Ocegellanon

==Ocegellanon's properties==
===Physicals===
This world has an equatorial diameter of 10119.37 miles, with the mean diameter being 10086.53 miles, and the polar diameter is 10021.17 miles. The oblateness is 0.0097048, with the mass being 2.8313 M⨁, or 1.691*10^25 kilograms, and the density is 7.5504 grams per cubic centimeter. The insolation is 0.8794, with the effective temperature being 221.71 kelvin, and the Earth similarity index is 0.853. The rotational period is 12 hours, 4 minutes, and 20.73 seconds, with the solar day being 12 hours, 3 minutes, and 7.83 seconds, and the axial tilt is 155*29’47.51”. The gravity on the equator is 16.865 meters per second, with the gravity on average being 17.108 meters per second, and the gravity on the poles is 17.332 meters per second. The circular / escape velocity is 26402.40 miles per hour and 37338.63 miles per hour, with the age being 11.908 billion years, and the tidal heating is 4.1234*10^8 Watts. Silicate mantle makes up 58.4% of the insides, with metallic core making up 41.6%.
===Atmospherics===
The height of the atmosphere is 29.07 miles, with the tropopause height being 47811.10 feet, and the height of the homogeneous atmosphere is 17480.77 feet. The atmospheric pressure is 20 atm, with the air density being 22.375 kilograms per cubic meter, and the air temperature is 305.45 kelvin, 90.14 *F, 32.3 *C. The speed of sound here is 777.32 miles per hour, with the exosphere temperature being 1391.3 kelvin, and the greenhouse effect is 83.715 kelvin. The average molar mass is 28.634, with the relative mass being 5.3018*10^-6, and the real mass of the atmosphere is 18.764 times that of the Earth's atmosphere. Nitrogen makes up 48.4% of the atmosphere, with Oxygen at 35.9%, Water Vapor at 12.6%, and Carbon dioxide makes up 3.05%.
===Hydrospherics===
The maximum depth of the oceans here is 42569.98 feet, with the average molar mass being 18.015, and the density is 1 gram per cubic centimeter. The atmospheric pressure is 20 atm, with the bottom pressure being 2.21*10^3 atm, and the bottom composition is rock. Water, salt and some fresh water, make up 100% of the oceans here.
===Orbitals===
The planet’s parent star is the main in a binary, and the orbital type is elliptical. The orbital period is 299.491 days, with the semimajor axis being 0.8455 AU. The pericenter is 0.8145 AU, with the apocenter being 0.8766 AU, and the eccentricity is 0.037. The inclination is -0*07’33.90”, with the ascending node being 155*47’6.50”, and the argument of pericenter is 229*40’23.66”. The mean anomaly is 314*51’54.95”, with the longitude of pericenter being 385* 27’30.17”, and the mean longitude is 700*19’25.12”. The orbital velocity is 68705.17 miles per hour, with the orbital resonances being 4:3 (A5), and the hill sphere radius is 1110159 miles. The influence sphere radius is 768673 miles, and the Roche limit for satellites is 8340 miles.
==Store==
===Internals===
The planet has an active internal structure, way more active than the Earth. In addition to the core being larger in proportion to the rest of the planet, the internal structure is mostly molten, which causes each layer to sort of blend into each other. The mantle does not have a clear boundary with the outer core, and the crust actively breaks, which allows for the hot mantle to pour out in large amounts from even the smallest cracks. This is why there are so many volcanic islands. Because the mantle blends in many places with the outer core, the magnetic field is not stable and will act in interesting ways, giving it an odd shape that leaves weak spots. 
This shouldn’t be surprising, but the active insides cause faster and more destructive tectonic drift; the average drift is 2.109 times the speed of the Earth’s drift, of which some drift has been tracked in the short time the planet has been known. The core, while not having a defined border, has a roughly known composition. It is mostly made up of nickel, iron, and silicon, with some trace amounts of other similar resources. The mantle has a similar composition, but the top has more silicon, and the crust follows the same trend.
===Geography===
This planet has a very oceanic geography; in other words, 94% of the planet is covered by a global, deep ocean that is made up of exclusively salt water. Salt water is way “saltier” than the water we have on Earth on average. This ocean is not uniform, and it is punctured by a large number of volcanic islands. These volcanic islands are small in size, around the size of Rhode Island, with the largest island being half the size of New Jersey. These islands are normally isolated from each other; 
they are evenly distributed among each other, and their average distance is around a full Caspian sea, which is pretty far. These volcanic islands make up around 76% of the land area here, but where is that 24% from? That 24% is from a small archipelago in the southern hemisphere, which is an old mountain chain from a sunken continent. That sunken continent seems to be the only one present in the planet’s crust. Its age is around 600 million years, and there are no other continental structures either, so it is assumed that the planet, even before that continent was sunken, was a primarily oceanic one. The geography here is one of the fastest-changing, with two new islands appearing since 2020 and five since 2013.
===Climate===
This planet has a cool climate despite its hot interior. While the planet’s average temperature is higher than the Earth’s, the environment is more like the fringes of middle Alaska; snowfall is a regular occurrence here; and the trees are not like those found in tropical rainforests; they would find home in the wilderness of the Taiga. How often is there snow here? Most days in a 365-day, 24-hour term, around 41%±2% have at least 1 inch of snowfall (on average) across the land area of this planet; the rest of the term is occupied by either heavy rain (thunderstorms), thick cloudy, or partly cloudy days. The climate has made sure that there is not a single day where the sky is completely clear all day, and that is because of the volcanoes that were mentioned earlier. These volcanoes produce large amounts of greenhouse gases, which heat the planet and cause higher amounts of evaporation, which would cause higher amounts of cloud formation.
These volcanoes erupting would heat the planet, but over time they can cover the planet, and eventually, the climate cools, which would result in a cooler climate, like the one we see here. This climate could also explain why one continent got sunk, and that would be from a past ice age that ended when the volcanoes began erupting more than usual, causing the cool climate to heat up and melt the ice. This could also mean that the volcanoes here may be the main driving force behind the climate’s change. These volcanoes have not made the planet cool enough though that strong storms could not form, they form quite regularly. Category 4 cyclones form here every few days, and they live for a few weeks even, circling the planet’s equator at a moderately large size, with the largest cyclones here getting to the size of the Eastern United states. 
===Biosphere===
====Landsphere====
Since the amount of land here is limited, the biosphere is limited in what it can be, but because of how far apart the landmasses are from each other, the biodiversity, despite the limited number of possibilities, can shoot up. Most bear species here are small, as their habitat is small, and most species of bear here do not hibernate, contrary to how their Earth counterparts would behave. Most bears here are also adept at swimming, considering most of their prey is out in the ocean, which is why their fur has evolved to be waterproof or at least able to dry out quickly. One species of bear has even evolved to have a fin-like structure at the back and some gills. Most bears here have a light brown coloration. Moving to another group, we have foxes, which here are a shade of bright purple (though on some islands they have a more reddish tone), and most of them have two tails (some islands have foxes with three tails even!) instead of one, though it is a bit unfair to consider it a second tail, more like a 5th leg, which is able to pick at trees if needed to make a storage place for food.
These foxes are way smaller than our foxes, allowing them to go at a quick pace to run away from predators, but the smaller size also gives them a higher metabolism, which makes them eat more. A species of plant here has even evolved to fit their needs, growing large amounts of berries over a short period of time so it can take advantage of the short and fast diet of these purple foxes to spread its seed. Some of those two-tailed foxes have gills of their own, though those are for the species that mainly feed off of underwater plants and some fish (no, there are no “onland” fish, only underwater fish). Moving to the plants, we find that most plants are trees. These trees, on average, can grow up to 500 feet, and they grow massive leaves that are several feet wide and long, which also produce a dark environment below the canopy. This has led many animals, those that live natively in those dark environments in particular, to evolve a form of limited nightvision. That does not matter here, though.
What does matter is that most plants on land are massive 500-foot trees with sometimes 8-foot-long, 6-foot-wide leaves that have trunks that can be up to 160 feet wide. That is massive! These trees have massive leaves because the climate makes clear and regular days impossible, and days where the clouds cover the entire sky, which most of the time release rain or snow onto the land, are quite common. Thus, they must maximize the amount of light they can get from the parent star. You may be asking how plants on the ground live; it must be impossible, right? Wrong; they thrive, actually. The plants on the ground tend to be parasites, growing on the roots of the massive trees, and while the immune systems of those trees will try to get rid of them, they ultimately have to live with massive amounts of parasitic plants growing on them. 
These plants don’t look like parasites; yes, most of them have thorns and have roots growing around their host trees, but most of them are regular berry bushes. Most of them are regular-sized and produce regular-sized berries, though the amount may vary from plant to plant. There are some species of flowers here, but most plants here are berry bushes. What is described here is the typical land biosphere, but it varies a lot from island to island, and some islands have large variations of the typical, but these are the general strokes.
==== Hydrosphere ====
While the land biosphere is diverse, the ocean biosphere is the opposite. Because of the amount of salt in the ocean, life down there is way more limited and small in quantity, restricted to the bottom of the ocean. Most of the fish are large in size, live near hydrothermal vents, and are all blind, relying instead on their other senses to find food, mates, and a shelter. There are a few species of plants in the oceans that, instead of relying on sunlight for energy, rely on the heat from the hydrothermal vents, and they have underwater fruit that these fish feed off of. Moving a bit further up to the sunlight zone of the oceans, we find that the only real life here is coastal algae and plants, who are not really special.
They are green like the plants we have; they rely on the parent star’s light; they are mostly kelp-like, though some are bushes themselves; and all of them don’t have fruit; they are the land animals' vegetables essentially. How do they spread? They spread by spores (normally, some have the island’s near coastal fish to spread them). It was previously mentioned that the only real life on the ocean's surface is plants, but this is a bit of a lie. There is a small community of fish that live here, but they primarily inhabit the island's numerous rivers and ponds, not the ocean, which is also where most of these plants reside. It is not too well known how the ocean life deals with the large amounts of salt.
====Arialsphere====
The biosphere in the air is mostly tied to the ground, though not on the ground, but a little higher than the ground in the trees. Most birds here live, scavenge, and build their nests in the massive canopies of the trees, and they are generally very social with each other, even with members of other species. Some birds here even build co-nests with other species of birds, essentially inter-species nurseries. This social environment has led to some interesting evolutionary consequences.
First, some species have an elevated level of social intelligence, forming a proto-culture in the most advanced cases, and some species have evolved parasitic behaviors that take advantage of interspecies good will, like how some have eggs colored in the same pattern as other birds so that they can easily switch out eggs, allowing a bird to give the job of raising to another bird. Overall, the arialsphere here is a very social one, and it may be the place where the first planetary civilization arises.
==Gallery==
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==Entras==
===Moon system===
The planet has a moderately sized moon system: 5 moons, 2 of which are majors and 3 of which are minors. The 2 major moons are close to the parent planet and are on the planetary plain, unlike the 3 other moons, which are captured asteroids that orbit in a cloud formation. The two major moons have a similar composition to the parent planet, though they have more silicon and platinum than their parent planet. The moons have a composition more like the planets from the inner part of the primary half of the star system, which points to them being captured as mentioned before. This is a moderate moon system, average for a planet of this size and mass.
 	Arbarton 	Ovengell
Image 	
File:Ocegellanon-011.png 	
File:Ocegellanon-012.png
Class 	Temperate airless microterra	Temperate airless microterra
Mass 	0.062107 M◑ 	0.10858 M◑
Diameter	734.15 Miles 	899.24 miles
Orbital 	11h 55m 31.03s 	25h 36m 22.87s
===Star system===
The star system is a binary one, with the primary star being a yellow dwarf (G9 V), which has 9 planets, 2 with life, and a secondary star, a red dwarf (M0 V), which has 6 planets, 1 with life. The primary has an asteroid belt in the orbit of the first planet and a large oort cloud, with the secondary having an asteroid belt in the orbits of the 3rd and 4th planets, and a large oort cloud of its own. The binary system has a single planet orbiting both stars, with its orbit being 11819.496 years.
File:Ocegellanon-013.png|General system
File:Ocegellanon-014.png|Primary
File:Ocegellanon-015.png|Secondary
Category:Procedural objects
Category:Objects
Category:Terrae
Category:Life
Category:Terra with Rings
Category:Planets