Tidringa

==Tidringa's Abfrontals==
===General summary===
A tropical paradise in the bowels of a star cluster. A sky of lamps surrounds this world of palms, jungles, beaches, deserts, and more. This is a scenic world which has a great potential to develop a future civilization too! The waters are cool, the beaches are wide and sandy, and the vibe here is an eternal summer. Flamingos are quite common here too!
===Trivia===
*This was one of the few worlds that I specifically looked for
*Half of the planet is calm (weather wise), the other is not, the reason fro this is unknown, which is also why I created 2 images.
===Key featurals===
This world is mostly covered in large, navy blue seas, with the continents being mostly small in size. The planet does not have that many clouds, just various unstructured clouds which are also small in size and are weakly connected to eachother, with a similar distribution and appearance to the South Pacific. The lands below those clouds are mostly orange and green, with the oranges and greens being darkish in color. There are not too many islands here, and the ones that do exist here are randomly distributed mostly, though they do follow some sort of structure, that structure being archipelagoes near the coasts. 
There is one universal ocean here, and there are no real polar climates that can be seen. The climate is universal, and the biome distribution is favoring tropical climates over arid deserts, which are isolated from each other and are, and are small in size. There are also no other biomes really. The clouds mentioned before are mostly uniform, south pacific distribution, low amount, small in size, but occasionally, there are a few exceptions to this cloud distribution,  in the form of large cyclones and moderately sized cloud covers. Last feature to note here is the large ring system which surrounds this blue atmosphere covered world, this ring system has a purplish tint to it, is pretty large, and is uniform, not having that many large breaks in it as compared to other planets. Additionally, there are small but bright Shepard moons. 
==Tidringa's Properties==
===Physicals===
The planet has an equatorial diameter of 10403.85 miles, with the mean diameter being 10371.97 miles, and the polar diameter is 10308.48 miles. The oblateness is 0.009167, with the mass being 2.3108 M⨁, and the density is 5.6673 grams per cubic centimeter. The insolation is 1.2039, with the effective temperature being 242.38 kelvin, and the Earth similarity index is 0.863. The rotational period is 14 hours, 17 minutes, and 42.28 seconds, with the solar day being 14 hours, 19 minutes, and 38.20 seconds, and the axial tilt is 25*38’49.27”. The gravity on the equator is 13.029 meters per second, with the gravity on average being 13.205 meters per second, and the gravity on the poles is 13.368 meters per second. The circular / escape velocity is 23519.53 miles per hour and 33261.64 miles per hour, with the age of the planet being an old 12.648 billion years, and the tidal heating is 9.2034*10^7 watts. 
===Atmospherics===
The height of the atmosphere here is 44.02 miles, with the tropopause height being 12.81 miles, and the height of the homogeneous atmosphere is 25530.15 feet. The atmospheric pressure is 15.4 atm, with the air density being 15.264 kilograms per cubic meter, and the air temperature is 324.11 kelvin, (123.728 * F, 50.96 *C). The speed of sound here is 825.45 miles per hour, with the exosphere temperature being 1437.9 kelvin, and the greenhouse effect is 81.717 kelvin. The average molar mass is 26.792, with the relative mass being 6.8413*10^-6, and the actual mass of the atmosphere is 19.761 Earth atmospheres. 
===Hydrospherics===
The maximum depth of the oceans here is 35844.05 feet, with the average molar mass being 18.015, and the density is 1 gram per cubic centimeter. The temperature is 324.11 kelvin, with the atmospheric pressure being 15.4 atm, and the bottom pressure is 1.44*10^3 atm, additionally, the bottom composition is rock. Water makes up an observed 100% of the oceans here, with Sulfur dioxide at 1.11 parts per million.
===Orbitals===
The parent of the planet is a solitary star, with the orbital type being elliptical, and the orbital period is 265.007 days. The semimajor axis is 0.7908 AU, with the pericenter being 0.7723 AU, and the apocenter is 0.8092 AU. The eccentricity is 0.023, with the inclination being -0*07’16.78”, and the ascending node is 174*17’40.91”. The argument of pericenter is 14*40’31.74”, with the mean anomaly being 195*51’24.11”, and the longitude of pericenter is 188*58’12.66”. The mean longitude is 384*49’36.77”, with the orbital velocity being 72616.80 miles per hour, and the hill sphere radius is 969527 miles. The influence sphere radius is 651274 miles, with the Roche limit for satellites being 7794 miles. 
==Tidringa's informationals==
===Internals===
====Core====
The planet’s core is a peanut. This core makes up only 7.62% of the planet’s insides, leaving the rest to the mantle. This core is mostly made up of silicon and nickel, with some other metals being included as well. This small core has a similar composition to the Earth’s and is quite average in that aspect, but not in its speed, which makes up for the small size. This core spins almost triple that of the Earth’s core, and it has a definite boundary with the mantle surrounding it. It spins fast enough that it can sometimes rip away at the mantle directly around it. The inner and outer core are quite similar to each other, not having that many differences besides the material density of the inner core being slightly higher than the outer. Both share a similar temperature gradient, and both are of a similar size to each other. This core is like a little molten ball which spins so fast that it scrapes at the stuff around it. This core spins fast enough that it produces more magma plumes then that is expected of it, way more. They however do not go far beyond the initial mantle around the pebble core. 
==== Mantle ====
The mantle of this planet is harder then the average, and it is way larger, taking up a ratio of planet which forces out the crust and mantle to 2 small extremes. The mantle here, as previously mentioned, is harder then average, stopping the majority of magma plumes that go through it. It has a temperature slightly lower then the Earth’s mantle, and the only part which is not rock is the area of mantle right around the core, which has been eroded away to a weaker and hotter state. One thing to note about this mantle is how slow it is. The colder temperatures do not allow for easy movement of divergent parts of the mantle or the cycles that go through the mantle, which means that the crust above it moves less. Another thing to note is how effective the mantle is at stopping magma plumes.
This anti-volcanic wall of “cool” rock stops around 87.88% of all plumes that come through it, thus, any volcano which is here, is typically a supervolcano of some kind, as those are the only ones that get through the mantle, they’re similar in strength to Yellowstone. Last thing to note about this mantle is the composition and density of it. The materials in the mantle are mostly uniform, with high amounts of nickel and other such similar metals, excluding silicon and cobalt. The density of those materials is as high as the rock they make up, creating a material worth 1.566 times that of the Earth’s mantle, which means that any mining operations here will pull up more resources per kilogram on average. This is also not excluding this mantle’s unusual high amount of precious resources. The higher pressures force out more kinds of crystals, most of which are not found on Earth as well. 
==== Crust ====
The crust here is a hard and very thin layer which surrounds the even harder mantle. This crust’s parts (tectonic plates) don’t move at a regular speed, instead appearing to hover / float in one general location for long periods of time, rarely pushing out any other plates until a great amount of force is acted upon them, and even then it takes them ages to move. The tectonic plates here take 1.666 times the amount of time it takes for the Earth’s plates, which means it takes over 1 ½ times as long for a continent to merge with another one as here. 
This also means that the mountains here don’t have a great chance to get tall, as erosion would chip away at their height faster then they grow. Besides this crust being slow and short, the materials and consistency in this crust are similar to the mantle, just with higher amounts of other metals and alloys besides nickel, still excluding silicon and cobalt for some reason. This crust, however, has a way lower temperature compared to the mantle right below it, acting more like a hard metal shell than a slightly cooler continuation of the mantle as expected. A last thing to mention about this crust is that because of how slow it is, the repairing process for rifts and other such faults / cracks in the ground is more constant and easier, which means that you wouldn’t see as many rift / fault lines here as you would see on Earth, this also means, no Hollywood earthquake canyons. 
=== Geography ===
==== Northern Hemisphere ====
The northern hemisphere of this planet is ocean-dominated, like the southern hemisphere. The northern hemisphere has one supercontinent, and that supercontinent has three continents inside of it. That landmass follows along an east-to-west line, and it seems to be moving to the west as the third continent towards the “back” of the supercontinent is being lost to sea, turning into a bunch of swamps, lakes, and islands. Speaking of which, the northern hemisphere does not have that many lakes; either they are in marshlands, of which there is only one here, or they are all centralized into one large mini-sea, which is thinly out of reach of becoming a bay because of a thin strip of land. 
This supercontinent is wider than it is long; it is way taller than it is long by a large shot, with dimensions of 1:3. This supercontinent and the northern hemisphere in general have a large number of islands. These islands form consistent archipelagos and don’t really diverge from their archipelago. All of the islands are approximately close to the supercontinent and are generally small. The number of islands here is small compared to the southern hemisphere, but the size of the oceans they reside in is not. The northern hemisphere specializes in large, blissful, empty oceans. It has 2, technically, 3 of them, and they are around the same size as the Pacific Ocean. At best, they have little volcanic scraps that have nothing of real value.
==== Southern Hemisphere ====
The southern hemisphere has one main continent, like the north, but it is not a supercontinent. This is a polar continent since it is located on the south pole, and it has a large and diverse number of islands, more so than the north. The continent itself is not that interesting—an average landmass with fractured coastlines that resemble fractured asphalt more than actual coastlines. It does not have that many rivers or lakes; it does have a planet of islands. They range from volcanic scraps to landmasses in their own right, with the largest of which being around the same size as Europe. This continent follows a great circle around the south pole, and it has a great bay that nearly reaches the south pole. Most of the islands, which are in the southern hemisphere, follow an archipelago format like the North, though they are poorer at it. 
The southern hemisphere also has more independent islands, which comes with having more total islands. The north has a few; though they are pebbles, here they are country-sized rafts in the middle of the ocean. The south does not have as many rivers or lakes as the north does, unsurprisingly, considering the main continent lacks them. The south is also more arid than the north, which explains the continental deserts and larger coastal islands, especially the tidal ones, with a group joining into one massive island. Speaking of giant islands, the southern hemisphere has the largest volcano on this planet, a volcano around the size of Texas. It has, unfortunately, passed away a long time ago, as it has lost many of its distinctive features and the vast majority of its height over time. Since the island hasn’t been destroyed, that points to the idea that the geography of this world, both north and south, is very slow.
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Category:Procedural objects
Category:Objects
Category:Superterra
Category:Superhabitable
Category:Life
Category:Terrae
Category:Terra with Rings
Category:Planets