Загрузка...

PORTUGAL ON EDGE! Massive Magma Surge Beneath São Jorge Sparks La Palma-Style Fears

A newly published scientific study has revealed that one of the most dramatic underground magma intrusions in recent European history happened silently beneath São Jorge Island in the Azores — and almost nobody realized how close the island may have come to a volcanic eruption. Researchers now say that nearly 20 million cubic meters of magma surged upward from deep beneath the Atlantic Ocean during the 2022 seismic crisis on São Jorge, a volume even larger than the magma intrusion that preceded the destructive 2021 La Palma eruption in the Canary Islands. Yet despite the enormous scale of magma movement beneath the island, no eruption occurred. The reason why is changing the way volcanologists think about eruption forecasting around the world.

This video breaks down the new 2026 Nature Communications study that reconstructed the hidden magma intrusion beneath São Jorge using roughly 18,000 precisely relocated earthquakes, ocean-bottom seismometers, GPS deformation data, and satellite radar imaging. Scientists discovered that the magma rose rapidly from more than 20 kilometers deep to within about one mile of the surface in only a matter of hours — and much of that ascent happened with little to no obvious seismic warning. By the time intense earthquake swarms triggered emergency alerts, evacuations, military preparations, and volcanic warnings across the island, the magma had already stalled beneath the surface.

The study reveals how the Pico do Carvão Fault Zone acted both as a pathway and a pressure-release system for the magma, allowing it to travel upward silently through pre-existing fractures before gas pressure escaped sideways through the fault network, preventing a full eruption. Researchers warn that this kind of “stealth” magma ascent may not be unique to São Jorge and could potentially occur in other volcanic regions where fault systems provide fast underground pathways for magma movement.

The video also explores the geological history of São Jorge and the Azores Triple Junction, where the North American, Eurasian, and African tectonic plates interact beneath the Atlantic Ocean. Historical eruptions on São Jorge in 1580, 1808, and probable offshore volcanic activity in 1964 demonstrate that this is an active volcanic system with a long history of seismic unrest, lava flows, explosive interactions with groundwater, landslides, and evacuations.

Comparisons to the 2021 Tajogaite eruption on La Palma highlight just how significant the São Jorge intrusion really was. The La Palma eruption destroyed thousands of buildings, buried communities beneath lava, displaced thousands of residents, and caused massive economic losses after a smaller magma intrusion than the one now documented beneath São Jorge. Scientists now believe the 2022 Azores crisis may represent one of the clearest modern examples of a failed eruption that came extremely close to breaking the surface.

This documentary-style breakdown covers the science behind volcanic intrusions, dike propagation, tectonic fault systems, earthquake swarms, magma migration, volcanic monitoring technology, eruption forecasting challenges, and why the São Jorge event is now being studied as a warning sign for volcanic regions across the planet. From the Azores to the Canary Islands, Alaska, Italy, and beyond, scientists are now asking an urgent question: how many volcanoes are capable of rapid magma ascent with warning signs that arrive too late?

This is one of the most important volcanic research stories of 2026 — and a powerful reminder that some of the most dangerous geological events on Earth can happen deep underground long before the world realizes what is unfolding beneath the surface.

Видео PORTUGAL ON EDGE! Massive Magma Surge Beneath São Jorge Sparks La Palma-Style Fears канала GeoDisaster Hub
Яндекс.Метрика
Все заметки Новая заметка Страницу в заметки
Страницу в закладки Мои закладки
На информационно-развлекательном портале SALDA.WS применяются cookie-файлы. Нажимая кнопку Принять, вы подтверждаете свое согласие на их использование.
О CookiesНапомнить позжеПринять