Tseiload

(I hate writing biospheres.)
==Tseiload==
===Technicals===
====Physicals====
The moon has an equatorial diameter of 5319.67 miles, with the mean diameter being 5312.02 miles, and the polar diameter is 5296.77 miles. The moon has a mass of 0.3262 M⨁, or 1.9482*10^24 kilograms, with the density being 5.9553 grams per cubic centimeter, and the insolation is 1.7774. The effective temperature here is 265.01 kelvin, with the Earth Similarity Index is 0.863. The rotational period is 20 hours, 17 minutes, and 38.52 seconds, with the solar day being 20 hours, 22 minutes, and 8.71 seconds, and the axial tilt is 0*00’00.00”, or 22*53’2.65 to the parent star. The gravity on the equator is 7.0704 meters per second, with the gravity on average being 7.1066 meters per second, and the gravity on the poles is 7.1476 meters per second. The circular velocity is 12337.74 miles per hour, with the escape velocity is 17448.19 miles per hour, and the age of the moon is 8.209 billion years, additionally the tidal heating is 5.806*10^13 watts. 
====Atmospherics====
The moon’s atmosphere has a tall height of 85.79 miles, with the tropopause height being 19.14 miles, and the height of the homogeneous atmosphere is 43681.28 feet. The atmospheric pressure is 6.34 atm, with the air density being 6.8062 kilograms per cubic meter, and the air temperature here is 315.16 kelvin, (42.01 *C, 107.618 *F). The speed of sound is 793.38 miles per hour, with the exosphere temperature being 1498 kelvin, and the greenhouse effect is 50.048 kelvin. The average molar mass is 28.044, with the relative mass being 9.6665*10^-6, and the actual mass of the atmosphere is 3.9415 Earth atmospheres, or 1.8832*10^19 kilograms. Oxygen makes up 46.5%, with Nitrogen at 25.9%, Water vapor at 24%, and Carbon dioxide at 3.61%. 
====Hydrospherics====
The moon’s oceans have a maximum depth of 16584.95 feet, with the average molar mass being 18.015, and the density of the oceans is 1 gram per cubic centimeter. The atmospheric pressure is 6.34 atm, with the bottom pressure being 361 atm, and the bottom composition is rock. The oceans are completely made up of fresh and saltwater, with no other components.
====Orbitals====
The moon’s parent is a superjupiter, with the orbital type being an elliptical, and the orbital period is 20 hours, 17 minutes, and 38.52 seconds. The semimajor axis is 233033.2593 miles (4.8567 Rp), with the pericenter being 233024.5365 miles, and the apocenter is 23304.9822 miles. The eccentricity is 0.000, with the inclination being 0*29’7.19”, and the ascending node is 34*3’14.05”. The argument of pericenter is -87*31’6.19”, with the mean anomaly being -138*4’50.85”, and the longitude of pericenter is 53*27’52.13”. The mean longitude is -191*32’42.99”, with the orbital velocity being 72148.84 miles per hour, and the hill / influence sphere radius is 11204 miles / 9476 miles. The roche limit for satellites is 4058 miles as well.
===Store===
====Internals====
The moon’s internal structure is more active than most other worlds. This is due to the moon being close to its parent gas giant, unlike most other moons which are habitable, them being far out from the parent planet, this moon is closer to the parent world. This has made the tidal forces between it and the parent star more intense, thus making the internals more hot and stretched, more flexible. The crust is sort of torn apart, cracks though not seen on the surface most of them time, stretch down to the mantle, thus these cracks have created new tectonic plates, even this late into the moon’s life. These cracks also make it easier for the mantle / core to spew out magma onto the surface. The new tectonic plates are also fast, smashing and pulling each other, creating the scarred geography that is seen today. The core here also spins a little faster than the rotational period, creating a magnetic field which is 0.10s stronger than the Earth’s field. In short, tidal heating has created a very active and destructive internal structure which could be likened to a primordial world, creating new plates even this late into the moon’s life.
====Geography====
The moon’s geography, due to the constant tectonic destruction, reformation, creation, and destruction again, is very peninsular. The continents here are made up of lots of peninsulas; essentially, there is only one continent here that is not only made up of peninsulas, and that is the southernmost one. Even then, it has plenty of large peninsulas that come off of it. The abstract painting of geography here has created hundreds of small seas and lakes, as well as opposing small islands and continentlets. Interestingly enough, there are not that many mountains here; instead, the highest islands here are hills. This may be due to the lack of a consistent geographical contraction. In short, the geography here is like that of an abstract painting—random and spontaneous. Note: Navigation here on the seas is nearly impossible, as there are also plenty of landbridges.
====Climate====
The climate here is considered to be generally tropical. A massive tropical rainforest, akin to the Amazon rainforest, largely covers the moon. It is way more humid, more windy whenever there is a storm of some kind, and way more rainy whenever said storm passes over, and the environment is more susceptible to mudslides and large-scale flooding. This environment is, of course, propagated by the destructive tectonic-tidal system, which generates uneasy and low ground. This global rainforest may exist due to an interesting biosphere, but also to the constant greenhouse-related eruptions by volcanoes and occasional cracks in the ground that spew out large amounts of magma. This greenhouse effect might have raised the humidity globally and may have shaped the biosphere to form one global tropical climate. This global rainforest, however, does have some interruptions. There are drier climate zones, which act like small red-deserts, and they also give an insight into what areas of the moon are most susceptible to fault opening or eruption. These smaller climates are way drier, more arid, and more windy, considering the flatter terrain. Overall, there is a global tropical climate with some arid interruptions.
====Biosphere====
The dense foliage is most likely an indication that most of the moon’s biosphere is concentrated in plant life. Most of this plant life is tall, deep green, and has very large and thick leaves, making it most likely to compete over sunlight while starving out competition. This may also indicate that the biosphere is currently in a highly competitive stage. Biospheres are always in that stage if they are healthy, but if the conditions are right, they can cause large amounts of new species and adaptations to appear at a pace that would not be normal. It would be like a new forest of species every decade if it were on Earth. In the few cases where we are able to see animal life or bug life, we would see that these creatures are very fierce with each other. Most of these animals also appear to be feline in their structure, indicating that most of this moon’s animal biosphere is made up of Lion, Tiger, Puma, Jaguar, Tiger, and Cheetah analogues. These fierce creatures also seem to have resilience to the extreme temperatures of magma, sometimes being able to survive in it for around 10–15 seconds. 
This may be an adaptation to the competitive environment; there are no creatures on Earth that have evolved this trait. Lastly, into the seas, where they may be, lie coral reefs. This moon’s waters are infested with them. During the first observations of this world, the seas glimmered colors that were presumed impossible for any regular liquid, but later it turned out that it was just the coral reefs that were tall enough that very large swaths of the ocean were penetrated by the reflected colors of said reefs. Because of this abundance of corals, there are large populations of various fish. Most of these fish exist in schools—large, vibrant swarms going at fast speeds across the light seas. In the deeper waters, there exists a unique type of species that acts as a very large collective predator once it forms into a school, able to feast on what would have been dangerous foes to any other normal species of fish. In short, large and towering trees with massive leaves, coral reefs that cover the majority of water in vibrant colors, predatory collectives of small fish, lava-resistant felines, and a hypercompetitive environment.
===Gallery===
File:Tseiload-001.png
File:Tseiload-002.png
File:Tseiload-003.png|Ontop of an overgrown volcano with the parent planet in view.
File:Tseiload-004.png
File:Tseiload-005.png|A typical fault found here. Most of these faults after they open up get filled in with water.
File:Tseiload-006.png
File:Tseiload-007.png
File:Tseiload-008.png
File:Tseiload-009.png
File:Tseiload-010.png
===Moon system===
The moon exists in a very simple moon system. It is the only major moon around the superjuptier which it also orbits close to. There are however plenty of minor asteroid moons that orbit around the parent planet, both in the large cloud, and the small orbital plane. These asteroids are not that unique, and in the sky of this moon, they are sort of like fast moving stars. 
(There are no other moons to compare it to so there is no table here)
File:Tseiload-011.png|The moon system in total is very large in physical size. This world is barely seen from here!
===Star system===
The moon exists in a binary star system. The system has a primary, (which this moon also orbits by proxy) , yellow dwarf (G6.2 V), and a secondary red dwarf (M2.1 V). The primary has 5 planets and a small asteroid belt around the first position. The secondary has 6 planets, a small asteroid belt around the first position, and a small oort cloud of its own. The system does not have a collective oort cloud. 
File:Tseiload-012.png
Category:Procedural objects
Category:Objects
Category:Terrae
Category:Life
Category:Moons