The System’s 6th planet, and first world I’ve come across in my journey that has life on the surface. This is one odd life-supporting world. It is a small world, roughly the size of Mars, but only half of Mars’ mass, with a low average density. The atmosphere is 99.8% carbon dioxide and 0.2% oxygen, with a thickness only 4% that of Earth’s atmosphere. The surface has an average temperature of 181 K or -133 °F. And it has one large moon in orbit.
Unfortunately Space Engine only shows life as coloring on the planet’s surface; therefore, I have no idea what form or appearance it has. Based off of the temperatures and atmospheric composition, this the life likely has has a low metabolic rate that uses a liquid other than just water to metabolize, possibly an Eutectic Water-Ammonia solution. Carbon-based if feasible, but involves significantly different chemistry than we are familiar with. The purple coloring likely an adaptation to utilize the low sunlight levels and probably uses primarily red or near infrared light for photosynthesis.
High Resolution Pics
Picture 1 - Planet and Moon
Picture 2 -
Picture 3 - The Equator
Picture 4 - Northern Ice Cap
Picture 5 - Planet, Moon, Sun, Inner Planets and Andromeda
Picture 6 - The Surface
Picture 7 - Moon and Nebula Rising
The shadow of a moon's eclipse is visible across this gas giant’s rings.
First post of the Insight A system. Insight A is the larger or primary of Insight’s 2 stars. The Insight System is a wide-spaced binary system consisting of a type G1V and type K5V star that orbit one another at an average distance of 192.3 AU once every 2,432 years. Insight A is 1.6 times the luminosity of our sun, and Insight B just 1/6th that of our sun.
Below are the first five worlds orbiting Insight A.
Insight A-I (0.56 Earth Masses - Rocky, 0.04 AU)
Insight A-II (2.66 Earth Masses, Rocky Super Earth, 0.07 AU)
Insight A-III (13.22 Earth Mass, Ice-Giant, 0.12 AU)
Insight A-IV (41.38 Earth Masses, Ice Giant, 0.36 AU)
Insight A-V (0.14 Earth Masses, Rocky with Liquid Water, 0.69 AU)
On Sept. 15, 2017, our Cassini spacecraft ended its epic exploration of Saturn with a planned dive into the planet’s atmosphere–sending back new science to the very last second. The spacecraft is gone, but the science continues!
New research emerging from the final orbits represents a huge leap forward in our understanding of the Saturn system – especially the mysterious, never-before-explored region between the planet and its rings. Some preconceived ideas are turning out to be wrong while new questions are being raised. How did they form? What holds them in place? What are they made of?
Six teams of researchers are publishing their work Oct. 5 in the journal Science, based on findings from Cassini’s Grand Finale. That’s when, as the spacecraft was running out of fuel, the mission team steered Cassini spectacularly close to Saturn in 22 orbits before deliberately vaporizing it in a final plunge into the atmosphere in September 2017.
Knowing Cassini’s days were numbered, its mission team went for gold. The spacecraft flew where it was never designed to fly. For the first time, it probed Saturn’s magnetized environment, flew through icy, rocky ring particles and sniffed the atmosphere in the 1,200-mile-wide (2,000-kilometer-wide) gap between the rings and the cloud tops. Not only did the engineering push the spacecraft to its limits, the new findings illustrate how powerful and agile the instruments were.
Many more Grand Finale science results are to come, but today’s highlights include:
Complex organic compounds embedded in water nanograins rain down from Saturn’s rings into its upper atmosphere. Scientists saw water and silicates, but they were surprised to see also methane, ammonia, carbon monoxide, nitrogen and carbon dioxide. The composition of organics is different from that found on moon Enceladus – and also different from those on moon Titan, meaning there are at least three distinct reservoirs of organic molecules in the Saturn system.
For the first time, Cassini saw up close how rings interact with the planet and observed inner-ring particles and gases falling directly into the atmosphere. Some particles take on electric charges and spiral along magnetic-field lines, falling into Saturn at higher latitudes – a phenomenon known as “ring rain.” But scientists were surprised to see that others are dragged quickly into Saturn at the equator. And it’s all falling out of the rings faster than scientists thought – as much as 10,000 kg of material per second.
Scientists were surprised to see what the material looks like in the gap between the rings and Saturn’s atmosphere. They knew that the particles throughout the rings ranged from large to small. They thought material in the gap would look the same. But the sampling showed mostly tiny, nanograin- and micron-sized particles, like smoke, telling us that some yet-unknown process is grinding up particles. What could it be? Future research into the final bits of data sent by Cassini may hold the answer.
Saturn and its rings are even more interconnected than scientists thought. Cassini revealed a previously unknown electric current system that connects the rings to the top of Saturn’s atmosphere.
Scientists discovered a new radiation belt around Saturn, close to the planet and composed of energetic particles. They found that while the belt actually intersects with the innermost ring, the ring is so tenuous that it doesn’t block the belt from forming.
Unlike every other planet with a magnetic field in our Solar System, Saturn’s magnetic field is almost completely aligned with its spin axis. Think of the planet and the magnetic field as completely separate things that are both spinning. Both have the same center point, but they each have their own axis about which they spin. But for Saturn the two axes are essentially the same – no other planet does that, and we did not think it was even possible for this to happen. This new data shows a magnetic-field tilt of less than 0.0095 degrees. (Earth’s magnetic field is tilted 11 degrees from its spin axis.) According to everything scientists know about how planetary magnetic fields are generated, Saturn should not have one. It’s a mystery physicists will be working to solve.
Cassini flew above Saturn’s magnetic poles, directly sampling regions where radio emissions are generated. The findings more than doubled the number of reported crossings of radio sources from the planet, one of the few non-terrestrial locations where scientists have been able to study a mechanism believed to operate throughout the universe. How are these signals generated? That’s still a mystery researchers are looking to uncover.
For the Cassini mission, the science rolling out from Grand Finale orbits confirms that the calculated risk of diving into the gap – skimming the upper atmosphere and skirting the edge of the inner rings – was worthwhile.
Almost everything going on in that region turned out to be a surprise, which was the importance of going there, to explore a place we’d never been before. And the expedition really paid off!
Analysis of Cassini data from the spacecraft’s instruments will be ongoing for years to come, helping to paint a clearer picture of Saturn.
To read the papers published in Science, visit: URL to papers
To learn more about the ground-breaking Cassini mission and its 13 years at Saturn, visit: https://www.nasa.gov/mission_pages/cassini/main/index.html
Make sure to follow us on Tumblr for your regular dose of space: http://nasa.tumblr.com.
We’ve moved away from the last system and traveled nearly 13,000 light years to another system on the edge of Triangulum.
Here we come across a system which I have called the Vista system, due to some of the stunning views of gas giants and their moons.
This system is configured rather unusually, in that the asteroid belt forms the inner-most part of the system, orbiting close to the star with a single dwarf planet orbiting within. Above are pics of the inner-most dwarf planet.
This moon-sized world orbits 0.13 AU from the sun, with a scorching surface temperature of 760°.
More pics of worlds in this system to come.
Links to high resolution pics above.
Image 1
Image 2
Image 3
Image 4
Picture of the day - February 6, 2019 - (Very late post)
Ringed ocean world with greenish-gray colored oceans. The Carina Nebula fills the sky in the background.
Picture of the day - November 20, 2018
Dark red nebula rises over a dim set of rings orbiting a gas giant.
Picture of the Day - October 22, 2018
Another gas-giant and its moons. Here the atmosphere of the gas giant and its inner moon glow against the dark background, illuminated by scattered light, viewed from just above the atmosphere of a second satellite.
Picture of the day - January 23, 2019
Galaxy looms large behind the rings of a gas giant.
Picture of the Day 2 - October 19, 2019
Large hazy blue world rising about an asteroid moon.
Picture of the Day - October 13, 2018
The sky of a large moon orbiting a gas giant right before an eclipse.
My Space Engine Adventures, also any space related topic or news. www.spaceengine.org to download space engine. The game is free by the way. Please feel free to ask me anything, provide suggestions on systems to visit or post any space related topic.Check out my other blog https://bunsandsharks.tumblr.com for rabbit and shark blog.
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