US SHUTS DOWN Oregon After This Terrifying Discoveries on Volcanoes Before It's Too Late!

looking good out there. Uh, still very busy on area highways and freeways. And we have these significant closures this morning as well because of down power lines. Highway 26 still closed at Welches and also a closure on Highway 99W at Highway 18. ODOT just put out a list of about a dozen highways in the valley and north coast area that are closed because of down lines. This is unfolding right now. In a single breathtaking span, federal authorities have made a drastic move, shutting down vast stretches of Oregon in the wake of discoveries so alarming, scientists say the entire Pacific Northwest has entered a new age of geological risk. In this broadcast, we follow the evidence as it arrives. The trembling of ancient mountains, the swelling of ground once thought forever stable, and the ominous energy pulsing miles beneath the surface. Government agencies have mobilized. Emergency protocols rarely invoked are suddenly in motion. And the reason, as we'll see, is rooted in the scientific understanding of geology, earthquakes, and volcanic forces gathering [music] strength. From the restless lava chambers of Mount St. Helens to the hidden threat of the undersea axial volcano, every new warning points to an escalating scenario. Toxic spills, hazardous gas plumes, and the everpresent shadow of a [music] mega quake. Each chapter of this drama brings a new revelation, a threat more intense than the last. What invisible forces are emerging below Oregon right now? Why is the US government drawn an unprecedented line in the sand, locking down communities, closing infrastructure, and warning residents to keep out? The answers are stranger and more unsettling than anyone expected. [music] Stay with us as we open the case file on Oregon's awakening, one chapter at a time. Chapter 1. Oregon's ground rising, a slow, steady threat. It started as an anomaly, almost a rumor within geological circles. Out in central Oregon, ground that seemed immutable began to rise almost imperceptibly but steadily year after year. The measurements [music] were undeniable. Satellite data confirmed a swelling bulge [music] well outside the ordinary cycles of the region's geology. Could the earth beneath Oregon [music] be silently, inexraably inflated from below? Dr. Belinda Stewart Harkness, geologist and seismic risk specialist, points [music] to two decades of precise GPS and satellite data. Across an expanse of once quiet countryside, the crust is lifting by inches, [music] more than normal tectonic drift would explain. The source deep-seated changes likely related to slowly accumulating magma or other dynamic processes within the crust. What makes this so extraordinary, Stuart Harkness explains, is the quiet. No dramatic earthquakes, no visible eruptions, only the patient, relentless upward push of natural forces below. The phenomenon has prompted scientists to reconsider Oregon's volcanic history. Small increases in hotring activity and subtle ecological shifts like changing tree lines were noted, but only when added to the pattern of uplift did the full picture emerge. In remote [music] forests, isolated geothermal vents have appeared, accompanied by observations of wildlife behaving unusually in these areas. The science is clear. Steady, long-term ground inflation is a warning sign of unrest. The bulge signals building pressure in underground geological chambers which could eventually lead [music] to rapid transformations. While there is currently no sign of imminent eruption, ongoing monitoring is essential as the region continues [music] to change quietly but with the potential for sudden transition. What else is being [music] concealed under our feet? Chapter 2. Underwater volcano axial volcano activity. Picture this. 5,000 ft beneath the Pacific off Oregon's coast, a behemoth is stirring, a gigantic underwater volcano known as Axial Volcano. On monitoring screens, scientists observe a rising tempo, pressure building, low-frequency tremors echoing through the seafloor, and temperature spikes. Could one of the ocean's most active volcanoes erupt without warning right at [music] Oregon's doorstep? Dr. William Chadwick of the Pacific Marine Environmental Laboratory points to instrument records, pressure sensors showing the caldera floor rising by feet in only months, seismicity ticking upward in clusters, and superheated fluids venting from fissures. In the silent dark, magma is gathering force. Notably, Axial's past eruptions have occasionally occurred with only hours or days of warning, making it one of the most closely monitored underwater volcanoes in the world. The science behind this is sobering. Underwater eruptions can generate local hazards such as hot mineral-rich water plumes [music] and in some cases trigger underwater landslides, which can in turn cause tsunamis. Researchers tracking Axial's inflation cycles know that the next eruption, whenever it comes, could threaten marine life, disrupt fisheries, and create research opportunities and public concern in equal measure. Surveys show that volcanic gas releases and hot mineral-laden water from axial can drop oxygen levels locally and form temporary dead zones near the coasts. These changes affect local ecosystems and fisheries, adding ecological stress to the geological risks beneath the waves. Are we truly prepared for a blast from beneath the ocean? Chapter 3. Mount St. Helens, the sleeping giant stirs. Shock waves ripple through the scientific community each time Mount St. Helens, burned into memory by its 1980 eruption, shows new activity. [music] The signals this time are uncomfortably familiar. Hundreds of small earthquakes rattle its slopes. Gas [music] readings spike and the mountain surface pulses in rhythm with forces miles below. Could the infamous volcano be gearing [music] up for renewed activity? Dr. Seth Moran, lead scientist at the USGS Cascades Volcano Observatory, confirms the data. Seismic swarms, clusters of shallow earthquakes are occurring. These are closely monitored as past patterns have sometimes preceded dome building eruptions. Instruments detect tremors rising through magma conduits carrying heat and pressure toward the surface. While no eruption is imminent, increased seismicity and ground deformation are [music] reminders that Mount St. Helens remains active, not dormant. As more heat and gas migrate upward, [music] the chance of future eruptions remains real. Though their timing, size, and impact are difficult to predict, scientists are maintaining vigilant observation, including remote cameras, gas [music] sensors, and satellite monitoring for ground movement. Seismic swarms, bulging of the crater [music] floor, and minor landslides are watched closely for any sign of escalation. These observations reinforce the reality that the system beneath Mount St. and Helens is dynamic. [music] Will the Northwest ever again see a major eruption or will these rumblings remain [music] warnings for the future? Chapter 4. Tremors in the deep. Subductions silent [music] power. Unexplained tremors have been detected thousands of feet beneath the Pacific seabed near Oregon, a depth beyond human reach. Sensors pick up slow slip events. Massive blocks of earth shifting against each other over days or weeks instead of seconds. Is a hidden tectonic monster preparing to make itself known? Dr. Emily Roland, an earthquake specialist, interprets these signals as slow slip events. This process, nearly invisible at the surface, adds strain to the deeper subduction zone offshore. When this pressure eventually releases, it could unleash a mega thrust earthquake, the kind seen only a handful of times in recorded history. These slow slip events extend for hundreds of miles along the fault and are monitored intensively. Researchers use high-tech underwater seismometers and pressure gauges to track this silent activity. Marine life sometimes displays migration patterns [music] coinciding with heightened seismic periods, though cause and effect are difficult to prove. Within the scientific perspective, slow slip events often precede or influence larger earthquakes by increasing strain. [music] Every tremor brings Oregon closer to another chapter in its seismic story. Is the chain reaction already gathering momentum beneath the Pacific Northwest? Chapter 5. Cascadia Mega Thrust, [music] the greatest threat. Off Oregon's coastline lies the Cascadia Subduction Zone. A mega- thrust fault hundreds of miles long, silent for centuries. When this fault slips, it can produce one of the planet's most powerful earthquakes. Could a single shift turn Oregon's coast into the epicenter of a [music] national disaster? Data from the Pacific Northwest Seismic Network and geological records confirm a repeating cycle. catastrophic events separated by intervals of 200 to 600 years, the last occurring in 1700 and documented by both Native American oral histories and tsunami deposits as far away [music] as Japan. Scientists stress that the next event is a question of when, not if. Modern infrastructure faces challenges from this looming threat. Preparations include evacuation drills, increased warning sirens along the coast, and paleocismic research, the excavation of coastal layers to reveal evidence of past tsunamis. These findings reinforce how regularly the region has been reshaped by powerful earthquakes. Even moderate increases in regional seismicity are now seen as possible harbingers of a larger event. The urgent hope that improved monitoring and preparation [music] will offer crucial lead time for millions at risk. Will this ancient cycle's next chapter begin in our lifetime? Chapter 6. Toxic gas plumes. An invisible hazard. Imagine an invisible threat. [music] Plumes of volcanic gases such as sulfur dioxide and carbon dioxide rising from unseen fractures. Recent research underscores that such emissions can be dangerous, especially [music] if concentrated in valleys or depressions. Could silent clouds of deadly gas present one of Oregon's [music] greatest ongoing hazards? Analysis of volcanic and geothermal systems reveals scenarios where shifting ground might open vents, suddenly releasing gases. While these incidents are more common in other regions, the hazards are not theoretical. Dense [music] volcanic gases have injured or killed both people and animals elsewhere. In Oregon, first responders increasingly carry gas meters and take precautions [music] in known geothermal zones, livestock, and disrupt agriculture. While widespread poisoning has not been reported in Oregon, monitoring networks have expanded to better safeguard rural areas, and scientists are studying gas emissions more intensively. Are these invisible emissions the next public safety challenge for the Northwest? Chapter 7. Shattering infrastructure, collapse on the horizon. Steel, concrete, glass, none of these are immune to Earth's power. Recent research and disaster planning underscore a looming risk. Widespread infrastructure collapse if Oregon is struck by a combination of geological threats. Could critical lifelines fail not from lava, but from quakes and ground deformation. Engineers warn of vulnerabilities across Oregon's bridges, tunnels, [music] and utilities. Many structures date back decades and were not built to modern seismic standards. Even modest earthquakes or ground movement from magma shifts can damage or collapse vital infrastructure. Data from other catastrophes around the world repeatedly reveal that infrastructure is often among the first and most debilitating losses. Utilities are planning, water treatment plants are being upgraded, hospitals retrofitted, and transportation routes mapped for redundancy. Yet, Oregon's geography filled with bottleneck passages and remote towns means a single failure could isolate large areas. Can Oregon's built environment withstand the simultaneous effects of earthquake, landslide, and volcanic emergencies? Chapter eight. Wildfires fueled by eruption. Volcanic hazards often conjure images of lava, but in forested states like Oregon, wildfires are serious secondary risks. Hot ash, lightning, [music] and heat from eruptions can ignite forests and grasslands, especially during droughts. Could eruptions or vigorous geothermal activity trigger wildfires that overwhelm the land? History shows that volcanic ash falls and heat have sparked wildfires. Mount St. Helens's 1980 eruption ignited blazes on its slopes and wind carried embers help them spread. Scientists note that volcanic ash smothers vegetation and combined with dry conditions and heat creates perfect wildfire conditions. Recent seasons shaped by climate change and droughts have primed Oregon's forests for more intense [music] burning. Emergency responders warn that concurrent volcanic and wildfire incidents could stretch their capacity to the limits. Our wildfires the overlooked hazard intertwined with Oregon's volcanic landscape. Chapter nine. Seismic swarms prelude to disaster. A series of tiny nearly constant earthquakes. Seismic swarms. sometimes herald significant geological change. These patterns may precede volcanic eruptions or shifts in the landscape. Are these swarms Oregon's ticking clock, counting down to possible upheaval? Scientific records from volcanic regions demonstrate a link. Before eruptions, swarms of tiny quakes often mark magma rising and fracturing overlying rock. In Oregon, increasing swarm activity in previously quiet areas raises concern. [music] These swarms can also loosen slopes, increasing landslide and infrastructure risks. Communities have already experienced minor swarms, [music] reporting shaking windows, and restless animals. Emergency managers use these events to educate the public about early warnings, evacuation routes, and the importance of rapid response. Is Oregon [music] in the calm before a geologic storm? Chapter 10. Deep earthquakes. Pressure from below. While most people fear surface quakes, some of Oregon's recent seismic alarms come from deep underground. These quakes originating many miles beneath the surface reflect the ongoing dynamism of Earth's mantle and crust. Could deep sourced quakes help trigger surprises closer to home? Geophysical data show that deep earthquakes occasionally transmit energy upward, possibly disturbing shallower fault zones. Dr. Linda Stewart Harkness and colleagues have documented deep tremors and their relationship to shifting crustal conditions above. While these events rarely cause surface damage directly, scientists watch for signs that deep movement might catalyze near surface changes. Borehole sensors in Oregon occasionally detect shock waves rising from [music] great depths, offering researchers precious seconds of advanced notice for certain events. Sometimes surface hydrothermal features become active after deep tremors, hinting at connections from the deep earth to what [music] we see above. Is the ground beneath Oregon concealing even greater forces waiting their turn? Chapter 11. The invisible bulge. Silent crisis. Not all threats announce themselves loudly. Some creep incrementally over years. [music] Oregon's measured surface uplift shows that major geological changes [music] can unfold almost unnoticed. Can slow steady deformationation signal disaster in the making? Satellites equipped with interferometric synthetic [music] aperture radar ins have tracked persistent subtle ground swelling in [music] central Oregon. Scientists compare this to stretching a rubber band. Tension grows slowly, but if a threshold is reached, sudden change becomes possible. Mathematical models treat the bulge as a warning that the area's crust is under increasing stress. Hydraologic studies reveal changes in spring chemistry above the bulge, a potential sign of deeper shifts. Local ground surveys also detect emerging surface cracks and minor faults. Residents previously unconcerned now keep watch from emergency agencies and for changes in local geography. Is slow ground movement a silent alarm from nature? Chapter 12. Tsunami warnings, disaster on two fronts. It's a chilling scenario. The ground shakes, then minutes later, a wall of water barrels toward the coast. Studies show Oregon is vulnerable to tsunamis from both distant [music] and local sources. Could multiple triggers create the ultimate coastal disaster? Collaborative research with NOA has identified two main tsunami sources. subduction earthquakes like those from the Cascadia fault and underwater landslides or [music] volcanic eruptions. Modeling predicts inundation patterns for vulnerable coastal towns with little time for warning. Some waves could arrive from as far as Japan, others from local sources [music] within minutes. Coastal communities hold regular evacuation drills, install warning sirens and towers, and map escape routes to higher ground. While technology offers alerts, the gap between detection and arrival leaves most people [music] with only minutes to act. A sobering reality that compels ongoing preparation. Will Oregon's next warning lead to life-saving action? Chapter 13. Infrastructure on edge. The human challenge. As authorities work to retrofit bridges, fortify dams, and secure vital communications, Oregonians face the reality of living within a complex risk landscape. Will human ingenuity hold back [music] the tide of natural hazards and safeguard communities during disaster? Civil engineers, emergency planners, and policymakers are focused on shoring up vulnerable infrastructure. Seismic upgrades are underway for schools, hospitals, and key transportation routes. Satellite-based tools are being deployed for backup communications if ground systems fail. Despite these efforts, many rural areas, and old structures remain at risk. Simulated emergencies reveal gaps, blocked roads, downed power lines, and damaged water supplies could turn short-term events into long-term crises. The consensus among planners and scientists is clear. Redundancy, preparation, and rapid mobilization are crucial, but there will always be limits to what can be protected. Is Oregon prepared to rebuild [music] and adapt again and again in the wake of disaster. Chapter 14. Wildcard hazards. The unknowns lurking [music] below. Despite decades of research, Oregon's geology contains unsolved mysteries. Unmapped faults, hidden magma [music] chambers, and chemical pathways could still surprise scientists and residents alike. Have we only begun to understand the dangers below? Dr. William Chadwick, among others, highlights the limitations [music] of our current knowledge. Evolving magma pathways, unexpected gas interactions, and vast unmapped regions [music] mean unforeseen events remain possible. Geological history is full of surprises. Eruptions larger than modeled, [music] quakes beyond predicted strength, landslides that transform entire valleys overnight. Field reports tell tales. Lost sensors, sudden unmapped mud flows, valleys subtly shifting in a year's span. Oregon's rugged [music] back country, rarely visited, may still hold the next unexpected threat. One that could reshape the landscape in days. With each study, we realize the greatest threats may be those [music] not yet detected. Chapter 15. A new era for Oregon. In the shadow of converging forces, Oregon stands at a crossroads. Ground closures, public warnings, and scientific vigilance form a tapestry of measured preparation in [music] the face of geologic risk. Each story, uplifts, tremors, gas emissions, contributes [music] to a mosaic of transformation that transcends any one event. No single disaster has struck. Yet, an unfolding drama plays out quietly beneath Oregon's mountains, forests, and coasts. The region's fate hangs not on luck, but on the community's willingness to remain informed, ready, and resilient. Every factor, risk of eruption, [music] seismic threat, vulnerability of infrastructure, adds to the sense of urgency that drives collaboration among scientists, officials, and the public. If hope exists, it is found in vigilance. Scientists like Dr. Linda Stewart Harkness, Dr. William Chadwick, and Dr. Emily Roland and others continue to scrutinize every tremor and every [music] change, working closely with emergency managers and public officials. Decisions, including regional closures and evacuations, [music] are made carefully and with deep respect for both science and community well-being. The questions linger unanswered after each [music] warning. Could this be the beginning of a legendary eruption? Will another catastrophic quake strike without warning? Or are there dangers no one has yet [music] imagined stirring silently below? For now, Oregon waits, alert, aware, and prepared for whatever comes next. In this new age of geological transformation, the most vital resources remain preparation, vigilance, and the enduring spirit of those determined to meet [music] the unknown head on. Thank you for joining us for this urgent journey into Oregon's awakening. The ground beneath our feet may never feel the same, but through awareness and science, we equip ourselves for the challenges ahead. Keep informed, heed warnings, and remember, in a world shaped by deep time and sudden upheaval, the most important resource is preparedness. Stay alert, stay safe, and together we can weather even the Earth's mightiest storms.