In a striking event last year, a colossal landslide in Alaska set off a megatsunami, now recognized as having produced the second-highest wave ever documented. This phenomenon has been meticulously mapped and studied by researchers.
In the predawn hours of August 10, 2025, an immense section of a mountainside collapsed atop a melting glacier in Alaska’s Tracy Arm fjord. The resulting landslide catapulted debris into the fjord, generating a towering wave that soared over 1,500 feet, carving through the picturesque landscape.
This towering 1,578-foot wave surged through an Alaskan fjord situated 45 miles south of Juneau, leaving a profound impact on the region.
A recent analysis has shed light on the unfolding of this catastrophic landslide and the subsequent wave, offering rare insights into these dramatic natural events.
Published in the journal Science, the study delves into the precursors that triggered the landslide and the resulting megatsunami, which rose to heights surpassing even New York City’s Empire State Building.
“The wave generated was unimaginably large. It’s hard to fathom the terror of witnessing such a phenomenon,” remarked Dan Shugar, the study’s corresponding author and an associate professor in the Department of Earth, Energy and Environment at the University of Calgary.
While tsunamis are most often triggered by earthquakes, this one was driven by a massive landslide that hurled 64 million cubic meters of debris—enough to fill the Great Pyramid of Giza about 24 times—into the fjord, generating seismic signals detected worldwide for days.
Shagger likened the displacement of water to jumping into a swimming pool – with water rushing nearly 1,600 feet up the gigantic valley walls of the fjord below.
The colossal debris fall triggered what the study says is the second-largest tsunami wave of all time – narrowly behind the largest tsunami of all time recorded in Lituya Bay, Alaska, on July 9, 1958, that reached a run-up height of 524 meters, or 1,720 feet.
The jaw-dropping scale of the megatsunami was made possible by its setting, with the narrow fjord amplifying the wave and driving water high up the surrounding mountain walls. A similar effect was observed in the Lituya Bay tsunami, which also occurred in a fjord.
As it turned out, there were no obvious warning signs that the second-largest tsunami in recorded history was going to happen. However, in the days leading up to the collapse, repeated microseismic activity in the Tracy Arm area increased in frequency, continuing until less than an hour before the slope finally failed.
According to the study, one of the main factors that led to the landslide was the retreat of the glacier below the wall, which Shugar said in the year before the slide had retreated 1,800 feet, removing support for the valley wall that eventually tumbled into the water below.
The study identified the blazing speed of the skyscraper-sized tsunami – with computer simulations estimating that the Goliath wave traveled over 150 mph, the cruising speed of a high-speed train — except in the form of a deadly 100-meter-high wall of water moving through a narrow fjord.
Understanding the landscape and geography of the Tracy Arm fjord is essential to understanding the landslide and megatsunami.
“The valley walls of that fjord are so steep and so tight, so narrow, that the water really has only one way to go, and that’s up,” Shugar said.
Tracy Arm is a roughly 30-mile-long, 0.8-mile-wide fjord, about 380 meters deep, surrounded by towering peaks rising up to 2,000 meters.
When the landslide occurred, the powerful tsunami surged through the narrow valley, scouring the landscape and changing the face of the scenic waterway.
The vibrant turquoise glacial tidewaters have popularized the scenic Alaskan landscape in the Tracy Arm area, frequently visited by tourists. During the summer months, more than 20 boats a day visit Tracy Arms and a neighboring fjord, including large cruise vessels that carry up to 6,000 passengers.
Thankfully, although the megatsunami had numerous witnesses across a wide area, no fatalities were reported.
The landslide occurred around 5:30 a.m. local time—well before tourists typically enter the fjord. Had it happened later in the day, the consequences could have been catastrophic.
The study highlighted a critical threat to the popular tourist area: the hazardous nature of tsunami landslides.
“It’s important to remember that if this event had happened five or six hours later, it probably would have been a very different situation. A disaster with hundreds of people killed because this fjord is very popular with cruise ship traffic,” Shugar said. “If they were up at the head of the fjord to look at the glacier caving, which is what they are there to go look at, I can’t see any way that a ship would survive a wave like this.”
