Juno Reveals Volcanoes on Io

The Juno spacecraft used its JIRAM (Jovian Infrared Auroral Mapper) instrument to capture these images of Jupiter's volcanic moon Io. It captured the four images in sequence to gain different viewing angles of the moon's volcanic activity. Image Credit: NASA/JPL-Caltech/SwRI/ASI/INAF/JIRAM

Jupiter’s moon Io is the most volcanic world in the Solar System, with over 400 volcanoes. Some of them eject plumes as high as 500 km (300 mi) above the surface. Its surface is almost entirely shaped by all this volcanic activity, with large regions covered by silicates, sulphur, and sulphur dioxide brought up from the moon’s interior. The intense volcanic activity has created over 100 mountains, and some of them are taller than Mt. Everest.

Io is unique in the Solar System, and the Juno orbiter’s JunoCam captured some new images of Io’s abundant volcanic activity.

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The Tonga Eruption Was So Powerful it Disrupted Satellites Half a World Away

The Tonga eruption in 2022 sent tons of ash and water into the air and sent an atmospheric pressure wave that helped create an equatorial plasma bubble that disrupted satellite communications that depend on the ionosphere. Courtesy of Himawari-8 satellite.
The Tonga eruption in 2022 sent ash and water into the air and created an atmospheric pressure wave that helped create an equatorial plasma bubble that disrupted satellite communications that depend on the ionosphere. Courtesy of Himawari-8 satellite.

Remember the huge Tonga eruption in the South Pacific in January 2022? This underwater volcano sent tons of ash into the air. It also blew 146 teragrams of water into our atmosphere and the effect of the explosion reached space. It also made life very difficult for people on Tonga, wiping out their communications and sending tsunamis across the South Pacific.

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There's a Giant Magma Plume on Mars, Bulging the Surface out Across a Vast Region

Lava flows in Mars' Elysium Planitia region have left a rather good likeness of a woolly mammoth or elephant. The region is known for some of the planet's youngest lavas - this one may formed in the past 100 million years.

Billions of years ago, Mars was a much different place than it is today. Its atmosphere was thicker and warmer, liquid water flowed on its surface, and the planet was geologically active. Due to its lower gravity, this activity led to the largest volcanoes in the Solar System (Olympus Mons and the Thetis Mons region) and the longest, deepest canyon in the world (Valles Marineris). Unfortunately, Mars’ interior began to cool rapidly, its inner core solidified, and geological activity largely stopped. For some time, geologists have believed that Mars was essentially “dead” in the geological sense.

However, recent studies have provided seismic and geophysical evidence that Mars may still be “slightly alive.” In a recent study, scientists from the University of Arizona (ASU) challenged conventional views of Martian geodynamic evolution by discovering evidence of an active mantle plume pushing its way through the crust, causing earthquakes and volcanic eruptions. Combined with some serious marsquakes recorded by NASA’s InSight lander, these finding suggests that there is still some powerful volcanic action beneath the surface of Mars.

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Mauna Loa is Erupting for the First Time in 40 Years. Here’s What it Looks Like From Space.

Mauna Loa eruption
Fissure 3 of the current Mauna Loa eruption on the Big island of Hawaii. Courtesy USGS.

A sleeping giant of a volcano woke up this past week on the Big Island of Hawaii. Mauna Loa, which last erupted in the early 1980s, has been rattling the island with earthquakes for weeks. Finally, on November 27th, the mountain opened up. Not only did residents see this eruption, but NASA and NOAA satellites captured an infrared view of it.

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Volcanoes are the worst. They’ve caused extinctions on Earth, and probably killed Venus

This is a computer-generated, three-dimensional perspective of the surface of Venus showing Maat Mons. It's Venus's highest volcano and is 8 kilometres (5.0 mi) high. The viewpoint is located 634 kilometers (393 miles) north of Maat Mons at an elevation of 3 kilometers (2 miles) above the terrain. Lava flows extend for hundreds of kilometers across the fractured plains shown in the foreground, to the base of Maat Mons. The vertical scale in this perspective has been exaggerated 10 times. Credits: NASA/JPL

Is there anything good about volcanoes? They can be violent, dangerous, and unpredictable. For modern humans, volcanoes are mostly an inconvenience, sometimes an intriguing visual display, and occasionally deadly.

But when there’s enough of them, and when they’re powerful and prolonged, they can kill the planet that hosts them.

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The Moon had Volcanoes More Recently Than Previously Believed

New measurements of lunar rocks have demonstrated that the ancient moon generated a dynamo magnetic field in its liquid metallic core (innermost red shell). The results raise the possibility of two different mechanisms — one that may have driven an earlier, much stronger dynamo, and a second that kept the moon’s core simmering at a much slower boil toward the end of its lifetime. Credit: Hernán Cañellas/Benjamin Weiss

Fifty years ago, NASA and the Soviet space program conducted the first sample-return missions from the Moon. This included lunar rocks brought back to Earth by the Apollo astronauts and those obtained by robotic missions that were part of the Soviet Luna Program. The analysis of these rocks revealed a great deal about the Moon’s composition, formation, and geological history. In particular, scientists concluded that the rocks were formed from volcanic eruptions more than three billion years ago.

In recent years, there has been a resurgence in lunar exploration as NASA and other space agencies have sent robotic missions to the Moon (in preparation for crewed missions). For instance, China has sent multiple orbiters, landers, and rovers to the Moon as part of the Chang’e program, including sample-return missions. A new study led by planetary scientists from the Chinese Academy of Sciences (CAS) analyzed samples obtained by the Chang’e-5 rover dated to two billion years ago. Their research could provide valuable insight into how young volcanism shaped the lunar surface.

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Satellite View of Stromboli’s New Eruption in Italy. You Can See a River of Lava Flowing to the Ocean

stromboli
ESA's Copernicus Sentinel-2 satellite captured this view of Stromboli volcano's latest eruption. contains modified Copernicus Sentinel data (2022), processed by ESA, CC BY-SA 3.0 IGO

Mount Stromboli is one of the busiest volcanoes on the planet. It’s been erupting off and on for thousands of years, and almost continuously since the early 1930s. So, it’s no surprise that ESA’s orbiting Copernicus Sentinel-2 mission caught its latest eruption in the act. It used infrared-sensitive instruments to chart the flow and follow its course to the sea.

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Volcanism on the Moon Ended About 2 Billion Years ago

According to the most widely accepted theories, the Moon formed about 4.5 billion years ago after a Mars-sized object (Theia) collided with Earth. After the resulting debris accreted to create the Earth-Moon system, the Moon spent many eons cooling down. This meant that a few billion years ago, lakes of lava were flowing across the surface of the Moon, which eventually hardened to form the vast dark patches (lunar maria) that are still there today.

Thanks to the samples of lunar rock brought back to Earth by China’s Chang’e 5 mission, scientists are learning more about how the Moon formed and evolved. According to a recent study led by the Chinese Academy of Geological Sciences (CGAS), an international team examined these samples to investigate when volcanism on the Moon ended. Their results are not only filling in the gaps of the Moon’s geological history but also of other bodies in the Solar System.

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Although it’s Quiet Today, Mars Once had Thousands of Volcanic Eruptions on its Surface

Sarychev volcano, (located in Russia's Kuril Islands, northeast of Japan) in an early stage of eruption on June 12, 2009. Credit: NASA

Earth is a geologically active planet, which means it has plate tectonics and volcanic eruptions that have not ceased. This activity extends all the way to the core, where action between a liquid outer core and a solid inner core generates a planetary magnetic field. In comparison, Mars is an almost perfect example of a “stagnant lid” planet, where geological activity billions of years ago and the surface has remained stagnant ever since.

But as indicated by the many mountains on Mars, which includes the tallest in the Solar System (Olympus Mons), the planet was once a hotbed of volcanic activity. And according to a recent NASA-supported study, there is evidence that thousands of “super-eruptions” happened in the Arabia Terra region in northern Mars 4 billion years ago. These eruptions occurred over the course of 500-million years and had a drastic effect on the Martian climate.

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Seen From Space, Iceland’s new Volcano Lights up the Island at Night

You’ve probably seen stunning images of the night side of the Earth from space. Most people have seen the veritable constellations of city lights scattered familiarly across the continents, separated by wide oceans of darkness. You very well may have seen some stunning videos from the ISS showing the dynamic and mesmerizing ribbons of the polar aurorae and the even more frenetic flashes of nighttime lightning storms. If you’re a frequent reader of this site, you’ve likely even seen the effects of rolling blackouts during the catastrophic winter storms of February 2021 in Houston, as seen from space. Add another explosively extraordinary phenomenon to the list of nighttime space views; the March 2021 volcanic eruption in Iceland!.

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