Coidoid

(I also could've done a 992 word paragraph.)
== Coidoid's technicals ==
=== Physicals ===
The planet has an equatorial diameter of 4738.58 miles, with the mean diameter being 4738.58 miles, and the polar diameter is 4738.58 miles. The oblateness is 0, with the mass being 1.3981*10^24 kilograms, or 0.23409 M⨁, and the density is 6.0205 grams per cubic centimeters. The insolation here is 0.87855, with the effective temperature being 216.72 kelvin, and the earth similarity index is 0.863. The rotational period is 5.403 days, with the solar day being 5.152 days, and the axial tilt is 100*45’56.74”. The gravity on the equator is 6.4225 meters per second, with the gravity on average being 6.4088 meters per second, and the gravity on the poles is 6.4088 meters per second. The circular velocity is 11057.99 miles per hour, with the escape velocity being 15638.36 miles per hour, and the age of the planet is an elder 9.789 billion years, additionally, the tidal heating is 2.9122*10^11 watts. 
=== Atmospherics ===
The height of the atmosphere here is 75.32 miles, with the tropopause height being 25.43 miles, and the height of the homogeneous atmosphere is 47349.78 feet. The atmospheric pressure is 27.9 atm, with the air density being 30.532 kilograms per cubic meter, and the air temperature is 307.74 kelvin, 34.59 *C, 94.262 *F. The speed of sound here is 785.56 miles per hour, with the exosphere temperature 1202.7 kelvin, and the greenhouse effect is 91.001 kelvin. The average molar mass is 27.705, with the relative mass being 5.1974*10^-5, and the actual mass of the atmosphere is 15.208 Earth atmospheres. Nitrogen makes up 86.6% of the atmosphere, with Oxygen at 12.1%, Water vapor at 0.774%, and Carbon dioxide at 0.533%. 
=== Hydrospherics ===
The maximum depth of the oceans here is 6630.98 feet, with the average molar mass being 18.017, and the density of the oceans is 1 gram per cubic centimeter. The temperature of the oceans is 307.74 kelvin, with the atmospheric pressure being 27.9 atm, and the bottom pressure is 156 atm, additionally, the bottom composition is rock. Water makes up a relative 100% of the liquids here, with Sulfur dioxide making up 34.8 parts per million.
=== Orbitals ===
The parent of this planet is the barycenter between it and another world, with the type of orbit being elliptical, and the orbital period is 5.403 days. The semimajor axis is 4216.1065 miles, with the pericenter being 4163.6491 miles, and the apocenter is 4268.5639 miles. The eccentricity is 0.012, with the inclination being 176*55’43.90”, and the ascending node is 162*10’56.34”. The argument of pericenter is 144*9’32.59”, with the mean anomaly being 166*30’17.79”, and the longitude of pericenter is 306*20’28.93”. The mean longitude is 472*50’46.72”, with the orbital velocity being 204.27 miles per hour, and the orbital resonance is 2:1 (5). The hill sphere radius is 263730 miles, with the influence sphere radius being 155185 miles, and the Roche limit for satellites is 3633 miles. 
== Store ==
=== Internals ===
The planet has a fiery internal structure with a very active core and a well-oiled mantle that regularly pushes and pulls the crust at a fast pace, way faster than what is found on Earth, all of this despite the planet’s advanced age. The core here is larger than the Earth’s relative to the parent planet, and this core is mostly made up of silicon, silver, and other silverite materials. This core spins at a faster rate than the Earth’s, at around 29% faster; in other words, this is a fast-spinning molten ball, and thus, the mantle is made hotter and faster, and the magnetic field is made stronger. The magnetic field here is stronger than the Earth’s by 43.013556%, which means that the planet is better protected from the parent star’s outbursts, but it also means that any civilization that lives here can’t develop past the late information age; in other words, it can’t advance past a few interplanetary colonies. The other thing that was mentioned was the more energized mantle.
The mantle here, because of the more active core, is way more molten and mobile than is expected for a planet of a similar age. This mantle moves around more often and is softer, which means that magma plumes can pass through it with less resistance than most planets. This is also the reason the planet has a lot of volcanoes across its surface, most of which are also active. Because of the mantle’s higher movements and general activity, plate tectonics moves faster, at a rate 5.1% higher than the Earth’s. This faster rate of tectonic progress means that the topography and geography are more chaotic and random, and while the lack of water won’t show it immediately, the topography does show it, with flat areas being randomly interrupted by new mountain ranges and volcanoes. There has even been a plate that cracked under pressure into two smaller plates only 400 thousand years ago. Overall, a more active planet and even small percentage changes, no matter how much, can make an environment radically change; a millimeter difference leads to a 1000-mile loss.
=== Geography ===
Most of the planet is covered by large swaths of land. This land surrounds two large seas of salt water, with thousands of smaller ponds, rivers, estuaries, lakes, and other such things surrounding them. The lands that surround the water are a patchwork of scattered flatlands that are randomly interrupted by 'misplaced’ mountains and hills. These scattered lands have no real semblance of consistent topography, featuring large changes over short land areas, with the only consistent topographical regions being the ones directly on top of tectonic plate boundaries. Going from the wastelands, we go closer to the water, where we find the coastal marshlands. These marshlands are a result of violent tectonic drifting and odd typography, creating lots of individual places that water can accumulate in. These marshlands are random and without real form, and so are the rivers that flow through them, going in random directions, which would make a kayaker’s arms fall off because of how many twists and turns there are. These rivers sometimes meet up and create shallow lakes that can only go down a few hundred feet at their deepest. These marshlands, wet as they are, from space look like they were part of a past ocean or sea, and it seems that they were, at least for a large group of them. There used to be an additional sea in the far south, but it seemed to be crushed into thousands of smaller lakes and mini-seas by tectonic plates. This marshland has the most lakes in total and is home to this planet’s only swamp-like sub-climate.
Following the rivers from lake to lake will eventually lead us to the seas—the two of them. There is an eastern and western one, both medium-sized, and are proto-oceans. These oceans are shallow, and all their islands are near the coast, with few exceptions. They are vertical in their size, and they are surrounded by generally flat coastlines. These seas are quite similar, but they have some differences. The eastern one has more large and fertile rivers flowing into it, and it has a more geographically consistent form. It also seems to follow a straight line, with little deviation to the east or west. It also has more smooth coastlines. The western ocean, while vertical, follows an east-to-west line, and it has jagged coastlines. This ocean (or sea) has more islands, and it has more marshlands, with it being home to the largest continuous marshland (not the southern one; that one just has the most lakes and is a swamp), featuring over 10,000 islands. Most of them are small though, only a few hundred feet in width at most. Those islands are connected to each other by very thin isthmuses and are separated by small lakes and ponds. Those islands are mostly sand dunes in appearance as well. The western ocean is bigger than the eastern one in total size and has more deviation from its core line. It has more marshlands around it, and it has less salt in it, which has led to decent biodiversity there. Overall, This is an uninteresting, mostly dry planet.
=== Climate ===
The climate here is mostly dry but still somewhat temperate or humid. The poles and equator don’t have that much variation in their sub-climates, and the humidity and weather between the two don’t have any real noticeable variation. The climates in the lands further in are drier and more desert-like, much like a more arid version of Oregon, and the climates near the coast are like those of Georgia, but with slightly less humidity and rain. The climates in between are like those of the Scottish Highlands, gradually getting more humid the further coastal or high you go. The weather near the coasts is more rainy but also way less thunderous than the inland deserts, which feature a commonality of dry thunderstorms. The climate here seems to disrespect the poles from a biomes’ perspective, with dense forests like that of the said Scottish Highlands being featured near or at both poles. This also goes for the inland deserts. This local rule seems to get violated by the lowland coastal climates getting more humid towards the equator, but this is a very gradual change, and it’s hard to tell if you are just monitoring the conditions on the ground. During the winter, the marshlands freeze over, mostly turning these swamps into icy wastelands that have an average temperature similar to Alaska.
=== Biosphere ===
==== Landsphere ====
The land biosphere is pretty limited in biological scope, considering there are not any real variations for the majority of the planet, but there are still some things to note here. Most animals are small and fast and normally have either 6 or 4 legs. They also are normally furless and much resemble a hairless dog. Yes, that’s disgusting, but that's the common animal here. The most common animal here is the Coidoidian Wast, a wolf-like animal that features a way faster top-land speed than even the cheetah. This animal has a top speed of 100 miles per hour, and its embers tend to group up into packs, which have a similar hierarchy to wolves. These animals are small in size and have six legs, which allows them to run at way faster rates than the rest of their counterparts. They are also universal carnivores, which means they also eat dead animals if necessary. They are much like piranhas, which is the opposite of the next species, the Coidoidian forest giant, a large dog-bear-like animal that lives in the low parts of the forested mountains. 
This animal can grow to 8’0” in height, and it features an omnivore diet that favors plants. This species has a dog-like form but a bear-like mentality, with its members being loners who kick out their offspring at an early age, and they tend to be very protective of their offspring when they do have them. They hibernate for large stretches of the year, the winter and fall, and they have fur, though not a lot of it at all, and what fur they do have is a whitish color that is easy to see through the skin. This species lives in the forest, which is unlike the next species, the Coidoidian Sog, a dog-like species that lives near the coasts and survives off a diet of fish and seagrass. It is small, around the size of a miniature Dachshund, and it has a moderate land speed. It has a thick skin, which allows it to fight off various carnivorous fish without too much damage, and this species is very adept at swimming, even more so than running or walking on land. This common species may transition from a land species to an ocean species in the near future, considering their ability to swim and proximity to the coast. It is quite odd considering there is so much land here.
==== Oceansphere ====
The ocean biosphere is quite diverse considering the limited amount of water on this planet, though most of this diversity is focused in the eastern sea. While it is quite diverse here, there are some common species that you will find that have their descendents everywhere. There are 3 fish and 3 plants in the eastern sea, and there are 5 fish and 2 plants in the western one. The eastern sea will be described first, and they will be described very briefly.
===== Eastern sea =====
The most common fish in the eastern sea is the Coidoidian photosynthetic fish, a brownish-colored fish of small size that uses photosynthesis to get its energy. It makes its own food, and it has no real diet besides water, the nutrients found on the skins of rocks, and the sun. A similar species can be found on the moon of Eefeesed. The next species is the Coidoidian kelp bounder, a multicellular organism that acts like a parasite by binding itself to the various plants on the seafloor. Its color is dictated by the plant it attaches itself to, and it is around the size of your palm. It has no real structure, and it grows around the plant it's a parasite on. It has its own root system, though here there are nerves that connect with the various internal structures of the plant, and these nerves lead to a brain, which is the only organ in members of this species besides a nervous-processing organ and a rudimentary heart. 
The next species of animal in the eastern sea is the Coidoidian whale, a large animal with a whale-like appearance that has a mouth that is flexible enough that it can open all the way to the underside of the whale. Its primary food source is plant fragments and microorganisms that float in the sea, and the size of the whale is around ½ the size of a blue whale. There are 3 plants in the eastern sea: the Coidoidian: red moss, jelly flower, and beach greens. Red moss is like regular moss, except underwater. It grows in deep caves and on the seafloor. It can also grow around jelly flowers, a plant with a super robust immune system that can repel everything from its system and even around it, except for red moss for some reason. The flower that blooms on it has a jelly-like form, and it's pollinated by whatever fish eat the flower’s core. Going a little further up onto the coast, we get to the last of the 3, the Beachgreens, a type of grass that grows in or near beaches, and it’s a food source for the Coidoidian Sogs. 
===== Western sea =====
We are moving across a thick land divider to the Western Sea, a larger sea that features many of the same species but has a few additional ones. The reason for why it has many of the same species is unknown, but it may be due to the two seas being united by a seabridge in the past. The 5 common species here are: (Coidoidian) Icy Parana, Hairy Fish, Fungus Back, Lake Wanderer, and Swarm Eel. The icy piranha is a piranha-like fish that swims primarily in the marshlands, and it swarms whatever prey it encounters. It has a carnivorous diet, and it also feeds off of land animals that get too close to the sea. What do these piranhas do whenever the winter comes around and the marshlands freeze over? They just hibernate in large collective “beds” in deep caves. How do they do this? They sacrifice some of their members as food so that the collective can survive! The next fish that is sort of like that is the hairy fish, a large vegetarian fish that has an interesting quality, which is the presence of hair on its skin. These are used to sense the environment around them, and they seemed to evolve out of the necessity of visual blindness. They live in the deepest parts of the ocean, where it is completely dark, and they tend to be loners. 
They are around the size of the Coidoidian whales and are most likely descendents of them. The next species is the fungus back, a small fish that, although it is like any other seafish in size and coloration, has a fungus growing on its back. This fungus seems to serve the purpose of cleaning the fish, which is necessary considering that it tends to live and feed in muddy and polluted waters. This seemed to form as a symbiotic relationship in the recent past, and it will most likely continue, unlike the Swarm Eel, an ancient and dying species whose members are small, eel-like fish who live in rivers and in very large groups, sometimes large enough that they can block their river with their amount. They are half the width of your finger and around the same length; they have a black coloration; they primarily eat various undersea mosses and plants; and for some reason, they have a good diet of whale meat and hairy fish meat; the former is rarer than the latter. There are two plants here: the Coidoidian black coral and the Coidoidian bubble flower. The Coidoidian black coral is a species of coral-like organisms that have the same functions as their earthly counterparts but also have a very dark coloration. It is unknown why they have this, but they live on the coasts in small coral reefs, which can sometimes give the appearance that an oil spill just happened there. The Coidoidian bubble flower is a descendent of the jelly flower, except they grow taller, they don’t have a singular flower, and the jelly pedals from before are now just large spheres of jelly. They have much of the same diet and structure, and that feature is why they are believed to be descendants. These plants also grow deeper in the sea than their eastern counterparts.
===== Arialsphere =====
The aerial biosphere has a small genepool and is the least biodiverse out of the three. It has only two common species, whose descendants make up most of the biosphere’s species. They normally live in the mountains and rarely leave their mountain range. They seemed to have spread via accidental and sometimes (rarely) purposeful means. These two common ancestor species are the Coidoidian eagle and the Coidoidian small bird. The Coidoidian eagle is, as the name implies, an eagle-like bird that has a form similar to an eagle but is not quite there. This bird has a red coloration for its male members and a brownish coloration for its female members. This species lives a loner lifestyle, and it tends to raise its young with a single parent, that parent being the female. These birds tend to live high in the mountains and are omnivorous, eating small animals (sometimes other birds) and some grasses. These birds are 25% smaller than a white eagle* on Earth, and they have a lifespan that can reach up to 60 years. This species’ members find mates with the male calling, and with the loud sound going through the valleys, naturally this means a larger and stronger vocal box. They eventually find each other and dance, and if the female is dissatisfied with the male’s performance, she leaves. 
These birds are loners, unlike the Coidoidian small bird, a hive-minded bird that follows its flock like a fish follows its school. These yellow or green birds are around the size of a canary, and they can fly in flocks that can have thousands of members. They live in the lowlands of the mountains and can sometimes go out to the plains, though not far. These birds survive off a vegetarian diet, as animals would be depleted rapidly if they were carnivorous. Their vegetarian diet is mostly of leaves and ground flowers, and they mate and live in large collective nests in whatever massive tree they find. These nests can fit (on average) 17 men of average stature, and they are built out of large branches, which are lifted by subsections of flocks in a collective effort to build their nest. These flocks don’t really die out naturally; only through catastrophic events do they fully die out. These flocks can be hundreds of years old and recruit new members through their offspring. If, for some reason, the rest of the flock moves too fast and there are at least 2 birds left, they will form their own flock, having offspring and growing their group. Sometimes when their old flock comes by, they join it, but if it has been too long, they will have identified themselves with their own collective and will reject their old flock. These birds chirp a lot, and thus the forests are very loud when they are around, and whenever they harmonize, that means they have come to an agreement. There is no head of the group; rather, the flock moves on whatever the majority wants, with the minority following out of necessity as they do not want to starve to death.
== Gallery==
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File:Coidoid-005.png|Could make an oil painting out of this.
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==Entras==
===Moon system===
This planet has one singular moon, sort of how we have it, and this planet has a moderately sized moon, around 1.7x the mass of the moon. This moon, however, despite its apparently small size, is large enough that it can act as a binary partner to its parent planet. This moon is believed to have come from a theira-like collision similar to what we had on Earth, just more destructive, and this is evidenced by the composition of the moon being similar to the insides of its parent planet a few billion years ago if accounting for reverse simulations. This moon is covered by an icy wasteland, with impact craters looking like little flashes, minus the flash of light part. This icy hellscape, which would impress the likes of Phobos and Deimos, -
has lots of exposed copper and gold and is rich enough in Helium-3 (towards the craters and poles) that any up-and-coming civilization could use this moon to support a small colonial fleet and prospect area. I lied a little bit earlier; those ‘flash craters’ aren’t the only craters. Because of this moon’s lack of an atmosphere, thousands of craters, even more so than the moon (300 more than the moon, ±6 to be exact), litter the surface, most of which are not that deep and, because of their shallowness, are not really noticeable, the exception to that being the southern craters. These characters all come from the same time period, and thus a great bombardment of sorts must have happened. Some of these asteroids would launch out large amounts of copper and gold, which are seen in little marks of the material in subterranean environments across the parent world.
 	Coidoid Secondary
Image 	
File:Coidoid-015.png
Class 	Cool airless subterra
Mass 	1.7054 M◑
Diameter	2227.89 Miles
Orbital 	5.403d
===Planetary system===
The planetary system that is home to this world is an 11-planet system that orbits an orange dwarf (K7.7 V). The first five planets are grouped together, forming an ‘inner’ system, and the last five planets are evenly spread out from each other, forming an ‘outer’ system. There is no asteroid belt in this system, and the planetary plane only includes 10 of the planets, with the last planet being in a seemingly “right” orientation. There are 11 planets, but 2 of those are binary planets, so that would lower the planetary count to 9, and there are 2 planets with life, those being the 4th and 6th worlds. Or, more accurately, the 4th (A) and (6th) 3rd worlds. This system is like any other in its local region.
File:Coidoid-016.png
Category:Procedural objects
Category:Objects
Category:Terrae
Category:Life
Category:Planets