Downey & LA County
The Devastating Floods of 1868: Downey Was Born in a Floodplain
The river that runs past Downey today is not where it used to be. In 1868 it moved — and the newspaper account of that week is remarkable reading.
The short answer
In late 1868 the San Gabriel River abandoned its channel — the watercourse now called the Rio Hondo — and cut a new course through what was then Los Nietos. Governor Downey lost about 200 acres, Pío Pico about 200, and the Murphy family spent eight hours on a drift awaiting rescue.

In late 1868, the area that is now Downey was called Los Nietos, after the vast Rancho Los Nietos land grant. It was farmland on the floodplain between two rivers, and that winter the rivers demonstrated exactly what that meant.
What the newspaper reported
The Los Angeles Semi-Weekly News of December 3, 1868 carried an account of severe losses in Los Nietos. The named landowners give a sense of the scale.
| Landowner | Loss reported |
|---|---|
| Governor John G. Downey | About 200 acres |
| Mr. Murphy | 100 acres of his 150 |
| Don Pío Pico | About 200 acres — the river forming a new channel at that place |
Governor Downey is the man the city is named for — the former and youngest-ever governor of California, born in Ireland, who pioneered modern subdivision on land he acquired between the Rio Hondo and the San Gabriel River around 1865. Pío Pico was the last governor of Alta California under Mexican rule.
The Murphy family's night
The account of what happened to the Murphys is worth reproducing in outline, because it conveys what a floodplain event actually meant before flood control.
When the river began rising on the Monday evening, Mr. Murphy and his family — fearing water reaching the floor of the house — set out to wade to high ground. Mr. Murphy and three of the children made it to safety. Mrs. Murphy, her daughter, and a Mr. Casserly did not. They were caught by the water and managed to reach a drift, where they remained from four o'clock in the afternoon until midnight, when they were finally reached by a boat built for the emergency.
Eight hours clinging to accumulated debris in a flooding river, waiting for a rescue boat that had to be constructed on the spot.
The river moved
The most remarkable consequence was geographic. The floods of 1867–1868 caused the San Gabriel River to abandon its former channel and take a new course.
A river relocated itself by several miles in a single wet season, and the two channels that now define Downey's eastern and western edges are the before and after of that event. The relocated watercourse also washed away a substantial part of Pío Pico's house.
Why this stopped happening
The nineteenth and early twentieth centuries produced repeated flood catastrophes across the Los Angeles basin, and the eventual response was the Los Angeles County Flood Control District and the system it built.
Both the San Gabriel River and the Rio Hondo were channelized in concrete, fixing them permanently in place. Whittier Narrows Dam was built upstream at the gap where both watercourses pass through, controlling the flows that would otherwise reach the Downey basin.
It worked. Rivers in this basin do not relocate themselves any more, and the kind of event that stranded the Murphy family does not happen here now.
What replaced it
Downey's flood risk did not disappear — it changed form. Climate risk modeling puts roughly 24% of Downey buildings at meaningful flood exposure today, with five census tracts above 50%.
The mechanism is now urban rather than riverine. A dense, heavily paved city sheds rain rather than absorbing it, so the storm drain system carries the entire load. When rainfall intensity exceeds its design capacity — as it did repeatedly during the nine consecutive atmospheric rivers that hit California in three weeks over December 2022 and January 2023 — water backs up at the inlets and finds the lowest doorway.
There is a local echo of this within living memory. Before storm drains were installed in the northern part of the city in the summer of 1957, Firestone Boulevard ran like a river in heavy rain, and merchants kept sandbags at their doorways as a matter of routine.
Why the history is still useful
Two practical reasons.
First, it explains the ground. Downey's soil is river-deposited alluvium laid down by exactly these events — clay-rich, water-retentive, and seasonally expansive. That soil is why slab leaks are so common here, why cast-iron drain lines crack, and why clay-tile sewer joints work open enough for roots to enter.
Second, it explains the geography of risk. The lowest ground near the river channel — the Rio San Gabriel neighborhood, and South Downey below Imperial Highway — is low because of where the water used to go. It still goes there when the drains are overwhelmed.
The engineering changed what a flood looks like in Downey. It did not change the elevation of the ground.
Frequently asked
Yes. The floods of 1867-68 caused the San Gabriel River to abandon its former channel — the watercourse now called the Rio Hondo — and cut a new course, following an irrigation ditch used by Pío Pico and others. That new course is the one the river still runs today, and the relocated water washed away a substantial part of Pico's house.
Riverine flooding of that kind, essentially no. Both the San Gabriel River and the Rio Hondo are now concrete channels operated by the LA County Flood Control District, with Whittier Narrows Dam controlling upstream flows. What does still happen is urban flooding, when rainfall intensity exceeds what the storm drains can carry — a different mechanism with a much smaller scale, but real.
Yes. John Gately Downey was the former and youngest-ever governor of California, born in Ireland, and he pioneered modern subdivision on land he acquired between the Rio Hondo and the San Gabriel River around 1865. He is recorded as losing about 200 acres in the 1868 flooding, on land that would later become the city bearing his name.
Why nineteenth-century history still matters here
Two practical reasons. First, it explains the ground: Downey's soil is river-deposited alluvium laid down by exactly these events — clay-rich, water-retentive and seasonally expansive, which is why slab leaks and cracked laterals are so common.
Second, it explains the geography of risk. The lowest ground near the channel — Rio San Gabriel, and South Downey below Imperial Highway — is low because of where the water used to go, and it still goes there when the drains are overwhelmed.
The engineering changed what a flood looks like in Downey. It did not change the elevation of the ground.
Services mentioned in this article
Flood Cleanup
Storm and overflow flooding handled end to end — pump-out, contaminated material removal, disinfection, and documented drying.
Learn moreStorm Damage Cleanup
Emergency tarping to stop the water first, then extraction, drying, and full documentation for the claim.
Learn moreStructural Drying & Dehumidification
Metered, monitored drying that takes the structure back to its dry standard — not just the surface you can touch.
Learn moreAreas covered in this article
Historic core along Firestone Blvd and Old River School Rd — 1920s–40s commercial buildings and pre-1960 homes with…
about 6 minutes from our Florence Ave baseRio San GabrielAdjacent to the historic San Gabriel River channel — the lowest-elevation homes in Downey, with the city's highest…
6 to 9 minutes from our Florence Ave base


