7.3-magnitude quake triggers tsunami warning off Alaska coast, canceled after 2 hours

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Nov, 28 2025

A 7.3-magnitude earthquake ripped through the seafloor 54 miles south of Sand Point, Alaska, on Wednesday, July 16, 2025, at 12:38 p.m. Alaska Time — a violent jolt that sent coastal residents scrambling for higher ground, only to be told, two hours later, that the worst had passed. The National Weather Service issued a tsunami warning stretching 700 miles along Alaska’s southern coastline, from Kennedy Entrance to Unimak Pass, including the island community of Kodiak with its 5,200 residents. By 2:42 p.m., the alert was lifted. No tsunami arrived. But the fear? That was real.

What Happened Beneath the Sea

The quake struck at a depth of 38.0 kilometers (23.6 miles), according to the United States Geological Survey, which later upgraded its initial 7.2 reading to 7.3. That’s not just a technical adjustment — it’s the difference between a major quake and a truly powerful one. The rupture extended roughly 300 kilometers along the subduction zone stretching from southern Kodiak Island to the northern tip of the Shumagin Islands, a geologically restless stretch where the Pacific Plate dives beneath the North American Plate. It’s the same fault system that unleashed the 1964 Great Alaska Earthquake — a 9.2 monster that still holds the record for the strongest ever recorded in North America.

Residents in Sand Point, a fishing village perched on Popof Island, reported violent shaking that rattled windows and knocked items off shelves. But with a population of just under 1,000, the immediate damage was minimal. The real concern was the water. Tsunami warnings aren’t issued lightly. They’re based on models that predict how much the seafloor displaced — and how far the resulting waves might travel. In this case, the models showed potential for waves up to 3 meters (10 feet) in some bays and inlets.

Evacuations and the Quiet After the Alarm

Emergency sirens blared in Kodiak. Boats were pulled from the water. Families drove inland, some heading to schools or community centers designated as evacuation hubs. One resident, Maria Tukel, told LiveNOW from FOX: “We’ve lived here 20 years. We’ve practiced this drill. But you never get used to the sound of the siren.”

The U.S. Tsunami Warning Center, based in Palmer, Alaska, coordinated the response with state and local agencies. Their message was clear: “Evacuate now. Wait for official confirmation before returning.”

By 2:42 p.m., after analyzing data from tide gauges across the region — none of which showed a significant rise in sea level — the warning was canceled. “The ocean didn’t cooperate,” said NWS meteorologist Dan Hines in a press briefing. “The earthquake was powerful, but the seafloor movement didn’t generate the kind of vertical displacement needed to create a destructive tsunami.”

Why the West Coast Was Never in Danger

It’s worth noting: no threat reached Oregon, Washington, or British Columbia. The quake’s location — deep in the Gulf of Alaska, far from the continental shelf — meant the energy was absorbed by the ocean floor rather than projected toward the U.S. West Coast. The National Weather Service explicitly stated this multiple times, even as social media buzzed with doomsday clips.

That’s the irony of modern seismic monitoring: we can detect quakes faster than ever, but we’re still learning how to predict their consequences. The same system that issued the warning also had the precision to cancel it within hours — a testament to decades of investment in Alaska’s early-warning infrastructure.

Mount Rainier’s Quiet Tremors and the Bigger Picture

While Alaska was on alert, another seismic story unfolded thousands of miles away. The USGS Cascades Volcano Observatory reported over 300 small earthquakes beneath Mount Rainier in the past week. Alex Iezzi, a research geophysicist there, offered sobering context: “It’s the most significant swarm we’ve seen since we started monitoring in the 1970s. But Mount Rainier is 500,000 years old. We’ve only watched it for a blink.”

That’s the thing about earthquakes — they’re not always warnings. Sometimes, they’re just reminders. The Earth moves. It always has. Alaska, perched on the Ring of Fire, lives with this truth daily. The Sand Point quake was the 12th event of magnitude 7.0 or greater worldwide in 2025 — and the most powerful in U.S. territory this year.

What’s Next for Alaska’s Coast

The state is already reviewing its evacuation protocols. Some villages, like Sand Point, rely on small boats for emergency transport. Others, like Kodiak, have paved roads leading inland — but many elderly residents don’t drive. Officials are now discussing mobile alert systems that can target neighborhoods, not just entire regions.

Meanwhile, scientists are poring over data from the quake. The USGS has labeled it “significant” — a classification reserved for events scoring over 600 on their formula: magnitude × 100 × (magnitude ÷ 6.5). This one scored 788. That means it’s now archived in the global database of major seismic events, a reference point for future research.

For now, the coast is quiet. Fishermen are back on the water. Kids are back at school. But the memory of that siren? That lingers.

Frequently Asked Questions

Why was the tsunami warning canceled so quickly?

The warning was canceled because tide gauges across Alaska’s southern coast showed no significant rise in sea level — the key indicator of an incoming tsunami. While the earthquake was powerful, the type of fault movement — mostly horizontal slip rather than vertical uplift — didn’t displace enough water to generate destructive waves. The U.S. Tsunami Warning Center uses real-time ocean data, not just seismic readings, to make final decisions.

How often do earthquakes of this magnitude happen in Alaska?

Alaska averages one magnitude 7.0 or greater earthquake every 13 months on average, making it the most seismically active U.S. state. The 7.3 quake near Sand Point is the strongest in Alaska since a 7.1 event near the Aleutians in 2023. The region’s geology — where tectonic plates collide — ensures frequent activity, but most quakes occur offshore or in remote areas, minimizing human impact.

Was this earthquake related to the recent activity at Mount Rainier?

No. The Sand Point quake occurred along the Aleutian Trench, while Mount Rainier’s seismic swarm is tied to volcanic activity in the Cascade Range — over 2,000 miles away. These are separate tectonic systems. The coincidence in timing is just that: coincidental. The USGS confirmed no connection between the two events.

Why didn’t the tsunami reach the West Coast of the U.S.?

The earthquake’s location, depth, and rupture direction meant the energy was directed into the deep ocean basin of the Gulf of Alaska, not toward the continental shelf. Tsunamis require vertical displacement of the seafloor to generate large waves. This quake involved mostly lateral movement, and its distance from the U.S. mainland — over 1,500 miles — gave any minor waves time to dissipate before reaching Oregon or Washington.

How did the National Weather Service coordinate the response?

The National Weather Service activated its Tsunami Warning System, which includes automated alerts to local emergency managers, NOAA weather radios, and digital platforms like the NWS website and mobile apps. They also coordinated with the Alaska Department of Homeland Security and tribal governments. In rural areas like Sand Point, community volunteers helped spread the word door-to-door when internet or cell service failed.

What makes this earthquake scientifically significant?

Beyond its magnitude, the Sand Point quake ruptured a 300-kilometer segment of a known fault zone, offering valuable data for modeling future earthquakes. The USGS classifies it as “significant” under its mathematical threshold (score > 600), placing it among the top 50 global quakes of 2025. Scientists will study its aftershock pattern to better understand stress transfer along the Aleutian Arc — information critical for improving long-term hazard forecasts.