The Palos Verdes landslide is not one event — it is a 70-year (and counting) chapter of an ancient story written into the rock of the peninsula itself.
The Palos Verdes Hills are a fault-bounded block of Cenozoic sedimentary and volcanic rocks draped over a core of much older Mesozoic schist. The critical weakness lies in the Altamira Shale member of the Miocene Monterey Formation — layers that contain thin seams of bentonite clay, formed from ancient volcanic ash.
When bentonite gets wet, it becomes extraordinarily slippery. On the peninsula's south slope these weak layers dip seaward, roughly parallel to the ground surface — a natural slide ramp aimed at the ocean. Wet winters raise groundwater, pressurize and lubricate those clay seams, and the hillside above them creeps toward the sea. That is why nearly every intervention — dewatering wells, hydraugers, winterization ditches — targets one thing: getting water out of the slide mass.
All four sit within (and are "inset into") the much larger dormant ancient Portuguese Bend landslide complex mapped by the California Geological Survey. See the schematic map of the complex to visualize how they fit together.
Massive prehistoric sliding creates a roughly two-square-mile landslide complex on the peninsula's south flank. It eventually goes dormant, leaving hummocky terrain later called Portuguese Bend.
After the San Pedro Bay whaling station on Deadman's Island closes, Azorean captain José Machado brings shore whaling to the bend in the coastline north of the bay. For two decades, Portuguese crews row out through the surf to harpoon passing gray whales, tow them ashore, and render the blubber in iron try-pots — one captain alone producing 2,166 barrels of whale oil from 1874 to 1877. Petroleum kills the trade by 1885; the last try-pots and crumbling furnaces vanish by about 1928. The station's site — California Historical Landmark #381, marked along Palos Verdes Drive South — lies within today's slide zone, where the ground has since traveled hundreds of feet seaward: whaling gave this coast its name, and the landslide has been rearranging the ground it stood on ever since.
History: Palos Verdes Library District · Historical Marker Database (CHL #381).
The Palos Verdes Corporation opens the Portuguese Bend Club on 105 oceanfront acres — a private beach colony envisioned by Kelvin Vanderlip (son of peninsula founder Frank Vanderlip) with a clubhouse, restaurant, swimming pool, paddle-tennis courts, rental cottages, boating facilities, and a 485-foot pier reaching into the cove. It becomes one of the South Bay's most popular seaside destinations, hosting dances, swim meets, and tournaments. It has eight years left.
Historic photos: Palos Verdes Library District local history collection.
During extension of Crenshaw Boulevard, Los Angeles County crews place over 300,000 cubic yards of fill on the head of the ancient slide. The eastern portion reactivates. Roughly 130 homes are ultimately destroyed or removed in the Portuguese Bend community, and litigation against the County follows. The slide also kills the Portuguese Bend Club in its prime: the clubhouse, restaurant, and pool are destroyed as the ground beneath them breaks apart and rafts toward the sea, and the pier and beach colony's glory days end with them (a private beach club community survives at the site today). The land has not stopped moving since — over the following decades it carries the ground hundreds of feet seaward.
The 1956 slide also breaks a water line — beginning a lesson the peninsula has relearned ever since: buried pipes and moving ground don't mix, and leaking lines feed the very slide that breaks them. In the moving area, utilities have long been adapted to flex — including water lines run above ground on flexible connections, a decades-old Portuguese Bend practice that Cal Water dramatically expanded across the complex in 2024 (see below).
A second lobe of the ancient complex, west of Portuguese Bend, starts sliding — threatening homes above Abalone Cove and Palos Verdes Drive South.
The Klondike Canyon slide begins moving near the Seaview neighborhood. Under California's Beverly Act, property owners form two Geologic Hazard Abatement Districts — ACLAD (Abalone Cove, 1981) and KCLAD (Klondike Canyon, 1981) — to fund and operate dewatering wells and drainage. Early dewatering succeeds in dramatically slowing Abalone Cove.
On June 2, 1999 — weeks before the new Ocean Trails Golf Club east of the Portuguese Bend complex was to open — a slice of coastal bluff roughly 600 feet long and 220 feet wide gave way, dropping most of the 18th hole's fairway and green toward the ocean and snapping a 27-inch county sewer main, which spilled raw sewage onto the beach below. The failure occurred on a lobe of ancient landslide ("Landslide C") beneath the course; its trigger was disputed in years of litigation — the developers pointed to leaking buried pipes, others to the ancient slide plane itself. The landslide bankrupted the project, and in November 2002 Donald Trump bought the course for $27 million, rebuilt the 18th hole, and reopened it as Trump National Golf Club Los Angeles. A separate slide from the Portuguese Bend complex — but the same geology, and another chapter in the peninsula's long argument between water, pipes, and ancient slide planes.
Background: Trump National Golf Club Los Angeles (Wikipedia) · CBS News (1999) · South Bay History.
The City's landslide moratorium, first adopted in 1978, barred new homes across the moving area — including "Zone 2," a portion of the ancient slide above Abalone Cove that had shown little modern movement. In 2002, after minor movement nearby, the City Council effectively froze Zone 2 development with a resolution requiring owners to prove a new home would not aggravate any existing geologic condition — a bar owners called impossible to clear. Sixteen lot owners sued, and in 2008 the California Court of Appeal ruled in Monks v. City of Rancho Palos Verdes that the moratorium as applied was a regulatory taking of the plaintiffs' property. In 2009 the City amended its code to let the "Monks lots" develop, and homes were subsequently built in Zone 2 — several owners had obtained entitlements by 2012.
The arc closed in 2025: after the 2023–24 acceleration redrew the map of what this ground can do, Ordinance 692 permanently banned new residential construction throughout the complex — the restriction the courts had once forced the City to loosen, reimposed by the land itself.
Case background: City of RPV — Zone 2 / Monks lots · case summary.
Portuguese Bend creeps on — bending Palos Verdes Drive South, which the City repairs continuously. The City adopts a landslide moratorium restricting new development in the moving area, studies remediation options, and installs GPS monitoring. Movement waxes with wet winters and wanes with dry ones.
Historic storms saturate the peninsula. Movement accelerates across the complex; fissures open in the Portuguese Bend Reserve; the City declares a local emergency and begins winterization measures.
The four slides begin moving as one broad mass across ~700 acres — in places several inches per week, with NASA/JPL radar measuring up to ~4 inches per week in residential areas that fall. The Wayfarers Chapel closes in February and is dismantled for preservation by September. Power is cut to about 245 homes and gas to entire neighborhoods. The shifting ground also breaks buried utility lines over and over — including pressurized water mains and private service lines, whose leaks put still more water into a slide already driven by groundwater. Cal Water responds by rebuilding the system in the open: during 2024 its crews install above-ground water mains with flexible swing joints through most of the Portuguese Bend community, western Seaview, stretches of Palos Verdes Drive South, and part of the Beach Club — the pipes still visible along roadways today, where leaks can be spotted immediately and the lines adjusted as the land moves. FEMA and Cal OES announce a $42 million voluntary buyout program in October. Deep dewatering wells begin pumping at the slide's toe. And at the shoreline, the slide does something almost unbelievable: the advancing toe shoves the seafloor upward, raising hundreds of feet of new rocky land out of the surf below Portuguese Bend — "landslide debris... being pushed up and out of the ocean," in the city geologist's words, visible in before-and-after photos just months apart.
The new shoreline: CBS Los Angeles (July 2024) · L.A. Times via Coastal Care.
Dewatering removes hundreds of millions of gallons; movement decelerates sharply. Seaview and the Beach Club effectively stop moving; gas restoration begins in Seaview; the City's $2.8M financial assistance program pays out to 223 households; seven additional wells are installed with ACLAD and KCLAD; the ~$33M remediation project moves through environmental review. In August, Ordinance 692 makes the construction restrictions permanent — no new residential construction in the complex (~400 homes and ~130 vacant lots), replacing the emergency moratorium in place since 2023.
By July 2026 the complex is moving 60% slower than a year earlier, averaging about 1.1 inches per week in the still-active interior, and dewatering passes half a billion gallons removed. Buyouts inch forward awaiting FEMA awards, the Council advances work on a possible third abatement district for Portuguese Bend, and in August it renews the local emergency and extends the home-stabilization ordinance through 2028. The emergency — and the management effort — continues.
What moving ground looks like up close: upset, fissured earth in the Portuguese Bend landslide, photographed in 2016 — years before the 2023–24 acceleration. Photo: Pricetveyron, CC BY-SA 4.0.
The slide as landscape: the Portuguese Bend Reserve's hummocky terrain running down to Inspiration Point and Portuguese Point — dormant-looking, never still. Photo: Pricetveyron, CC BY-SA 4.0.
Wayfarers Chapel as generations knew it — Lloyd Wright's glass sanctuary in its redwood grove, before land movement forced its 2024 dismantling. Photo: Dmitry Kotov via Wikimedia Commons (CC0).
For historic photographs of the Portuguese Bend Club, its pier, and the 1956 destruction, see the Palos Verdes Library District's local history collection — a remarkable archive we can link but not reproduce here. NASA's radar imagery of the modern slide is on the Maps & Data page.
Lloyd Wright's 1951 "glass church," a National Historic Landmark, closed in February 2024 as land movement warped its structures. It was meticulously dismantled — thousands of parts catalogued and stored — with a prospective new campus identified at Battery Barnes near Rancho Palos Verdes City Hall, about 1.7 miles from its original site.
The coastal road crossing the slide is among the most-repaired stretches of pavement in California — inspected constantly, repaved repeatedly, and now the subject of a planned regrading project. In the 2024 acceleration it deformed dramatically, at times requiring escorts and overnight closures.
The beloved open-space preserve above the slide saw trails torn by fissures and scarps during the acceleration, forcing extended closures and permanently altering some routes. It remains the clearest place to see the landslide's raw geology.
The 1948 beach colony — clubhouse, restaurant, pool, cottages, and a 485-foot pier — was the peninsula's seaside social hub until the 1956 slide destroyed its facilities just eight years in. A private gated beach community remains at the site today; the resort that Kelvin Vanderlip imagined lives on only in photographs.
East of the complex, the golf course lost most of its 18th hole to a 1999 landslide on a separate ancient slide lobe weeks before opening — bankrupting its developers before Donald Trump bought and rebuilt it in 2002. The rebuilt hole plays today atop some of the most intensively engineered ground on the coast.
Since 2024 the slide's advancing toe has shoved the seafloor upward below Portuguese Bend, raising hundreds of feet of new rocky land out of the surf — not yet a beach, geologists caution, but the newest land in Los Angeles County, made by the slide itself.