Megahmoon

(*IDK if I should continue with the Safari method of "lore" for the locations like this, or not.* *This passage also takes some liberties with its object, a moon, and its properties.*)

## Megahmoon

* Dominant
* Disappointed

## Discovery Information

### Discoverer

CALASE (1990)Named by Henry Sterling (1991)

## Additional Information

### Life

Organic multicellular (marine, terrestrial)

## Megahmoon's information

### Technical information

The equatorial diameter of this world is 14814.46 miles, with the mean diameter being 14804.55 miles, and the polar diameter is 14784.73 miles, or converted to the unit “⨁”, equals 1.8698 D⨁, witch is almost double the diameter of the Earth, this is a mega moon indeed. The oblateness of the moon is 0.0020072, with the mass being 11.248 M⨁, or 6.7177\*10^25 kilograms, with the physical density being 9.4861 grams per cubic centimeter, and the insolation of the moon is 0.47583. The effective temperature of the moon is 188.92 kelvin, -119.614 degrees Fahrenheit, or -84.23 degrees Celsius, a cold temperature. The earth similarity of the moon is 0.781, with the albedo bond being 0.55182. The rotational period is 23 hours, 23 minutes, and 2.39 seconds, with the solar day being 23 hours, 21 minutes, and 52.72 seconds, with the axial tilt of the moon being 14\*23’6.73”. The gravity on the moon’s equator is 31.511 meters per second, with the gravity on average being 31.549 meters per second, and the gravity on the poles is 31.633 meters per second, The circular velocity of the moon is 43380.72 miles per hour, with the escape velocity being 61349.61 miles per hour, and the age of the moon is 3.826 billion years, in addition to that the tidal heating is 5.1544\*10^12 Watts / 1.0219 P⨁. The height of the atmosphere is 44129 feet, with the tropopause height bein g 18702.51 feet, and the height of the homogeneous atmosphere being 6005.89 feet  The atmospheric pressure of the moon is 83.1 atm, high!, with the air density being 145.99 kilograms per cubic meter, with the air temperature being 3.36 degrees Celsius, or 38.048 degrees Fahrenheit, and the speed of sound here is 620.32 miles per hour.

The exosphere temperature is 1402.9 kelvin, with the greenhouse effect being 87.555 kelvin, and the average molar mass is 40.485. The relative mass is 6.4117\*10^-6, with the real mass being 4.3072\*10^20 kilograms, or 90 times the Earth’s atmosphere. The maximum depth of the oceans on this moon is 10276.23 feet, with the average molar mass being 23.370, and the density of the water is more than average, 1.0209 kilograms per cubic centimeter, in addition to that the bottom pressure being 1.08\*10^3 atm, and the bottom composition is rock. The ocean here is made up of 79.4% water, yes 79.4%, with Carbon dioxide making 20.6% of the ocean, and sulfur dioxide makes 150 parts per million. The moon’s orbital type is elliptical, with the orbital period of the moon being 77.397 days, and the semimajor axis being 0.0705 AU. The pericenter and apocenter is 5996011.5420 miles, and 0.0764 AU, with the eccentricity being 0.085, and the inclination is 152\*37’30.71”. The ascending node of the moon is 107\*56’22.98”, with the argument of pericenter being 70\*18’7.36”. The mean anomaly of this world is 2\*20’26.76”, with the longitude of pericenter being 178\*14’30.34”, and the mean longitude 180\*34’57.11”. The orbital velocity of the moon is 22154.18 miles per hour, with the hill sphere radius being 678960 miles, and the influence sphere radius is 744458 miles, in addition to that the Roche limit for satellites is 13209 miles.

### Infolore

This is an intriguing world, one that is exceptionally rare, and it may have had a submoon in the recent to distant past that was torn to shreds. As we descend onto the moon, we can pass through the stunning rings. These rings are reminiscent of the remnants of an ancient moon, about a quarter to an eighth of the size of our moon. This moon is believed to be a captured planet in the system, it is too massive and has too odd of an orbit to have been formed along with the planet, rather it was captured millions or billions of years ago, most likely along with the moon of this former-planet bering torn creating the ring system, it orbits in a retrograde fashion, which is odd for natural moons, but normal for captured planets. When you venture through the rings, which are not tight on the moon which is odd for most ringed moons, you'll notice their striking cyanic-turquoise color, which is due to their composition primarily consisting of dust, silicate, nickel, and Kyanite. This unique hue is uncommon for ring systems but not unexpected given the uniqueness of the moon itself. Moving closer to the moon, you'll find a gap in the ring system, followed by a thin ring composed of dust, silicate, and nickel, likely materials that have accumulated in this region.

As we descend further to the moon's surface, it could be described as a "moonatoid" due to its significant mass. The spacecraft experiences a gravitational force three times greater than that of Earth, resulting in increased acceleration. Upon landing, you'll observe that the atmosphere is rather thin and lackluster, with occasional wispy clouds interrupting the dull yellow backdrop. This moonatoid's muted color is a consequence of its vast size, which causes the atmosphere to spread thinly across it. Moreover, the atmosphere is denser, making the moonatoid appear smaller. As you touch down on the moonatoid, be prepared for a slower descent since the atmosphere is much denser than what we're accustomed to on Earth, approximately 1/10th the density of water. Once on the surface, you'll find yourself surrounded by a semi-dense forest and shrubland that stretches for miles. As you walk for miles and encounter a mountain, you'll notice that it stands high above the ground. In the distance, you can spot other mountains of similar size that, despite appearing close, are quite distant.

The shrubland, when viewed from this elevation, is broken up by several small plains and arid regions. In the sky, the moonatoid's ring system can be seen. If you gaze around, you'll catch sight of a large, desert-like environment in the far distance, although the atmosphere partially obscures it with a distant fog. On the horizon, you can spot the parent planet of this moonatoid, a massive gas giant surrounded by many moons. Descending from the mountain, either on foot or with the aid of a vehicle to expedite travel, it takes several hours to reach the nearest large body of water. Along the way, you'll come across a desert landscape with dry rocks that reveal exposed minerals. Dry bushes populate the land, and in the distance, you can see large mountains. The path is strewn with various types of sand and sand arrangements. After exiting the desert and returning to the shrublands, you'll encounter a new creature: a bird with a massive beak and wings the size of a small school bus, necessary for navigating the moonatoid's atmosphere and gravity. These birds drop diverse-colored fruits, with light blue being the most common. These fruits are roughly the size of a human hand and serve as a source of sustenance. Continuing along the trail, you'll eventually reach a body of water, a small bay with a limited fish population. Nearby, there's a substantial cliff, and you can see the parent gas giant rising further on the moonatoid's horizon. As night falls, the sunset is relatively unremarkable, with the most intriguing aspect being the ring system next to it.

Gazing up at the night sky, you'll see several stars within this galaxy, although they appear somewhat dim majorly. Surprisingly, the brightest "stars" in the sky are not stars at all but rather asteroids, which are actually dwarf moons orbiting the parent gas giant. These asteroids can move across the night sky, appearing bright. This phenomenon has influenced the local culture to distinguish between "moving stars" and "unmoving stars”. among the asteroids, you'll notice a nearby nebula as a dark spot in the sky with hints of pink. This stellar nursery is located approximately 11 light years away from the moonatoid. If you look directly overhead, you'll see the parent planet, high in the sky with its distant splendor. Unfortunately, the position of the moon at this time prevents us from observing the other two galaxies near the one to which this moonatoid belongs. However, the moonatoid compensates for this lack by offering its own version of fireflies: large buzzing insects that are 1 to 2 feet in size. They emit glowing sacs producing a soothing pink glow, perfect for a restful night's sleep. But if you want to, you can take a boat ride across the oceans of this world, whose geography is very flowy and has a lot of circular seas and smooth/flowing coastlines, but to avoid confusion, take a rest. And speaking of sleep, this concludes our safari on this captivating world. This description is compiled from various forms of  data to provide a model of what an actual safari on this world might be like.

### Hypothesized past moons

The ring system around this moon has been formed from 1 or possibly 2 moons. The ring system is split into 2 parts, and the 2nd part is from accumulated dust, but there is a theory out there that thinks that the former-planet used to have, a small major moon, and a smaller moon that is more like an asteroid like that fell apart and formed the rest of the ring system. These two potential moons are Megahfirsus and Megahsecondus, they would have been both selenas that would have been temperate to cold, they would not have been that interesting if we were able to see them. They would have orbited close to the former-planet and when being captured they might have existed for a brief period of time where they were submoons, but eventually they fell into the roche limit and got turned into rings. Examples of other moons will be used for what they would have looked like, and their hypothesized details listed. The second moon is less accepted in the scientific community, but it is possible and more fun to imagine.

\*Details may not be accurate.

 Mass
 Diameter

### Gallery

Looking through the clouds you can see the nebula.Misty hills.Some hills.Inside the cyanic rings.An arid, desertic plain with hills, valleys, and dust devils. In the savanna we passed by this region.Some hills and mountains. These were the ones that were seen in the distance in the beginning when looking at the hroizon.If the moon is in the correct position and time, you could see the other two galaxies, CRTW and CRTW S1.
### Moon system

The moon system this former planet is part of consists of 5 core moons that were formed along with the parent planet, and a cloud of debris known as dwarf moons or asteroids. The former-moon orbits within the cloud of asteroids and due to the massive size of the moon/former-planet, the asteroid’s orbits are all out of whack, and sometimes these asteroids collide with the moon, creating craters that are visible from topographical maps and VLRS images of said moon. Because of the former planet’s position in the moon system, it gets regular meteor showers, unlike its non-familial moons closer to the gas giant.

### Star system

This world is part of a 9 planet system, this system is a GTG system, meaning it is a pattern of Gas Giant, Terrestrial, Gas Giant, and this system is pretty barren.

The hot jupiter.Barren, but has an atmosphere.The parent planet of Megahmoon.The world with two sets of rings and some water, not that much though.The beautiful, neon pruple world with tight rings.