Tesnapun

(The 1 year anniversary for my presence on this wiki was 2 days ago. ChatGPT was used to expand the text to make it not look like some sort of stub, without it, it would not make any real size difference, so both ways this article is huge. This world to be discovered requires a mod, this mod is downloadable here) 
==Tesnapun's information==
===Technical information===
This is a warm gas giant that has a diameter of 86911.35 miles, with the mass of the planet being 12.874 M♃, or 2.4444*10^28 kilograms, and the density of the planet is 17.178 grams per cubic centimeter. The oblateness of the planet is 0.0068337, with the effective temperature being 258.98 kelvin (6.494 degrees Fahrenheit, -14.17 degrees Celsius), and the Earth similarity of the planet being 0.364, and in addition to that the albedo bond / geom is 0.456769 and 0.548122. The rotational period of the planet is 8 hours, 48 minutes, and 16.75 seconds, with the solar day being 8 hours, 48 minutes, and 19.19 seconds, and the axial tilt of the planet is 7*32’48.69”. The age of the planet is very young, only 55.685 million years old, though a multitude of scientists disagree with this number considering the distance from the parent galaxy, it could not be this young, it was orbiting an intergalactic star, which could not form, go to the center, get ejected, and reach this distance in only 55.685 million years, so this number has an asterisk next to it in data sheets. The gravity on the poles and equator is 338.47 meters per second, with the gravity on the equator being 331.11 meters per second, which is 34.503 g and 33.753 g, and the circular / escape velocity is 94.95 miles per second and 134.28 miles per second.  The height of the atmosphere is 131.13 miles, with the tropopause height being 4960.61 feet, and the height of the homogeneous atmosphere is 34.71 miles.
The atmospheric pressure is 1*10^6 atm, with the air density being 5433.6 kilograms per cubic meter, and the air temperature is 5000 kelvin. Yea the data on some of the properties is odd and unnatural, through personal observations, the planet’s air temperature has been estimated to be 345 - 400 kelvin, more likely, and the exosphere temperature is 1719.9 kelvin. The greenhouse effect is 0 kelvin, with the average molar mass is 2.229, and the relative mass is 0.95, in addition to that, the the mass of the atmosphere is 12.23 M♃. Hydrogen makes up 92.3% of the atmosphere, with Helium making 7.29%, and Methane makes up 0.356% of the atmosphere. The orbital type of the planet is elliptical, with the parent of this planet being the star 88-TARG3, and the orbital period of the planet is 13.002 years. The semimajor axis of the planet is 8.66 AU, with the pericentric distance being 8.31 AU, and the eccentricity being 0.041, in addition to that the inclination being 0*33’14.95”. The ascending node of the planet is -161*50’9.22”, with the argument of pericenter being 227*3’58.94”, and the mean anomaly is  87*36’47.47”. In addition to that the  longitude of pericenter is 65*13’49.71”, plus the longitude of pericenter being 65*13’49.71”. The hill sphere radius of the planet is 0.85 AU, with the influence sphere radius being 0.87 AU, and the Roche limit for satellites is 94291.29 miles.
===Infolore===
This massive celestial body is a true megagiant, boasting a staggering mass that ranges from 12 to 13 times that of Jupiter. What makes this behemoth truly fascinating is the presence of a colossal ring system, a celestial ornament that encircles it. Within this intricate ring system, one can observe several shepherd moons and distinct major parts, including sub-parts denoted as A, B, C, and D. Remarkably, these sub-parts, resembling independent rings in their own right, further divide into decimalized components, adding layers of complexity to this captivating spectacle. Comprising an array of materials, the ring system is predominantly composed of silicate, nickel, copper, and iron. This amalgamation of elements contributes to the breathtaking visual diversity that graces the heavens around this megagiant.
Beyond the ring system, a separate moon system orbits this colossal gas giant. This moon system bears a striking resemblance to a miniature star system, seemingly formed from meager amounts of material compared to typical star systems. These moons orbit the giant in a mesmerizing dance, and the gas giant itself exhibits weather patterns akin to those of Jupiter, featuring massive storms and atmospheric turbulence. One of the most notable features of this celestial giant is a massive storm, akin to a red giant in its own right, which has endured for approximately 670 years. Curiously, despite its mammoth appearance, this storm is relatively smaller than Earth, which may be attributed to the gradual weakening and fragmentation of the storm over time. This reduction in size is likely influenced by the presence of numerous other storms, which are quite generic in structure and exist as temporary eddies lasting only a few years, located within one of the planet's 13 bands. 
The sheer size, mass, and its nearly brown dwarf status enable this megagiant to exert a gravitational pull, drawing in hundreds of smaller asteroids and comets. These celestial wanderers, although frequently attracted to the megagiant, typically do not collide with the planet or its moons. However, anecdotal accounts from personal observers and a select few CALASE/SKYNAV observations have documented instances of asteroids and comets impacting the planet and its moons. Intriguingly, many of these celestial bodies carry the essential ingredients for the initiation of life, giving rise to the intriguing possibility of moons with the potential for life existing in the vast intergalactic void. Regrettably, or perhaps not, depending on one's perspective regarding intergalactic life, the emergence of life on this celestial body and its moons might face a limited existence. The main factor is the star around which the planet orbits.
It orbits a rare and relatively undocumented blue subgiant star, which is approaching the later stages of its lifecycle. As the star transitions into a red giant, this change in stellar phase could render the two moons that harbor the potential for intelligent life barren, significantly impacting the possibility of life on these moons. However, if life does manage to evolve on this planet and its moons, and if it can endure the red giant phase and the subsequent cool-down to a white dwarf, it could represent a unique and isolated instance of life within a planetary nebula that would eventually form a star cluster, far removed from the rest of the universe. In conclusion, this megagiant, while seemingly generic in its classification, possesses a series of enthralling features, including its diverse ring system, complex moon system, and the intriguing possibility of life emerging in the vastness of the cosmos. It stands as a remarkable cosmic outlier, gracing the universe with its unique position and captivating characteristics.
===Gallery===
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==Moons ==
This section lists all the major moons around the planet, some of them more interesting than others.
===Baesnapun===
Let's delve into the first moon orbiting this colossal gas giant. It's a scorched desert world, boasting a mass more than six and a half times that of Earth, with a diameter exceeding one and a half times that of our home planet. This moon is veiled in a thick layer of inky blackish storms that break up its otherwise pale and blue-tinted atmosphere. Beneath these tempestuous layers, we can discern a lunar landscape etched with numerous craters, likely remnants of past and ongoing celestial bombardments. These craters appear massive on the moon's surface, their hollows filled with magma sourced from a vast, lavaic ocean that covers approximately 80% of the moon's surface. This molten ocean surrounds barren land masses that are generally flat and desolate. The moon's scorching temperature is primarily a consequence of its proximity to the parent planet. This proximity intensifies tidal forces to a significant degree, contributing to the moon's extreme conditions.
As previously mentioned, its thick atmosphere is composed predominantly of greenhouse gasses, namely carbon dioxide and methane, which have accumulated to the extent that they create an effect reminiscent of Venus, trapping heat and intensifying the moon's searing temperatures. Despite its massive size and proximity to the parent planet, this moon remarkably has not disrupted the planet's ring system. Nevertheless, its gravitational pull exerts influence over the ring, causing occasional disturbances that result in meteor showers as fragments from the ring system cascade onto the moon's surface. This moon holds the distinction of being the largest among its celestial companions orbiting the gas giant, having likely accumulated the lion's share of carbon and other materials during its formation, effectively starving the other moons of significant resources.
====Gallery====
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===Heasnapun===
The second moon, and the smallest satellite orbiting its parent planet, is a scorching desert world, characterized by aridity. It possesses a mass of 0.77764 M⨁. Despite the absence of water and the vast expanses of dry, desolate sand dunes and rocky mountains and basins, it hosts a modest weather system, featuring sandstorms and small cyclones. These cyclones resemble sandstorms but are more structured, with expansive arms sweeping across the open sands. In their centers, there lies a serene eye surrounded by towering walls of sand and occasionally rocklets. The moon's bluish-colored atmosphere consists of Methane, Carbon dioxide, Acetylene, Hydrogen sulfide, and oddly, Water vapor. Now, let's delve into the moon's biomes. First, we have the Salt pan basin, the rarest biome on this celestial body. These basins are large depressions that appear to have once been filled with water. Their edges take on the form of rolling hills, transitioning into the most common biome, the Standard arid desert. This biome consists of extensive sand dunes, sculpted by the moon's relentless winds. The third biome, Elevated hills, is also referred to as "rocky" or "sedimentary" in nature. 
These hills, higher than the average dunes, are akin to sand dunes with a rocky core. This rocky core appears to be of sedimentary origin, contradicting the common notion of "rocky" as something directly from the parent world. These hills are formed by mounds of rocklets and sand sediment shaped by millennia of sandstorms and sand cyclones. They originate from small mounds created by the moon's tectonic plates, which remain active, likely due to the presence of active volcanoes. Though it's possible that tidal forces from other moons may contribute to the volcanic activity, this is less likely. A prevailing theory suggests that this moon once had liquid oceans and was once a habitable terra. Over millions of years, volcanic activity and rising temperatures caused the water to evaporate into the atmosphere. Observers have noticed signs of past water presence in the dry salt pans and basins, evident from distinct liquid erosion marks on the edges and surfaces. These erosion marks, unlike those created by wind, display a unique organization and calmness. In 1998, both this moon and the first moon were struck by a barrage of small asteroids, resulting in small craters that have since been buried by geological processes.
====Gallery====
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===Eerrasnapun===
This is the third moon away from the parent planet, and also the most livable one, provided the atmospheric conditions were a bit nicer for Human breathing, but I digress. The moon is the most earth-like, it being a terra, and it has an ocean, one that is just a bit smaller than that of the Pacific ocean. The first thing that you will notice about this world is the ring system that is around it, this ring system seems to be a remnant from the formation of this moon, it seems to comprise the same elements that the moon is made of, Iron, Silicate, Nickel, Cobalt, Copper, Platinum, Gold, and other such compounds found on a rocky world. The moon’s landscape is mostly barren, it is a typical lifeless terra, not too many interesting things about it on the face of it, but there are three biomes on this world, Lowlands, Craggy plains, and the rarest of the three, Magma cools. The most common of the three biomes, the Craggy planes, these fair planes are barren flat landscapes that sometimes have rocky mounds shooting out of them, occasionally there is also some indentation in the ground, past impact craters not too long ago from the formation of the moon, these planes make up over 87% of the landmass here, and are also the most dry part of the moon. The next biome, lowlands, is the lower elevation version of the Craggy planes, it typically on this world exists as a valley that exists between the Craggy planes and itself or the Magma cools, this biome also tends to flood alot, with whole dry valleys becoming large river channels and sounds over the course of whatever a season counts here.
And lastly, the least common biome, the Magma cools, these regions on this moon are as the name implies, large swaths of land which are just Igneous rock, these plains seem to be remnants from the formation of the moon, left as scars, and they do form in a scar like formation, with them going on a horizontal angle most of the time. The dark spot on this moon’s surface is one of the largest Magma cools, it was the result of a massive eruption millions of years ago that changed a lot of characteristics about this moon from the amount of water present to the temperature. This eruption also scattered magma across a large swath of land, making even the elevation there on average lower than the rest of  the moon, and it was powerful enough that the original volcano that formed this eruption no longer exists at all, there does not seem to be a noticeable remnant of it atleast from the visual sides of things. Using topographical mapping, we can see a notable indentation in that region, and a medium sized caldera like structure which represents the lowest place there. This moon lately does have the highest potential for life, as hydrothermal vents have been observed at the bottoms of the ocean here, and a volley of comets that have the building blocks of life have seeded this world multiple times in the past, 1982, 1987, 1994, 1997, 2001, 2004, and most recently, 2009. These said comets or cometoids have landed on a world (this one) that also does not seem to have that much water vapor, even though there is an entire ocean just a little smaller or bigger than the Pacific ocean on it, this may be due to the evaporation here being suppressed, and all the clouds that you see that roam this world are made up of methane, carbon, and the other compounds of this atmosphere.
====Gallery====
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===Oesnapun===
This celestial body is the fourth moon orbiting its parent star, boasting characteristics of a temperate oceanic world. It possesses a mass and diameter that slightly surpass those of Earth. What distinguishes this temperate oceanic expanse is its conspicuous absence of remarkable geographical features or landmarks, presenting an uninterrupted expanse of water. Strikingly, the evaporation of this seemingly boundless ocean appears to be curiously suppressed, an intriguing phenomenon given the planet's status as an oceanic world. This anomaly becomes more perplexing when we consider the moon's relatively scant atmospheric water vapor content. Upon first setting foot on this enigmatic planet, one would be struck by the profusion of cloud-like formations that envelop the skies. The occurrence of a clear day on this world is a rare event, if it happens at all. The abundance of these clouds can be attributed to the presence of hydrogen sulfide in the atmosphere, which, when combined with other compounds such as methane, coalesces to form immense cloud banks. 
Occasionally, these cloud masses assemble into formidable cyclones, characterized by their peculiar absence of rain. Remarkably, the concept of rainfall remains an alien one on this world, primarily because the critical component for rain, water, is conspicuously absent, as previously mentioned. However, the most captivating facet of this celestial body is the tantalizing prospect of life lurking beneath its surface. Observing the moon, one might perceive only the seemingly dormant ocean, but what lies beneath is an unending rocky seabed dotted with hydrothermal vents. These hydrothermal vents are structures that closely resemble undersea volcanoes and serve as conduits to the planet's subterranean realm, generating heat in the process. This heat is a crucial factor in initiating the initial stages of life, and it appears that this planet has been inadvertently seeded by comets and numerous asteroids in its distant past. Life in this vast oceanic realm would be confined to the watery depths, as the atmospheric conditions above it are inhospitable. Nevertheless, these subaquatic organisms are hardly missing out on the riches of the world above, given its extreme and challenging nature.
====Gallery====
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===Aresnapun===
This is the 5th moon away from the parent planet, and is twin-like with the second moon around the parent planet. The moon, though very similar to its twin further in, does have several differences with said twin. First, the moon has a sea-like basin in its northern hemisphere that does have several erosion structures that seem to come from liquid water. This old basin seems to be around 20 - 30 million years old, meaning that it formed almost right after the moon finished forming. Several small lakes and ponds (of course evaporated now) have been observed on this world, these share the same type of erosion marks that the largest seamass, the sea/ocean mentioned before had. Unfortunately, this moon’s possible liquid seamasses evaporated 30 - 20 million years ago, with the only evidence that liquid water or some form of it existed on this world being the amounts that can be found in the atmosphere.
Unlike its twin, the weather here is way calmer. Sandstorms are a rarity, with the last one occurring in the Spring of 2019. Cyclones are almost non-existent on this world, with only 3 ever being observed, and all of them occurred during a small 3-month time span during 1995. Though unrelated to weather, the PO (Personal Observer) of this world has a pet theory, that being that the moon has more resources than its twin, this is due to the scans of this world revealing that the moon for every square 10 x 10 miles on average has more Silicon, Iron, Copper, and Cobalt, and if there was a civilization that ever develops on any of the moons, that this moon would be a mineral mining colony, opposed to its twin further in. In conclusion, this moon is pretty much the calmer version of its twin further in the moon system. It has way fewer storms on average, cooler temperatures, and there might have been larger liquid oceans here. Large spherical dead seas litter this world, most likely from asteroid impacts in the "recent" past.
====Gallery====
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===Icesnapun===
The one gaseous world around this parent planet, it being the 6th away, it is also the largest and coldest amongst the other worlds around said parent planet. The planet has a mass around 15 times that of the Earth, with the diameter being 3 times that of the Earth. This world was noted by PO as being a pretty visible one, with it being observable from 6 out of the 7 moons. The ice giant on its own is not that interesting, but it might have an odd secret below its clouds. PO along with CALASE and SKYNAV whilst observing this world have noted that even though the clouds extend down for a long time like many other gaseous worlds, this one’s may be shorter, and it may be hiding a spiky surface, laced with 2 possible biomes. Flatlands, and Pikelands, both of these possible biomes here are more speculative in nature, and do not have that much data on each, but we can make some educated assumptions about the planet’s possible rocky surface. Unlike the cores of many other gaseous worlds, this one’s is a lot larger, with it being more than the atmospheric mass by a long shot, and by atmospheric, we mean the gaseous part, not the “atmosphere” that is listed being only several hundred or thousand miles above some supposed surface.As mentioned before, 
the two possible biomes are very molded to the moon’s weather, with scans of the world’s possible surface revealing that the ‘land’ is very flowy, swirly, and I guess what you would call it, spiky. The mountains and hills seem to jut out in random locations, and they are very resistant to the conditions down there for somerason, maybe some hyper strong rock possibly? Than there are the flat lands, these are the lesser likely of the two to exist, as they seem to manifest whenever the data is just not good enough on one particular location, but if they do exist, they are sublime, slightly-rolly landscapes that re being slowly being edged every day, becoming the rest of the moon’s atmosphere. Moving off the moon’s surface, we can see that due to the massive size of it, the moon attracts and thus absorbs the brunt of asteroid and comet bombardments, with it taking on 23 of them in the last 40 years of observation, with the rest either hitting the moons or being sligshooted out of the moon system all together, and whilst looking up at the skies of the other moons, excluding the seventh, this moon exists as a sometimes faint, large blue banded ball in the sky, acting as the sort of vanguard of the moons.
====Gallery====
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===Faresnapun===
This moon is a truly unique celestial body, distinctive in several ways. It's the outermost moon orbiting the parent planet, and its considerable distance from the planet, at approximately 0.17 astronomical units (AU), sets it apart. This distance is truly remarkable and contributes to the moon's distinct characteristics. One of the most striking features of this moon is its cloudy exterior. Much like the first moon in the system, it's shrouded in a thick layer of clouds. These clouds create formidable storm systems that tower high above the moon's surface, generating an atmosphere of mystery and intrigue. The moon's geography is a blend of the second and fifth moons in the system. Its terrain is a mix of rugged, cratered landscapes and vast, barren expanses. The surface is marked by rocky outcrops, vast dunes, and numerous basins. These basins are scattered across the moon's landscape and hold small lakes and ponds, which add to the moon's mystique and allure. 
Beneath the enigmatic veil of clouds, explorers and scientists have managed to catch glimpses of these intriguing geological features, offering tantalizing hints of what lies beneath. These features hint at a complex history and geological evolution. One intriguing theory about this moon involves its origin. Some experts propose that it may have been captured by the parent planet during its formation. This hypothesis suggests that the moon was once a distant, wandering planetoid, which the parent planet's gravitational pull trapped within its orbit. This intriguing concept adds a layer of fascination to this already captivating moon, suggesting it may have a more ancient and tumultuous history than initially thought.In conclusion, this distant and cloud-covered moon, with its enigmatic storms, unique geological features, and captivating capture theory, is a celestial wonder waiting to be explored and understood by future generations of astronomers and planetary scientists.
====Gallery====
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==Star system==
(This is a heading because of the whole table of contents thing, you would not really want "Star system" under "Moons" now would you?)
The star system that the planet is part of is a young intergalactic star system which exists 388.13 kila-light years away from the Earth. The star system has 8 total celestial bodies, (1 star (B6 IV), 6 planets, and 1 dwarf planet). The system also boasts both an asteroid belt and an oort cloud. The age of the system is technically unverified due to the position of the system being too far for the system to have just migrated from the edges of the milky way, around the black hole, than shot out to travel this far distance, which is not that feasible under that time span. The system is estimated to be 0.98 billion years old instead.
===Star system gallery===
File:Tesnapun-048.png|88-TARG3 in its bland glory.
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Category:Procedural objects
Category:Objects
Category:Gas giants
Category:Alternative generation
Category:Megajupiter
Category:Megaplanets
Category:Planets