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Evidence has emerged pointing to a significant role played by an ancient geographic hotspot in shaping the Great Lakes. Researchers have linked the formation of these massive water bodies to a hotspot that interacted with the Earth’s lithosphere millions of years ago. While the lakes are commonly attributed to glacial activity during the Ice Age, recent findings suggest that deeper geological processes may have contributed to their formation, providing insight into their extraordinary depth and size.

Study Highlights Geological Interactions

According to research published in Geophysical Research Letters, a team of scientists from the University of Houston and the University of Arizona investigated the Cape Verde hotspot’s historical activity. Hotspots, known for generating heat and material flow from the Earth’s mantle, are believed to have influenced the Great Lakes region approximately 225 to 300 million years ago. As Pangea, the ancient supercontinent, moved over this hotspot, thinning of the lithosphere occurred, making the ground beneath more susceptible to external forces.

Seismic Clues Support Hotspot Theory

As reported by phys.org, data from seismic wave analyses supported these claims. Unusual horizontal wave movement beneath the lakes indicated lithospheric deformation. This anomaly aligned with the passage of North America over the hotspot during its drift over geological time. These conditions, as reported, would have created a weakened crust, later amplified by glacial activity during the Ice Age.

Hotspot’s Legacy in the Great Lakes Formation

The research outlines how the Cape Verde hotspot likely underlay Lake Superior, Lake Huron, and Lake Erie at different points in history, contributing to the geological features that enabled the Great Lakes to form. The fragile crust allowed ice to carve deeper and larger depressions than would have been possible otherwise, creating the unique landscape seen today.

These findings reshape understanding of the Great Lakes’ origins, suggesting that both deep-Earth processes and surface phenomena played critical roles in their formation.

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Webb Telescope Spots Possible Jellyfish Galaxy 12 Billion Light-Years Away

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Webb Telescope Spots Possible Jellyfish Galaxy 12 Billion Light-Years Away

Astronomers have discovered a new “jellyfish” galaxy about 12 billion light-years away using the James Webb Space Telescope. It appears to have tentacle-like streams of gas and stars trailing off one side, a signature feature of jellyfish galaxies. These galaxies develop such trails via ram pressure stripping as they move through dense cluster environments, triggering star formation in the stripped gas. The find was made by Ian Roberts of Waterloo University, and details are described in a preprint on arXiv. More analysis is needed to confirm the classification, but early signs strongly suggest this object is indeed a jellyfish galaxy.

What Are Jellyfish Galaxies?

According to NASA, jellyfish galaxies are so named because of the long, trailing streams of gas and young stars that extend from one side of the galaxy. This phenomenon occurs when a galaxy moves rapidly through the hot, dense gas in a cluster, and ram pressure strips material away. The stripped gas forms a wake behind the galaxy, and this wake often lights up with bursts of new star formation. At the same time, the process can deprive the galaxy’s core of gas, potentially slowing star formation in the galaxy’s center.

Because the jellyfish stage is short-lived on cosmic timescales, astronomers rarely catch galaxies in this act. Studying jellyfish galaxies gives scientists insight into how dense environments affect galaxy evolution and star formation.

Discovery and Future Research

The researchers caution that the galaxy’s apparent “tentacles” may partly be an artifact of the imaging method. If confirmed, this object (COSMOS2020-635829) would be the most distant known jellyfish galaxy, offering a rare glimpse of how ram pressure stripping and cluster-driven quenching operated in the early cosmos. As the study authors note, finding a jellyfish at z>1 reinforces the idea that these environmental effects were already at work near the peak of cosmic star formation.

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Mars Dust Devils May Spark Lightning, Might Pose Risks to Rovers: Study

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Mars Dust Devils May Spark Lightning, Might Pose Risks to Rovers: Study

Dust devils on Mars – swirling columns of dust and air that often scour the Red Planet’s surface – may be crackling with electricity, a new computer-modeling study suggests. Researchers led by Varun Sheel simulated how Mars’s dry atmosphere and frictional dust collisions charge up grains inside a vortex. They found these fields could grow so strong that brief lightning-like discharges might occur. This electrification is a concern for surface missions, since charged dust could cling to rover wheels, solar panels and antennas, blocking sunlight and interfering with communications.

Formation and Features of Martian Dust Devils

According to the study, dust devils form when the Sun heats Mars’s surface, causing warm air to rise and spin into vortices. Colder air rushes inward along the ground, stretching the rising column upward and whipping dust high into the sky. Because Mars has lower gravity and a thinner atmosphere than Earth, its dust devils can tower much higher, three times larger than storms on Earth. NASA’s Viking mission first detected Martian dust devils; later rovers like Curiosity and Perseverance have filmed them sweeping across the dusty plains. These whirlwinds clean off solar panels – as happened with Spirit in 2005 – but more often they stir up fine dust that can coat instruments.

Electrification and Risks to Rovers

Dust grains in Martian whirlwinds can pick up charge through collisions (a triboelectric effect). Sheel’s models predict that this charge separation can create strong electric fields inside a dust devil. These fields could even exceed Mars’s atmospheric breakdown threshold (around 25 kV/m), enough to spark lightning in the vortex. NASA’s Perseverance rover recorded what appears to be a small triboelectric discharge when a dust devil passed overhead.

Even without lightning, any static buildup is problematic. As planetary scientist Yoav Yair notes, “Electrified dust will adhere to conducting surfaces such as wheels, solar panels and antennas,” potentially reducing sunlight reaching panels and jamming communications. Rovers may need new design features or procedures to handle this unusual Martian weather.

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NASA’s Perseverance Grinds Into ‘Weird’ Martian Rock to Uncover Signs of Ancient Habitability

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NASA's Perseverance Grinds Into ‘Weird’ Martian Rock to Uncover Signs of Ancient Habitability

NASA’s Perseverance rover has begun drilling into a rock on Mars as it tries to collect more information about the Red Planet’s ancient environment. The Rover could help in finding the answers to the most-asked question: Mars was previously habitable. Previously, the rover abraded a spot called “Kenmore”, a rocky outcrop in Jezero Crater. The rover took away the outer layer, which exposed the unadulterated material below. This method, which involves mechanical grinding and puffs of nitrogen gas, allowed scientists to study rock interiors that have been protected from wind, radiation, and dust for billions of years. The mission represents a move from reconnoitering to examining, applying advanced technologies to detect stones of a bygone era, past water, and possibly life.

Perseverance Uncovers Water-Rich Minerals in Stubborn Mars Rock, Aiding Future Exploration Plans

As per a NASA report, the Kenmore rock proved unexpectedly difficult. “It vibrated all over the place, and small chunks broke off,” stated Ken Farley, Perseverance’s deputy project scientist. Despite the challenge, the team managed to expose enough of the surface for analysis. Instruments like WATSON and SuperCam revealed clay minerals—hydrated compounds containing iron and magnesium, suggesting prolonged water exposure. These findings align with Jezero Crater’s history as a river delta and lakebed, making it a prime site for biosignature exploration.

Additional SHERLOC and PIXL measurements verified the presence of feldspar and atomically dispersed manganese – a first for the Martian samples. Why they were important: They grew in water-rich environments, a hint that the red planet had a more watery past. The rover’s instruments will also be used to assess whether such rocks could be exploited in future human missions, extracting fuel or constructing habitats. “The data we’re getting now is what we’ll use to position ourselves so that future missions don’t land on uncooperative rocks,” Farley mentioned.

Kenmore is the 30th rock that Perseverance has examined up close, and the rover continues to drill and seal core samples that might someday be brought back to Earth. Yet the future of Mars Sample Return (MSR) overall is uncertain, with a proposed NASA budget for Fiscal Year (FY) 2026 under the Trump Administration cutting the campaign. All the same, the present mission still is serving up important bits of Mars’s geologic and possibly habitable past.

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