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History & Geology

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.

Why This Ground Moves

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.

The four active slides

  • Portuguese Bend Landslide
    The largest and most famous; moving continuously since 1956.
  • Abalone Cove Landslide
    Began moving in 1974; slowed by early dewatering, reactivated in the 2020s.
  • Klondike Canyon Landslide
    Began moving around 1980, beneath the Seaview neighborhood's edge.
  • Beach Club Landslide
    Small coastal slide beneath the Portuguese Bend Beach Club community.

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.

Timeline of the Landslide

The Landslide in Pictures

Deeply fissured and jumbled earth in the Portuguese Bend landslide area, with broken tan soil and displaced vegetation

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.

View across the hummocky Portuguese Bend landslide terrain and nature preserve toward Inspiration Point, Portuguese Point, and the Pacific Ocean

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's glass and redwood sanctuary among trees, photographed before the chapel was dismantled

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.

Landmarks of the Slide

Wayfarers Chapel

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.

Palos Verdes Drive South

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.

Portuguese Bend Reserve

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 Portuguese Bend Club & Pier

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.

Ocean Trails / Trump National

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.

The New Shoreline

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.