Earcapoillo

(I guess Chatgpt's new update has made grammar correcting / readability worse, because most of the time it just copies the text back. Also the reason why I took a week on this world is because I was preoccupied with other stuff.)
==Earcapoillo's information==
===Technical details===
The equatorial diameter of the planet is 15717.01 miles, with the mean diameter being 15662.86 miles, and the polar diameter is 15555.11 miles. The oblateness is 0.010301, with the real mass being 9.6724 M⨁, or 5.7767*10^25 kilograms, and the density is 6.8884 grams per cubic centimeter. The insolation of the carbonia is 0.091926, with the effective temperature being 140.02 kelvin, and the Earth similarity index being 0.699, which is way higher than expected considering it is a warm supercarbonia. The rotational period of the planet is 12 hours, 11 minutes, and 0.7.17 seconds, with the gravity on average being 24.238 meters per second, and the gravity on the poles is 24.574 meters per second. The circular velocity is 39164.46 miles per hour, with the escape velocity being 55386.92 miles per hour, and the age of the planet is 6.650 billion years, in addition to that the tidal heating being 4.2441*10^10 watts.The height of the atmosphere is 49890.76 feet, with the tropopause height being 29695.59 feet, and the height of the homogeneous atmosphere is 8480.47 feet. The atmospheric pressure is a very high 830 atm, with the air density being 1351.8 kilograms per cubic meter, the air here is effectively solid rock if you were to attempt walking through it, with the air temperature being 362.64 kelvin, (89.49 degrees Celsius, or 193.082 degrees Fahrenheit), and the speed of sound is 644.30 miles per hour. The exosphere temperature is 889.48 kelvin, with the greenhouse effect being 222.51 kelvin, and the average molar mass is 42.284, in addition to that the relative mass is 0.00010973, plus the real mass of the atmosphere is 1326.7 Earth atmospheres or 6.3386*10^21 kilograms. 
Carbon dioxide makes up 70.7% of the atmosphere, with regular Carbon Monoxide being 25.8% of the atmosphere, Nitrogen makes 3.25%, and Water vapor makes up the rest at 0.122%.  The maximum depth of the oecaeans here is 12932.15 feet or 2.5 miles, which is just slightly deeper than our oceans’ average depth, with that, the average molar mass is 18.033, with the density of the oceans being 1.0002 grams per cubic centimeter. The temperature of the oceans is 362.64 kelvin, with the atmospheric pressure down there being 830 atm, (which due to some ingame reasoning may be the maximum for terrestrial planets), and the bottom pressure is 1.77*10^3 atm, in addition to that the bottom composition is rock. Despite it being a Carbonia, regular water makers up all the liquids here at 100%. The parent of this planet is the secondary of a binary star system, with this planet’s orbital type being elliptical, the most common and most likely only real type of orbit, the planet also has an orbital period of 160.048 days. The semimajor axis is 0.3900 AU, with the pericenter / apocenter being 0.3702 AU and 0.4098 AU, and the eccentricity is 0.051, in addition to that the inclination is 1*18’44.58”. The ascending node is 48*19’49.45”, with the argument of pericenter being 157*53’57.07”. The mean anomaly is 240*01’55.13”, with the longitude of pericenter being 206*13’46.52”, and the mean longitude is 446*15’41.65”. The orbital velocity is 59302.33 miles per hour, with the hill / influence sphere radius(s) being 1085031 miles and 888537 miles, and the Roche limit for satellites is 12561 miles.
===Infolore===
This is a large, nearly mega carbonia in the small dwarf galaxy, the Sagittarius Spheroidal Dwarf Galaxy. This supercarbonia features five notable biomes, descending from the most common to the least common: Carbon plains, Carbon beach, Silicate hills, Archipelagoic wastes, and Carbon dunes. The first of these biomes is the Carbon plains. Similar to their counterparts, Carbon beaches, they are wide, sweeping, large, and grand spaces. The difference lies in their elevation; Carbon plains are situated higher up. This biome experiences the most chaotic weather on the planet. Whether this weather would be considered chaotic for us is subjective. The weather across the plains ranges from Kansan Clouds, making the golden sky more interesting, to large and powerful tornadoes, some reaching several miles in width. Moving closer to the sea, the next biome is the Carbon beach. These low-lying plains are more prone to flooding than their higher-elevation counterpart. They tend to be less eventful in terms of weather, with peaks occurring during the planet's cyclone season. The cyclones that flood these coastal plains typically range from category 1 to 2. Occasionally, these hurricanes may approach more inland regions, transitioning into the next biome, Silicate hills. Silicate hills is a biome that consists of several smaller subtypes, most of which are mountainous, rich in diamonds, and very cold despite the planet's high average temperature. These "hills" are, in fact, mountains formed from tectonic shifting. In some cases, they can grow to heights surpassing even Mount Everest. One such mountain, Mt. Earcapoillo hyperborus, impressively stands at a height of 10.6 miles. It's worth noting that this mountain, with an age of only a few million years (based on observations), will eventually reduce to a more manageable height due to the planet's gravity. Looking down from Mt. Earcapoillo hyperborus, one can observe the sea (somehow, for infolore purposes), and the next biome on our list, the Archipelagoic wastes. 
This biome is related to the Carbon beaches in many ways, but this biome is the more dry and craggy version, it is flat, uninteresting, and the ground looks like something straight out of a Mad Max movie. This biome is found in one of the planet’s many archipelagos, and typically gives the islands the ability to change shape if enough force is applied, like if one of the several tsunamis that happen here every few years occurs, and these tall and imposing titanic waves of water can sometimes crash through the land, and deposit in the Carbon dunes, the next and final biome on this list. The Carbon dunes are a desert-like geologic region that is composed of mostly sand. Many would argue that this is a desert, and it is, but the thing that separates it from a regular dry desert is the fact that it can have regular rain. These geologic formations that are the result of dust from other regions over time collecting in one region  get regular rain from whatever weak water cycle that exists here, and “oasiss” are commonly found here. These 5 biomes are spread across 3 continents, two of the continents are island-like, surrounded by massive seas that in their calm nature, you can find the many islands that surround these 2 continents. The other continent is in fact a supercontinent, this large land mass made up of 4 other continents formed a few deca-millenia ago, and makes up over 85% of the planet’s land mass. 
It is positioned on the northern half of the planet, and dominates the northern hemisphere, and has a foothold in the southern with a continental peninsula the size of the larger of the two island continents existing in said southern hemisphere as an extension of the main supercontinent. Besides the 3 continents (2 continents, 1 supercontinent), there are a few dozen volcanic islands that dot the oceans. Now that we are done with geography, we can move on to other stuff. The ring system of this planet is split into 4 sections, A, B, C, and D, and this ring system is made up of the typical materials that you would find on any terrestrial world. The only mention of this world outside of scientific journals, is a map of the Carbonias in the Sagittarius Dwarf Spheroidal galaxy, in the “Carbonica Observers” newspaper (2015), where it was featured as a “Large, and titanic Carbonia, nearly twice the size of the Earth, and nearly 10 times the mass, this world is like many other Carbonias, just warmer, and is the larger version of another, more interesting Carbonia.” We do not know that much about the recent history of this world, no one has taken any key interest, and the only major things that happen here are a few comets that fall onto this world. In conclusion, this is a massive Carbonia that happens to be uninteresting. 
===Gallery===
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===Moons===
There are no major moons around this planet, instead, there are 8 small dwarf moons that orbit in two groups, the first 3 on the planetary plane of the parent planet, and the last 5, that orbit within a cloud-like formation. 
Categories 	Cleasmen 	Tarfoia 	Earcapoillo III	Earcapoillo IV	Earcapoillo V 	Earcapoillo VI 	Earcapoillo VII	Earcapoillo VIII
Photograph 	
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Class 	Cool asteroid 	Cool asteroid 	Cold asteroid 	Cold asteroid 	Cold asteroid 	Cold asteroid 	Cold asteroid 	Cold asteroid
Mass 	3.6742*10^6 M◐	4.9916*10^6 M◐	6.7943*10^6 M◐ 	9.274*10^6 M◐ 	1.2707*10^-5 M◐	1.7495*10^-5 M◐	2.4234*10^-5 M◐	3.3817*10^5 M◐
Diameter 	25.47 Miles 	32.08 Miles 	37.14 Miles 	43.66 Miles 	48.26 Miles 	53.48 Miles 	58.91 Miles 	66.49 Miles
Orbital period	4h 1m 32,74s 	7h 29m 48.46s 	9h 37m 50.86s 	7.644d 	10.686d 	12.716d 	16.739d 	19.441d
===Star system===
The star system that the planet is part of, is a typical binary star system between two red dwarfs. The primary has 8 planets and has both the Carbonia in this article, and the only planet with life in this system, a temperate minineptune with a mass less than the Earth, that has multicellular aerial life. The system has 17 planets in total, and both stars have an asteroid belt, and an oort cloud. The secondary star has 7 planets, and 2 planets orbit the Barycenter between the 2 stars.
====Star system (A)====
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====Star system (B)====
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====Star system (A & B's Barycenter)====
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Category:Procedural objects
Category:Objects
Category:Carbonia
Category:Supercarbonia
Category:Planets
Category:Marine