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A volcanic eruption of unprecedented scale has been observed on Jupiter’s moon Io, with a massive hotspot detected in the southern hemisphere. The discovery was made by NASA’s Juno spacecraft during a flyby on 27 December 2024. The heat energy released from this eruption has been estimated at around 80 trillion watts, surpassing the total energy output of all power plants on Earth by six times. Io, the most volcanically active body in the solar system, experiences extreme geological activity due to the gravitational forces exerted by Jupiter. This tidal flexing causes internal heating, leading to continuous volcanic eruptions across its surface.

New Hotspot Revealed by NASA’s Juno Spacecraft

According to NASA, data from the Juno spacecraft’s Jovian Infrared Auroral Mapper (JIRAM) instrument has confirmed the presence of a massive new volcanic hotspot on Io. The eruption site appears to be fueled by a single, extensive magma chamber, covering an estimated 105,000 square kilometres. This newly detected feature is believed to be the largest volcanic structure on Io, exceeding the well-documented Loki Patera lava lake, which spans around 21,000 square kilometres.

In a statement in an official press release by NASA, Scott Bolton, principal investigator of the Juno mission and space physicist at the Southwest Research Institute, noted that the intensity of this volcanic event was unexpected. Bolton stated, that the data from this latest flyby blew their minds as this is the most powerful volcanic event ever recorded on the most volcanic world in our solar system.

Io’s Surface Shows Signs of Change

New images captured by Juno have revealed a large, dark region on Io’s surface. This area is thought to be covered in solidified lava from the eruption, though further observations will be needed to confirm its exact nature. Due to the spacecraft’s distance from Io during the recent flyby, high-resolution images of the region were not obtained.

Io’s extreme volcanic activity has long been attributed to tidal forces exerted by Jupiter’s gravity. Unlike Earth, where volcanic eruptions result from internal heat generated by a molten metal core, Io’s eruptions are primarily driven by external gravitational stresses. These forces cause constant deformation of the moon’s surface, heating its interior and producing vast magma reservoirs beneath its crust.

Earlier theories suggested that Io’s subsurface was entirely composed of molten magma, but recent studies have disproved this assumption. Instead, researchers now believe that magma is concentrated in specific areas beneath the moon’s active volcanoes, such as the newly identified hotspot.

Further Observations Expected in March

A closer flyby of Io is scheduled for 3 March, with Juno expected to capture more detailed data on the newly discovered magma chamber. Scientists anticipate that these observations will provide further insights into Io’s volcanic processes and contribute to a broader understanding of similar activity on other celestial bodies.

Bolton added in his statement that this discovery could significantly enhance knowledge about volcanic activity beyond Earth. He said that while it was always great to witness events that rewrite the record books, this new hot spot can potentially do much more.

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Greek Authorities Respond to Intensifying Earthquake Swarm Near Santorini

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Greek Authorities Respond to Intensifying Earthquake Swarm Near Santorini

Greek authorities have responded to an intensifying earthquake swarm near Santorini by closing schools and deploying emergency teams. The tremors, which began last week, have been growing in frequency and magnitude, raising concerns over potential stronger quakes in the region. While experts have ruled out immediate volcanic activity, the situation remains unpredictable due to the swarm’s unusual characteristics. The most powerful tremor recorded so far was a magnitude 5 earthquake, striking approximately 34 kilometres northeast of Santorini. The event occurred at 2:27 p.m. local time, as per the University of Athens’ earthquake monitoring system.

Seismic Activity Driven by Faults, Not Volcanic Unrest

According to reports, the ongoing tremors are attributed to fault movement rather than volcanic activity. Santorini, positioned on the Aegean Sea’s tectonic boundary, sits on the exposed section of a submerged volcano known as the Santorini caldera. David Pyle, Professor of Earth Sciences at the University of Oxford, told Live Science that the quakes are likely caused by fault lines shifting rather than magma activity. He described the swarm as unusual, highlighting the challenge of predicting future developments due to its underwater location.

Historical Earthquake Swarms and Regional Tectonics

The Aegean region experiences significant seismic activity due to the African plate moving beneath the Eurasian plate. Similar earthquake swarms have been recorded in the past, including a 2011-2012 event linked to magma movement beneath Santorini. However, the current swarm appears more extensive and is concentrated outside the Santorini caldera. Most tremors have been recorded between the underwater Kolumbo volcano and Anydros Island.

Kolumbo, last erupting in 1650, previously triggered a tsunami that affected nearby islands. While researchers remain uncertain about a direct link between current tectonic activity and potential volcanic unrest, ongoing monitoring continues to assess the evolving situation.

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NASA’s Juno Detects Io’s Most Powerful Volcanic Eruption Yet



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Moon’s Deepest Canyons Formed in Minutes by High-Speed Impact Debris

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Moon’s Deepest Canyons Formed in Minutes by High-Speed Impact Debris

Two colossal canyons on the moon, both deeper than the Grand Canyon, were formed in under ten minutes by surges of high-speed rock debris, as per reports. These valleys, named Vallis Schrödinger and Vallis Planck, extend for 270 kilometres and 280 kilometres, respectively, with depths of up to 3.5 kilometres. Comparatively, the Grand Canyon reaches a maximum depth of approximately 1.9 kilometres. The canyons are located near the Schrödinger impact basin in the lunar south polar region, an area marked by towering mountains and deep craters.

Impact that shaped the lunar landscape

According to the study published in Nature Communications, these canyons are part of several valleys that formed from the debris ejected during the impact that created Schrödinger basin, a 320-kilometre-wide crater formed around 3.81 billion years ago. The basin is positioned on the outer edge of the South Pole–Aitken basin, the moon’s largest and oldest remaining impact structure, which dates back more than 4.2 billion years.

Unprecedented energy levels behind the canyons

As per findings, rocky debris from the impact travelled at speeds ranging between 3,420 and 4,600 kilometres per hour. In comparison, a bullet from a 9mm handgun reaches speeds of about 2,200 kilometres per hour. The force required to carve these canyons is estimated to have been over 130 times greater than the total energy stored in the current global nuclear arsenal.

Key insights for future lunar exploration

Speaking to Space.com, David Kring, a geologist at the Lunar and Planetary Institute, highlighted that unlike the Grand Canyon, which was shaped by water over millions of years, these lunar canyons were formed in a matter of minutes by rock flows. The distribution of impact debris also suggests that astronauts landing near the South Pole–Aitken basin may find better access to some of the moon’s oldest geological samples. These insights contribute to ongoing research on potential landing sites for future lunar missions.

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NASA Looks for Private Partners To Revive VIPER Moon Rover Mission

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NASA Looks for Private Partners To Revive VIPER Moon Rover Mission

NASA is inviting U.S. companies to collaborate on the Volatiles Investigating Polar Exploration Rover (VIPER), a mission initially halted due to budget constraints. Designed to search for water ice near the lunar south pole, VIPER was originally planned as a $450 million project. The agency had cancelled the mission in July 2024, citing cost-saving measures. Now, a fresh call has been made to private firms willing to take on the challenge of delivering the rover to the Moon, conducting exploration, and sharing scientific data. A final decision is expected in the coming months.

VIPER’s Role in Lunar Exploration

According to NASA’s announcement, VIPER was designed to support Artemis program objectives by locating potential water ice deposits. These resources are crucial for future human missions and lunar surface operations. Initially set to launch aboard the Griffin lander by Astrobotic Technology, the mission was shelved before its deployment. Following interest from private firms, NASA has decided to explore new avenues for its deployment while ensuring that the scientific goals remain intact.

Proposals and Selection Process

NASA officials have confirmed that responses from interested companies must be submitted by February 20, 2025. Selected candidates will be invited to provide more detailed proposals, with final selections anticipated by mid-year. The agency has clarified that while VIPER will be handed over in its current state, modifications involving dismantling its instruments for use on other spacecraft will not be permitted. Companies will be required to manage landing operations, conduct scientific research, and ensure data dissemination as part of the agreement.

Potential Benefits for Private Firms

In a statement in an official press release by NASA, Joel Kearns, Deputy Associate Administrator for Exploration in NASA’s Science Mission Directorate, stated that the partnership would provide significant opportunities for private firms looking to advance their lunar surface capabilities. He emphasised that VIPER’s deployment could mark a critical step toward commercial involvement in lunar exploration, reinforcing NASA’s commitment to fostering public-private collaborations.

Future of Lunar Resource Exploration

As NASA continues to push for sustainable lunar exploration, the integration of private-sector capabilities is seen as a key element in reducing costs and expanding mission possibilities. With lunar resource utilisation playing a major role in future space endeavours, the agency remains focused on ensuring that scientific objectives are met while advancing commercial lunar operations. The final selection of partners for VIPER is expected to set the stage for upcoming exploration missions and resource prospecting efforts on the Moon.

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