Before you know it, I just saw looks of horrors on fellow people standing by and we just started running.
Destruction up and down the Oregon coast as high surf advisory continues for tonight.
It is 11:00.
Good evening everyone.
I’m Jeff Gianola and I’m Jennifer Hoff.
Tonight we’re learning the Coast Guard calling off the search for a man who was swept to sea by those huge waves in Depot Bay.
Scientists are sounding the alarm as extreme conditions hit the Oregon coast without warning.
Massive unpredictable waves are battering coastal towns, overwhelming defenses and forecasts alike.
Scientists are sounding the alarm with a sense of urgency and mounting dread.
What is unfolding along the Oregon coast right now sits far beyond what anyone imagined possible.

In the pre-dawn dark, without warning or obvious precedent, the Pacific Ocean has unleashed a violent onslaught of massive waves surging with an energy and unpredictability that has emergency officials and scientists deeply concerned.
The events of this morning defied every forecast, leaving coastal towns exposed and defenses reeling from the first impact.
Overnight, what should have been a routine winter watch transformed into something raw and terrifying.
Reports of extraordinary wave heights reaching up to 90 ft, overtaking entire beaches, slamming seaw walls with shocking force, began to overload county command centers.
The usual vigilance unraveled as emergency alerts drawn from raw sensor data struggled to keep pace.
Residents were pulled from sleep by the tremors rolling through their homes and the unmistakable sound of crashing water from the darkness.
It is not merely the magnitude that has officials gripped by concern, but the sheer unpredictability.
How these waves generated by faroff powerful storms struck the coast with virtually no warning.
Coastal roads disappeared beneath angry tides.
Headlands were battered and the boundary between land and ocean was redrawn almost instantly.
At dawn, first responders used the term coastal reset as nature overturned assumptions at direct, merciless speed.
Even seasoned meteorologists and oceanographers used to decoding Pacific Tempests admit they’ve never seen a convergence of such intense oceanic energy and seismic activity combined with unusual atmospheric patterns.
Across the coastline, fear is palpable.
Residents know the usual cues, but on this day, instincts signal that something is fundamentally different.
A new chapter of risk and destruction underway.
But the danger is not confined to what’s visible.
What is unfolding along Oregon’s shore is only the visible front beneath.
The ocean’s turmoil is triggering deeper threats.
As the waves crash ashore, scientists detect unusual activity on the ocean floor.
A tremor strong enough to rattle kitchen cabinets and set windchimes trembling hints at hidden forces in motion below.
Emergency officials are warning.
What began as an onslaught of water may now be evolving, shifting the very ground beneath the coastline and threatening everything built at top it.
Each new surge blurs the line between natural disaster and geological upheaval.
How did this happen? Why did the ocean so suddenly and forcefully defy projections? And what combination of forces is driving these events into unknown territory? Scientists warn that a rare and severe combination is at play.
Unusually intense Pacific storms, abnormal offshore seismic disturbances, and an atmosphere marked by instability have all converged to put Oregon at the epicenter of coastal upheaval.
As the first light exposes the devastation, one question grows louder than the roar of surf.

If danger can arrive so suddenly with such power, what further hazards may still be lurking beneath the waves? Just hours before disaster, the Oregon coast was quiet beneath brooding skies.
Fishermen prepared for the next round of winter storms, and locals, seasoned by years of severe seasons, trusted in their seaw walls and the familiar shape of headlands.
Conversations at harbor cafes revolved around fishing prospects and the latest talk of monster waves, which until now had been more rumor than reality.
This routine was shattered by what nature had poised offshore.
As evening fell, scientists at the Pacific Northwest Seismic Research Center began to note troubling signals.
Ocean sensors miles offshore relayed erratic pulses, seismic tremors beneath the rising hum of an intensifying Pacific storm system.
The data did not fit known patterns.
The signs blurred together.
Wind-driven wave energy overlaid with seismic ripples, more typical of undersea quakes.
Concern grew among the researchers.
Dr Marcus Holloway’s team flagged their readings as unprecedented convergence, a warning to those who understand the coast’s volatile history.
The unnerving question hung in the air.
Could the merging of a deepening storm and sudden tectonic activity create a feedback capable of supercharging waves? Data pointed toward that possibility.
On shore, officials began issuing watch advisories, hesitant to trigger evacuations.
The horizon remained deceptively still, but the numbers rolling in from boys raised clear alarms.
No historic pattern, no storm catalog could fully explain the collision of atmospheric and seismic forces occurring offshore.
As midnight approached, animal behavior changed.
Dogs barked at the surf.
Seabirds gathered inland.
Locals well attuned to nature felt a growing unease, a hum beneath the ground, an unnatural charge in the night air.
Most would not grasp what these signs meant until it was nearly too late.
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Vigilance could prove vital.
Official records mark the disaster as striking before dawn.
In truth, however, it began in the restless hours of morning as the first surges advanced unseen beneath the cover of darkness.
At exactly 4:17 a.m., a single wave close to 90 ft high was recorded moving toward the shore near Newport.
A wall of water illuminated only by the moonlight, progressing with chilling force.
In moments, the ocean pushed hundreds of yards in land, erasing dunes, flooding roads, and toppling parking lots.
The violence astonished even veteran observers.
Eyewitnesses likened the impact to an explosion.
Houses shook, windows blew out, seaw walls fractured.
In Yahhatz, long stretches of shoreline vanished underwater and debris, vehicles flipped, cabins dragged off their foundations.
On the headlands, the resonance of the waves seemed to shake the earth itself.
“The first emergency calls quickly overwhelmed dispatchers.
” “The waves keep coming,” reported one caller from Florence.
“Roads are gone.
It’s like the ocean is erasing the land.
In Depot Bay, the boardwalk was torn apart.
Lifeguards and responders trapped between surging water and collapsing ground rushed to account for missing residents as more waves battered the coast.
Even more unsettling for officials was the silence that preceded the disaster.
There was no clear warning.

The ocean, typically foreshadowing its fury with plummeting barometers and roaring winds, struck without the usual signs.
Standard cues for evacuation.
Rising tides, bent trees, lashing gales were missing.
The blow landed suddenly, well outside the boundaries believed possible.
By dawn, the scope was clear.
This was not just a severe winter storm, but a catastrophic convergence.
Rare Pacific storm energy amplified by seismic unrest offshore.
Oregon’s treasured coastline from Brookings to Atoria was ground zero for an event that Dr Marcus Holay himself said should not have been possible but now redefineses the limits of what we expect here.
Again and again the question arises how could the ocean turn so violent driven by forces greater than wind and water alone as news helicopters circled ruined highways and waterlogged neighborhoods.
The story forming among data analysts and researchers deepened the puzzle.
The event was not only about wind or tides, but the outcome of rarelyseen cooperation between atmosphere and tectonics felt in every home left in silence after the first wave.
Two principal forces drove the event.
An explosive winter storm system in the open Pacific and renewed seismic activity on the ocean floor.
In the days prior, sensors picked up an accelerating vibration under the sea.
Like a distant drum beat, now understood as a warning of instability along regional fault lines, marine researchers traced tremors strong enough to rattle windows and vibrate glass felt by communities up and down the coast.
At the Cascadia Oceanic Institute, Dr Abigail Renard’s team worked to connect these threads.
We’ve seen big waves and tremors before, but never together and never amplified on this scale, she reported early in the aftermath.
Her team traced the roots.
A sudden atmospheric pressure drop over the Pacific, timed with the seismic activity, sparked what oceanographers call a compound surge, a phenomenon that multiplies the destructive capacity of waves, surging heights and speeds beyond standard models.
The implications were alarming.
The offshore winter storm locked with warm unstable air propelled long traveling swell trains, waves crossing ocean depths only to increase in size.
When these encountered seismic disturbances near Oregon’s undersea faults, the result was devastating.
Unexpectedly powerful waves overwhelming every planned barrier and warning system.
Offshore, automated boys tried to relay information, but as Dr Renard pointed out the window between detection and disaster had shrunk to mere minutes.
Normally, our systems can see the risk develop.
Today, the events outpaced even our fastest alerts.
By the time the warnings went out, the damage was done.
For coastal Oregon, the event posed the biggest test yet, not only to budget and infrastructure, but to the scientific assumptions regarding the region’s vulnerability.
As the day unfolded with scientists unraveling the data in real time, the consensus was clear.
This disaster, while technically possible, was almost beyond rare probability.
What allowed it to occur at such scale, with tremors still faintly registering at sea.
Could greater threats still loom? The devastation reached far beyond battered neighborhoods and cracked seaw walls.
With every tide, land itself faltered.
At Gearhart, a stretch of dunes became a ragged lagoon by midday.
Salt water pouring through broken barriers, roots laid bare as homes hung perilously close.
Officials in Tielemuk reported parts of the coast highway collapsed into churning surf.
Waves gouging new inlets before onlooker’s eyes.
Warnings escalated with each high tide.
Emergency crews struggled to keep pace.
Villages cut off.
Lifeboats fing stranded families from flooded second stories.
Familiar streets unrecognizable under waves and trash.
A less visible danger emerged below ground along vulnerable bluffs.
Dr Victor Jang and local geologists recorded subtle persistent ground movements.
Areas battered by waves started to slip.
Incremental but detectable.
Once latent tremor signatures surfaced as shifting landforms.
We’re not just fighting water, explained Dr Jang.
The coastline itself is moving.
Erosion, hastened by the seismic episode, advances faster than anyone planned.
The immediate crisis was overwhelming flooding.
But the lasting threat may be the hidden disaster beneath.
Subsiding earth and creeping landslides destined to trouble these areas for months.
In Arch Cape, cliffside homes that stood for generations lost entire gardens overnight.
In Gold Beach, neighborhoods evacuated for both flooding and the risk of land sliding to sea after any fresh tremor.
Above the battered coast, other disasters compounded.
Power failures as water invaded substations, weakened towers losing signal, floodwaters isolating entire towns.
In command centers, the term compound hazard event replaced any illusions of reassurance.
Water, earth, and wind joined in ways too complex for the usual response, forcing evacuations farther inland than ever anticipated.
As day faded to night, a deeper anxiety crept in.
If the Pacific can orchestrate this convergence once, what might another season bring? Are isolated disasters now a thing of the past, replaced by risks that interact, amplify, and sidestep familiar patterns? If you find this coverage essential, subscribe now for ongoing updates into coastal safety, seismic risk, and disaster response.
Be ready for the future, not the past.
By midday, all sense of normaly along the coast evaporated.
Zones labeled low risk for decades now faced the raging sea.
Typically reserved for the wildest winter headlands in Seaside and Cannon Beach, homes and businesses supposedly above safe lines encountered flood waters they were never designed to withstand.
Sections of US 101 rebuilt after earlier storms failed in moments.
At Manzanita, a once stable stretch broke away beneath relentless wave attack.
Drivers halted inches from new cliffs that hours earlier had been pavement.
Rockaway Beaches schools became makeshift shelters cut off by floodwaters and downed communications.
Officials were most haunted by one reality, the events sheer unexpectedness.
For years, infrastructure was planned for patterns reflected in the past.
Surges rare, floods manageable, and land shifts slow.
This new storm changed all that.
In a few hours, every traditional forecast, every map of safe ground was overrun.
Dr Abigail Renard emphasized in an emergency field interview, “Our systems are built for single hazards, not for multiple events converging, “When storms and tremors happen together, our calculations break down.
We need new strategies.
” The implications went beyond immediate response.
Insurance, zoning, and even evacuation plans suddenly seemed outdated.
Lawmakers were forced to reconsider not just how to repair, but how to reshape coastal living.
At the water’s edge, residents faced a choice.
Adapt to these emerging threats or risk all to the next storm.
Slowly, old certainties faded.
The reliance on generational memory, the comfort in concrete and elevation, leaving only new questions.
How can communities design for resilience against threats more unpredictable than ever? If these events are just the beginning, what further storms might lie offshore? Through the evening, it became evident the ocean was not done remaking Oregon’s coast.
This was not a single wild surge or a brief moment of chaos.
Each new tide compounded the destruction, pushing water deeper, destabilizing land, eroding at foundations still water logged from earlier waves.
The Portland Coastal Research Center, guided by Dr Elsa McGregor reported with increasing urgency.
There was no break between surges, no chance for drainage, for repairs, for reprieve.
Instead, each cycle trapped water farther inland.
Rivers already high from weeks of rain now reversed, forced in by the advancing tides.
Inland valleys miles from the sea began to flood from underneath as seaater backed up riverbeds and filled low-lying land never before threatened.
Compound hazard is an understatement.
Dr McGregor’s team warned.
We see wave surges, persistent flooding, seismic ground shifts, each crisis feeding the next.
If one defense fails, the others quickly follow.
The phrase feedback loop of disaster emerged in briefings.
Wet hillsides began to crack and slip, battered by rain above and invaded by salt water below.
Even inland towns prepared for evacuation as rising waters overtook familiar drainage.
Night closed on a coastline transformed.
Satellite images showed the reality.
Washed out highways, reshaped esties, drowned forests.
Search crews cautioned that entire neighborhoods might remain cut off for days.
And with tremors still occasionally shaking the ground, there was no assurance the worst was over.
A deep sense of uncertainty lingered.
If forces this rare can collide once, could it mark the start of a new era where ocean, weather, and geology entwine in unpredictable ways? If you value detailed science-based coverage of disaster and resilience on the coast, stay connected.
Share your questions and experiences.
We are stronger together in preparedness.
Now in the quiet after this historic assault, communities look outward toward the ocean, the unsettled sky, and the ground that continues to shift.
Damage is everywhere.
Splintered boardwalks, lost roads, families carrying what they can as they seek shelter.
Nature has redrawn the map, but the deeper impact is psychological.
The Oregon coast, once defined by enduring traditions and the seeming permanence of rugged headlands, faces the reality that the rules are changing.
Community leaders turn to scientists and residents to one another as everyone asks, “How can we defend a shifting coastline when risk no longer follows familiar cycles?” Dr Marcus Holay, standing amid the remnants of a field station, captured the new challenge.
We are in a new era.
Every protective measure, be it maps, walls, dunes, or geology, has been stressed beyond past limits.
The future depends on what we learn and how willing we are to prepare for the unknown.
Yet, amid broken landscapes, resilience emerges.
Neighbors support one another.
Volunteers shore up makeshift barriers, and urgent efforts to adapt accelerate.
Every act of rescue, every gesture of solidarity helps hold the region together.
Scientists now say the Oregon coast is a lesson, a warning about what happens when rare disasters overlap and the margin for error disappears.
The ocean must be seen a new, not just as backdrop or foe, but as a powerful evolving force, always in tension with the land.
As night returns and families regroup, a quiet vigilance grows.
Alerts are heeded.
Hillsides are scanned for movement.
All eyes remain on the Pacific, watching for any signal that another round or the long process of rebuilding is at hand.
This story is still unfolding, written in silt and splintered timber, tracked by satellites, and etched into memory.
One fact remains.
The Oregon coast will not return to what it was.
But as long as the community listens and learns, there is hope that these lessons will serve not only to survive, but to thrive on a newly drawn edge between sea and land.
Stay alert for updates.
Your awareness and preparedness are key to the coast’s future.
Share your stories, thoughts, and questions.
Each is a thread in the fabric of resilience we now must weave
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