Hoover Dam

Hoover Damn Bypass seen from the top with Hoover Damn. Photo by James L Rathbun
Hoover Damn Bypass seen from the top with Hoover Damn. Photo by James L Rathbun

Hoover Dam (originally authorized as Boulder Dam or the Boulder Canyon Project) is a concrete arch-gravity dam in Black Canyon on the Colorado River, on the Arizona–Nevada border about 30 miles southeast of Las Vegas. Built between 1931 and 1936 during the Great Depression, it stands 726.4 feet high, stretches 1,244 feet along its crest, is 660 feet thick at the base and 45 feet at the crest, and contains about 3.25 million cubic yards of concrete (roughly 4.4 million cubic yards including appurtenant works). It creates Lake Mead, one of the largest reservoirs in the United States by capacity (historically around 28–32 million acre-feet depending on sedimentation surveys and measurement basis).

Why It Was Built

Hoover Dam takes shape from the concrete columns in which it was poured (shot from cableway control tower downstream on Nevada rim, so looking upstream)
Hoover Dam takes shape from the concrete columns in which it was poured (shot from cableway control tower downstream on Nevada rim, so looking upstream)

In the early 20th century, the Colorado River was both a vital resource and a destructive force for the arid Southwest. Seasonal floods devastated farmland (most dramatically in 1905–1907, when the river broke through irrigation canals and created the Salton Sea in California’s Imperial Valley), while dry periods left water supplies unreliable. Growing cities such as Los Angeles needed dependable municipal water, and the region sought hydroelectric power to support development.

The U.S. Bureau of Reclamation (then the Reclamation Service) saw a large multipurpose dam as the solution: flood control, irrigation water storage and delivery (including via the later All-American Canal to the Imperial and Coachella Valleys), municipal supply, river regulation, and hydropower. Power sales were intended to make the project self-supporting by repaying construction costs. Early advocates included Arthur Powell Davis of the Reclamation Service. Herbert Hoover, as Secretary of Commerce, strongly supported the project and helped resolve interstate water disputes.

A major political obstacle was allocating the river’s water among the seven basin states (Wyoming, Colorado, Utah, New Mexico, Arizona, Nevada, and California). Upper Basin states feared Lower Basin (especially California) development would claim most of the water under prior-appropriation rules. In 1922, Hoover chaired negotiations that produced the Colorado River Compact. It divided the basin at Lee Ferry, Arizona, allocating 7.5 million acre-feet annually to each basin (with the Lower Basin allowed an additional 1 million acre-feet under certain conditions) and requiring the Upper Basin not to deplete flows at Lee Ferry below 75 million acre-feet over any 10-year period. Arizona initially refused to ratify; the Compact became effective after six states approved it.

Photograph of the Hoover Dam (formerly Boulder Dam) from Across the Colorado River; From the series Ansel Adams Photographs of National Parks and Monuments, compiled 1941 - 1942, documenting the period ca. 1933 - 1942
Photograph of the Hoover Dam (formerly Boulder Dam) from Across the Colorado River; From the series Ansel Adams Photographs of National Parks and Monuments, compiled 1941 – 1942, documenting the period ca. 1933 – 1942

Congress authorized the project via the Boulder Canyon Project Act, signed by President Calvin Coolidge on December 21, 1928. The Act ratified the Compact (with California limited to 4.4 million acre-feet of the Lower Basin share), authorized the dam and related works (including the All-American Canal), and apportioned Lower Basin water roughly as California 4.4 million acre-feet, Arizona 2.8 million, and Nevada 0.3 million. President Hoover proclaimed the Compact effective in 1929. A later 1944 treaty allocated 1.5 million acre-feet annually to Mexico.

How the Site Was Chosen

Surveys of potential dam sites along the lower Colorado began in the early 1900s. The 1922 Fall-Davis Report recommended a high dam “at or near Boulder Canyon.” Boulder Canyon sites offered strong granite foundations but presented problems: one was crossed by a geologic fault; others were too narrow for construction camps or spillways; accessibility was poorer; and depth to bedrock was greater in places.

Further investigations (including the Weymouth Report) compared Boulder and nearby Black Canyon (about 20 miles downstream). Black Canyon was selected primarily for practical advantages: greater accessibility (a railroad spur could more easily connect from Las Vegas), shallower depth to solid bedrock in key locations, a narrower gorge with steeper walls, lower construction cost for a given height, and somewhat greater reservoir capacity for the same dam height. Geologic conditions were judged adequate (though Boulder’s granite was sometimes rated superior for load-bearing). The project retained the “Boulder Canyon” name even after the site shift. An independent Colorado River Board later confirmed the upper Black Canyon site.

The design chosen was a massive concrete arch-gravity dam (convex upstream face), developed under Bureau engineer John L. Savage and others. It transfers water pressure into the canyon walls while relying on its own weight for stability—an ultra-conservative approach after the 1928 St. Francis Dam failure raised safety concerns.

Construction

Six Companies, Inc. (a joint venture of major contractors including Utah Construction, Bechtel, Kaiser, Morrison-Knudsen, and others) won the contract in March 1931 with a bid of about $48.9 million—the largest U.S. government construction contract to that point. Work began in the spring of 1931 under Bureau construction engineer Walker Young and Six Companies superintendent Frank Crowe.

Key challenges included extreme desert heat, isolation, and the need to divert the entire river. Workers blasted four massive diversion tunnels (two on each side of the river, roughly 56 feet in diameter and totaling several miles in length) through the canyon walls. The river was diverted in November 1932. Cofferdams protected the site; the riverbed was excavated to solid rock; and canyon walls were scaled of loose rock. Concrete placement began June 6, 1933, and the last dam concrete was poured May 29, 1935. Cooling pipes embedded in the concrete controlled the heat of hydration so the massive structure would not crack. The dam began impounding water in February 1935, forming Lake Mead. Power generation started in late 1936. The project finished more than two years ahead of the seven-year contract schedule and was dedicated by President Franklin D. Roosevelt on September 30, 1935.

Roughly 21,000 people worked on the project at various times (peak employment over 5,000). Conditions were harsh; official figures record around 96–112 worker deaths from construction accidents (the exact total varies by counting method and whether indirect causes are included). Boulder City was built as a planned community for workers and their families. The dam was initially called Hoover Dam by the Hoover administration, renamed Boulder Dam under Roosevelt, and officially restored as Hoover Dam by Congress in 1947.

The Hoover Damn Bypass Bridge viewed from the Colorado River - Photo by James L Rathbun
The Hoover Damn Bypass Bridge viewed from the Colorado River – Photo by James L Rathbun

Hydropower revenues repaid the federal construction costs decades later. The powerplant (nameplate capacity roughly 2,080 MW after later uprates, with 17 main turbines) has historically supplied electricity to utilities in Arizona, Nevada, and California.

Current Struggles with Low Water

Lake Mead and the broader Colorado River system have been under severe stress from a multi-decade megadrought (intensified by climate change, higher temperatures, and increased evaporation), combined with chronic overuse relative to long-term average flows. The original Compact allocations assumed higher average river flows (around 16–17+ million acre-feet) than the observed long-term average (closer to 14–15 million acre-feet, and significantly lower in recent decades).

As of late August 2026, Lake Mead stood near record-low elevations for the modern period—approximately 1,038.87 feet, about 26% full (storage roughly 6.9 million acre-feet on a ~26 million acre-feet capacity basis used in some daily reporting). This is well below the full-pool elevation of about 1,220 feet and marks new lows relative to recent historical records (surpassing previous lows from 2022 in some metrics). Levels have continued a multi-year decline, with further drops expected until the next major snowmelt runoff.

Low water reduces hydropower generation because lower “head” (water pressure/height above the turbines) decreases output. Capacity falls sharply at lower elevations; generation has already been substantially reduced from historical averages, with further declines projected. Minimum power pool is around 950 feet (with some older turbines limited higher); dead pool (where water can no longer pass the dam by gravity) is about 895 feet. The reservoir remains above these critical thresholds but with a narrowing buffer.

Shortage declarations under existing guidelines have already triggered cuts in Lower Basin deliveries. Federal operating guidelines for 2027–2028 and the post-2026 framework emphasize protecting critical elevations at both Lake Mead and upstream Lake Powell (itself also near or at record lows). Measures include reduced releases from Powell to protect its infrastructure and power generation, mandatory and voluntary reductions in Lower Basin consumptive use (on the order of 1.25 million acre-feet annually plus additional conservation in early years of the new guidelines), and efforts to balance the system. Arizona faces particularly large percentage cuts under priority-based shortage sharing. Power production at Hoover is expected to remain constrained, raising costs for replacement energy and affecting ratepayers.

These challenges highlight the tension between the river’s engineered development (which enabled vast agricultural and urban growth in the Southwest) and the physical limits of a variable, arid basin under climate pressure. Ongoing negotiations among the basin states, tribes, Mexico, and the federal government focus on reducing overall use to match available supply while protecting critical infrastructure and ecosystems.

Hoover Dam remains an engineering landmark, a National Historic Landmark, and a major tourist destination, while continuing to serve its original purposes of flood control, water storage, and power generation—albeit under increasingly constrained hydrologic conditions.

Desert Gold Poppy (Eschscholzia glyptosperma)

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. It is a member of the poppy family and a smaller, desert-adapted relative of the more widespread California Poppy (Eschscholzia californica). This species is particularly notable for its vibrant blooms during spring “superbloom” events following adequate winter rainfall, when it can carpet desert washes and flats in golden hues.

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

Taxonomic Classification

  • Kingdom: Plantae
  • Clade: Tracheophytes (vascular plants)
  • Clade: Angiosperms (flowering plants)
  • Clade: Eudicots
  • Order: Ranunculales
  • Family: Papaveraceae (Poppy family)
  • Genus: Eschscholzia
  • Species: Eschscholzia glyptosperma Greene (described by botanist Edward Lee Greene)

The binomial name Eschscholzia glyptosperma reflects the genus honoring Estonian botanist Johann Friedrich von Eschscholtz and the species epithet referring to its sculptured or “engraved” seeds (glyptosperma). It is a strictly annual herb.

Plant and Flower Description

Eschscholzia glyptosperma is a small, scapose (mostly leafless-stemmed) annual herb. It grows from a basal rosette of finely dissected, pointed, grayish-green leaves that are 1–4 times pinnately divided into narrow, pointed segments— an adaptation that reduces water loss in harsh desert conditions. The plant typically reaches 5–25 cm (2–10 inches) in height, with one or more erect, slender stems arising from the base. Each stem bears a single flower atop a long peduncle.

Flower Morphology: The flowers are bright yellow (occasionally with a subtle orange tint), solitary, and actinomorphic (radially symmetrical). They feature four broad, satiny petals, each measuring approximately 1–2.5 cm (⅜–1 inch) long, giving the bloom a cup- or saucer-like appearance when fully open in sunlight. The petals are silky-textured and close at night or in cloudy/cold conditions (nyctinasty). There are typically two (sometimes three) sepals that are glabrous (smooth), often glaucous (waxy blue-green), and shed soon after the flower opens. The center displays numerous yellow stamens surrounding a single superior ovary. Flowers bloom primarily from February to May, peaking in March–April depending on rainfall and elevation.

The fruit is a slender, cylindrical capsule (4–8 cm long) that dehisces (splits) from the base when dry, explosively releasing numerous tiny, rounded, tan-to-brown seeds.

Range and Distribution

The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. - Photograph by James L Rathbun
The Desert Gold Poppy, also known as the Desert Golden Poppy or Mojave Poppy, is a striking annual wildflower native to the arid regions of the southwestern United States. – Photograph by James L Rathbun

The Desert Gold Poppy is endemic to the Mojave and Sonoran Deserts of the southwestern United States. Its distribution includes:

It occurs at elevations from near sea level (30 m / 98 ft) to approximately 1,600 m (5,249 ft). In suitable years, it contributes to spectacular desert wildflower displays.

Habitat and Ecology

This species thrives in desert washes, alluvial fans, dry streambeds, open flats, and gentle slopes within creosote bush scrub and Joshua tree woodland plant communities. It prefers well-drained, sandy or gravelly soils and sheltered microhabitats that protect against wind and extreme desiccation. As an annual, its population fluctuates dramatically with winter precipitation; it is a key component of “superbloom” events. The flowers provide nectar and pollen for native bees, butterflies, and other pollinators, while the foliage supports various caterpillars and the seeds are consumed by birds.

In summary, Eschscholzia glyptosperma exemplifies elegant desert adaptation—compact size, efficient water use, and brilliant, ephemeral blooms that signal the brief bounty of spring in the arid Southwest. Its presence in southern Nevada (including areas near Las Vegas) makes it a locally observable and ecologically important wildflower.

Colorado Steamships

The Colorado River, flowing from the Rocky Mountains through the arid Southwest to the Gulf of California, was a challenging waterway—shallow, swift, and prone to sandbars, floods, and shifting channels. Despite these obstacles, steam-powered vessels played a vital role in its navigation from the mid-19th century until the early 20th century. Primarily operating on the lower Colorado River (from the Gulf of California upstream to areas near modern-day Nevada), steamboats transported military supplies, miners, settlers, and freight, fueling the development of Arizona, California, Nevada, and parts of Mexico. They were the most economical means of moving goods across the desert until railroads supplanted them.

View showing steamboat Cochan on the Colorado River near Yuma, Arizona in 1900 - U.S. National Archives and Records Administration
View showing steamboat Cochan on the Colorado River near Yuma, Arizona in 1900 – U.S. National Archives and Records Administration

Early Attempts and the Birth of Steam Navigation (1850–1854)

The need for reliable transport arose after the Mexican-American War (1846–1848), when the U.S. Army established Fort Yuma at the confluence of the Gila and Colorado Rivers to protect emigrants heading to California during the Gold Rush. Supplying the isolated fort overland from San Diego cost up to $500 per ton. River transport from the Gulf of California offered a cheaper alternative.

Initial efforts used schooners and barges. In 1850–1851, the schooner Invincible and longboats reached only partway upriver. Lieutenant George Derby recommended shallow-draft sternwheel steamboats.

The first successful steamboat was the small iron-hulled Uncle Sam, a 65-foot tug with a 20-horsepower engine, assembled at the river’s mouth in 1852 by Captain James Turnbull. It reached Fort Yuma in December 1852 but later proved unreliable and sank.

In 1853–1854, George Alonzo Johnson, partnering with Benjamin M. Hartshorne and others, formed George A. Johnson & Company. They brought parts for the sidewheeler General Jesup from San Francisco, assembling it at the river mouth. The General Jesup carried 50 tons of cargo to Fort Yuma in five days, reducing costs to $75 per ton and proving commercial viability.

Mohave II at Yuma, Arizona, with Sunday school group embarked, 1876 - Unknown author - MacMullen, Jerry, Paddle-Wheel Days in California, Stanford University Press, 1944
Mohave II at Yuma, Arizona, with Sunday school group embarked, 1876 – Unknown author – MacMullen, Jerry, Paddle-Wheel Days in California, Stanford University Press, 1944

Expansion and Exploration (1855–1860s)

Johnson’s company built wood yards staffed by Cocopah Indians and added vessels like the sternwheeler Colorado (1855, captained by Isaac Polhamus) and others. By the late 1850s, steamboats regularly serviced Fort Yuma and emerging mining camps.

Exploration pushed limits:

  • In 1857, Johnson took the General Jesup to El Dorado Canyon (near Las Vegas).
  • The U.S. Army’s 1857–1858 expedition, led by Lt. Joseph Christmas Ives, used the 54-foot iron steamboat Explorer (built in Philadelphia and reassembled on the river). It reached Black Canyon but struck a rock; Ives deemed further navigation impractical at low water. Johnson later bought the Explorer and converted it to a barge.

Mormon leader Brigham Young sought a sea-to-Utah route via the Colorado. In 1864–1866, Anson Call established Callville (near modern Lake Mead) as a potential port. Steamboats like the Esmeralda reached it in 1866.

Boom Years: Mining Rushes and Competition (1860s–1870s)

The 1862 Colorado River gold rush near La Paz (Arizona) and later discoveries in Eldorado Canyon and elsewhere created explosive demand. Ports like Ehrenberg, Hardyville, and Aubrey emerged. Steamboats hauled machinery, food, and ore, often towing barges for extra capacity.

George A. Johnson & Company dominated initially but faced rivals like Thomas Trueworthy’s Union Line in the 1860s. Competition ended when Johnson’s company absorbed opponents. In 1869, it reorganized as the Colorado Steam Navigation Company (C.S.N.Co.), expanding the fleet with vessels like Cocopah, Mohave, and larger ones like the 149-foot Mohave II (1876) and Gila.

Key captains included Isaac Polhamus (“Dean of the Colorado River”) and later Jack Mellon. Ocean steamships connected San Francisco to the river mouth at Port Isabel, feeding river traffic.

Colorado II in a tidal dry dock in the shipyard above Port Isabel, Sonora - MacMullen, Jerry, Paddle-Wheel Days in California, Stanford University Press, 1944
Colorado II in a tidal dry dock in the shipyard above Port Isabel, Sonora – MacMullen, Jerry, Paddle-Wheel Days in California, Stanford University Press, 1944

Peak and Decline (1870s–1900s)

The 1870s marked the peak, with scheduled services and luxurious boats offering passenger excursions. The C.S.N.Co. monopolized trade, profiting immensely from military contracts, mining,, and Mormon supplies.

Railroads spelled doom. The Southern Pacific reached Yuma in 1877, bridging the river. That year, Johnson and partners sold the C.S.N.Co. to Southern Pacific interests for a massive profit. Steamboats continued but focused on upper reaches and local freight.

Later vessels included the Cochan (1900, the last major sternwheeler) and Searchlight (1903–1909), hauling ore from Nevada mines.

End of an Era (1909–1916)

The 1909 completion of Laguna Dam (for irrigation) blocked navigation. Final operations involved limited freight and dam-related work. The last commercial steamboat, Searchlight, retired around 1916.

Attempts on the upper Colorado (e.g., Glen Canyon, Green River) were short-lived due to rapids and low water.

Legacy

For over 50 years, Colorado River steamboats connected isolated frontiers, enabling settlement and extraction in a harsh desert. They carried millions in gold, supplied forts and mines, and linked the Pacific to inland territories. Though overshadowed by railroads and dams, their era transformed the Southwest, leaving behind ghost towns, historic sites like Yuma Quartermaster Depot, and a romantic chapter in Western transportation history.

Colorado River Steamship Landings

The steamboat Mohave departing the landing in El Dorado Canyon.
The steamboat Mohave departing the landing in El Dorado Canyon.
Potholes, California, From 185918 mi (29 km)
La Laguna, Arizona Territory, 1860-186320 mi (32 km)
Castle Dome Landing, Arizona Territory, 1863-188435 mi (56 km)
Eureka, Arizona Territory, 1863-1870s45 mi (72 km)
Williamsport, Arizona Territory, 1863-1870s47 mi (76 km)
Picacho, California, 1862-191048 mi (77 km)
Nortons Landing, Arizona Territory, 1882-189452 mi (84 km)
Clip, Arizona Territory, 1882-188870 mi (110 km)
California Camp, California72 mi (116 km)
Camp Gaston, California, 1859-186780 mi (130 km)
Drift Desert, Arizona Territory102 mi (164 km)
Bradshaw’s Ferry, California, 1862-1884126 mi (203 km)
Mineral City, Arizona Territory, 1864-1866126 mi (203 km)
Ehrenberg, Arizona Territory, from 1866126.5 mi (203.6 km)
Olive City, Arizona Territory, 1862-1866127 mi (204 km)
La Paz, Arizona Territory, 1862-1870131 mi (211 km)
Parker’s Landing, Arizona Territory, 1864-1905
Camp Colorado, Arizona, 1864-1869
200 mi (320 km)
Parker, Arizona Territory, from 1908203 mi (327 km)
Empire Flat, Arizona Territory, 1866-1905210 mi (340 km)
Bill Williams River, Arizona220 mi (350 km)
Aubrey City, Arizona Territory, 1862-1888220 mi (350 km)
Chimehuevis Landing, California240 mi (390 km)
Liverpool Landing, Arizona Territory242 mi (389 km)
Grand Turn, Arizona/California257 mi (414 km)
The Needles, Mohave Mountains, Arizona263 mi (423 km)
Mellen, Arizona Territory 1890 – 1909267 mi (430 km)
Eastbridge, Arizona Territory 1883 – 1890279 mi (449 km)
Needles, California, from 1883282 mi (454 km)
Iretaba City, Arizona Territory, 1864298 mi (480 km)
Fort Mohave, Arizona Territory, 1859-1890
Beale’s Crossing 1858 –
300 mi (480 km)
Mohave City, Arizona Territory, 1864-1869305 mi (491 km)
Hardyville, Arizona Territory, 1864-1893
Low Water Head of Navigation 1864-1881
310 mi (500 km)
Camp Alexander, Arizona Territory, 1867312 mi (502 km)
Polhamus Landing, Arizona Territory
Low Water Head of Navigation 1881-1882
315 mi (507 km)
Pyramid Canyon, Arizona/Nevada316 mi (509 km)
Cottonwood Island, Nevada
Cottonwood Valley
339 mi (546 km)
Quartette, Nevada, 1900-1906342 mi (550 km)
Murphyville, Arizona Territory, 1891353 mi (568 km)
Eldorado Canyon, Nevada, 1857-1905
Colorado City, Nevada 1861-1905
365 mi (587 km)
Explorer’s Rock, Black Canyon of the Colorado, Mouth, Arizona/Nevada369 mi (594 km)
Roaring Rapids, Black Canyon of the Colorado, Arizona/Nevada375 mi (604 km)
Ringbolt Rapids, Black Canyon of the Colorado, Arizona/Nevada387 mi (623 km)
Fortification Rock, Nevada
High Water Head of Navigation, 1858-1866
400 mi (640 km)
Las Vegas Wash, Nevada402 mi (647 km)
Callville, Nevada, 1864-1869
High Water Head of Navigation 1866-78
408 mi (657 km)
Boulder Canyon, Mouth, Arizona/Nevada409 mi (658 km)
Stone’s Ferry, Nevada 1866-1876438 mi (705 km)
Virgin River, Nevada440 mi (710 km)
Bonelli’s Ferry, 1876-1935
Rioville, Nevada 1869-1906
High Water Head of Navigation from 1879 to 1887
440 mi (710 km
Soruce: Wikipedia

Colorado River Steamship Landings

Steamboats on the Colorado River

Gila Steamboat at the Yuma Crossing Arizona, 1873.
Gila Steamboat at the Yuma Crossing Arizona, 1873.
NameTypeTonsLengthBeamLaunchedDisposition
Black EagleScrew40 feet6 feetGreen River, Utah
June 1907
Exploded 1907
Charles H. SpencerStern92.5 feet25 feetWarm Creek, Arizona
February 1912
Abandoned
Spring 1912
Cliff DwellerStern70 feet20 feetHalverson’s Utah
November 1905
To Salt Lake
April 1907
CochanStern234135 feet31 feetYuma, Arizona
November 1899
Dismantled
Spring 1910
Cocopah IStern140 feet29 feetGridiron, Mexico
August 1859
Dismantled
1867
Cocopah IIStern231147.5 feet28 feetYuma, Arizona
March 1867
Dismantled
1881
Colorado IStern120 feetEstuary, Mexico
December 1855
Dismantled
August 1862
Colorado IIStern179145 feet29 feetYuma, Arizona
May 1862
Dismantled
August 1882
CometStern60 feet20 feetGreen River, Wyoming
July 1908
Abandoned
1908
EsmeraldaStern93 feet13 feetRobinson’s, Mexico
December 1857
Dismantled
1868
General JesupSide104 feet17 feetEstuary, Mexico
January, 1864
Engine Removed
1858
General RosalesSternYuma, Arizona
July 1878
Dismantled
1859
GilaStern236149 feet31 feetPort Isabel, Mexico
January 1873
Rebuilt as Cochan
1889
Major PowellScrew35 feet8 feetGreen River, Utah
August 1891
Dismantled
1894
Mohave IStern193135 feet28 feetEstuary, Mexico
May 1864
Dismantled
1875
Mohave IIStern188149.5 feet31.5 feetPort Isabel, Mexico
February 1876
Dismantled
Jan 1900
Nina TildenStern12097 feet22 feetSan Francisco, California
July 1864
Wrecked
September 1874
RettaStern36 feet6 feetYuma, Arizona
1900
Sunk
Feburary, 1905
St. VallierStern9274 feet17 feetNeedles, California
Early 1899
Sunk
March 1909
San JorgeScrew38 feet9 feetYuma, Arizona
June 1901
To Gulf
July 1901
SearchlightStern9891 feet18feetNeedles, California
December 1902
Lost
October 1916
Uncle SamSide4065 feet16 feetEstuary, Mexico
November 1852
Sunk
May 1853
UndineStern60 feet10 feetGreen River, Utah
November 1901
Wrecked
May 1902
Steamboats on the Colorado River 1852-1916 – Appendix A

Resources

Cerbat Arizona – Mohave County Ghost Town

Cerbat is a historic mining camp and former town located in the Cerbat Mountains of Mohave County, northwestern Arizona, approximately 9-15 miles northwest of present-day Kingman. Nestled in a rugged canyon west of the main Cerbat Mountain range, the site sits at an elevation of around 4,580 feet. The name “Cerbat” derives from a Native American term meaning “Big Horn mountain sheep,” reflecting the wildlife once abundant in the area.

The town’s origins trace back to the late 1860s, when prospectors discovered rich deposits of gold and silver in the Cerbat Mountains. Following initial finds, mining camps quickly emerged, with Cerbat established around key claims including the Esmeralda, Golden Gem, Vanderbilt, Idaho, Flores, Night Hawk, and Big Bethel mines. By 1870-1871, a small settlement had formed, supported by a mill, smelter, stores, saloons, a school, a post office (opened December 23, 1872), and professional services such as a doctor’s office and a lawyer’s office. Cabins housed over 100 residents at its peak, making it a modest but prosperous frontier community isolated in the harsh desert terrain.

Cerbat Arizona in 1870
Cerbat Arizona in 1870

Boom Period and Significance (1870s-1880s)

Cerbat’s early growth was fueled by the broader mining boom in Mohave County, which began with gold discoveries along the Colorado River in the 1860s. Prospectors often arrived via steamboat to Hardyville (now part of Bullhead City), then trekked inland 38 miles to the Cerbat area. The town’s remote location necessitated infrastructure improvements: in 1872, a $6,000 dirt road was constructed over the mountains to connect Cerbat to eastern settlements like Fort Rock, Camp Hualapai, Williamson Valley, and Prescott.

In 1871, Cerbat briefly achieved prominence as the third county seat of Mohave County, building the county’s first permanent court house. However, it lost this status in 1873 (some sources cite 1877) to the nearby rival mining town of Mineral Park. Despite this, Cerbat remained active, with stage lines like the California and Arizona Stage Company providing weekly service in the 1880s, linking it to Mineral Park, Chloride, Prescott, and Hardyville via toll roads.

The surrounding Wallapai Mining District (encompassing Cerbat, Chloride, Mineral Park, and Stockton Hill) produced significant gold, silver, lead, zinc, and later turquoise. Cerbat’s mines contributed substantially, with the Golden Gem alone yielding around $400,000 in precious metals between 1871 and 1907.

Life in Cerbat reflected the turbulent Old West: conflicts with local Hualapai and other Native American groups led to miner deaths, while internal violence included murders, suicides, and at least one legal hanging (carpenter Michael DeHay in 1876 for killing his wife). The town’s pioneer cemetery preserves graves reflecting these hardships, including victims of mining accidents, disease (e.g., tuberculosis), and insanity-related incidents.

Decline and Abandonment (Late 19th to Early 20th Century)

Cerbat’s prosperity waned as richer deposits were exhausted or eclipsed by nearby camps. The post office, a key indicator of viability, operated until June 15, 1912 (with a brief name change to “Campbell” from 1890-1902). By the early 20th century, residents drifted away, and the town faded into obscurity. Sporadic mining continued in the district into the 20th century, but Cerbat itself never recovered.

Current Status

Cerbat is classified as a classic Arizona ghost town—uninhabited and abandoned, with no permanent residents. The site consists primarily of scattered ruins: faint stone foundations, crumbling walls, old mine shafts, tailings piles, and remnants of buildings overgrown by desert vegetation. A semi-modern warehouse and large steel safe from later eras remain, along with an active ranch at the canyon’s base. The pioneer cemetery is one of the better-preserved features, accessible for historical visits.

Access is via dirt roads off U.S. Highway 93 north of Kingman (near Milepost 62), requiring high-clearance or four-wheel-drive vehicles for the final stretches, especially after rain. The area falls within public lands managed in part by the Bureau of Land Management, and nearby modern mining operations (e.g., at Mineral Park) have altered parts of the landscape with large open pits.

Cerbat attracts ghost town enthusiasts, hikers, and off-road explorers seeking remnants of Arizona’s mining heritage. It is not commercialized like some sites (e.g., no tours or facilities), emphasizing its raw, desolate character. The broader Cerbat Mountains remain notable for wild Cerbat mustangs (a protected feral herd of possible Spanish descent) and ongoing mineral exploration, but the town itself stands as a silent testament to the boom-and-bust cycles of the American West.

Town Summary

NameCerbat
LocationMohave County, Arizona
Latitude, Longitude35.303413,-114.1380277
GNS24353
Elevation3,872 Feet
Population100
Post OfficeDecember 23, 1872 – June 15, 1912
Alternate NamesCampbell (June 25, 1890 to October 24 1902 )

Cerbat Trail Map

References

Chloride Arizona

Chloride Arizona is the oldest continuously inhabited Silver Mining town located in Mohave County, Arizona. The name derives its named from Silver Chloride (AgCl) which is found in abundance in the local Cerbet mountains.

1916 Chloride Main Street. Arizona.
1916 Chloride Main Street. Arizona.

Chloride’s modern history began in the late 19th century when prospectors, drawn by rumors of silver and other valuable minerals, began to explore the nearby hills and canyons. In 1863, a prospector named John Moss struck silver in the area, leading to a flurry of activity as more miners and settlers arrived. The first official post office was established in 1866, and Chloride was officially born.

Chloride experienced rapid growth during the late 1800s as mines produced substantial amounts of silver, lead, zinc, and other valuable minerals. The town’s population swelled. Businesses, saloons, and other establishments sprung up to cater to the needs of the growing community. At its peak, Chloride boasted a theater, several hotels, and a bustling main street.

Chloride Arizona and part of the Cerbat Range, looking easy from Silver Hill,  with Tennessee Avenue in the foreground - 1906- Photo U.S. Geological Survey
Chloride and part of the Cerbat Range, looking easy from Silver Hill, with Tennessee Avenue in the foreground. 1906 – Photo U.S. Geological Survey

However, like many mining towns of the era, Chloride’s prosperity was short-lived. Fluctuating metal prices, mine closures, and the depletion of easily accessible minerals led to a decline in the town’s fortunes. By the early 20th century, Chloride entered a period of decline. Much of its population began to dwindle as residents sought opportunities elsewhere.

Despite the challenges, some residents remained in Chloride, and the town managed to maintain a semblance of its former self. The 20th century saw the rise of tourism as visitors were drawn to Chloride’s picturesque desert landscapes, historical buildings, and remnants of its mining heritage. Efforts to preserve the town’s history led to the restoration of several historic structures, including the Monte Cristo Saloon. The saloon proudly claims to be Arizona’s oldest continuously operating bar.

Modern Relevance

In recent decades, Chloride has experienced a revival fueled by a mix of nostalgia, artistic expression, and a desire to escape the hustle and bustle of city life. The town has attracted a diverse group of residents, including artists, retirees, and those seeking a slower pace of life.

One of Chloride’s most unique and captivating features is the open-air Chloride Murals project. In the early 1960s by local artist Roy Purcell, this project has transformed the town into a vibrant canvas. Murals depicting scenes from Chloride’s history, Native American culture, and the American West decorate the sides of buildings and rock formations.

Chloride Arizona Town Summary

NameChloride, Arizona
LocationMohave County, Arizona
Latitude, Longitude35.4047, -114.1812
Elevation4,022 ft (1,226 m)
GNIS2882
Population229
Max Population2000

Trail Map

References