Chaotya

( I have a lot of work tomorrow :( )
== Chaotya's Abfrontals ==
=== Condensed summary ===
This is a taiga and desert world inhabited by insects which are also pretty large for some reason. 
=== Trivia ===
* This world is actually quite common when I am searching for things, the reason for that is unknown.
=== Featurals ===
This world is covered mostly by land, and that land is mostly covered by shades of evergreen green. That green is sometimes punctured by deserts and lowlands, brown, and yellowish-white. Those biomes are centered around the equator, which is also where most of the water generally sticks for some reason. The planet’s largest oceans and most of the seas and lakes stick to the equator, though a few lakes diverge from that row along the equator, and they exist along a line going to the north pole. 
Beyond the surface, we find the atmosphere, which is a uniform blue color. Going a bit further up, we can see the planet as a whole, or can we? We forgot one thing, the cloud cover, which is normally large and common here. This blue atmosphere is dirtied with spots and holes of white or gray, which are random and follow a similar distribution to that of an abstract painting. While they may not follow a consistent form on their own, they all collectively form along a direction, an arrow that points to the right (relative to the parent star). Last thing to note here is the islands, which are random but small, and are mostly volcanic in nature, how small those volcanoes will be.
== Chaotya's Properties ==
=== Physicals ===
The equatorial diameter of the planet is 7587.47 miles, with the mean diameter being 7570.39 miles, and the polar diameter is 7536.35 miles. The oblateness is 0.0067371, with the mass of the planet being 1.119 M⨁, and the density is 7.0576 grams per cubic centimeter. The insolation is 0.91868, with the effective temperature being 222.81 kelvin, and the Earth similarity index is 0.921. The rotational period is 14 hours, 52 minutes, and 36.17 seconds, with the solar day being 14 hours, 54 minutes, and 54.57 seconds, and the axial tilt is 0*51’9.93”. The gravity on the equator is 11.891 meters per second, with the gravity on average being 12.003 meter per second, and the gravity on the poles is 12.111 meters per second. The circular / escape velocity is 19149.13 miles per hour, and 27080.96 miles per hour, with the age of the planet being 9.841 billion years, and the tidal heating is 2.2032*10^8 watts. The silicate mantle makes up 52% of the planet’s insides, with the metallic core making up the rest at 48%. 
=== Atmospherics ===
The height of the atmosphere is 40.71 miles, with the tropopause height being 11.99 miles, and the height of the homogeneous atmosphere is 23760.27 feet. The atmospheric pressure is 16.1, with the air density being 18.849 kilograms per cubic meter, and the air temperature is 299.22 kelvin (78.926 *F, 26.07 *C). The speed of sound here is 759.83 miles per hour, with the exosphere temperature being 1383.9 kelvin, and the greenhouse effect is 76.383 kelvin. The average molar mass is 29.157, with the relative mass being 8.6357*10^-6, and the real atmospheric mass is 12.079 Earth atmospheres. Nitrogen makes up 50.6%, with Oxygen at 42.8%, Water vapor at 3.95%, and Carbon dioxide is at 2.57%.
=== Hydrospherics ===
The maximum depth of the oceans here is 11799.19 feet, with the average molar mass being 18.016, and the density is 1 gram per cubic centimeter. The temperature is 299.22 kelvin, with the atmospheric pressure being 16.1 atm, and the bottom pressure is 442 atm, additionally, the bottom composition is rock. Water makes up an observed 100% of the planet’s oceans, and Sulfur dioxide is at 20.8 parts per million. 
=== Orbitals ===
The parent of this world is a singular star, with the orbital type being elliptical, and the orbital period is 240.426 days. The semimajor axis is 0.7048 AU, with the pericenter being 0.6576 AU, and the apocenter is 0.7521 AU. The eccentricity is 0.067, with the inclination being -0*04’23.97”, and the ascending node is 116*54’20.48”. The argument of pericenter is 102*21’14.70”, with the mean anomaly being 159*12’10.98”, and the longitude of pericenter is 219*15’35.18”. The mean longitude is 378*27’46.16”, with the orbital velocity being 71342.26 miles per hour, and the hill sphere radius is 681557 miles, additionally, the influence sphere radius is 461271 miles, plus the roche limit for satellites is 6120 miles. 
== Chaotya's Properties ==
=== Internals ===
==== Core ====
The planet has a large core, which makes up almost half of the planet’s insides. This core is mostly made up of nickel, silver, and iron, with some trace amounts of silicon detected as well, and these materials are distributed unevenly throughout the core, with silver and silicon staying on the outside of the outer core and nickel and iron tending to stay in the inner core. The core also has an uneven heat gradient, with the outer core having a cooler temperature than the inner core, and it is enough that traveling between the two would be noticeable. 
The reason why the planet has so few volcanoes, or at least large ones, is because the outer core is cool enough, and the ability of the core to produce and shoot out magma plumes is decreased by a large amount, large enough that the expected plumes either don’t form or don’t have enough energy to continue through the mantle. Despite the two layers having some, at least noticeable differences, they do have some differences. For example, they have a consistent density gradient, and both layers have a consistent material concentration despite the composition of both being slightly different. The core has a definite boundary with the mantle above it, having a significantly different rotational period than the mantle, and the composition of the two is surprisingly different.
==== Mantle ====
The mantle here is quite average; it is like the Earth in density, temperature gradient, sub-layers, strength, and whatnot, and it is able to stop most magma plumes from coming through it. This mantle is mostly made up of aluminum, nickel, silicon, and iron, and some trace amounts of cobalt and other such materials are found as well. This mantle makes up a little over half of the planet’s insides, and it has a definite boundary with the core below it and a definite boundary with the crust above it. Besides those two things, there is not that much to describe about the mantle; most of the things in the mantle are consistent with the Earth’s, and the mantle is not that interesting here.
==== Crust ====
This planet does not have that unique of a crust. This crust is mostly made up of silicon, nickel, aluminum, iron, oxygen, etc, and has a moderate strength only 0.29% stronger then the Earth’s. This crust is thin, slightly thinner then the Earth by around 9.88%, and it because of the mantle having a stable convection current which goes at a moderate pace, the tectonic plates move at a pace which is also moderate, only slightly slower then the Earth by 1.28%. There is nothing else really to say about this core considering how typical it is, only deviating slightly off the average and being fully in line with what is expected of it.
=== Geography ===
I managed to finish the climate section before the geography section some how.
==== Northern Hemisphere ====
The northern hemisphere is comprised mostly of a massive flat plain with a few hills and maybe a mountain or two here and there. This part of the globe is pretty dry, with the rivers and lakes here either being very thin or non-existent, and the reason for this is unknown. The geography up north is unified in its look, sharing little to no jaggedness only on the coasts, of which there are so few. While the “big parts’ of the southern seas lie here, they don’t compensate for the lack of water here. 
The northern hemisphere does not have that many islands; the ones it does have are little volcanic scraps that follow no real form or pattern, with the lakes here normally being small in size and being more like ponds, if anything. Most of the bodies of water in the northern hemisphere derive from the south or equator, with only one body of water up north that is not derive from anything south. A glacial melt area that hails from the sloping hills of the far north. Speaking of which, the topography here isn’t that interesting or varied, only featuring a wide and long line of various hills and mountains, all of which are of similar height, and all of them follow the SMA general line of tectonic convergence. The lands up north are unified and are not connected by land bridges. The only land bridges here are the ones that connect to the Southern Landmasses.
==== Southern Hemisphere ====
The southern hemisphere has way more water than the northern hemisphere, and because of that, the bodies of water in the southern hemisphere are way larger, and there are more of them. The lakes in the northern hemisphere dramatically rise in size by 12.5% on average, and they rise in quantity by 89%. The landmasses of the south are connected to each other by thin land bridges that are often marshlands that are below sea level. The south seemed to have more glaciers in the past, as there are more glacial retreat and melt areas, in which there are two seas, both of which are around the same size as the northern hemisphere’s biggest sea. Speaking of seas, all of the bodies of water except for one sea and the lakes in the north derive from the southern hemisphere, with the majority of those bodies of water being below the equator. 
The mountains in the south are also taller, less organized, and more varied, and a few of them still have the glaciers of old or are capped with ice. The last thing to mention about the south is the islands. In the south, there are more than double the number of them, and there is also more variety. In addition to the little volcanic scraps, there are tidal islands, landmass islands, marshlands, etc., all of which have some sort of organizational form and structure, and they all stick to the coast, which there is also more of in the southern hemisphere. The landmasses in the southern hemisphere are jagged and less unified; coastlines don’t follow general curves and instead follow erosion and marshland patterns. There are also more continents in the southern hemisphere.
=== Climate ===
The climate on this planet is a temperate one. The average wind speeds in this climate are around the same amount as the ones found on Earth, and this climate produces consistent weather patterns at a rate only 0.1106% less than the Earth. This climate is a bit chilly at times, the winds do that here for some reason despite hoe close they are to the Earth’s, though, a 4 mph difference could do this for Humans. This climate is considered non-global, which means that the climate experiences variation between ends of the planet. The poles and the equator don’t vary as much as the Earth, but the poles are noticeably cooler, by around 10 - 20 degrees at points on average, and the patterns of weather are different. 
While globally the climate has a lowend with cleary weather and a highend for moderate cyclones, category 3s, the poles tell a different story, only experiencing clear and partly cloudy weather, with the occasional shower and calm blizzard. This is opposed to the equator, a tropical hole here which experiences more showers per year than the poles do in 5 years. The equator also has a slightly higher amount of cloud-cover, and the winspeeds at the equator are a little lower by 19% on average. While going from the poles to the equator will be noticeable, the environment itself isn't. This climate is livable by most standards, provided you have the right equipment, and the conditions here reflect a period of time right before the holocene era in the Earth’s climate, where the glaciers just melted, and the climate became more suitable for agriculture and development away form the hunter-gatherer lifestyle. 
== ~000~ ==
Category:Procedural objects
Category:Objects
Category:Terrae
Category:Life