Underwater Landslides off Southern California

Science Center Objects

An earthquake can trigger a landslide along the ocean floor, which can then set off a tsunami. Without modern, high-resolution imaging of the seafloor, many historical slides and threats from future slides remain undetected.

A man sits at a computer screen holding a mouse with a keyboard in front of him, looking at the monitor talking and gesturing.

Jared Kluesner displays a 3D view of seismic data collected off Santa Barbara. This visualization helps him analyze the Earth’s layers from the seafloor (rainbow-colored surface) to several kilometers below (slices extending down from the colored surface).

Using equipment that stretched several kilometers behind their vessels, the petroleum industry ran 3D seismic surveys off Santa Barbara in the 1990s. When they released their data to the public in 2015, USGS geophysicist Jared Kluesner could finally sift through the values to create a 3D view of the Earth extending thousands of meters beneath the seafloor. This view was a vast improvement over the paper-thin slices of Earth’s crust that are constructed from 2D surveys. Tens of gigabytes of data required months of number crunching and the largest monitor that could fit on Kluesner’s desk. His “geologic Hubble telescope” allowed him to virtually explore kilometers below the seafloor in any direction, map faults, and study how fluid moves through the Earth’s crust.


Underwater landslides threaten offshore structures such as seafloor pipelines, cables, and equipment for oil and gas exploration. These landslides can also trigger tsunamis that endanger coastal communities. A 1998 earthquake in Papua New Guinea triggered a landslide on the seafloor, which generated a 10-meter high tsunami that killed more than 2,000 people along the nearest shoreline.

Map of offshore southern California showing the contours of the seafloor, with labels pointing to circles showing landslides.

Large submarine slides off southern California (outlined in small white dots). Low-resolution bathymetry shown in light grey (approximately 100 meters/pixel). High-resolution bathymetry shown in darker grey (less than 20 meters/pixel).

Offshore map shows the contours of the seafloor and outlines some underwater landslides with labels.

The small Gaviota slide (center) near Santa Barbara is the youngest landslide discovered in the area—about 200 years old.

Until recently, scientists had not looked closely for similar landslides off the Southern California coast. Previously known slides in the region are the Goleta slide in Santa Barbara Channel and the Palos Verdes debris avalanche off Palos Verdes Peninsula, each less than half a cubic kilometer in size. Underwater landslides might have triggered significant tsunamis in Santa Barbara in 1812 and Point Arguello in 1927. But inadequate seafloor mapping in the area limits what scientists know about the size, distribution, and age of potential tsunami-generated landslides. Numerous banks and ridges beneath the waters off the Southern California coast could hide undiscovered slides. 

As an example, a 2010 NOAA cruise to map the seafloor around the Santa Cruz Basin 50 to 80 kilometers from Ventura, accidentally discovered several underwater landslide scars. The scars show considerable variation in appearance, suggesting a wide range of ages for individual slides. The landslides range in size from less than 1 to more than 50 square kilometers, making this one of the largest underwater landslide complexes found off Southern California.

Illustration shows contours of the seafloor and outlines geologic features such as landslide features.

Computer image looking west from shore across the Santa Cruz Basin. At least 11 separate landslides have slumped from the side of Santa Rosa Ridge, which was pushed up by the fault movement that created Santa Cruz Basin.

What the USGS is doing

To understand the potential tsunami hazards that underwater landslides pose to Southern California, the USGS led a high-resolution 2D seismic study in Santa Cruz Basin and nearby basins in November 2014. This work should help identify what makes slopes unstable, what may trigger them to slide (active faults, sediment buildup, fluid channels beneath the seabed), and what potential exists for slides to generate local tsunamis.

To dig further into the complexities of these landslides, USGS researchers used advanced techniques to analyze 3D seismic data collected by the oil industry. These data from near the Goleta slide in Santa Barbara Basin help USGS scientists make connections between underwater landslides and natural events that make a slope fail. Researchers compare lower resolution 3D seismic images with higher resolution 2D data to link the 3D data to the landslides seen on the seafloor.

USGS scientists continue to collect more seafloor mapping data looking for changes to the seafloor and seafloor seeps, which can indicate mounting fluid pressure that could trigger landslides.

Block with swirls of color and one edge pointing forward gets cut away then built back up little by little on two faces.

A 3D animation of seismic reflection data takes viewers through the layers of a chunk of Earth below the seafloor. Different colors represent different layers of sediment and rock.

What the USGS has learned

Recent research within Santa Cruz Basin shows landslides ranging from 6,000 to 8,000 years old.

New seafloor data revealed the Del Mar slide, just north of San Diego. The steep slope here has landslides more than 6 kilometers wide, about 8 kilometers west of Del Mar, along the edge of the continental shelf. Seismic data show the slide deposit is up to 20 meters thick and extends nearly 10 kilometers to the west. Data also reveal older slide deposits buried beneath the seafloor. A sediment core taken near the toe of the slide indicates it may be about 14,000 to16,000 years old, and that slides could recur here on a timescale of tens of thousands of years.

It’s likely that more offshore landslides are yet to be discovered.

Large ship on the ocean in calm seas has many antennas, an elevated platform midships, equipment stacked in 4 levels on stern.

Research vessel (R/V) Marcus G. Langseth, operated by Lamont-Doherty Earth Observatory's Office of Marine Operations, can deploy several kilometers of cable to collect seismic data from beneath the seafloor.

Looking off the stern of a large ship to the horizon with long ropes and hoses and other floating instruments being towed.

Four tan cables, each 6 kilometers long, trail behind R/V Marcus G. Langseth. These cables record seismic sound waves that travel down into the Earth and reflect back from layers beneath the seafloor. The green cables provide the sound.


Artificial-Gas-Seep Test Produces 3D Images of Bubble Plumes in the OceanSound Waves, January 2016 

Are American Cities Prepared For Massive Tsunamis, NBC news, September 2015

Weighing the risks of a southern California tsunami, Christian Science Monitor, June 2015

Here’s What Seismologists Have to Say About the Science of ‘San Andreas,’ Time, May 2015

Researcher says a sinking Santa Catalina could pose tsunami threatLA Times, April 2015

Sliding on the SeafloorSanta Barbara Independent, November 2010

Potential Triggers of Tsunamis That Could Strike the U.S. East CoastSound Waves, August 2009

Experts Find Clues to Cause of Deadly Pacific TsunamiNew York Times, April 2002