Potholes California – Colorado River Steamship Landing

Potholes, California, is a former gold mining camp and short-lived settlement in Imperial County on the west bank of the Colorado River, near the present-day site of Laguna Dam (about 15–18 miles upriver from Fort Yuma / Yuma, Arizona, and roughly 4 miles northeast of Bard). It sits in the southeastern Chocolate Mountains at the edge of what is now the All-American Canal system. The site is a ghost town with little remaining surface evidence of its mining or steamboat eras; a cemetery lies about a mile south along the riverbank.

Potholes California

Early Spanish Mining and Loss of Knowledge

Placer gold deposits at the “Pot Holes” (natural depressions in the desert gravels) were likely worked by Spanish miners associated with Mission San Pedro y San Pablo de Bicuñer, established in 1781 near the site. Knowledge of the diggings was largely lost after the Yuma (Quechan) uprising of 1781, in which the missionaries and settlers were killed. The location remained obscure for decades.

Rediscovery and 19th-Century Placer Mining

In early 1859, placer gold was rediscovered about 15 miles above Fort Yuma on the California side of the Colorado. Contemporary reports (including from the Daily Alta California) described paying claims: one operation reportedly yielded $200 per day for a short period, with others producing $10–$16 per day. Miners carried dirt to the river to wash in cradles; better results were expected if water could be brought to the diggings for sluicing. Mining continued intermittently through the later 19th century, largely by Hispanic prospectors familiar with dry-washing techniques suited to the arid environment. Estimates suggest hundreds of Mexican miners worked the district at peak times. A failed dredging attempt on the river near the site in 1900–1901 recovered little gold because the particles were too fine for the equipment. Total historical production from the district has been estimated in the range of around $2 million (period values).

There has been some little excitement in this part of the, country, caused by the discovery of new gold fields on the Rio Colorado, some fifteen miles above Fort Yuma, on the California side. I have just returned from the diggings, and find, after a careful examination of three days, that gold exists there in paying quantities, for many miles on both sides of the river. While at the newly discovered diggings, a considerable quantity of the oro has been taken out, considering the short time- they have been worked. From the claim of Messrs. Crandell & Co., $200 per day have been dug daily for the past six days. The manner of working is the same at at Jila city, heretofore described. The earth must be carried on the back a distance of one mile, and washed in a cradle. It is said that the total amount of the gold taken from Crandell & Co ‘s claim is about $4,000. – They have now constructed a cart-road from the mine to the river, and hereafter will be able to work at better advantage. Several other claims in the vicinity are paying from $10 to $16 per day; but most of the claims — for a good manner have been located — will not pay more than $2 per day to the hand, by the present process of working. If water could be obtained and sluice* used, from $40 to $100 per day might be washed. [We had news of these diggings in oar San Diego correspondence, published this morning, and the corroborating testimony of .our Fort Yuma correspondent is of much value, as confirmatory of the reports from San Diego. — Eds. Alta.]

I think, however, that the Gila mines are much more valuable, or will yield much more gold than these new diggings on the Colorado. Th« former have the advantage of being easily supplied with water, works for that purpose being now in progress.

Mining operations resumed again in 1859 with the rediscovery of gold. Placier mining operations proved successful in the 19th century. A steamship landing was established to ferry people and supplies to the location 15 miles up river from Yuma, Arizona.

The town of Potholes California was established during the building of the All American Canal and Laguna Dam.

Daily Alta California, Volume XI, Number 42, 12 February 1859

Role as a Colorado River Steamboat Landing and Supply Point

From 1852 to 1909, shallow-draft paddle-wheel steamboats were the primary commercial transportation on the lower Colorado River, moving people, military supplies, mining equipment, food, and ore between the Gulf of California (and later ocean connections) and upriver settlements and mines as far as the Virgin River area. George A. Johnson & Company (later the Colorado Steam Navigation Company) dominated the trade after early experiments with vessels such as the Uncle Sam (1852) and General Jesup.

Potholes appears on historical lists of steamboat landings beginning in 1859, located roughly 18 miles (29 km) above Fort Yuma. A landing was established specifically to deliver people and supplies to the newly active gold diggings. It served the local mining camp and the surrounding area (including the nearby Laguna placers across the river in Arizona Territory that opened around 1860). Steamboats provided a far cheaper and more practical alternative to overland wagon freight across the desert. Landings like Potholes functioned as local hubs: boats tied up overnight (night navigation was too hazardous on the shifting, shallow, sandbar-filled river), took on wood fuel cut by local Indigenous workers, discharged cargo for the mines and camps, and loaded any ore or goods for the return trip. This river network supported the broader mining boom of the 1860s along the lower Colorado and enabled isolated desert camps to obtain provisions that would otherwise have been prohibitively expensive.

Steamboat traffic declined after railroads reached the region (notably the Southern Pacific’s arrival at Yuma in the late 1870s) and effectively ended with the completion of Laguna Dam in 1909, which blocked further upriver navigation.

Early 20th-Century Construction Camp and Post Office

A town named Potholes was re-established (or formalized) during construction of Laguna Dam (completed 1909) and related work on the All-American Canal system, which diverted Colorado River water for Imperial Valley irrigation. A post office operated there from 1905 to 1909 and again from 1920 to 1922. The settlement was also served by a short Southern Pacific Laguna Branch railroad spur. Once the major construction projects finished and steamboat service ceased, the community faded. The canal and dam works altered the landscape, and much of the earlier mining and mission-era evidence was affected by flooding or later infrastructure.

Legacy

Potholes illustrates the layered history of the lower Colorado River corridor: early Spanish exploration and mining, mid-19th-century gold rushes sustained by steamboat logistics, and early-20th-century water infrastructure that transformed the desert into irrigated farmland. Today the site is largely unmarked and accessible mainly via local roads near Laguna Dam; remnant activity has been limited to occasional recreational prospecting. Its brief but documented role as a steamboat landing underscores how river transport once linked remote mining camps to distant supply centers, enabling settlement and extraction in an otherwise isolated frontier.

Town Summary

NamePotholes, California
LocationImperial County, California
Latitude, Longitude32.8289329, -114.5046713
Elevation160 feet
GNIS247730
Post Office1905 – 1909, 1920 – 1922

Potholes California Map

References

Nivloc Nevada – Esmeralda County Ghost Town

In 1907, Gold was discovered at the town site which would be known as Nivloc Nevada by a Native American prospector. The town derived its name from for the former owners “Colvin” who operated the site in 1923. The name spelled backwards was Nivloc and such is the haste in the Nevadan desert.

Nivloc mine and camp - Tonopah Times-Bonanza -  Nevada Ghost Towns and Mining Camps - Paher
Nivloc mine and camp – Tonopah Times-Bonanza – Nevada Ghost Towns and Mining Camps – Paher

The original mining operations were short lived. The town experienced a bit of a resurgence in the 1930s. The town never amounted to much boasting only one saloon. At its height of operation from 1940 to 1943 the town could claim a post office. Between 1937 and 1943 the small town produced between $2 and $3 million dollars of Gold and Silver. The 400,000 tons of ore was pulled from mines reaching depths 440 feet and 600 feet of below the surface. During this time, the mines of Nivloc ranked as Nevada’s number one silver producer.

Nivloc Today

We have not made a trip to Nivloc, however the townsite is very high on my ghost town “to do” list. There are several standing structures and buildings intact. The mine headframe is still standing at and a rail trestle bridge which is one hundred and twenty feet in length and forty feet tall.

Town Summary

TownNivloc, Nevada
LocationEsmeralda County, Nevada
Latitude, Longitude37.71583, -117.75722
Elevation6,170 feet
GNIS851592
Post OfficeOctober 1940 to November 1943

Nivloc Map

Resources

Gideon Roberts

Gideon Roberts was a minor but notable figure in the legend of the Lost Dutchman Gold Mine, a fabled gold deposit hidden in Arizona’s Superstition Mountains. Little is known about his personal life, as historical records provide sparse details, and he is primarily referenced in connection to the events surrounding Jacob Waltz’s death in 1891.

The Lost Dutchman’s Gold Mine

The Lost Dutchman Gold Mine is a legendary treasure shrouded in mystery, believed to be hidden in the rugged Superstition Mountains of Arizona. The tale originates from Jacob Waltz, a German immigrant known as “the Dutchman,” who allegedly discovered a rich gold vein in the mid-19th century but took its precise location to his grave in 1891. Over the years, the mine has become a focal point of American folklore, with countless prospectors, adventurers, and treasure hunters scouring the treacherous terrain for clues, guided by vague maps, cryptic stories, and supposed landmarks like Weaver’s Needle. Despite extensive searches, no verified evidence of the mine’s existence has been found, leading some to dismiss it as a myth, while others believe it remains concealed, protected by the mountains’ harsh conditions and the secrecy of its original discoverer. The legend persists, fueled by tales of danger, betrayal, and untold riches.

Early Life and Background

Virtually no verifiable information exists about Gideon Roberts’ birth, upbringing, or early life. Some accounts suggest he was a Phoenix local and possibly a miner by trade, as he owned a lot in Phoenix near Julia Thomas’ property around 1891. One source indicates he hailed from Trinidad, Las Animas County, Colorado, and spent winters in Phoenix, but this lacks corroboration. His age is also unclear, though some narratives describe him as significantly older than his associate, Dick Holmes, and possibly closer in age to Jacob Waltz, who was around 80 at the time of his death.

Role in the Lost Dutchman Legend

Gideon Roberts is most prominently mentioned in connection to the deathbed scene of Jacob Waltz, the German immigrant known as “the Dutchman,” who allegedly discovered the mine. In October 1891, Waltz was gravely ill with pneumonia and was being cared for by Julia Thomas in Phoenix. According to accounts, Thomas left to find a doctor and encountered Roberts and Dick Holmes, a young prospector, on the street. She brought them to her home to watch over Waltz. That night, on October 25, 1891, Waltz reportedly shared the location of his mine and bequeathed a box containing 48 pounds of rich gold ore to Holmes, with Roberts present as a witness.

Roberts’ presence during this pivotal moment lends credibility to Holmes’ claim to the gold and the mine’s clues, as he corroborated Holmes’ story. However, unlike Holmes, who spent years searching for the mine, there is no definitive record of Roberts actively pursuing it himself. Some sources speculate he may have been too old or lacked the means to undertake such a quest.

Later Life and Legacy

Details about Gideon Roberts’ life after 1891 are scarce. It is generally reported that he died shortly after Waltz’s death, though no specific date or cause is provided in most accounts. This lack of information has led to speculation about his role and even his existence, with some modern researchers questioning whether he was a distinct individual or conflated with other figures in the legend. For example, one source references a “Gideon O. Roberds” (note the spelling variation) as a possible identity, but this remains unverified.

Roberts’ legacy is overshadowed by more prominent figures like Dick Holmes and Julia Thomas, and he is often omitted from detailed retellings of the Lost Dutchman story. His brief role as a witness to Waltz’s final moments remains his primary contribution to the legend, adding a layer of intrigue to the conflicting narratives surrounding the mine’s location.

Historical Context and Challenges

The scarcity of information about Gideon Roberts reflects the broader challenges of the Lost Dutchman legend, which is riddled with contradictory accounts and unverifiable details. Most books on the subject focus on Waltz, Holmes, or later treasure hunters, leaving Roberts as a footnote. His fleeting presence underscores the elusive nature of the mine itself, which has captivated treasure hunters for over a century but remains undiscovered.

Callville, Nevada – Colorado River Steamship Landing

Callville Nevada is a ghost town and Colorado River Steamboat port, which is now submerged below the waters of Lake Mead. Bishop Anson Call founded and established a colony and warehouse on the Colorado River at the direction of the Mormon Leader Brigham Young. The settlement was located about 15 miles up river from the location of the future site of Hoover Damn.

  Call's Landing or Callville looking toward the west as it appeared in 1926 - Photo courtesy of R. F. Perkins
Call’s Landing or Callville looking toward the west as it appeared in 1926 – Photo courtesy of R. F. Perkins
Bishop Anson Call, Mormon Colonizer, May 13, 1810 – August 31, 1890
Bishop Anson Call, Mormon Colonizer, May 13, 1810 – August 31, 1890

Callville was established on December 2, 1864 when Anson Call arrived on a small bluff over looking the Colorado River in the Arizona Territory. The settlement was located at the conjunction of the later named Callville wash and the Colorado River.

The founding of the settlement was the churches effort to expand trade routes and European immigration into Utah from the south. The small portgage and landing site was one of several along the Colorado including St. Thomas, Saint Joseph, Overton, West Point, Mill Point ( Simonsville ) and Rioville.

During the Civil War, the army of the United States garrisoned at the site, to protect the Colorado River Steamboats and serve as a landing point for army. In December 1865, the outpost had the honor to become the county seat for Pah-Ute County, Arizona Territory. The station was short lived and transferred to St Thomas just two years later.

In 1869, the army garrison was removed. Following the war, Congress redrew some of the state boundaries and the settlement in the Arizona Territory is moved to Nevada. From 1866 to 1878, the landing at Callville was the High Water of Navigation for steamboat traffic on the Colorado River, which is 408 miles from Fort Yuma. The town was abandoned in June 1869 when the Steamships discontinued service to the site.

Today, the town lies in under 400 feet of water. However, the water levels in Lake Mead are at an all time low, and St. Thomas is currently above water.

“Take a suitable company, locate a road to the Colorado, explore the river, find a suitable place for a warehouse, build it, and form a settlement at or near the landing.” 

Brigham Young instructing Anson Call, 1864

Town Summary

LocationCallville
LocationLake Mead, Clark County, Nevada
Latitude, Longitude36.1133128, -114.6888720
GNIS863773
Other Common NamesCall’s Fort, Old Callville

Callville Map

Resources

Western Wallflower (Erysimum capitatium)

A member of the mustard family, the Western Wallflower ( Erysimum capitatium ) is a brightly colored yellow flower which is quite common across the western United States, including Arizona, Utah and Nevada.. In European countries, the wallflower earned its name from a habit of growing on… you guess it, walls. More specifically stone, masonry or wooden fences. The name was transposed to the American species despite the fact the plants have no preference for walls.

Western Wallflower (Erysimum capitatium)
Western Wallflower (Erysimum capitatium)

Scientific Taxonomy and Categorization

  • Kingdom: Plantae
  • Clades: Tracheophytes, Angiosperms, Eudicots, Rosids
  • Order: Brassicales
  • Family: Brassicaceae (mustard or cabbage family)
  • Genus: Erysimum
  • Species: Erysimum capitatum (Douglas ex Hook.) Greene (binomial name)

The species belongs to the tribe Erysimeae within Brassicaceae. It is a dicot angiosperm (eudicot) herb. Flora of North America recognizes two main varieties: E. c. var. capitatum (often called western or sanddune wallflower) and E. c. var. purshii (Pursh’s wallflower). Numerous synonyms exist due to high morphological variability and past taxonomic confusion with E. asperum (prairie rocket). Chromosome number is 2n = 36. The plant is categorized as a biennial or short-lived perennial herb (sometimes behaving as a winter annual in southern deserts), with a taproot and variable growth form depending on elevation and habitat.

Detailed Plant Description

Erysimum capitatum is a highly variable, taprooted herb that produces one to several erect, leafy stems (0.5–12 dm / 1.5–12 ft tall) arising from a basal rosette. Stems are often branched distally, coarse, and covered in stiff, appressed, forked or branched (malpighiaceous/dolabriform) hairs. The plant leaks a pungent, watery juice when damaged.

Basal leaves are simple, alternate, spatulate to narrowly oblanceolate or linear (2–27 cm long × 3–30 mm wide), with prominent midribs and margins ranging from entire to dentate or denticulate. Stem leaves are smaller, sessile, and angled upward. Leaves are typically deep green and hairy (rayed hairs vary by variety: mostly 3–7-rayed in var. capitatum; 2–3-rayed in var. purshii). Plants develop short to elongate caudices clothed in old leaf bases.

Growth habit and life cycle show plasticity: low-elevation plants are often taller, less branched biennials and more drought-resistant; high-elevation (alpine) plants are dwarf, multi-stemmed perennials. The species is early-seral, thriving in disturbed sites, and exhibits semelparity (single reproductive event) in dry lowlands versus iteroparity (multiple events) in moist high-elevation habitats.

Detailed Flower Description

Flowers are perfect, arranged in congested terminal racemes that elongate in fruit. Each flower is 2.5–3.8 cm wide with four distinct, rounded petals arranged in a cross shape (typical of Brassicaceae). Petals are usually bright yellow to orange (occasionally lavender, maroon, red, white, or purple in certain populations or high elevations); var. capitatum tends toward orange-yellow, var. purshii toward yellow. Flowers have four sepals, six stamens (tetradynamous: four long, two short), a stout style (up to 3 mm), and a superior ovary. They are fragrant and bloom primarily April–August (as early as January in southern ranges or to September).

Fruits are linear, narrow siliques (3.5–15 cm long × 1.3–3.3 mm wide), upright or nearly parallel to the stem, four-sided or slightly flattened, with prominent midveins. Each valve contains 40–80 seeds; siliques dehisce at maturity. Seeds are small, oblong (~1.5 mm), lightweight, and winged in var. capitatum. Pollination is required for full seed set; visitors include bees, flies, butterflies, and beetles.

Habitat

The western wallflower occupies diverse dry, open sites from valley bottoms to alpine summits. It prefers well-drained, sandy, gravelly, or rocky soils with low organic matter and fertility. Substrates include sandstone, granite, basalt, limestone, serpentine, dunes, and talus. It occurs in desert grasslands/shrublands, chaparral, pinyon-juniper woodlands, aspen groves, montane meadows, forest openings, sagebrush flats, and alpine tundra. Elevation range is sea level to 13,120 ft (4,000 m), with var. capitatum generally lower (0–5,600 ft) and var. purshii higher (3,280–13,120 ft). It tolerates full sun, drought, and disturbance (roadsides, burns, grazed areas).

Range and Distribution

Erysimum capitatum is one of the most widespread native North American wallflowers. Its range spans western North America from Alaska and Yukon Territory south through British Columbia, Washington, Oregon, California, Idaho, Montana, Wyoming, Utah, Colorado, Nevada, Arizona, New Mexico, and into northern Mexico (Chihuahua, Sonora, etc.). It extends eastward across the Great Plains to the Great Lakes region (Illinois, Indiana, Missouri, etc.) with scattered disjunct populations as far as Ohio and Tennessee. Var. capitatum has the broadest distribution; some California varieties (e.g., var. angustatum) are narrowly endemic and endangered. It has been introduced in parts of New England. Overall, it is considered secure (NatureServe).

This adaptable species plays ecological roles as a nectar source for pollinators (including butterflies), larval host plant, and early colonizer of disturbed or post-fire sites. It also provides forage for wildlife such as elk, deer, bighorn sheep, and small mammals.

Other Names

  • Coast wallflower
  • Douglas’ wallflower
  • Sanddune wallflower
  • Prairie rocket

Resources