Relamination and the growth of continents

New research led by scientists at the National Museum of Natural Sciences has identified a major geological process that helps explain how Earth’s continents have evolved over billions of years. The study focuses on a mechanism known as relamination, which occurs during continental collisions when one tectonic plate is forced beneath another through subduction. Rather than disappearing permanently into Earth’s interior, fragments of the lighter continental crust can detach from the sinking plate, rise upward again, and become incorporated into the lithospheric mantle of the overlying plate. This process creates a hybrid zone of crust and mantle material that later produces distinctive magmas associated with mountain-building events.

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Earth Index and the searchable planet 

The concept of searching the Earth like a vast digital database has existed for years in scientific and technical discussions, but recent advances in artificial intelligence are finally making it practical. At the center of this shift is Earth Index, a platform developed by the nonprofit Earth Genome that enables users to search satellite imagery based on visual similarity rather than traditional map analysis. Instead of manually reviewing massive datasets, users can simply highlight an example—such as a mining site, illegal airstrip, patch of deforestation, fishing vessel, or industrial facility—and ask the system to locate similar patterns across other regions of the world.

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Mount Etna’s strange magma mystery

Mount Etna is one of the oldest and most active volcanoes in Europe, with a history stretching back over 500,000 years. Rising to about 3,400 meters on the island of Sicily, it erupts frequently—often several times each year—yet continues to puzzle scientists. Unlike most stratovolcanoes, which typically produce more silica-rich magma, Mount Etna is known for its unusually high output of alkaline lava. This type of lava is typically associated with slower formation processes, making Etna’s sustained and prolific eruptions difficult to explain using conventional geological models.

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East African Rift shapes human fossil record

New research suggests that the slow breakup of Africa may be closely tied to one of the most important records of human evolution on Earth. In eastern Africa, the Turkana Rift—part of the broader East African Rift—is revealing how deep geological forces not only reshape continents but also influence what evidence of early human life is preserved. Scientists have discovered that the Earth’s crust beneath this region is significantly thinner than previously believed, indicating that the rifting process is far more advanced and could eventually lead to the continent splitting apart.

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Hidden activity beneath silent volcano

For more than 100,000 years, the Methana volcano in Greece appeared inactive, showing no visible signs of eruptions such as lava flows, ash clouds, or explosions. Because of this long period of silence, it was widely assumed to be extinct. However, new research led by ETH Zurich and published in Science Advances reveals a very different story. Beneath the surface, the volcano remained highly active, steadily accumulating large volumes of magma within its underground chambers.

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Sperm whale communication mirrors human speech 

Recent research into sperm whale communication is revealing striking similarities between how these massive marine mammals interact and how humans use language. Although sperm whales and humans diverged evolutionarily more than 90 million years ago, scientists are discovering that their communication systems share surprising structural features. A new study shows that sperm whales use patterns of clicks, known as codas, that resemble elements of human speech, including something akin to an “alphabet” and vowel-like variations.

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Supereruptions and hidden magma forces

Supervolcanoes are capable of producing some of the most powerful natural events on Earth, known as supereruptions, which can eject more than 1,000 cubic kilometers of material into the atmosphere. These massive eruptions can alter global climate by blocking sunlight, lowering temperatures, and disrupting ecosystems for years. Because of these far-reaching consequences, scientists are working to better understand the processes that lead to supereruptions and how these systems behave beneath Earth’s surface.

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AI maps ocean currents in real time

Scientists have developed an innovative technique to measure ocean currents with unprecedented detail and frequency, addressing a long-standing gap in ocean observation. The method, known as GOFLOW (Geostationary Ocean Flow), uses deep learning to analyze thermal imagery from existing weather satellites, eliminating the need for new hardware. By leveraging satellites already in orbit, this approach represents a major advancement in understanding how the ocean moves and interacts with Earth’s climate system.

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Nitrous oxide lifetime shrinks in warming climate

Scientists at the University of California, Irvine have identified an important and previously underappreciated climate feedback involving nitrous oxide that could significantly influence future climate projections. Using two decades of satellite data from NASA’s Microwave Limb Sounder (2004–2024), researchers found that the atmospheric lifetime of this gas is decreasing by approximately 1.4 percent per decade. This means that nitrous oxide, a potent greenhouse gas and ozone-depleting substance, is being broken down faster in the atmosphere than previously understood.

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Arctic permafrost thaw accelerates emissions

For decades, Arctic permafrost has functioned as a massive natural storage system, effectively trapping carbon-rich organic material beneath frozen ground and slowing the release of climate-warming gases. However, new experimental research from the University of Leeds reveals that this system may be far more vulnerable than previously understood. As temperatures rise and frozen soils begin to thaw, the physical properties of permafrost change in ways that significantly accelerate the movement of gases into the atmosphere, potentially amplifying climate change.

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