Bveitrha

(This world will be a focus considering how long it is taking me to write basic things about it.)
==Bveitrha's Abfrontals==
===General Summary===
This is a blue hazed world of massive trees and lanky creatures. It is average in size, but not in composition. 
===Trivia===
* Wow
===Key features===
This world is of a saturated blue color, and is covered by various forms of clouds. This planet is made up of roughly 50 / 50 land and sea area, and the plants here are dark in coloration, black actually. The lands are covered mostly by black plants, and these said lands have islands, lots of islands. Those islands stick close to the land and they are in the thousands, and they are normally small pebbles in size. The black coloration that covers the majority of this planet’s lands, is sometimes interrupted by desert dunes in the form of a goldish yellow. 
They are like a yellow oasis is a desert of jet black. They also don’t really follow a consistent form, though they tend to be in lowlands.Those lands also have plenty of large rivers, which slice them into large fragments. All of these oceans are connected in some way, wether that be in wide seas or narrow straits. It should also be noted that there are a few patches of gray which are from dead flats, the reason for their existence is unknown, but they are normally really small, and they are found in lowlands that seasonally flood. 
==Bveitrha's Properties==
===Physicals===
The planet has an equatorial diameter of 8037.13 miles, with the mean diameter being 8037.13 miles, and the polar diameter is 8037.13 miles. The oblateness is 0, with the mass being 1.2611 M⨁, and the density is 6.6472 grams per cubic centimeter. The insolation is 0.8689, with the effective temperature being 221.85 kelvin, and the Earth similarity index is 0.938. The rotational period is 17.080 days, with the solar day being 51.240 days, and the axial tilt is 0*00’00.00”. The gravity on the equator is 12.028 meters per second, with the gravity on average being 12.002 meters per second, and the gravity on the poles is 12.002 meters per second. The circular velocity is 19707.52 miles per hour, with the escape velocity being 27870.65 miles per hour, and the age of this planet is an old 12.246 billion years, additionally, the tidal heating is 2.4127*10^13 watts. 
===Atmospherics===
The height of the atmosphere here is 40.40 miles, with the tropopause height being 10.20 miles, and the height of the homogeneous atmosphere is 21811.75 feet. The atmospheric pressure is 9.35 miles, with the air density being 11.871 kilograms per cubic meter, and the air temperature is 271.47 kelvin, -1.68 *C, or 28.976*F. The speed of sound here is 729.62 miles per hour, with the exosphere temperature being 1107.3 kelvin, and the greenhouse effect is 49.581 kelvin. The average molar mass is 28.865, with the relative mass being 4.9706*10^-6, and the actual mass of the atmosphere is 7.8353 Earth atmospheres. Nitrogen makes up 60.8% of the atmosphere, with Oxygen at 36.9%, Water vapor at 1.32%, and Carbon dioxide at 0.977%. 
===Hydrospherics===
The maximum depth of the oceans here is 15445.88 feet, with the average molar mass being 18.016, and the density is 1 gram per cubic centimeter. The temperature is 271.47 kelvin, the atmospheric pressure is 9.35 atm, and the bottom pressure is 567 atm, additionally, the bottom composition is rock. Water makes up a relative 100% of the waters here, with Sulfur dioxide at 16.5 parts per million. 
===Orbitals===
The parent of this world is the primary in a star system, with the orbital  period being 25.619 days, and the semimajor axis is 0.1074 AU. The pericenter  is 0.1005 AU, with the apocenter being 01143 AU, and the eccentricity is 0.064. The inclination is -0*44’54.85”, with the ascending node being 50*3’29.16”, and the argument of pericenter is 136*45’50.67”. The mean anomaly is 340*35’5.14”, with the longitude of pericenter being 186*49’19.84”, and the mean longitude is 527*24’24.98”. The orbital velocity is 102026.91 miles per hour, with the orbital resonances being 7:4 (A4), and the hill sphere radius is 159924 miles. The influence sphere radius is 117546 miles, with the roche limit being 6369 miles. 
== Bveitrha's informationals ==
=== Internals ===
==== Core ====
The core here is nominally active, it has a size slightly higher than the Earth’s, and an activity level similar to the Earth’s. This core is made up of mostly cobalt and nickel, with some trace amounts of silicon and other such metallic materials. The core here produces an average amount of successful magma plumes, distributing the volcanoes evenly across the surface. This core has a rough 60/40 split between the outer and inner core, and both sections of the core produce a similar amount of heat. The core’s rotation is moderate, similar to the Earth’s core, and this core has a definite boundary with the mantle, indicating that it has a slightly different rotational period and composition then the mantle.
==== Mantle ====
The mantle above the core has average strength, allowing for an average amount of magma plumes, which are evenly distributed, as there are no weakspots here. The mantle has a density slightly less than the Earth’s mantle, and the materials featured in this mantle are nickel, silicon, cobalt, and some trace amounts of other materials similar to the ones listed. The mantle has a generally uniform temperature gradient, not allowing for that much variation from the core to the crust. The material gradient is not uniform, however. The further from the core you go, the more silicon there will be, with a negative trend for nickel following a similar line. The density of materials seems to get higher further down, so mining operations would have to dig way deeper to get any special results. This mantle has an average cycle speed and heat, which makes above-crustal movement average and not too out of line with what is expected of the planet, which this mantle also is.
==== Crust ====
The crust here is like a continuation of the mantle below it. It has a gradient similar to the mantle below it when it comes to materials, with the amount of silicon increasing the higher up you go, and the densities of the two are similar, which means that they do not share a definite boundary and instead their boundary is more blurry. This also means that the tectonic plates are a little wonky, as the crust suddenly has to decide which parts of it are going to move with the plate and which are not. This causes some odd effects where the mantle below gets stretched and destroyed, which also explains why the density of the mantle right next to the crust is lower than it should be. 
However, because the convection currents below the crust are not too active, it does not have to do what and instead can move its individual plates at a steady pace without tearing apart the deep-underground every time. This crust is mostly silicon and cobalt, with little trace amounts of other materials being found, along with nickel, which is in 5th place behind aluminum. This silicon crust has a similar thickness (estimated) to the Earth’s, and the hardness of this crust is like the Earth’s, although it is slightly weaker. The last thing to note here is the movement of the plates. While they are slower than expected, when they are forced to move at a pace that is higher than the Earth’s, they will sometimes funnel the mantle out through a rift line in the crust, which creates some odd material distributions that any future civilization that likes nickel but does not want to drill too much can be aware of.
=== Geography ===
==== Northern hemisphere ====
The northern hemisphere of this planet is an ocean-dominated stretch of continents with a large number of islands. The northern hemisphere has 1 ocean and 4 continents. These continents are distributed in a ring-like formation around the polar ocean, leaving a small gap in the form of an island-rich sea. Three of these continents are small in size, around the size of North Africa and Europe combined, and the fourth one is around the size of Asia and North America combined. These continents are weakly connected to each other and are often separated by large floods. The northern hemisphere has a massive amount of islands; around ¾ of the islands on this planet exist in the northern hemisphere, and most of these islands are well-formed and follow archipelagoes. 
They are normally close to the coast, are moderately small, and form close to each other. The ocean, which they mainly inhabit, has high amounts of them, with a few even near the north pole, and the one gap that exists out of the polar ocean and into the rest of the world has even more, and the islands there appear to be formed out of a hammer striking a window. One last thing to note about the northern hemisphere is the lakes; there are large amounts of them here, though they tend to be small in size and are normally close to the sea, except for one exception. There are fewer rivers in the northern hemisphere for some reason.
==== Southern hemisphere ====
The southern hemisphere is more continental in nature, harboring the most land on the planet, and most of that land is on one massive polar continent around the same size as that of the of the northern continent mentioned earlier. Neither of them are supercontinents, surprisingly. There are more rivers here than in the south, with just the river lands in the northernmost parts of the polar (or antarctic) continent having more rivers than the entire northern hemisphere. There are also more lakes in the south; they are larger and don’t follow any particular form, seemingly appearing anywhere they feel. 
The southern hemisphere’s main continent and only continent is around the same size as the polar ocean up north, and this polar continent is the largest on this planet, and if put on the Earth, it would be connecting South America to Australia, and New Zealand and South Africa would be right off the coast of this thing. Most of the rivers in the southern hemisphere are focused in one region, the northern half of this polar continent. The geography of the southern hemisphere is sort of a flip on the geography in the northern hemisphere, with the ring of continents being flipped for a ring of oceans, the diverse and large well-formed islands for disorganized volcanic scraps, and the lowlands and plains of the north being replaced with taller hills and mountains that surround even larger lakes and rivers. The islands in the south tend to group near the coast, and there are only two archipelagos in the south compared to the 30 in the north.
=== Climate ===
This planet has a more chaotic and dangerous climate system than the Earth. The climate here is a little warmer than it is reported as, and this is due to the large amount of rainfall which covers this planet in a high humidity blanket, in which the environment feels like it just rained, This is consistent; rare will you find a day where it feels like a shower didn't just happen. This climate produces more weather on average, forming rainstorms, showers, thunderstorms, cyclones, and tornadoes at a rate 67% higher than the Earth. It should also be noted that this climate is global, with little to no variation from the poles to the equator. 
Only in the amount of cloud cover do you see any real differences between the two, and even then you wouldn’t really get a clear day, as those only happen 30 - 50 times a 365/24 hour term. Besides this climate being pretty humid, around 50% higher then the Earth in the driest of places, you also have to deal with regular severe weather. This climate is like the Earth at the very end of Global warming, far from it, but, the amount of category 4 cyclones here and daily thunderstorms is way higher than the Earth, by around 65%. The low end of this climate is partly cloudy, and the high end of this climate is a category 5 cyclone, with the amount of cloud cover here being over 50% in most if not all places. As previously stated, this is a global climate that experiences little variation when moving from the poles to the equator.
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