Tylenay

(Premature releasing makes work easier, and no, I will not explain how slow the erosion is here.)
==Tylenay's properties==
===Physicals===
The planet has an equatorial diameter of 4853.03 miles, with the mean diameter being 4853.03 miles, and the polar diameter is 4853.03 miles. The oblateness is 0, with the mass being 0.23923 M⨁, and the density is 5.7276 grams per cubic centimeter. The insolation is 1.7909, with the effective temperature being 259.63 kelvin, and the Earth similarity index is 0.904, high. The rotational period is 33.394 days, with the solar day being 100.181 days, and the axial tilt is 0*00’00.00”. The gravity on the equator is 6.2583 meters per second, with the gravity on average being 6.2443 meters per second, and the gravity on the poles is 6.2443 meters per second. The circular / escape velocities are 11046.20 miles per hour and 15621.69 miles per hour, with the age being 8.028 billion years, and the tidal heating is 8.7772*10^10 watts. 
===Atmospherics===
The height of the atmosphere is 100.93 miles, with the tropopause height being 16.65 miles, and the height of the homogeneous atmosphere is 45260.16 feet. The atmospheric pressure is 2.86 atm, with the air density being 3.3599 kilograms per cubic meter, and the air temperature is 285.81 kelvin, 12.66 *C, 54.788 *F. The speed of sound is 758.11 miles per hour, with the exosphere temperature being 1296.1 kelvin, and the greenhouse effect is 26.166 kelvin. The average molar mass is 28.229, with the relative mass being 5.6111*10^6, and the real mass is 1.6779 Earth atmospheres. Nitrogen makes 57.8% of the atmosphere, with Oxygen at 32.3%, Water vapor at 9.22%, Carbon dioxide at 0.541%, and Sulfur dioxide at 0.152%. 
===Hydrospherics===
The maximum depth of the oceans is 6699.45 feet, with the average molar mass being 18.015, and the density is 1 gram per cubic meter. The temperature of the oceans is 285.81 kelvin, with the atmospheric pressure being 2.86 atm, and the bottom pressure is 129 atm, additionally the bottom composition is rock. Water, fresh and salt, makes up an absolute 100% of the oceans here. 
===Orbitals ===
The planet’s parent is a singular star, with the orbital period being 50.091 days, and the semimajor axis is 0.2161 AU. The pericenter is 0.2048 AU, with the apocenter being 0.2274 AU, and the eccentricity is 0.052. The inclination is -0*37’59.45”, with the ascending node being 160*53’14.66”, and the argument of pericenter is 14*51’24.17”. The mean anomaly is 59*03’37.73”, with the longitude of pericenter being 175*44’38.84”, and the mean longitude is 234*48’16.57”. The orbital velocity is 104992.12 miles per hour, with the orbital resonances being 7:2 (3), and the hill sphere radius is 145505 miles. The influence sphere radius is 89879 miles, with the roche limit for satellites being 3660 miles. 
==Store ==
===Internals===
The plant has a moderate internal structure, as in, the structure is not too dissimilar to any other terrestrial planet that you would find. The core is made up of primarily silicon and nickel; said core has a relative size of 39.8%, which is not too far from the Earth’s core relative size. The internal structure here features a well-defined core of, as previously mentioned, silicon and nickel. Though not as mentioned, there seems to be a very small amount of iron that has formed a sort of shell of material on the outside, still core-like in function and appearance, but still something to note.
Besides the well-defined core, there is a moderate mantle, making up an appropriate amount of volume; it allows for some pushes of magma from inside to reach the crust. That crust is thin, like the Earth’s, has a composition not too dissimilar to the insides, and is strong enough that it does not break up whenever a magma plume forces through. That crust also allows for a tectonic drift roughly similar to the Earth’s rate, around 0.27% slower. The magnetic field produced by this internal structure is much like the Earth’s, though it is a bit weaker at 0.05% weaker.
===Geography===
The planet is mostly covered by land; a sprawling pangea-like continent covers most of the surface, and this continent is mostly elevated; coasts go up to steep flora that in some places are just slightly below the height of Mt. Everest on average. This mountainous geography has made all the islands here mountain chains of their own; you wouldn’t really find a smooth coast here; only sharp, jagged, and hard-to-climb shorelines, which fit more with the tops of mountains found here on Earth. The reason for this is because the islands used to be mountains in their own right; back when their tops were pointy instead of dull, they existed in a massive plain, which is now the planet’s only ocean. This plain would’ve been similar to the great plains found in North America or the Steppe found in Central Eurasia. 
This plain of sorts was not that interesting on its own, mostly uniform in elevation, but this wouldn’t last long as the ice age was starting to end. This, of course, means that the massive mountain glaciers (that today still exist, just reduced) had to melt, which brought with it large amounts of water. This can still be seen today, with most rivers coming directly from the glaciers. This ocean began to rise before it began overtaking the mountains of old, turning them into islands. This is backed by the visuals of the geography, with it being sharp and random, exhibiting a shape that’s only possible through glacial retreat and islandization of mountains. 
The only place here, at least for now, that is not too elevated is the southern steppe, a region of interconnected lakes and rivers from melting glaciers, and it will most likely be flooded in the next few million years if the current trend persists. In short, the geography here consists of mountains that have been brought down to sea level. If this description gives you the impression that the majority of this planet is Mt. Everest and palls, it’s not, as erosion has made most peaks into dull points, spare a few locations. Most of that erosion came from glacial retreat and melt, so we unfortunately have missed out in this planet’s glory days, ( geographically speaking).
===Climate===
Because of the higher elevation and persistent ice age, the planet has a cold and arid climate. This climate is split into three sub-climates: glacier, tundra, and grasslands. The tundra is the most common climate here, covering 30%–40% of the land surface area, with the average humidity of this biome being a dazzling low of 0.4%, and the weather here all year 'round, with the exception of certain days, is clear or partly cloudy. Breezes are a common thing here, with them sometimes reaching into the high 40s in their wind speed. This biome will most likely give you frostbite, but the next sub-climate or biome will most certainly be the glaciers. These glaciers are flat, deserted, and serene yet uninhabitable landscapes that have an average humidity of 0.09%, so low that it kind of hurts to breathe here. 
The climate here does not allow for storm formation besides blizzards, and even then they are weak. The tundra, however, allows for more rapid and strong formation of them. This glacial climate mostly exists in the northern hemisphere; said hemisphere is an arctic wasteland, but the southern hemisphere is a grassland utopia. This hemisphere is home to the final sub-climate or biome, the grasslands, a large area of steppe, and forest, which is at least semi-habitable. The northern hemisphere does have a more arid and flat version, a tundra grassland, but that is not relevant here; what is relevant is this grassland biome, the rain bucket of this planet. These grasslands have an average humidity of 31%–46%, with breezes being quite common here, and the weather is quite diverse (for an arid world at least). Rain, while rare, is still way more common than in the two (3) other biomes. It is common enough that you could (theoretically) grow crops in this climate. This climate also sticks to the coasts, and it's where the highest amount of humidity for this planet was recorded, 86%, which is astounding for a world like this.
===Biosphere===
====Landsphere====
Most life on land lives in a grassland climate, and most of that life is vegetation. This vegetation is normally brownish-ggreenish in color, has the ability to survive without water for long periods, and has the ability to live on little to no nutrients for extended time periods if needed by storing them somewhere else. There are three main species of planet here: The typical Tylenay (Ian) steppe grass is a short and unassuming grass that can be cultivated as a grain. It is short in height but not in roots, burying itself deep in the ground, which allows it to access water from deep below if needed. However, it is never seen alone, so it has some competition, which of course has developed to different varieties of grass that have found a way to outcompete themselves. 
The next plant is the Tylenay (Ian) flower, a flower (as the name suggests) with a tall and thick stem. It grows on the coasts of lakes but not in oceans, as it does not like salt water. This flower has thin petals, few in number too, and they are a deep green color. These flowers stored their nutrients and water in the weeds that surrounded them. These weeds also made the dirt and stone stick, keeping them stable. The final plant that is common is the Tylenay (Ian) open tree. It has a thick trunk with pouches on the ground and below for water and nutrients, and its trunk ends after 2–3 feet off the ground. After that, the trunk splits into petal-like structures of wood, which reveal the hollow inside. It turns out that it has a strategy of having insect food at the bottom of this trunk, and once enough insects get there, the trunk closes and releases digestive juices. This is a carnivorous plant, technically a carnivorous tree. 
The animals here are small and few in number; they live in herds, and they scavenge most of the time. There is a species of wolf here that has a proboscis in addition to the mouth for food consumption. Why do they have a proboscis? Because they seem to use the plants’ storage units as supplemental "food." These wolves live in very small herds, 4–5 members at most, with an “alpha” at the top and an “outcast” at the bottom. These wolves have small ears because the environment was echoey, so the sound was amplified for them. Because of the elevation of the land they’re on, they have large lungs and an improved cardiovascular system that uses oxygen more efficiently. Another animal that has large lungs is the typical Tylenay (Ian) hare, a small species of rabbit that lives in grasslands (like the wolves) and tundra, with a smaller species living near the massive glaciers. This rabbit moves very fast, reaching speeds of 50 miles per hour if needed. It looks like a regular rabbit, except with larger legs and large lungs, and the nose is also larger and more specialized. 
The reason for its form seems to be because of the food source, a specific type of grass it feeds off of that grows in patches far away from other patches, which explains the travel-related adaptations. The last animal that is also common is the Tylenay (Ian) mountain snake, which is a large, anaconda-sized, brownish snake whose habitat is mostly near glaciers and exceptionally tall mountains. This snake feeds off of any small animals that get near its dens, and it has the capability to burrow through thick walls of ice and stone with ease. It makes its home in large cave systems, and it tends to rarely go outside of its home, only when necessary to find food. It has a wide head and thick skin, and it is around 50 feet on average, bulking 700 pounds in addition. 
It is unknown why it has grown to this size or has moved to the edges of the landscape, but what is known are the adaptations, which include a large heart and a set of efficient and massive lungs, the most massive in this world. In addition to that, the snake has a drill-like organ on the front of its head, with that head being supported by a dense and wide neck. The snake is not venomous, but it does have a powerful biting force, strong enough to go through metal with little effort. The snake seemed to have lost its venom not too long ago because it still has fangs with venom-like structures going through them; said fangs are around 3 feet in length too.
====Hydrosphere====
The oceans here are primarily salty, though they are less salty than Earth’s ocean water. Because of how shallow the waters are and how new they are, the biodiversity here is super low, though it may begin to catch up in the near future. The first species to be reviewed is the Tylenay (Ian) beach flower, a short, disk-shaped flower plant that relies on pollination from fish, of all things. These flowers grow both on the water and on the sand, with the petals being a dark greenish color, and the head center is small, dwarfed by their petals, and its color is a very light brown. The next species to be reviewed is the Tylenay (ian) honeyfish, which is the primary pollinating species for those beach flowers. This small and pink fish has a large beak, which allows it to eat from the flower, which consequently gets pollen on its beak. This fish is fast and lives in little hive-like colonies near the coast; they too have hexagons.
These colonies act in the same way, with a queen at the top and subservient workers serving the colony or queen. The species, instead of making honey, creates a waxy substance; it is unknown what it is made up of, but it is used in the same manner as honey. This fish and all the other fish are prey for the next species. A large jump in the food chain allows us to view the Tylenay (ian) wharf, a whale-shark-like predator that uses the same feeding methods as whales but has a full row of complex teeth on the bottom and top. This species normally engulfs whole schools of fish at once and uses the teeth only when a school is overpopulated. It has two blowholes instead of one, and it ejects ocean water for a long distance, around 100 to 150 feet. Besides these 3, there is nothing really much to the oceans; most fish are what you would find on any other planet, and because of the age of the ocean, the biodiversity is low.
====Arialsphere====
The aerial life here is pretty limited, with a biodiversity even lower than the oceans. Most of the birds have large lungs, large wings, an efficient resource management system, and a forced low metabolism. Most birds here are ‘nomads’, they don’t stay in one place for long, and they live in large flocks. They feed off of the wild grasses they find, and they make their nests on their backs. Most of these birds are small, palm small, and are like parakeets and blue jays, minus the massive eyes they have, which allows them to see better. They can fly across the whole planet in the span of a 7(24 hour term) week, and they rarely rest. 
Most of them are omniturnal, as in they are active both in the day and night. Why would they need to be active so much? Predators, which may seem a bit odd, but they are everywhere relative to the birds. Wolves in the grasses, which some are carnivorous, snakes in the mountains, and sharks in the ocean, which can sometimes jump out to prey at the coast. Where do they get the energy to fly across the planet in a week? They get it from the food they eat, which, because of their low metabolism, allows them to store a day’s-worth-of-food for a month. Evolution has seemed to force the birds to lower their metabolism for longer travels, and it has given them the ability to stay up for long hours. They do get sleep though, it is estimated around 4 - 5 hours per 3 days. There is a species of bird here which has evolved photosynthesis on their skin, converting their feathers into more plant-like structures, which sort of makes them a flying bush. 
==Gallery==
File:Tylenay-004.png
File:Tylenay-006.png
File:Tylenay-001.png|A volcano, one of many on this world, though they are not high in quantity compared to the Earth.
File:Tylenay-002.png
File:Tylenay-005.png|On the edge of the massive mono-glacier here.
File:Tylenay-007.png
File:Tylenay-003.png|These once tall mountains are now eroded hills that happen to be tall.
File:Tylenay-008.png
File:Tylenay-009.png|A lake in the Southern Steppe.
File:Tylenay-010.png|Overlooking the great ocean-lake.
File:Tylenay-011.png|A standalone volcano in the great southern plains.
==Entras==
===Moon system===
The planet has a small moon system. The system has 4 asteroid moons, 2 of them orbit close on a plain, and 2 orbit in a cloud around the planet. All of these asteroids are from the formative days, though the asteroids that are out in the cloud are a few million years older then the ones on the plain. These asteroids have a composition and mass which would allow for a small-scale space fleet. Overall, this moon system is small, primordial, and remnantal. 
 	Niki 	Hiki 	Markus 	Phosorous
Image 	
File:Tylenay-012.png	
File:Tylenay-013.png	
File:Tylenay-014.png	
File:Tylenay-015.png
Class 	Temperate asteroid	Temperate asteroid	Temperate asteroid	Temperate asteroid
Mass 	1.7378*10^-6 M◑ 	2.3586*10^-6 M◑ 	3.2005*10^-6 M◑ 	4.3457*10^-6 M◑
Diameter	22.73 Miles 	25.28 Miles 	28.66 Miles 	30.97 Miles
Orbital 	9h 24m 48.31s 	7h 35m 00.55s 	2.387d 	8.943d
===Star system===
The planet is in a 10-planet system that orbits a solitary red dwarf (M0 V). The system has an asteroid belt in the positions of the 3rd–5th planets, and the system has an oort cloud, though not a large cloud. The system has a binary planet in the 10th position, and the system is made up of smaller-sized planets. The system has four gaseous worlds and seven terrestrial worlds. The central star has a mass slightly over half that of the Sun’s, and the first 7 planets are tightly clustered with each other, with the last 3 planets being spread apart from each other.
File:Tylenay-016.png
Category:Procedural objects
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Category:Terrae
Category:Life
Category:Planets