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.

Ashford Mill Site

Ashford Mill Site is a historic mining ruin located in Death Valley National Park, California. It represents one of the many short-lived gold mining operations that dotted the region during the early 20th century, embodying the boom-and-bust cycles typical of desert prospecting in one of the harshest environments in North America.

Ashford Mill Ruins Sign.  Photo by James L Rathbun
Ashford Mill Ruins Sign. Photo by James L Rathbun

Location and Setting

The site lies on the valley floor along Badwater Road (California State Route 178), approximately 28 miles (45 km) west of the Shoshone entrance to the park. The associated Ashford Mine (also known as the Golden Treasure Mine) is located about 5 miles (8 km) east in the Black Mountains, roughly 3,500 feet (1,067 m) higher in elevation within Ashford Canyon. The mill was strategically placed on the valley floor to process ore trucked down from the mine. Today, visitors find concrete foundations, scattered debris from machinery, and the crumbling walls of a former office building. The site includes parking, picnic tables, scenic viewpoints, and vault toilets. Nearby Shoreline Butte displays ancient wave-cut terraces from the prehistoric Lake Manly.

Discovery and Claim Acquisition (1907–1910)

In January 1907, prospector Harold J. Ashford arrived in the Death Valley region, drawn by recent gold strikes at the nearby Desert Hound Mine. He noticed that the Keys Gold Mining Company had failed to perform required assessment work on several claims in the Black Mountains. Ashford relocated (re-staked) the claims under mining law and began working them. The Keys company did not discover the issue for nearly two years. In January 1910, they sued to reclaim the property, but a judge ruled in Ashford’s favor, securing title for him and his brothers, Henry and Lewis. The Ashfords worked the mine intermittently from 1910 to 1914 but achieved only modest results.

Ashford Mill, Death Valley National Park. Photo by James L Rathbun
Ashford Mill, Death Valley National Park. Photo by James L Rathbun

Development and Mill Construction (1914–1915)

In November 1914, the Ashford brothers leased the mine to wealthy Los Angeles residents B.W. McCausland and his son Ross. Under their leadership, the operation expanded dramatically. They drove a 180-foot tunnel, developed approximately 2,000 feet of underground workings, and employed up to 28 men at peak. The lessees invested over $125,000 in infrastructure, including construction of a 40-ton-capacity mill on the valley floor in 1915. The mill featured a jaw crusher, a 10-foot Lane mill, a Wilfley concentrating table, and a Diester slime table. Ore was trucked five miles down the mountain for processing before shipment to a smelter. The mill became operational by late August 1915. A popular (but unverified) local legend claims that a double shipment of cement arrived during construction; rather than return the excess, the McCauslands used it to build the durable concrete foundations and office that still stand today.

Operations, Decline, and Initial Closure (1915)

Despite extracting an estimated $100,000 worth of gold ore, the operation proved unprofitable. The ore grade was too low to cover the enormous costs of extraction, processing, and transportation across the remote desert terrain. Operations ceased in September 1915, only weeks after the mill opened. The McCauslands withheld lease payments, leading the Ashfords to file a lawsuit that yielded no compensation. The mill and mine then lay idle for more than a decade.

Intermittent Later Activity (1926–1941)

Brief revivals occurred over the following years. In 1926, four men worked the mine briefly before abandoning it again. In 1935, the Ashfords leased the property to Golden Treasure Mines, Inc., which reopened the mine and shipped high-grade ore to Shoshone via the Tonopah & Tidewater Railroad. High trucking costs limited profitability; total production through 1938 was valued at no more than $18,000. The Ashfords briefly operated the mine themselves in 1938, shipping 38 tons of ore. Later that year they leased it to Bernard Granville and Associates of Los Angeles, who installed a short aerial tramway to consolidate ore from scattered workings. The operation employed about 10 men but produced no recorded shipments and ceased by 1941. The Ashfords retained ownership but performed no further significant work. Over its entire history (1910–1941), the mine yielded just enough gold to sustain the brothers in basic supplies and legal fees.

Legends, Myths, and Cultural Significance

Early tourists were drawn by colorful legends surrounding the mine, including a story that the Ashford brothers sold it for $50,000 to a Hungarian count, who then resold it to B.W. McCausland for $105,000. An old wooden interpretive sign at the site perpetuated this tale for decades. However, National Park Service records describe these stories as more intriguing than factual. The site nonetheless symbolizes the persistent yet often futile quest for riches in Death Valley’s extreme environment.

Abandonment and Preservation

The mill was never reopened after 1915; its wooden walls, windows, and most machinery were removed or decayed over time, leaving only the concrete foundation and debris. The nearby office building survives as crumbling concrete ruins. The Ashford Mill Site was incorporated into Death Valley National Monument (later National Park) and is preserved today as a historic resource. The mine site higher in the canyon contains collapsed shacks, bunkhouses, headframes, and tramway remnants from the 1930s–1940s era, accessible via a strenuous hike up Ashford Canyon (the old road is washed out).

Visiting the Site Today

The Ashford Mill Site remains a popular roadside stop along Badwater Road. A short walk reveals the ruins and interpretive signage (the older legend-bearing sign may still be present). It offers a poignant reminder of the human ambition and environmental challenges that defined early 20th-century mining in the American Southwest. The site is open year-round, though summer heat and flash-flood risks in the canyon require caution. No artifacts should be disturbed, as the area is protected within the national park.

Desert Five-Spot (Eremalche rotundifolia)


The Desert Five-Spot (Eremalche rotundifolia) is a striking annual wildflower commonly observed in Death Valley National Park, particularly during favorable bloom years following sufficient winter rainfall.

Desert Five-Spot (Eremalche rotundifolia) - Photo by James L Rathbun
Desert Five-Spot (Eremalche rotundifolia) – Photo by James L Rathbun

Scientific Taxonomy

  • Kingdom: Plantae
  • Phylum: Tracheophyta (vascular plants)
  • Class: Magnoliopsida (dicotyledons)
  • Order: Malvales
  • Family: Malvaceae (mallow family, which includes hibiscus and cotton)
  • Genus: Eremalche
  • Species: Eremalche rotundifolia (A. Gray) Greene

This species is a dicotyledonous annual herb native to desert regions.

Description

The desert five-spot is a low-growing annual herb typically reaching 8–60 cm (3–24 inches) in height. It has an erect, sparsely branched stem (often simple or branched only at the base) covered in bristly hairs; stems are frequently reddish-brown. The leaves are distinctive: rounded to kidney-shaped (reniform), 1.5–6 cm broad, with toothed or crenate margins, and borne on long petioles. Leaves are green (sometimes with reddish phases) and covered in short bristly hairs.

The most striking feature is the flower: bisexual, cup- to globe-shaped, with five overlapping petals 15–30 mm long. Petals are rose-pink to lilac or purplish-pink, each featuring a prominent dark red-to-purple spot at the base that serves as a nectar guide for pollinators. When fully open, the petals curve slightly inward, forming a nearly spherical “lantern” shape (hence the occasional nickname “Chinese lantern flower”). The center reveals a ring of light pink stigmas surrounding smaller stamens. The calyx has 5 lobes, and three small bractlets subtend it. After flowering, the plant produces a schizocarp fruit that splits into 25–35 wafer-like segments.

Note on identification: Do not confuse it with the unrelated “five-spot” (Nemophila maculata), a white-flowered plant of the Sierra Nevada and foothills with purple spots at the petal tips.

Blooming Period and Behavior

The beautiful and delicate flower of the Desert Five Spot Flower.  - Photo by James L Rathbun
The beautiful and delicate flower of the Desert Five Spot Flower. – Photo by James L Rathbun

Flowering occurs primarily from March to May, with peak displays in the lower desert elevations from mid-February through mid-April, depending on winter rainfall. In Death Valley National Park, it is a signature wildflower during “superbloom” years (such as the notable events following heavy rains).

The flowers exhibit daily nyctinastic movement: they open in the morning (or midday) to reveal the vivid red spots and close at night or late afternoon. Leaves also show diurnal movement to optimize sunlight exposure. The red basal spots on each petal function as “runways” directing bees and other insects to the nectar at the flower base, aiding pollination. The plant thrives in years with adequate winter precipitation and is one of the more sought-after desert wildflowers for its vivid color contrast against the arid landscape.

Range and Distribution

Eremalche rotundifolia is native to the Mojave Desert and Colorado Desert (part of the Sonoran Desert region) in the southwestern United States and northwestern Mexico. It occurs in southeastern California (including Death Valley National Park and Anza-Borrego Desert State Park), southern Nevada, western Arizona, and extends slightly into Utah. In California it is found primarily in the Desert bioregion (excluding the high Desert Mountains). Elevation range is approximately -50 to 1,500 m (-164 to 4,921 ft), though it is most common between 50 and 1,200 m.

The closed flower of the Desert Five Spot Flower.  Photo by James L Rathbun
The closed flower of the Desert Five Spot Flower. Photo by James L Rathbun

Habitat and Ecology

This species prefers open, sunny sites in dry desert scrub, desert flats, sandy or rocky washes, alluvial fans, and open stony areas. It grows best in fast-draining, gravelly alkaline soils and is frequently associated with creosote bush scrub communities. In Death Valley National Park it appears on lower-elevation alluvial fans, foothills, and along roadsides (e.g., Badwater Road areas) following sufficient winter rains.

As an annual, it completes its life cycle quickly after winter rains, producing abundant seeds that remain dormant in the soil until the next favorable season. It provides nectar for native bees and supports larvae of certain butterflies and skippers (including confirmed hosts for Northern White-Skipper and Common Checkered-Skipper).

The desert five-spot is a beautiful and iconic Mojave Desert wildflower, particularly celebrated in Death Valley for its glowing pink blooms and striking red-spotted “lantern” flowers during spring displays. Its presence is highly dependent on winter precipitation, making it a highlight of rare superbloom events.

Pebble Pincusion (Chaenactis carphoclinia)

Scientific Name: Chaenactis carphoclinia A. Gray (primarily var. carphoclinia in Death Valley and most of its range)

Pebble Pincusion (Chaenactis carphoclinia) Found near Ashford Mill, Death Valley National Park.  Photo Heather Rathbun
Pebble Pincusion (Chaenactis carphoclinia) Found near Ashford Mill, Death Valley National Park. Photo Heather Rathbun

Scientific Taxonomy

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Clade: Asterids
  • Order: Asterales
  • Family: Asteraceae (Sunflower or Daisy family)
  • Genus:Chaenactis (pincushions or dustymaidens)
  • Species:Chaenactis carphoclinia A. Gray

Common names include Pebble Pincushion, Pincushion Flower, and Straw-bed Pincushion. Two varieties exist: the widespread var. carphoclinia (smaller plant, common in Death Valley) and the rarer var. peirsonii (larger, limited to southern California’s Santa Rosa Mountains).

Description

Pebble Pincushion is a native annual forb/herb that grows from an erect, branching stem (usually one main stem) reaching 4–16 inches (10–40 cm) tall, occasionally up to 2 feet (60 cm) in favorable conditions. The stems are whitish-pubescent (hairy).

Leaves are green, mostly linear, and pinnately dissected or lobed (basal leaves highly divided and wither early; cauline leaves smaller with slender petioles), up to 4–10 cm long.

The inflorescence consists of 1–several small discoid flower heads (no ray flowers) per stem, each 0.25–1 cm wide. Heads feature white to pinkish-tinted disk florets with enlarged outer corollas and prominently exserted (protruding) anthers. Flat, sharp-pointed phyllaries (bracts) line the heads and often appear reddish. The fruit is a small achene tipped with a scaly pappus.

The plant resembles other desert Chaenactis species (e.g., Esteve’s Pincushion), but is generally smaller with multiple cream-to-white heads per stem.

Blooms

As a desert annual, Pebble Pincushion germinates after winter rains and blooms primarily in spring (January/February/March through May or June, depending on elevation and rainfall). In Death Valley, it is a signature species during “superbloom” years, often peaking in March–April alongside other desert annuals. The flowers are visited by bees, butterflies, and other small insects for nectar and pollen.

Range and Habitat

Pebble Pincushion is native to the southwestern United States and northwestern Mexico. Its range spans Arizona, California, Nevada, New Mexico, Utah, Baja California, and Sonora—primarily in the Mojave Desert, with extensions into the Sonoran Desert, southern Great Basin, and northwestern Chihuahuan Desert. Elevations range from 300–6,200 feet (90–1,900 m).

It thrives in rocky, gravelly, or sandy soils, including washes, open plains, mesas, slopes, and flats within desert shrublands. In Death Valley National Park, it is commonly found in gravelly washes and rocky areas (e.g., near Emigrant Pass, Badwater, and Mosaic Canyon), where it can form dense displays after sufficient winter precipitation. Seeds may be consumed by birds, small mammals, and desert tortoises.

Pebble Pincushion growing in typical Death Valley habitat—gravelly washes with mixed desert annuals under clear desert skies.

This hardy annual plays a key role in desert ecosystems as a quick-response bloomer that stabilizes soil and supports pollinators and wildlife following rainy periods.

San Francisco Chronicle newspaper of Jan. 13, 1895

San Francisco Chronicle newspaper of Jan. 13, 1895
San Francisco Chronicle newspaper of Jan. 13, 1895

The San Francisco Chronicle article published on January 13, 1895, titled something along the lines of “A Mine in the Superstition Mountains” (or variations like “A Mine in the Superstition Mountains–The Half-told Tale of an Old Miser–Afraid to Return to the Source of His Mysterious Wealth”), played a pivotal role in popularizing and shaping the modern legend of the Lost Dutchman Gold Mine.

Written by freelance writer and prospector Pierpont C. Bicknell (often abbreviated P.C. Bicknell), this piece is widely regarded by historians and researchers of the legend as one of the earliest—if not the earliest—nationally distributed accounts that crystallized many of the core elements associated with the tale today. Jacob Waltz (the German immigrant prospector nicknamed “the Dutchman,” despite not being Dutch) had died in Phoenix in October 1891, and local Arizona newspapers had mentioned his alleged rich mine and search efforts by associates like Julia Thomas and the Petrasch brothers as early as 1892 (e.g., in the Salt River Herald). However, Bicknell’s 1895 Chronicle article elevated the story from regional rumor to broader public fascination.

Key Content and Contributions from the Article

Bicknell’s piece drew heavily from accounts circulating in Arizona, likely including details from Julia Thomas (who cared for Waltz in his final days and attempted to locate the mine). It presented the mine as a real, extraordinarily rich gold deposit hidden in the Superstition Mountains east of Phoenix (then in Arizona Territory). Notable elements introduced or emphasized include:

  • A description of the mine’s location tied to landmarks in the Superstitions, within a roughly 5-mile radius of Weaver’s Needle (a prominent rock formation that became iconic in later tellings).
  • References to a hidden tunnel or shaft in a gulch, concealed by bushes, with a two-room rock house or cabin in a cave (sometimes described as “caverna con casa” or rock cabin in a cave) on the opposite slope.
  • Clues about accessing the site via a gulch, with the mine featuring rich gold ledges where flakes of nearly pure gold could be picked off.
  • The narrative framed around Waltz as an “old miser” who revealed partial details on his deathbed but was too fearful or infirm to return himself.
  • Broader claims of the mine’s “fabulous wealth” and consistency of witness/testimony pointing to a specific area.

These details aligned with earlier local reports but were packaged dramatically for a wider audience, making the story more compelling and clue-oriented.

Role in the Legend’s Development

The article’s significance lies in its dissemination and influence:

  • It is often credited as the first major national exposure of the “Lost Dutchman” story, helping transform a local Arizona prospector’s tale into a widespread American legend of hidden treasure.
  • Bicknell reportedly syndicated or republished elements of his work; the piece was reprinted in outlets like the Kansas City Journal (February 17, 1895), spreading it further across the U.S.
  • It introduced or solidified motifs that later writers and treasure hunters built upon, including connections to the Peralta family (Mexican miners allegedly massacred by Waltz or others to claim the site—though some sources note this link may have been embellished by Bicknell or absent in pre-1895 accounts), deathbed revelations, hidden cabins/tunnels, and Weaver’s Needle as a key reference point.
  • Historians (such as Tom Kollenborn and others studying Superstition Mountains lore) trace much of the persistent “clue” tradition directly to Bicknell’s descriptions, which influenced later searchers like Adolph Ruth (whose 1931 death in the mountains involved directions derived from this 1895 article).

While earlier mentions existed in Arizona papers (e.g., around Julia Thomas’s 1892 search), Bicknell’s Chronicle publication is seen as the catalyst that launched the legend into enduring popularity. It arrived at a time when tales of lost mines captivated the public during the waning years of the frontier era, fueling decades of expeditions, books (like Barry Storm’s Thunder God’s Gold), films, and ongoing searches—despite no verified discovery of the mine.

In summary, the January 13, 1895, San Francisco Chronicle article did not invent the story but was instrumental in standardizing its details, providing searchable “clues,” and propelling it from obscure regional folklore to one of the most famous lost-mine legends in American history.

One of Arizona’s Lost El Dorados

A Mine in the Superstition Mountains

The Half-told Tale of an Old Miser

Afraid to Return to the Source of His Mysterious Wealth.

Phoenix (A.T.), Jan. 9–That there exists an undiscovered gold mine of fabulous wealth near a point in the Superstition Mountains not more than fifty miles from Phoenix has long been an article of faith among a number of mining men in a position to sift the mass of evidence accumulated during the past twenty years. The facts and individual statements, although emanating from widely diverse sources and furnished by persons who could have had no possible communication with one other, all agree in a remarkable manner as to the description of the mine, and, what is still more convincing, are unanimous in indicating a particular quarter of the mountains in question as the place of its location. In a gulch in the Superstition mountains, the location of which is described by certain landmarks, there is a two-room house in the mouth of a cave on the left side of the slope near the gulch. Just across gulch, about two hundred yards, is a tunnel, covered up and concealed in the bushes. Here is the mine, the richest in the world, according to Dutch Jacob. Some distance above the tunnel on the side of the mountain is a shaft or incline that is not so steep but can climb down. The shaft goes right down in the midst of a rich gold ledge, where it can be picked off in big flakes of almost pure gold

San Francisco Chronicle newspaper of Jan. 13, 1895