Lwoma

(This moon is way to advanced to be only something million years old. This version, the ones before it, and 0.972, have a problem with clouds so ignore the occasional cut hurricane.)
==Lwoma==
===Technicals===
====Physicals====
The moon has a diameter of 6188.270 kilometers (0.48512 D⨁), with a mass of 0.15429 M⨁, and a density of 7.4287 grams per cubic centimeter. The oblateness is 0, with the effective temperature being 296.66 K, and the Earth similarity index is 0.834. The rotational period is 8.792 days, with the axial tilt being 0*00’00.01”, and the ascending node is 315*39’52.05”. The age of the moon is a young 671.510 million years, though some disagree, stating that it is actually 6.71 billion years old. The gravity on the equator is 6.4314 meters per second  with the gravity on the poles being 6.4316 meters per second, and the first cosmic value is 4.46 kilometers per second, additionally the second cosmic value is 6.31 kilometers per second.    
====Atmospherics====
The atmospheric pressure here is 0.13847, with the air density being 0.24378 grams per cubic centimeter, and the effective height is 26.888 kilometers. The average molar mass is 44, with the relative mass being 2.6846*10^-7, and the actual mass of the atmosphere is 4.1421*10^-8 M⨁. The average temperature is 296.66 kelvin, 23.51 *C, or 74.318 *F, with the greenhouse effect being 0 kelvin. 
====Orbitals====
The orbital type of the moon is elliptical, with the parent being a gaseous planet, and the orbital period of the moon is 8.792 days. The semimajor axis is 1072090.736 kilometers, with the pericentric distance being 1018888.150 kilometers, and the eccentricity is 0.050. The inclination is -0*32’32.81”, with the ascending node being 315*39’52.09”, and the argument of pericenter is 257*12’8.91”. The mean anomaly is 330*24’54.05”, with the longitude of pericenter being 572*52’1.01”, and the mean longitude is 903*16’55.06”.
===Store===
====Internals====
The moon has an active internal structure; though it does not generate that many volcanoes, it does move the tectonic plates at a higher speed than the Earth’s plates, and the magnetic field is 0.3001% stronger than the Earth’s. The core makes up 40.012% of the moon, with the mantle at 50.188% and the actual crust at 9.8%. This molten core is made up of 30% iron, 67.000011% nickel, and 2.999989% silicon. The mantle is a little more hot than the Earth’s mantle, allowing for tectonic plates to move around more, and it is also softer consequently, so volcanoes would be easier to form. It seems that in the current period, volcanic activity is at a low point, so that’s why they aren’t seen, despite the possibility being high. There’s nothing to mention about the crust besides the point that sometimes the mantle beneath it falls a little, causing that whole part of the crust to form a sinkhole, which gives us a look at what the mantle looks like. These sinkholes create noticeable dark spots on the sea.
====Georgaphy====
Most of the moon is covered by a large global ocean. The continents are arranged and have a polynesian chain of islands. The continents are more like archipelagoes themselves, made up of splattered, low-lying islands that create large bays and small canyonic lakes. In the best words, they are distributed in a way consistent with an abstractionist throwing paint at a canvas. Many of the islands that are not part of the archipelago continents are mountainous units, rising above their coastlines with white tops, surrounded by an ocean or orange, with no biome between mountain and sea. 
This may be due to several factors, mainly one of them being that this moon just came out of an ice age, and thus the rising of the sea levels may isolate mountain ranges like these. You may notice several dark spots in the oceans, and those dark spots are not patches or mega-colonies of plankton or some other organism; these are sinkholes. These large sinkholes are from the crust collapsing, and they might have played a role in sea level regulation and are most likely the reason why most of the mountain islands are still above the waters. Besides those two geological things, there is nothing really to mention here besides the moon having a 14-kilometer-tall mountain, which is shy of double the height of Mt. Everest.
====Climate====
The climate here is chaotic, humid, and windy. The humidity found here is on average around 60–70%, and the weather changes really fast on a dime. One hour it could be a sunny day, the other you are in a thick, powering shower that prevents sight beyond 6 feet around you, and then sunny again. A raincoat is necessary here, and so is some sort of grounder or heavy weight, as you could be knocked off of your feet by a random wind gust. It has been noted that many of the wind gusts here, though lasting a minute at most, get to an average strength similar to an EF1-EF2 tornado found on Earth. Pay attention to where you’re walking as well; the heavy amounts of daily showers here have made most of the ground muddy, and thus every part of the ground that is not right underneath a tree or is rocky is a mud pit, sort of like a swamp. You may also have to hide yourself under some very sturdy shelter, as the climate has lent itself to regular flash-cyclone formation. What this means is that cyclones form very rapidly and reach impressive sizes and strengths in around a few hours. Sometimes this process could happen even while the sky is clear! Luckily, these cyclones also fade away fast, around 7–8 hours after formation. Overall, despite the biosphere surviving here, you are unlikely to.
====Biosphere====
=====Terrestrial=====
Life on land is very diverse despite the limited amount of said land. That being said though, there are three primary groups of species. Snakes, territorial creatures which use the large swaths of mudscape as their hunting grounds and sometimes homes. Trees, which due to the chaotic environment have over time evolved to be very grounded and heavy to stay in place despite the regular severe weather. And bee-likes, a large and diverse group, 20 times what we have on Earth, like to take advantage of the trees’ large amounts of nectar during the blossoming season to bring back to their normally massive colonies. Sometimes they form into swarms that are visible from space even. A quick fact about the trees here, they have developed a symbiotic relationship with many of the animals, who use the insides of the trees as their homes. 
=====Marine=====
Despite the large amount of space available, there is not that much biodiversity in the oceans, especially towards the surface. The iron-tinted oceans seemingly killed off most of life, only allowing biodiversity at the bottoms of sinkholes. Life that does exist in the oceans is primarily plankton, which build large rafts that take advantage of the parent star’s light. There are some species of fish that live at the bottom of the sinkholes and sometimes on the seafloor as small herbivores that tend to live alone, kicking their offspring out of the “house” once they have reached adulthood. These herbivores nibble at the tall stacks of kelp and the long and tall carpets of green that extend all the way to the top of the ocean. They tend to be thick, sometimes bioluminescent (just like some whales here), and a shade of dark green. Overall, the ocean is mostly desolate.
=====Aerial=====
The aerial life here is a bit odd. Most birds are grounded, i.e., they don’t typically fly as much, preferring instead to skip on the ground. They make their nests on whatever beaches or grasslands there are, and these birds are small, around the size of an index finger. There is a species here—not really a bird, but rather some sort of blimp animal. It uses a massive gaseous sack to keep itself afloat; essentially, it’s an air whale. It seems to subsist on a diet of whatever particles are up there.
===Gallery===
File:Lwoma-001.png
File:Lwoma-002.png
File:Lwoma-003.png
File:Lwoma-004.png
File:Lwoma-005.png
File:Lwoma-006.png|A unique and beautiful aurora.
File:Lwoma-007.png
File:Lwoma-008.png
File:Lwoma-009.png
File:Lwoma-010.png
File:Lwoma-011.png
File:Lwoma-012.png
File:Lwoma-013.png
===Moon system===
The moon system which this moon is part of is large in its number. There are a total of 7 moderately sized moons. All except this one are temperate wastelands, good in their temperature, but barren and inhospitable in all other aspects. The moon system is mineral poor besides this moon and the last 2  lacking thre resources necessary to power a modern or advanced civilization. All of these moons are selenas, peppered with craters that seem to be at the same general age, indicating that there might have been a great bombardment.
~ 	Plyun 	Berecso 	Ventei 	Lwoma 	Chinol 	Asymmph 	Asipea
Image 	
File:Lwoma-014.png	
File:Lwoma-015.png	
File:Lwoma-016.png	
File:Lwoma-017.png	
File:Lwoma-018.png	
File:Lwoma-019.png	
File:Lwoma-020.png
Class 	Temperate selena	Temperate selena	Temperate selena	Temperate terra	Temperate selena	Temperate selena	Temperate selena
Mass 	0.0099523 M⨁ 	0.011523 M⨁ 	0.013334 M⨁ 	0.15429 M⨁ 	0.017864 M⨁ 	0.020708 M⨁ 	0.02405 M⨁
Diameter	2552.658 km 	3008.188 km 	2809.099 km 	6188.270 km 	3471.530 km 	3243.111 km 	4352.059 km
Period 	1.517d 	2.726d 	4.896d 	8.792d 	15.798d 	28.379d 	50.978d
===Star system===
This system is a binary, composed of a white main sequence star, and an orange dwarf. The system has a total of 13 planets, most of which are warmer on average than the planets in other star systems nearby. A core mention of this system is the life density, there are 4 worlds with life here, 2 planets  2 moons. 3 of the life bearing worlds are around the primary, and 1 is around the secondary. The primary has no asteroid belt or oort cloud, and the secondary has a super dense asteroid belt in the orbit of the last planet. There are two frozen worlds which orbit both stars.
File:Lwoma-021.png|Primary
File:Lwoma-022.png|Secondary
File:Lwoma-023.png|A ~ B
Category:Procedural objects
Category:Objects
Category:Terrae
Category:Life
Category:Moons