Read the Beforeitsnews.com story here. Advertise at Before It's News here.
Profile image
By Universe Today (Reporter)
Contributor profile | More stories
Story Views
Now:
Last hour:
Last 24 hours:
Total:

Juno Sees a Brand New Volcano on Io

% of readers think this story is Fact. Add your two cents.


Jupiter’s moon, Io, is the most volcanic body in the Solar System. NASA’s Juno spacecraft has been getting closer and closer to Io in the last couple of years, giving us our first close-up images of the moon in 25 years.

Recent JunoCam images show a new volcano that appeared sometime after the Galileo spacecraft visited the region.

The new volcano is just south of Io’s equator. Since tidal heating from Jupiter causes Io’s volcanic activity, most volcanoes are in the moon’s equatorial region, within about 30 degrees north and south of the equator. When NASA’s Galileo spacecraft imaged the region where the new volcano was spotted in 1997, the surface was featureless.

The new volcano is near an existing volcano called Kanehekili. JunoCam’s image from April 2024 revealed multiple lava flows and volcanic deposits covering an area of about 180 kilometres by 180 kilometres.


The grey inset image shows what the Galileo spacecraft saw about 25 years ago. The larger colour image is from JunoCam and clearly shows a new volcano and lava flows. Image Credit: NASA/JPL-Caltech/SwRI/MSSS/Europlanet.

“Our recent JunoCam images show many changes on Io, including this large, complicated volcanic feature that appears to have formed from nothing since 1997,” said Michael Ravine. Ravine is the Advanced Projects Manager at Malin Space Science Systems, the company that built and operates JunoCam for NASA’s Juno mission.

Of course, the volcano didn’t form from nothing. Io is in a tough spot orbitally. Tidal friction from massive Jupiter, and some from its fellow moon Europa, is dissipated as orbital and heat energy in Io. In its sibling ocean moons like Europa, Ganymede, and Callisto, the heat keeps their subsurface oceans in liquid form. But Io doesn’t have an ocean, so the heat causes magma to well up and break through the surface as volcanoes. Io has over 400 active volcanoes, and the surface is covered in sulphuric compounds from these eruptions, which give it its colours.

JunoCam’s best image of the region and the new volcano was taken on February 3rd, 2024, from a distance of about 2,530 km. The scale is about 1.7 km per pixel. In this image, Io is illuminated with sunlight reflected off of Jupiter.


This image shows the Galileo and JunoCam images sisde by side. NASA/JPL-Caltech/SwRI/MSSS.

There are unanswered questions about Io, its volcanism, and its interior composition. Scientists know that tidal heating from Jupiter is the moon’s primary heat source, but they aren’t certain how the heat is distributed inside. They are also uncertain about the extent of Io’s magma ocean.

They also want to know what initiates eruptions and what drives the different types of eruptions, like plumes, lava flows, and pyroclastic flows. There are unanswered questions about Io’s volcanic history and how often the surface is reshaped. There are no impact craters on Io, which means the surface must be young.

This schematic illustrates four competing explanations for Io's interior and how tidal heating is dissipated. Though Juno won't tell us which one is correct, every volcanic eruption is a piece of the puzzle. Image Credit: Chuck Carter and James Tuttle Keane / Keck Institute for Space Studies.
This schematic illustrates four competing explanations for Io’s interior and how tidal heating is dissipated. Though Juno won’t tell us which one is correct, every volcanic eruption is a piece of the puzzle. Image Credit: Chuck Carter and James Tuttle Keane / Keck Institute for Space Studies.

Researchers are also keen to understand how the gases from eruptions might affect the surface and the moon’s extremely thin atmosphere. Io’s volcanic activity has likely changed over time, and how that happens and what drives it are also unknown.

Answers to these questions will not only help us understand Io, but other rocky planets as well.

Juno’s discovery of a new volcano on Io is interesting, and its observations are a valuable contribution to the body of knowledge. However, Juno won’t provide the in-depth answers scientists seek. It has several more flybys of Io in the future, with the last one in 2025. Unfortunately, it’ll be getting further from the moon, and the last one will be at a distance of 94,000 km.

This graphic shows Juno's orbits around Jupiter. PJ (perijove) 58 was its closest approach to Io, and as time goes on, its flybys will be more and more distant. Image Credit: Scott Bolton/SWRI
This graphic shows Juno’s orbits around Jupiter. PJ (perijove) 58 was its closest approach to Io, and as time goes on, its flybys will be more and more distant. Image Credit: Scott Bolton/SWRI

These images do highlight an important part of the Juno mission, though. The JunoCam isn’t a scientific instrument, strictly speaking. It was included for the rest of us, and the images are freely available for anyone to work on and post.

By spotting the new volcano, JunoCam has proven its scientific value.

The post Juno Sees a Brand New Volcano on Io appeared first on Universe Today.


Source: https://www.universetoday.com/168465/juno-sees-a-brand-new-volcano-on-io/


Before It’s News® is a community of individuals who report on what’s going on around them, from all around the world.

Anyone can join.
Anyone can contribute.
Anyone can become informed about their world.

"United We Stand" Click Here To Create Your Personal Citizen Journalist Account Today, Be Sure To Invite Your Friends.


Humic & Fulvic Liquid Trace Mineral Complex


HerbAnomic’s Humic and Fulvic Liquid Trace Mineral Complex is a revolutionary new Humic and Fulvic Acid Complex designed to support your body at the cellular level. Our product has been thoroughly tested by an ISO/IEC Certified Lab for toxins and Heavy metals as well as for trace mineral content. We KNOW we have NO lead, arsenic, mercury, aluminum etc. in our Formula.


This Humic & Fulvic Liquid Trace Mineral complex has high trace levels of naturally occurring Humic and Fulvic Acids as well as high trace levels of Zinc, Iron, Magnesium, Molybdenum, Potassium and more. There is a wide range of up to 70 trace minerals which occur naturally in our Complex at varying levels. We Choose to list the 8 substances which occur in higher trace levels on our supplement panel. We don’t claim a high number of minerals as other Humic and Fulvic Supplements do and leave you to guess which elements you’ll be getting.


Order Your Humic Fulvic for Your Family by Clicking on this Link, or the Banner Below.



Our Formula is an exceptional value compared to other Humic Fulvic Minerals because...


It’s OXYGENATED

It Always Tests at 9.5+ pH

Preservative and Chemical Free

Allergen Free

Comes From a Pure, Unpolluted, Organic Source

Is an Excellent Source for Trace Minerals

Is From Whole, Prehisoric Plant Based Origin Material With Ionic Minerals and Constituents

Highly Conductive/Full of Extra Electrons

Is a Full Spectrum Complex


Our Humic and Fulvic Liquid Trace Mineral Complex has Minerals, Amino Acids, Poly Electrolytes, Phytochemicals, Polyphenols, Bioflavonoids and Trace Vitamins included with the Humic and Fulvic Acid. Our Source material is high in these constituents, where other manufacturers use inferior materials.


Try Our Humic and Fulvic Liquid Trace Mineral Complex today. Be 100% Satisfied or Receive a Full Money Back Guarantee. Order Yours Today by Following This Link.

Report abuse

Comments

Your Comments
Question   Razz  Sad   Evil  Exclaim  Smile  Redface  Biggrin  Surprised  Eek   Confused   Cool  LOL   Mad   Twisted  Rolleyes   Wink  Idea  Arrow  Neutral  Cry   Mr. Green

MOST RECENT
Load more ...

SignUp

Login

Newsletter

Email this story
Email this story

If you really want to ban this commenter, please write down the reason:

If you really want to disable all recommended stories, click on OK button. After that, you will be redirect to your options page.