provides forage for wildlife including desert tortoises and small mammals. Indigenous groups (e.g., Apache) historically used roots medicinally. It is an indicator species for productive desert bloom seasons and shows no recognized subspecies or varieties. Chromosome number: 2n=14.

In summary, Malacothrix glabrata exemplifies desert adaptation with its ephemeral beauty, glabrous form, and reliance on sporadic rains. Its presence signals healthy desert ecosystems in the American Southwest.

Lucky Jim Camp, Nevada

Lucky Jim Camp, sometimes referred to as Lucky Camp, was a short-lived mining camp and ghost town site in Clark County, Nevada. It is situated in El Dorado Canyon (also known as Eldorado Canyon) within the Colorado Mining District (later called the Eldorado Mining District) in the Eldorado Mountains. The site lies on the north side of the canyon, south of the Techatticup Mine, at an elevation of 2,444 feet (745 m), directly above the mouth of January Wash where it joins El Dorado Canyon.

Geographic coordinates are approximately 35°42′08″N 114°48′12″W. When established, the area was part of New Mexico Territory; it later became part of Nevada Territory and then the state of Nevada. The camp formed in a rugged desert canyon environment along the Colorado River corridor, which offered steamboat access for supplies in the 1860s.

Early History/Founding

Mining activity in El Dorado Canyon began intensifying in the early 1860s following discoveries of mineral deposits after the California Gold Rush waned. Lucky Jim Camp was founded in 1862 amid this boom. The origin of its name remains unknown.

The camp gained prominence during the American Civil War as a gathering place for miners sympathetic to the Confederate (Southern) cause. Roughly one mile up the canyon (above Huse Spring) was the rival Buster Falls camp, where Union (Northern) sympathizers congregated. The miners in the Colorado Mining District divided into these two separate communities based on their political leanings, though tensions remained largely verbal with no major hostilities reported. This split reflected national divisions even in remote desert mining areas. The broader district saw its population swell to around 300–500 workers in the early 1860s (and reportedly up to 1,500 at peak), with some individuals drawn to the lawless frontier to avoid military service elsewhere.

The camp’s location above the canyon floor also served a practical purpose: it acted as a refuge during the destructive Great Flood of 1862 (part of the widespread “Great Flood of 1861–1862” that affected the Western United States and Colorado River Basin). Lower camps near the Techatticup Mine, such as Alturas and Louisville, were destroyed or damaged, while Lucky Jim’s elevated position kept it safe. The name of nearby January Wash may commemorate the January 1862 flooding event.

Economic Activities

Lucky Jim Camp functioned as a transient support settlement for individual or small-party miners rather than a large organized town. The primary economic driver was prospecting and mining of high-grade silver chloride ores in the canyon (with gold becoming more prominent at greater depths). Ore was typically hand-sorted, sacked, and shipped—initially overland or by steamboat to San Francisco for processing—before local stamp mills were built.

No large-scale mills or smelters operated directly at Lucky Jim itself. Instead, it relied on the district’s emerging infrastructure. By late 1863, nearby El Dorado City (also called Eldorado City) was established a short distance down-canyon on the same side, featuring a stamp mill that supported ore processing. The camp’s residents likely worked claims in the surrounding Eldorado Mountains, contributing to the district’s output of silver and associated minerals. Supplies reached the area via the Colorado River, which served as a key transportation route.

Decline/Abandonment

Lucky Jim Camp was inherently temporary and declined rapidly after the Civil War. The establishment of El Dorado City in late 1863—with its stamp mill—likely supplanted the smaller camp, as mining operations consolidated. Following the end of the war, the district experienced a period of idleness and reduced activity. Many early mining camps in the canyon faded as richer surface ores were depleted and miners moved on to new strikes elsewhere in Nevada or the West.

By the mid-to-late 1860s, Lucky Jim had largely been abandoned as a distinct settlement. The Colorado Mining District continued sporadic operations into later decades (with revivals in the early 20th century at nearby Nelson), but the original 1860s camps like Lucky Jim did not persist.

Legacy/Current Status

Today, Lucky Jim Camp exists only as a historical site with no visible ruins or structures. Satellite imagery shows the area as barren, with no remaining traces of buildings, tents, or mining infrastructure. It stands as a reminder of the Civil War’s reach into Nevada’s remote mining frontiers and the boom-and-bust cycles of 1860s silver mining in the Eldorado Canyon region.

The broader Eldorado Canyon area retains historical significance through preserved sites like the Techatticup Mine (now a tourist attraction near the modern ghost town of Nelson) and connections to Colorado River steamboat navigation. Lucky Jim’s story highlights themes common to Clark County’s early mining history: political divisions, flood risks, and the transient nature of desert mining camps. The site is located on public or undeveloped land near modern-day Nelson and is accessible via backroads in the Eldorado Mountains, though it offers little for on-site exploration.

Borax, Nevada – Clark County Ghost Town

Ghost towns of Clark County, Nevada
Ghost towns of Clark County, Nevada

Borax, Nevada, is a ghost town and former railroad siding in Clark County, in the southern part of the state along the Union Pacific Railroad east of Interstate 15. It was settled in 1905 and explicitly named for borax (sodium borate) deposits discovered in the surrounding desert region. At its small peak around 1940, the settlement had a population of about 10 residents. Today, it has a recorded population of zero, with no remaining buildings—existing only as a functional railroad siding (elevation approximately 2,707 feet). While Borax itself left a minimal physical legacy, its name and location tie directly into Nevada’s broader and historically significant borax mining industry, which played a foundational role in the development of the U.S. borax trade in the late 19th and early 20th centuries.

This report provides context on Nevada’s borax mining history, as the town of Borax cannot be fully understood in isolation from the mineral that inspired its name and the industry that shaped the state’s desert economy.

Early Discoveries and the Birth of Nevada’s Borax Industry (1870s)

Nevada’s involvement with borax began in earnest in 1872 when Francis Marion “Borax” Smith (often called the “Borax King”) discovered high-quality borate deposits at Teel’s Marsh in Mineral County, western Nevada. Smith, originally from Wisconsin, had been supplying firewood to a small borax operation at nearby Columbus Marsh when he spotted the potential at Teel’s Marsh from a distance. He and his partners staked claims, and operations commenced under names such as Smith and Storey Brothers Borax Co. (later Teels Marsh Borax Co.). This discovery is widely credited with launching the commercial borax rush in the American West and forming the roots of what became the Pacific Coast Borax Company.

The Teel’s Marsh area quickly spurred the growth of Marietta, a mining camp established around 1877. Unlike typical Nevada silver or gold boomtowns, Marietta thrived on borax and salt extraction from the evaporated alkali flat of Teel’s Marsh. By the late 1870s and early 1880s, it featured a post office, newspaper, company store (operated in part by Borax Smith and his brother), and over 150 residents. Workers scraped borax and salt from the marsh surface under harsh desert conditions. Salt was particularly valuable for processing silver and gold ore elsewhere in the state (e.g., Virginia City and Bodie). However, the isolated location made the town vulnerable—stagecoaches were robbed frequently, including multiple times in a single day in 1880.

The stone ruins visible today at Marietta (including remnants of Borax Smith’s company store) stand as quiet reminders of this short-lived boom.

Nearby Columbus (established 1865 as a silver milling center) also became a borax hub in the early 1870s. Four companies, including the prominent Pacific Borax Company (which built facilities about five miles south of town in September 1872), extracted borax from the Columbus Salt Marsh. At its height in the mid-1870s, Columbus supported several hundred residents with stores, an adobe school, post office, iron foundry, and its own newspaper, the Borax Miner. Borax production briefly revitalized the declining silver town before larger deposits elsewhere shifted focus.

Expansion, Competition, and Shift to California (1880s–1890s)

Borax Smith consolidated operations and, by 1890, had acquired rival holdings (including those of William T. Coleman) to form the Pacific Coast Borax Company. Nevada’s early borax works supplied domestic needs and helped pioneer refining techniques. However, richer and more accessible colemanite (a borate ore) deposits were discovered in Death Valley, California, beginning in 1881 (e.g., the Harmony Borax Works). These California sites, famously served by the iconic 20-mule teams hauling borax 165 miles across the Mojave Desert, proved more economically viable. Nevada operations at Teel’s Marsh, Columbus, and similar sites (including Rhodes Marsh and Fish Lake Valley) largely declined or closed by the 1890s as production shifted southward.

20th-Century Activity and the Settlement of Borax (1900s–1940s)

Borax prospecting continued into the 20th century, particularly in southern Nevada’s Clark County. Significant colemanite deposits were identified in areas such as White Basin and Callville Wash (near present-day Lake Mead). A major find—the Anniversary Mine—was located in 1921 by prospectors F.M. Lovell and George Hartman and later operated by companies including the West End Chemical Company until around 1928.

The town of Borax itself was established in 1905, directly tied to these regional borax deposits. Its location along the railroad made it a logical siding for potential shipping or support activities related to mining. While never a large settlement, it persisted modestly into the mid-20th century before being fully abandoned. No major long-term mining infrastructure developed at the exact site of Borax, and by the 1940s it was already fading. Today it serves only as a minor railroad marker with ZIP code 89026.

Decline and Legacy

By the early 1900s, Nevada’s borax industry had largely been eclipsed by massive California operations (such as the eventual U.S. Borax mine at Boron, CA). Improved rail transport, cheaper extraction methods, and richer ore bodies in Death Valley and elsewhere ended most Nevada borax production. The state’s early contributions, however, were pivotal: Smith’s 1872 discovery at Teel’s Marsh helped establish the domestic borax market and the Pacific Coast Borax Company, which evolved into a global leader (now part of U.S. Borax / Rio Tinto).

The ghost towns and ruins—such as Marietta’s stone walls and Columbus’s abandoned works—along with place names like Borax, Nevada, preserve this chapter of Western mining history. Borax mining brought infrastructure, labor, and economic activity to Nevada’s remote deserts but also exemplified the boom-and-bust cycle typical of mineral extraction in the American West.

Stone’s Ferry, Nevada

Stone’s Ferry was a former settlement and Colorado River ferry crossing in Clark County, Nevada, established by members of the Church of Jesus Christ of Latter-day Saints (LDS Church, or Mormons). It served as a vital transportation link between Nevada and Arizona. The site shifted locations over time: initially near the mouth of the Virgin River, then approximately 6 miles downstream, and later 2 miles below the Virgin River mouth opposite Detrital Wash (its primary GNIS-recorded position from an 1875 survey at coordinates approximately 36°7′42″N 114°26′51″W). It lay opposite Detrital Valley, which offered an accessible route south from the Colorado River canyon into Arizona mining districts and north through the Virgin and Muddy Valleys toward Nevada and Utah. The ferry operated as both a commercial crossing and a barge landing in a remote desert-river environment.

Early History/Founding

The crossing originated informally in the late 1860s as Mormon colonists in the Muddy and Virgin River valleys (part of Pah-Ute County, Arizona Territory at the time) used boats left at the Virgin River mouth to cross the Colorado River. This connected their settlements to wagon roads leading south to Arizona mines (such as Chloride, Mineral Park, and Cerbat) and the Hardyville-Prescott Road. Brigham Young visited the area in 1870, but in 1870–1871 the colonists voted to abandon the settlements due to boundary disputes (the area was determined to be in Nevada) and high taxes imposed by Nevada authorities.

One colonist, Daniel Bonelli of St. Thomas, voted against abandonment and remained as the sole holdout. He moved his family to the site, acquired an existing ferry boat, and established a commercial ferry service known as Stone’s Ferry around 1871. The name’s origin is unclear; a 1875 Wheeler survey noted two early operators at the site, including James Thompson (who briefly held ferry rights) and possibly a settler named Stone. The ferry began operations about 6 miles downstream from the Virgin River mouth before being relocated upstream to a more favorable point opposite Detrital Wash.

Economic Activities

Stone’s Ferry functioned primarily as a commercial river crossing for passengers, freight, livestock, and emigrants traveling between Nevada and Arizona. It supported regional mining by providing access to Arizona’s silver districts and served as a landing for barges, such as those operated by Captain L. C. Wilburn. These barges transported salt mined from nearby Virgin River valley deposits downstream to the mills at El Dorado Canyon, where it was essential for processing silver ore.

Under Bonelli’s ownership (after he purchased the rights around 1870–1871), the ferry expanded to haul produce, feed, and salt from his St. Thomas farm and salt mines to mining camps like El Dorado, Chloride, and Cerbat. It also facilitated larger movements, including a band of sheep to Arizona in 1875 and a group of 83 Mormon emigrants in 1877. The operation relied on the river’s flow and manual or animal-assisted boat handling, tying directly into the broader network of Mormon agriculture, salt production, and support for southwestern mining booms.

Decline/Abandonment

The ferry’s original site and operations were short-lived in their initial form. In 1876, Daniel Bonelli relocated the ferry and his family upstream near the old settlement of Junction City (just east of the Virgin River mouth) and renamed it Bonelli’s Ferry. This move centralized operations closer to his St. Thomas holdings and improved access. By the early 1900s, competing railroads and improved overland roads reduced river traffic. Bonelli died of a stroke in 1903; a flood destroyed the ferry in 1904 (though his son later rebuilt and operated it into the 1920s). The associated post office at the renamed site (Rioville) closed in 1906 as irrigation water diminished and economic activity shifted away.

The original Stone’s Ferry site ceased independent operations with the relocation, and the entire area saw full abandonment as a settlement by the early 20th century. All river crossings in the region, including this one, were ultimately inundated by the rising waters of Lake Mead following the construction of Hoover Dam in the 1930s.

Legacy/Current Status

Stone’s Ferry exemplifies the pioneering role of Mormon settlers in developing early transportation infrastructure along the Colorado River in the American Southwest. It bridged isolated agricultural colonies with Arizona’s mining economy, supported salt transport for ore processing, and highlighted the challenges of remote river-based commerce before railroads dominated. The site transitioned into Bonelli’s Ferry (later associated with Rioville/Junction City), which operated longer but shared the same fate. Its history underscores themes of Mormon colonization in southern Nevada, boundary shifts between territories, and the eventual transformation of the Colorado River by large-scale dam projects.

Today, the site of Stone’s Ferry lies submerged beneath the Virgin Basin of Lake Mead. No surface remains are accessible, and it is recognized as one of Clark County’s ghost towns due to its complete inundation and abandonment. It joins other nearby historical sites (such as St. Thomas and Rioville) lost to reservoir waters but preserved in historical records and surveys.

Sources/References

  • Wikipedia: Stone’s Ferry, Nevada (drawing on primary historical accounts and surveys).
  • U.S. National Park Service, Lake Mead history documents (detailing operators, Bonelli’s purchase in 1877, uses, and submersion).
  • James H. McClintock, Mormon Settlement in Arizona: A Record of Peaceful Conquest of the Desert (1921).
  • Richard E. Lingenfelter, Steamboats on the Colorado River, 1852–1916 (University of Arizona Press, 1978).
  • Additional context from George M. Wheeler’s 1875 Topographical Atlas and surveys; Legends of America historical summaries on Colorado River crossings.

This report is based on documented historical records of Mormon settlement, river transportation, and mining support in the lower Colorado River region during the late 19th century. Stone’s Ferry illustrates the brief but essential role of such ferries in opening the desert Southwest before modern infrastructure rendered them obsolete.

Saint Joseph, Nevada – Clark County Ghost Town

Ghost towns of Clark County, Nevada
Ghost towns of Clark County, Nevada

Saint Joseph, Nevada, is a historic ghost town located in Clark County in the Moapa Valley along the east bank of the Muddy River. It played a brief but notable role in the mid-19th-century Mormon colonization efforts in southern Nevada. Today, little physical evidence remains of the original settlement, though its legacy connects to the modern community of Logandale.

Founding and Early Settlement (1865)

Mormon settlers, directed by Brigham Young as part of the broader Muddy Mission (or Moapa Mission), established Saint Joseph in May 1865. A group led by Thomas Smith initially founded the nearby community of St. Thomas at the confluence of the Muddy and Virgin Rivers earlier that year. In June 1865, a second group moved about nine miles north and built a fort on a bluff overlooking the east side of the Muddy River, roughly five miles north of present-day Overton.

The settlement was named Saint Joseph, reportedly after Joseph Young, a colonizer and son of Brigham Young. Like other Muddy Mission outposts, its purpose was agricultural: to grow crops such as cotton, wheat, and corn in the fertile river valley, while also securing the area against non-Mormon (“Gentile”) travelers and supporting the broader Latter-day Saints expansion in the American West.

Settlers constructed adobe buildings, a wooden gristmill (sometimes associated with the nearby Simonsville or Mill Point area), and other infrastructure. The mill processed salt, corn, and wheat. By 1867, the community had grown enough to receive its own post office (established August 26, 1867). It briefly served as the county seat when the Utah Territory created Rio Virgen County, even as the Arizona Territory claimed parts of the valley under Pah-Ute County.

The 1868 Fire and Relocation

In 1868, a fire—reportedly started by young boys attempting to roast potatoes—swept through the town and destroyed most of the structures, sparing at least one adobe building. Residents attempted to rebuild, but many relocated a few miles northwest to a new site along the Muddy River (sometimes described as on the west side or a short distance upstream). This new location also took the name Saint Joseph and grew to several hundred residents. The original post office transferred there.

Abandonment Due to Boundary Issues (1870–1871)

A major turning point came with the 1870 boundary survey, which determined that the Moapa Valley, including Saint Joseph, lay within Nevada rather than the Utah or Arizona territories as previously assumed. Nevada authorities demanded that the Mormon settlers pay substantial back taxes in gold coin—a burden the community found unsustainable. With permission from Brigham Young, most residents abandoned the settlement in 1871. Only one family reportedly remained initially.

This abandonment mirrored the fate of other Muddy Mission towns like St. Thomas. Non-Mormon settlers (“Gentiles”) soon moved in to claim the farmlands and remaining structures.

Later History and Connection to Logandale

Mormon pioneers began returning to the Moapa Valley around 1880, repurchasing land and re-establishing communities such as Overton and parts of the former Saint Joseph area. The relocated Saint Joseph site was renamed Logan (after an early pioneer or to avoid confusion) and later Logandale in 1917. Logandale incorporated the post office and became a lasting agricultural community in Clark County.

A Saint Joseph Cemetery in the area dates back to the 1860s, with initial use around 1864–1869 and additional burials in the 1890s. Some remnants, such as foundations or the occasional adobe structure, have been noted by historians and local explorers, though the original townsite is largely gone. Nearby historic buildings in the Logandale area, like the Gubler House (built 1909), reflect the continued settlement history.

Geographic and Modern Context

Saint Joseph (historical) is situated in Clark County, Nevada, with coordinates approximately 36°34′22″N 114°26′59″W. It lies in the Moapa Valley, part of the broader region that includes Overton and Logandale, north of Las Vegas. Clark County itself was not organized until 1909 (carved from Lincoln County), long after the town’s abandonment.

Today, Saint Joseph is classified as a ghost town, with minimal visible ruins compared to better-preserved sites like St. Thomas (partially submerged and later exposed due to Lake Mead fluctuations). The area’s history is preserved through local historical societies, the Clark County Museum, and accounts of the Muddy Mission.

Significance in Nevada History

Saint Joseph exemplifies the challenges faced by early Mormon settlements in the arid West: ambitious agricultural missions, conflicts over territorial boundaries, and tensions with state taxation. The Muddy Mission towns, including Saint Joseph, St. Thomas, and others, represented Brigham Young’s vision of a self-sustaining “Zion” corridor stretching from Utah southward. Their short-lived nature highlights how federal boundary decisions and economic pressures shaped settlement patterns in southern Nevada during the post-Civil War era.

The story of Saint Joseph underscores the resilience of the Moapa Valley’s communities, which transitioned from short-term missionary outposts to enduring agricultural towns like Logandale and Overton that still thrive today on farming and ties to Las Vegas.

Sources for further reading include local histories such as Pearson Starr Corbett’s work on the Muddy Mission, Nevada historical society publications, and sites documenting Clark County ghost towns. Remnants and related sites can sometimes be viewed in the Moapa Valley area, though visitors should respect private property and protected lands.