9 Alarming Truths About the Cascadia Mega-Tsunami Threat

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“In minutes, we’ll see two meters of sea levels rise,” said Virginia Tech’s Prof. Tina Dura in a recent discussion with BBC Science Focus. These are basically alarming words to anyone living along the Pacific Northwest coastline. Scientists today now believe the Cascadia Subduction Zone, a massive fault line running from Northern California to British Columbia, holds the potential to unleash a catastrophe so enormous that it will redefine the U.S. West Coast for many centuries to come.

This particular fault has remained ominously quiet for more than 300 years. But the absence of noise is not a comforting prospect in the world of geology. Finally unearthing the silence, the outcome could easily become a disaster in the books of worst natural calamities. Recent studies, integrating up-to-date mapping, paleoseismological data, and climate models, indicate a catastrophic combination of violent shaking, sinking land, monumental waves, and constant floodings.

This listicle will delve into the most alarming research that has emerged recently, addressing why experts believe that for communities stretching from California to Canada, and indeed all the way to Alaska and Hawaii, time is literally ticking away.

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1. A Fault with the Capability of Producing Earthquakes of Magn

The Cascadia Subduction Zone is the fault line where the Juan de Fuca Plate is being pulled under the North American Plate. Seismological studies indicate that it has generated earthquakes of magnitude 8.7 to 9.2 that recur every 200 to 800 years. The most recent major earthquake took place on January 26th in 1700. The tsunami formed from the earthquake was recorded on the shores of Japan. Based on the US National Seismic Hazard Model, the probability of the occurrence of an earthquake of magnitude 8.0 or larger in the next 50 years is 15%. All four fault segments can break simultaneously in the most pessimistic outlook. This is estimated to generate the same amount of power that was unleashed in the 2011 Tohoku Earthquake.

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2. Mega-Tsunami Waves Reaching 1

In contrast to normal tsunami events, which could result in waves of several meters in height, the possible Cascadia tsunami could generate waves reaching 300 meters (1,000 feet) in height. These would swiftly destroy cities along the coastal areas following the earthquake. According to scientists, the effects of the tsunami would not remain confined to the Pacific Northwest region but would also affect Alaska and the Hawaiian islands because of their own tectonic and volcanic patterns. The tsunami would continue for hours and even days in some regions.

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3. Sudden Land Subsidence Expanding Flood

Recent modeling predicts a land subsidence of up to 0.23 to 2.67 meters (0.76 to 8.76 feet) of coastal land in a matter of minutes following the earthquake. This will cause the land within the floodplain area to double in size by up to 300 km², effectively doubling the exposure of residential, transport, and vital infrastructure to flood levels. Even areas not affected by the tsunamis may end up permanently submerged, making them unfit for human habitation.

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4. Critical Infrastructure in the Crosshairs

“The preliminary flood maps call for an area much larger than originally anticipated to be placed inside the flood zones,” according to planning commission spokesperson Harold Earls. “It would inundate airports, facilities for emergencies, wastewater treatment plants, an electric station, and sources of possible pollution, such as gas stations and chemical storage units, totaling 57 locations.”Underwater roadways and flood-damaged emergency centers would damage abilities for responses to occur. “Sea water damage to soil can lead to an irreparable degradation of fertile land,” according to Alberto Arenas of SE joint venture.

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5. Climate Change Exacerbating the Disaster

“Sea level rise of up to 0.9 meters by the year 2100 could result in a three-fold increase in flood exposure if coupled with subsidence caused by an earthquake.” This could lead to an increase of flood plains by an estimated 370 km², thus making it impossible for people to live there due to rising high tides and storm surges that could cause even small weather changes to result in flooding.

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6. No Time for Evacuation

From violent shaking through tsunami arrival, time would be extremely short. Shaking might take four to six minutes, after which 15 to 20 minutes might pass before the first wave reaches land. In many places, the subsidence associated with a quake would result in immediate flooding that could arrive before tsunami inundation did. Scientists emphasize that this kind of catastrophe would result in “no time for adaptation and mitigation.”

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7. Modern Mapping Unveils Fault Segmentation Dangers

The high-resolution imagery of the fault obtained in a marine field experiment in 2021 has identified four segments of the fault separated by vertical faults. The segment in the north part of the fault system off the coasts of Washington State and B.C., Canada, has a shallow slope; hence the size of the rupture surface as well as the earthquake shaking and tsunami hazards areespecially dangerous. This segment alone has the capability of triggering a magnitude 9 earthquake that poses a threat to Seattle and Vancouver cities.

Image Credit to Wikimedia Commons

8. Historical Lessons from Global Quakes

Historical megathrust earthquakes are chillingly instructive. In 1960, the earthquake off Chile flooded agricultural land and led to massive displacements of people; the 1964 earthquake off Alaska damaged infrastructure and led to the displacement of people; the Sumatra-Andaman earthquake of 2004 led to the deaths of almost 230,000 people; and the 2011 earthquake off Japan led to the nuclear disaster at Fukushima.
This is all the more precarious for Cascadia because the region is much more heavily populated and

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9. Urgent Need for Preparedness

Specialists suggest that the information on earthquakes and subsidence should be incorporated in hazard maps, that critical infrastructure should be moved or made resilient, that wetlands should be restored, and that development in vulnerable areas should be prohibited. Public education campaigns must walk the tight rope between sense of urgency and reality. As Prof. Dura pointed out, “We’re all working together. And a lot of new information is coming out.”

The Cascadia Subduction Zone is a sleeping giant, and every passing year without an eruption only builds the pressure that this zone has. When this disruption finally happens, the forces that will come into play earthquake energy, massive waves, lowering ground levels, and a rise in sea levels may very well redesign the map for the Pacific Northwest. The data is unambiguous: this is a matter not of if, but of when. The only question now is how this danger will be acted on.

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