|Date||December 1861 – January 1862|
|Location||Oregon, Nevada, California, Idaho, Arizona, Idaho, New Mexico, Sonora, Mexico|
The Great Flood of 1862 was the largest flood in the recorded history of Oregon, Nevada, and California, occurring from December 1861 to January 1862. It was preceded by weeks of continuous rains and snows in the very high elevations that began in Oregon in November 1861 and continued into January 1862. This was followed by a record amount of rain from January 9–12, and contributed to a flood that extended from the Columbia River southward in western Oregon, and through California to San Diego, and extended as far inland as Idaho in the Washington Territory, Nevada and Utah in the Utah Territory, and Arizona in the western New Mexico Territory. Immense snowfalls in the mountains of the far western United States caused more flooding in Idaho, Arizona, New Mexico, and Sonora, Mexico the following spring and summer as the snow melted.
The event was capped by a warm intense storm that melted the high snow load. The resulting snow-melt flooded valleys, inundated or swept away towns, mills, dams, flumes, houses, fences, and domestic animals, and ruined fields. It has been described as the worst disaster ever to strike California. 
- 1 Background
- 2 Impact by region
- 3 Current interest
- 4 See also
- 5 References
- 6 Further reading
- 7 External links
The weather pattern that caused this flood was not from an El Niño type event, and from the existing Army and private weather records, it has been determined that the polar jet stream was to the north as the Pacific Northwest experienced a mild rainy pattern for the first half of December 1861. In 2012, hydrologists and meteorologists concluded that the precipitation was likely caused by a series of atmospheric rivers that hit the Western United States along the entire West Coast, from Oregon to Southern California. 
An atmospheric river is a wind-borne, deep layer of water vapor with origins in the tropics, extending from the surface to high altitudes, often above 10,000 feet, and concentrated into a relatively narrow band, typically about 400 to 600 kilometres (250 to 370 mi) wide, usually running ahead of a frontal boundary, or merging into it.   With the right dynamics in place to provide lift, an atmospheric river can produce astonishing amounts of precipitation, especially if it stalls over the same area for any length of time.
Prior to the flooding, Oregon had steady but heavier than normal rainfall during November and heavier snow in the mountains. :76–83 Researchers believe the jet stream slid south accompanied by freezing conditions reported at Oregon stations by December 25. Heavy rainfall began falling in California as the longwave trough moved down over the state, remaining there until the end of January 1862 and causing precipitation everywhere in the state for nearly 40 days. Eventually the trough moved even further south, causing snow to fall in the Central Valley and surrounding mountain ranges. 
There was an excessive amount of precipitation in November 1861 over most of Oregon, less so in the extreme northwest. It was cold enough at the higher elevations that much snow fell in the Cascade Range, which, when later melted by the warm rains produced a great quantity of water that flooded into the Willamette River and other streams in the Cascades. Tributaries of the Willamette rising in the Oregon Coast Range did not rise so high. Then the depression that came in at the beginning of December produced strong, warm southerly winds in Oregon, with extremely heavy rain. The crest of the flood was reached at Salem on December 3; at Oregon City on the 4th; at Milwaukie, between Oregon City and Portland, on the 5th; at Albany on December 8, a second rise at Albany greater than the first. The crest at Albany and Salem were the highest ever known at any time. In Oregon, the flood was one of the largest in the history of the Willamette Valley and the rest of Western Oregon. Flooding was heaviest on rivers with tributaries arising from the snow-covered Cascade Range. 
An article in the December 14, 1861, Oregon City Argus, described the course of the flood at Oregon City:
During the month of November the rain had been falling almost continuously, and a vast amount of snow must have accumulated in the mountains...
Tuesday evening a gloom settled on a scene such as probably never was witnessed in our Valley before. The ceaseless roar of the stream made a fearful elemental music widely different from the ordinary monotone of the Falls; while the darkness was only made more visible by the glare of torches and hurrying lights, which with the shouts of people from the windows of houses surrounded by the water, all conspired to render the hour one of intense and painful excitement. The flood has covered the highest mark of January '53, and is still rapidly rising. As late as anything could be seen the mills were still standing, but the insatiate monster is still creeping up inch by inch, winding its swelling folds round the pillars and foundations of all the houses in its way, crushing and grinding them in the maw of destruction, and sweeping the broken fragments into a common vortex of ruin. All night as on the night previous, people whose homes were being invaded hurried to places of security, glad to escape even with the sacrifice of all their goods.
The light of Wednesday morning revealed a scene of desolation terrible in its extent no less than in its completeness. The Oregon City and Island Mills, Willamette Iron Works, Foundry and Machine Shop were all gone... :76–77
Flood waters were so high that at Oregon City at the flood's crest on December 5, the steamer St. Clair was able to run the falls, and steamers were able to visit points at some distance from the normal river channel. Although large amounts of wheat and flour were swept away, some was recovered when Oregon City's Island Mill was found on Sauvie Island downriver from Portland. The nearby town of Linn City was completely destroyed by flooding and was not rebuilt.  In addition, the flood destroyed the historic town of Champoeg, site of the first provisional government in Oregon, and Orleans, across the Willamette River from Corvallis. Neither was rebuilt. :78
The flooding was also severe in other parts of Oregon; the Umpqua River had the greatest flood known even to the oldest Native Americans, and water was 10 to 15 feet (3.0 to 4.6 m) higher than the 1853 flood. It rose from November 3 to December 3, subsided for two days, then rose again until the 9th. At Fort Umpqua, communication upriver was cut off above Scottsburg, and the river was full of floating houses, barns, rails and produce. The Coquille River swept away settlers' property and there was also great damage on the Rogue River and on other small streams." :78–79
Flood damage was so great because the rivers in Oregon were the main routes of travel. The river front was the building site of mills, freight depots, and storehouses for grain and other foodstuffs. Business houses and many residences were near the landings. Farm buildings were mostly on sites convenient to the rivers, along with supplies of feed for livestock. Loss of so much wheat flour and demand from the new Idaho gold fields caused a spike in its price from $7 to $12 per barrel.
In the interior of Washington Territory, in what is now Idaho, the storm creating the flood in Oregon dumped its precipitation as an unprecedented snowfall. Flooding on the Columbia River and the snow in the mountains closed off supplies to the new mining towns on the Salmon River, causing starvation among the miners of Florence, cut off from December until May 1862. In early July, as the heavy burden of snow in the mountains melted, the runoff caused great flooding. The Boise River flooded from extremely high runoff and is believed to have been four times larger than its largest recorded flood in 1943. Flood waters made the river expand to a couple of miles wide.  It washed away or covered the original route of the Oregon Trail in the river valley. 
California was hit by a combination of incessant rain, snow, and then unseasonally high temperatures. In Northern California, it snowed heavily during the later part of November and the first few days of December, when the temperature rose unusually high, until it began to rain. There were four distinct rainy periods: The first occurred on December 9, 1861, the second on December 23–28, the third on January 9–12, and the fourth on January 15–17.  Native Americans knew that the Sacramento Valley could become an inland sea when the rains came. Their storytellers described water filling the valley from the Coast Range to the Sierra. 
Fort Ter-Waw, located in Klamath Glen, California, was destroyed by the flood in December 1861 and abandoned on June 10, 1862.  Bridges were washed away in Trinity and Shasta counties.  At Red Dog in Nevada County, William Begole reported that from December 23 to January 22 it rained a total of 25.5 inches (65 cm), and on January 10 and 11 alone, it rained over 11 inches (28 cm). 
At Weaverville, John Carr was a witness to the sudden melt of snow by the heavy rain and onset of the flood in December 1861 on the Trinity River:
From November until the latter part of March there was a succession of storms and floods... The ground was covered with snow 1 foot (0.30 m) deep, and on the mountains much deeper... The water in the river ... seemed like some mighty uncontrollable monster of destruction broken away from its bonds, rushing uncontrollably on, and everywhere carrying ruin and destruction in its course. When rising, the river seemed highest in the middle... From the head settlement to the mouth of the Trinity River, for a distance of one hundred and fifty miles, everything was swept to destruction. Not a bridge was left, or a mining-wheel or a sluce-box. Parts of ranches and miners cabins met the same fate. The labor of hundreds of men, and their savings of years, invested in bridges, mines and ranches, were all swept away. In forty-eight hours the valley of the Trinity was left desolate. The county never recovered from that disastrous flood. Many of the mining-wheels and bridges were never rebuilt. 
The floods of two years ago brought down an immense amount of driftwood from all the rivers along the coast, and it was cast up along this part of the coast in quantities that stagger belief. It looked to me as if I saw enough in ten miles along the shore to make a million cords of wood.... One I measured was 210 feet long and 3 1/2 feet at the little end, without the bark. :495
The entire Sacramento and San Joaquin valleys were inundated. An area about 300 miles (480 km) long, averaging 20 miles (32 km) in width,  and covering 5,000 to 6,000 square miles (13,000 to 16,000 km2) was under water.  The water flooding the Central Valley reached depths up to 30 feet (9.1 m), completely submerging telegraph poles that had just been installed between San Francisco and New York. Transportation, mail, and communications across the state were disrupted for a month.  Water covered portions of the valley from December 1861, through the spring, and into the summer of 1862. 
The rainy season commenced on the 8th of November, and for four weeks, with scarcely any intermission, the rain continued to fall very gently in San Francisco, but in heavy showers in the interior. According to the statement of a Grass Valley paper, nine inches of rain fell there in thirty-six hours on the 7th and 8th inst.... the next day the river-beds were full almost to the hilltops. The North Fork of the American River at Auburn rose thirty-five feet, and in many other mountain streams the rise was almost as great. On the 9th the flood reached the low land of the Sacramento Valley. 
In Knight's Ferry, in the foothills of the Sierra Nevada astride the Stanislaus River, about 40 miles (64 km) east of Modesto, the town's homes, its mill, and most of its businesses were ruined by the flood. The bridge spanning the river initially withstood the flood waters but was destroyed when the debris of the bridge at Two-Mile Bar, only a short distance up river, torn from its foundation, crashed into the Knights Ferry Bridge, crushing the truss supports and knocking it from its rock foundation.  All Sacramento, excepting one street, part of Marysville, part of Santa Rosa, part of Auburn, part of Sonora, part of Nevada City, and part of Napa were under water.  Some smaller towns like Empire City and Mokelumne City were entirely destroyed.
Sacramento, sited at the junction of the Sacramento and American Rivers, was originally built at 16 feet (4.9 m) above low-water mark, and the river usually rose 17 to 18 feet (5.2 to 5.5 m) almost every year. The New York Times reported on January 21, 1862 that a trapper who had spent more than 20 years in California had frequently boated over the city's site, and in 1846, the water at the location was 7 feet (2.1 m) deep for sixty days.  On 27 December 1861, the Sacramento River reached a flood level of 22 feet 7 inches (6.88 m) above the low water mark, after rising 10 feet (3.0 m) during the past 24 hours. 
The city of Sacramento suffered the worst damage due to its levee, which lay in a wide and flat valley at the junction of the American and Sacramento rivers. When the floodwaters entered from the higher ground on the east, the levee acted as a dam to keep the water in the city rather than let it flow out. Soon the water level was 10 feet (3.0 m) higher inside than the level of the Sacramento River on the outside. 
John Carr wrote of his riverboat trip up the Sacramento River when it was at one of its highest stages of flood:
... I was a passenger on the old steamer Gem, from Sacramento to Red Bluff. The only way the pilot could tell where the channel of the river was, was by the cottonwood trees on each side of the river. The boat had to stop several times and take men out of the tops of trees and off the roofs of houses. In our trip up the river we met property of every description floating down—dead horses and cattle, sheep, hogs, houses, haystacks, household furniture, and everything imaginable was on its way for the ocean. Arriving at Red Bluff, there was water everywhere as far as the eye could reach, and what few bridges there had been in the country were all swept away. 
Dozens of wood houses, some two stories high, were simply lifted up and carried off by the flood, as was "all the firewood, most of the fences and sheds, all the poultry, cats, rats and many of the cows and horses". The Chinese in their poorly built shantytowns were disproportionately affected. 
A chain gang was sent to break open the levee, which, when it finally broke, allowed the waters to rush out of the city center and lowered the level of the flooding by 5–6 feet (1.5–1.8 m). Eventually the waters fell to a level on a par with the lowest part of the city.  From January 23, 1862, the state capital was moved from flooded Sacramento to San Francisco. 
In Southern California, beginning on December 24, 1861, it rained for 28 days in Los Angeles. :243 In the San Gabriel Mountains the mining town of Eldoradoville was washed away by flood waters.  The flooding drowned thousands of cattle and washed away fruit trees and vineyards that grew along the Los Angeles River. No mail was received at Los Angeles for five weeks. The Los Angeles Star reported that:
The road from Tejon, we hear, has been almost washed away. The San Fernando mountain cannot be crossed except by the old trail ... over the top of the mountain. The plain has been cut up into gulches and arroyos, and streams are rushing down every declivity. 
The plains of Los Angeles County, at the time a marshy area with many small lakes and several meandering streams from the mountains, were extensively flooded, and much of the agricultural development that lay along the rivers was ruined. In most of the lower areas, small settlements were submerged. These flooded areas formed into a large lake system with many small streams. A few more powerful currents cut channels across the plain and carried the runoff to the sea.
In Los Angeles County, (including what is now Orange County) the flooding Santa Ana River created an inland sea lasting about three weeks with water standing 4 feet (1.2 m) deep up to 4 miles (6 km) from the river.  In February 1862, the Los Angeles, San Gabriel, and Santa Ana Rivers merged. Government surveys at the time indicated that a solid expanse of water covered the area from Signal Hill to Huntington Beach, a distance of approximately 18 miles (29 km). :38
At Santa Barbara County, the narrow coastal plains were flooded by the rivers coming out of the mountains. The San Buenaventura Mission Aqueduct that was still drawing water from a tributary of the Ventura River for the town of Ventura water system, was abandoned due to the damage in the area that become the separate Ventura County in 1873. 
In San Bernardino County, all the fertile riverside fields and all but the church and one house of the New Mexican colony of Agua Mansa, were swept away by the Santa Ana River, which overflowed its banks. Father Borgotta ringing the church bell on the night of January 22, 1862, alerted the inhabitants to the approach of the flood, and all escaped. 
In San Diego, a storm at sea backed up the flood water running into the bay from the San Diego River, resulting in a new river channel cut into San Diego Harbor. The continuous heavy downpour also changed the look of the land, the previously rounded hills were extensively cut by gulleys and canyons. 
To the north, in the Owens Valley, similar snow and flooding conditions as those to the east in Aurora, Nevada (see below), led to the local Paiute suffering the loss of much of the game they depended on. Cattle newly driven into the valley to feed the miners, competed with the native grazers and ate the native wild plant crops the Paiute depended on to survive. Starving, the Paiute began to kill the cattle and conflict with the cattlemen began, leading to the subsequent Owens Valley Indian War.
On March 1862, the Wool Growers Association reported that 100,000 sheep and 500,000 lambs were killed by the floods. Even oyster beds in San Francisco Bay near Oakland were reported to be dying from the effects of the immense amounts of freshwater entering the bay. Full of sediment, it covered the oyster beds.  One-quarter of California's estimated 800,000 cattle were killed by the flood, accelerating the end of the cattle-based ranchero society. One-fourth  to one-third of the state’s property was destroyed, and one home in eight was carried away or ruined by the flood-waters.  Mining equipment such as sluices, flumes, wheels and derricks were carried away across the state. 
An early estimate of property damage was $10 million.  However, later it was estimated that approximately one-quarter of the taxable real estate in the state of California was destroyed in the flood.  The state almost had to declare bankruptcy due to the costs of the damage and the loss of tax revenue. 
The Carson River Basin of the eastern California and western Utah Territory (now Nevada), suffered from a similar pattern of flooding. Flooding began in December 1861 in Carson Valley from a series of storms in the upper Carson River basin. Two feet (61 cm) of wet heavy snow fell on December 20, 1861, accumulating on the valley floor. Snow was followed by a period of very cold temperatures which froze the snow, followed by a three-day rain starting on December 25, 1861. By January 2, 1862, the town of Dayton and the area surrounding it had been flooded. 
In the vicinity of Aurora, there had been light snowfall in November, then mild weather until Christmas Eve, when there began a heavy and rapid snowfall for days. The temperature dropped below zero and the passes over the Sierras were closed. During the second week of January, it warmed slightly, and the snow became a torrential rain. Esmerelda and Willow gulches overflowed their banks and flooded Aurora. With water standing up to 3 inches (76 mm) deep in many buildings, adobe buildings turned to mud and collapsed. After a week, it cooled again, and snow began to fall again. Within a few days, the snow was deeper than it had been before the rains had begun to fall. Samuel Young of Aurora recorded in his diary that the snow and rain had fallen for 26 days out of 30 since December 24, 1861. 
The early southwestern Utah settlements in Washington County: Fort Clara, St. George, Grafton, Duncans Retreat, Adventure, and Northrop were nearly destroyed by a flood on the Virgin and Santa Clara Rivers, that followed 44 days of rainfall in January and February 1862.  Survivors of Fort Clara established the modern town of Santa Clara a mile east of the old fort on the Santa Clara River.  Springdale and Rockville were founded in 1862 by settlers flooded out of Adventure, Northup and other places in the vicinity. 
Settlers were driven from Fort Harmony when the fort had to be abandoned after most of its adobe walls were washed away during this flood. New Harmony and Kanarraville, in Iron County, were the settlements created by refugees from this disaster later in 1862. :174
In western New Mexico Territory, heavy rains fell in late January, causing severe flooding of the Colorado River and Gila River. On January 20, 1862, the Colorado River began to rise, and on the afternoon of January 22 it rose suddenly in three hours from an already high stage nearly 6 feet (1.8 m), overflowing its banks and turned Fort Yuma in California into an island in the midst of the Colorado River. At 1 o’clock on the morning of January 23, the river reached its crest.  Jaeger City a mile down river from Fort Yuma, and Colorado City, across the Colorado River from it were washed away. The river overflowed its banks to the extent that there was water 20 feet (6.1 m) deep on a ranch in the low-lying ground just above Arizona City where the Gila River joined the Colorado. The riverside home of steamboat entrepreneur George Alonzo Johnson and the nearby Hooper residence were the only places in the town unharmed because they were built on high ground.  Colorado City had to be rebuilt on higher ground after the 1862 flood. 
The Gila River also flooded, covering its whole valley at its mouth where it met the Colorado from the sand hills on the south to the foothills on the north. Twenty miles (32 km) to the east of Fort Yuma, it swept away most of the mining boomtown of Gila City along with a supply of hay being gathered there to supply the planned advance of the California Column into Confederate Arizona. Further east the road was flooded, buildings and vehicles swept away and traffic was disrupted for some time thereafter by the mud covering the road to Tucson.  The great flood in the Gila and Colorado rivers, covered their bottom lands with mud. Much of the livestock along the rivers drowned and the crops of the Indians along the river were destroyed. 
The overflow of the 1862 Colorado River spring flood waters reached the Salton Sink via the Alamo and New Rivers, filling it and creating a lake some 60 miles (97 km) long and 30 miles (48 km) wide. 
The great snow pack laid down during the winter of 1861–62, in the southern Rocky Mountains, and other ranges, the sources of the Rio Grande, caused a great spring flood in that river that changed its course in the Mesilla Valley. The flood also impeded the operations of the California Column attempting to cut off the retreating Confederate Army of New Mexico. On July 8, 1862, Lt. Col. Edward E. Eyre, First California Volunteer Cavalry wrote:
The Rio Grande has been unusually high this summer, almost the entire bottom between Fort Craig and Mesilla being still overflowed. It is impossible at this time to approach Mesilla on the west side of the river, a new channel having been washed out on that side of the town, through which the largest portion of the water flows; besides, the bottom for a long distance is overflowed, and, the soil being of a loose nature, animals mire down in attempting to get through it. 
Instead of crossing at Messilla, the high waters and course change forced Eyers detachment to cross the Rio Grande, up river at the old San Diego Crossing below Fort Thorn, after waiting another week for the water to go down, which allowed the rearguard of the Confederate Army to escape into Texas. Messilla, built on the west bank of the Rio Grande after the Mexican–American War, was left by the movement of the river on its east bank where it remains today.
Until the Great Flood of 1862, what became Port Isabel Slough, in Sonora, Mexico, was a shallow tidewater slough, but the extreme flood waters of that year cut its channel much deeper, so that at low tide it still was three fathoms deep. The mouth of this slough was only 5 miles (8.0 km) from the mouth of the river and sheltered from the extremes of the tidal bore of the Colorado River and deep enough to prevent stranding on shoals or mud flats at low tide.  This made it an ideal anchorage for maritime craft to load and unload their cargo and passengers from the steamboats that took them up and down river without the danger from the tides that they were having to risk in the estuary at Robinson's Landing.
In the month of March 1865, the schooner Isabel, from San Francisco, commanded by W. H. Pierson, found and entered this slough and discharged her cargo there for the first time. Subsequently, the steamers, sailing ships and later ocean-going steamships loaded and off-loaded their cargoes there, and the steamboat company established Port Isabel 2.5 miles (4.0 km) above the mouth of the slough. The port lasted until 1878. After the Southern Pacific Railroad reached Yuma, it was abandoned the following year, the shipyard there being removed to Yuma. 
The storm is not an isolated occurrence. Geologic evidence has been found that massive floods, caused by rainfall alone, have occurred in California every 100 to 200 years.  The flood has been studied by the United States Geological Survey and emergency planners, who use it as an example when modelling the impact of a similar event happening in modern-day California. The official name for such an event is " The ARkStorm", and it is unofficially called "The other big one".  
- List of floods
- Floods in the United States before 1901
- List of natural disasters in the United States
- Becker, Rachel (May 26, 2018). "The hardest part of preparing for disasters is overcoming human nature". The Verge. Retrieved May 29, 2018.
- "Dave Reynolds Recognized at 2012 California Extreme Precipitation Symposium". Earth System Research Laboratory, NOAA. August 10, 2012. Retrieved 1 March 2016.
- Ingram, B. Lynn (19 January 2013). "California Megaflood: Lessons from a Forgotten Catastrophe". Scientific American. Retrieved 10 April 2013.
- "Atmospheric River Information Page". Earth System Research Laboratory, NOAA. Retrieved 1 March 2016.
- Lansing Wells, Edward (1947). "Notes on the Winter of 1861–2 in the Pacific Northwest" (PDF). Northwest Science. 21. Archived from the original (PDF) on June 10, 2011.
- Null, Jan; Hulbert, Joelle (January–February 2007). "California Washed Away: The great flood of 1862" (PDF). Weatherwise. p. 29. Retrieved 3 October 2010.
- Thomas, Mike. "Linn City, Oregon: A Victim of Nature's Wrath". Bureau of Land Management. Archived from the original on September 30, 2016. Retrieved June 1, 2011.
- Ada County Hazard Vulnerability Analysis 2010, p. 34
- "Route of the Oregon Trail In The Upper Boise Valley, Idaho State Historical Society Reference Series" (PDF). 450 N. 4th Street, Boise, ID 83702. 1973. Archived from the original (PDF) on 4 February 2011. Retrieved 31 July 2011.
- Newbold, John D. "The Great California Flood of 1861–1862" (PDF). San Joaquin Historian. San Joaquin County Historical Society. 5 (4). Retrieved 1 March 2016.
- "The American River gave birth to Sacramento with the discovery of gold in 1848. Ever since then the river has been trying to take the city back". American River Watershed Project. Retrieved 1 March 2016.
- "Historic California Posts: Fort Ter-Waw". California State Military Museum. Retrieved 3 October 2010.
- Secrest, Jr., W.B.; Secrest, Sr., W.B. (2006). California Disasters, 1800–1900. Quill Driver Books/Word Dancer Press, Inc. ISBN 1-884995-49-7.
- Carr, John (1891). Pioneer days in California. Times publishing company. pp. 291–295, 397. Retrieved 7 October 2010.
- William H. Brewer, Up and Down California in 1860–1864: The Journal of William H. Brewer, Yale University Press, New Haven, 1930.
- "Historic Rainstorms in California". California Department of Water Resources. Archived from the original on 2007-08-24. Retrieved 2007-10-23.
- Ingram, B. Lynn (January 1, 2013). "California Megaflood: Lessons from a Forgotten Catastrophe". Scientific American. Retrieved 19 February 2016.
- Mildred Brooke Hoover, H. E. Rench, E. G. Rench, Historic Spots in California, Third Edition, Stanford University Press, Stanford, 1966. pp. 540–541 Knight's Ferry.
- "The Great Flood in California: Great Destruction of Property Damage $10,000,000". The New York Times. 21 January 1862.
- "The Great Floods of the San Gabriel Mountains" Archived 2008-04-26 at the Wayback Machine. by Cecile Page Vargo, Explore Historic California, February 2005
- Cleland, Robert Glass (1941). The Cattle on a Thousand Hills: Southern California, 1850–1880. Huntington Library; University of California Press. p. 128. ISBN 978-0-87328-097-6.
- McGlashan, H. D.; Ebert, F. C. (1918). "Southern California Floods of January 1916". U. S. Geologic Water Supply.
- "California Historical Landmark: Ventura County". Office of Historic Preservation. California State Parks. Retrieved 2012-10-15.
- Taylor, M.D., W. Leonard; Taylor, PhD, Robert W. (2007). "The Great California Flood of 1862". The Fortnightly Club of Redlands, California. Retrieved 3 October 2010.
- William H. Brewer, Up and down California in 1860–1864, New Haven, Yale University Press, 1930, p. 243 Retrieved 23 October 2010.
- U.S. Department of Agriculture, 1973, Water and related Land Resources, Central Lahontan Basin, Carson River Subbasin, Nevada and California, Special Report: History of Flooding, Carson Valley and Carson City Watershed, U.S. Soil Conservation Service, Minden, NV.
- Roger D. McGrath, Gunfighters, Highwaymen, and Vigilantes: Violence on the Frontier, University of California Press, 1987. p. 20. Retrieved 2 January 2011.
- P. Kyle House, Ancient floods, modern hazards: principles and applications of paleoflood hydrology, Volume 1, American Geophysical Union, 2002, p. 297
- FORT CLARA (aka FORT SANTA CLARA), Santa Clara, Utah from wchsutah.org accessed September 24, 2015
- "Janet Burton Seegmiller, A History of Iron County, Community Above Self". Utah State Historical Society, Iron County Commission. 1998.
- Official Records of the Union and Confederate Armies Ser. I, Vol. 50, P. I, Ch. LXII–Correspondence, January 23, 1862 Letter from Major Edwin A. Rigg, Fort Yuma, to Col. James H. Carlton, commanding Southern District, pp.815-818
- "Commanding Officer's Quarters & Kitchen Historical Marker".
- Thomas Edwin Farish, History of Arizona, Volume I. The Filmer Brothers Electrotype Company, San Francisco, 1915. pp. 252–253
- Official Records of the Union and Confederate Armies Ser. I, Vol. 50, P. I, Ch. LXII–Correspondence, pp. 865–868
- Official Records of the Union and Confederate Armies Ser. I, Vol. 50, P. I, Ch. LXII–Correspondence, p. 851
- Wheeler, G.M., Annual report on the geographical surveys West of the one-hundredth meridian, in California, Nevada, Utah, Colorado, Wyoming, New Mexico, Arizona, and Montana: Appendix JJ, AnnualReport of the Chief of Engineers for 1876: Washington, D.C., Government Printing Office. 1876,
- War of the Rebellion: A Compilation of the Official Records of the Union and Confederate Armies. Published Under The Direction Of The Hon. Daniel S. Lamont, Secretary of War, BY Maj. George W. Davis, U. S. Army, Mr. Leslie J. Perry, Civilian Expert, Mr. Joseph W Kirkley, Civilian Expert, Board of Publishers. Series I, Volume L, In Two Parts. Part I, Reports, Correspondence, Etc., Government Printing Office, Washington. 1897, p.125 Letter from Lieutenant- Colonel, E. E. Eyre, First California Volunteer Cavalry at Fort Thorn to Headquarters, Column from California, July 8, 1862.
- "What's in a Name?". The Arizona Sentinel. January 14, 1882. p. 2.
- The west coasts of Mexico and Central America from the United States to Panama including the gulfs of California and Panama. United States Hydrographic Office, Government Printing Office. 1904. pp. 155–157.
- "Overview of the ARkStorm Scenario" (PDF). USGS. p. 2.
- "ARkStorm: California's other "Big One"". USGS.
- "The 1861–1862 Floods: Informing Decisions 150 Years Later". California Extreme Precipitation Symposium. June 26, 2012. Retrieved March 1, 2016.
- Hunsaker, Leon; Curran, Claude (November 2005). "Lake Sacramento — Can It Happen Again?" (PDF). Retrieved March 1, 2016.
- Ingram, B. Lynn (2013-01-01). "California Megaflood: Lessons from a Forgotten Catastrophe". Scientific American. Retrieved 2017-01-09.