Annunance

(I have now split my day into blocks to make working on these worlds easier.)
== Annunance's Abfrontals ==
=== General summary ===
A world of large plains and the occasional volcano. This world is inhabited by large yet light creatures which are not that fierce, and are primarily herd vegetarians. The weather is calm and scenic here, and there is a constant breeze here. The skies here are normally clear with the occasional cloud, and the oceans are shallow and not that wavy, way less then what is found on the Earth. A small magnetic field accompanies this world, which would mean that it should be dead considering the area that it is in, but it is not for some reason, and the planet is in a binary with another planet, a small one, which creates some eerie yet scenic views. 
=== Trivia ===
* A past world that I had no real thought of including untill now
* It might or may not deal with a great deal of radiation
* I may refine the format that I did with the planet (right before this one chronologically) to be longer / easier to write.
* This world is quite average.
=== Key featurals ===
This planet is covered by eroded continents of desaturated green and yellow, and these continents are large, covering a slight majority of the planet. These eroded continents have a large amount of large islands just off their coasts, though not deep in the oceans. All of these continents follow from each other. The ocean which may or may not separate them is a lighter coloration of navy blue, with the atmosphere above it sharing a slightly darker version of sky blue. The planet is not really covered by clouds, only having slight splotches of white and grey which are separated and far from each other. They do not form into any real storm structures,and they are small in size. 
== Annunance's Properties ==
=== Physicals ===
The equatorial diameter of the planet is 7440.52 miles, with the mean diameter being 7440.52 miles, and the polar diameter is 7440.52 miles. The oblateness is 0, with the mass of the planet being 1.0428 M⨁, and the density is 6.9279 grams per cubic centimeter. The insolation is 0.4899, with the effective temperature being 190.04 kelvin, and the Earth similarity index is 0.891. The rotational period is 9.294 days, with the solar day being 8.851 days, and the axial tilt is 100*55’31.92”. The gravity on the equator is 11.605 meters per second, with the gravity on average being 11.58 meters per second, and the gravity on the poles is 11.58 meters per second. The circular velocity is 18625.84 miles per hour, with the escape velocity being 26340.92 miles per hour, and the age of this world is 8.455 billion years, additionally, the tidal heating is 3.2178*10^11 watts. Silicate mantle makes up 52.4% of the planet, and the metallic core makes up 47.6% of the planet. 
=== Atmospherics ===
The height of the atmosphere is 41.16 miles, with the tropopause height being 14.81 miles, and the height of the homogeneous atmosphere is 26827.77 feet. The atmospheric pressure is 36.9 atm, with the air density being 39.527 kilograms per cubic meter, and the air temperature is 318.27 kelvin (113.216*F, 45.12*C). The speed of sound here is 794.83 miles per hour, with the exosphere temperature being 1132.4 kelvin, and the greenhouse effect is 128.19 kelvin. The average molar mass is 28.085, with the relative mass being 2.1099*10^-5, and the actual mass of the atmosphere is 27.503 Earth atmospheres. Nitrogen makes up 82.3% of the atmosphere, with Oxygen at 14.8%, Water vapor at 1.99%, and Carbon dioxide is at 0.931%.
=== Hydrospherics ===
The maximum depth of the ocean is 11350.19 feet, with the average molar mass being 18.017, and the density is 1 gram per cubic meter. The  temperature is 318.27 kelvin, with the atmospheric pressure being 36.9 atm, and the bottom pressure is 432 atm, additionally, the bottom composition is rock. Water makes up an observed 100% of the ocean here, with Sulfur dioxide at 42.9 parts per million.
=== Orbitals ===
The parent of this world is the secondary in a binary star system, with the type of orbit being elliptical, and the orbital period is 9.294 days. The semimajor axis is 5337.1025 miles, with the pericenter being 5124.7843 miles, and the apocenter is 5549.4207 miles. The eccentricity is 0.040, with the inclination being 167*50’16.72”, and the ascending node is -103*55’7.65”. The argument of pericenter is 356*32’54.86”, with the mean anomaly being -25*5’26.80”, and the longitude of pericenter is 252*37’47.20”. The mean longitude is 227*32’20.40”, with the orbital velocity being 150.33 miles per hour, and the hill sphere radius is 606522 miles, additionally, the influence sphere radius is 391524 miles, plus the Roche limit for satellites is 5978 miles. 
== Annunance's Informationals ==
=== Internals ===
==== Core ====
The core of this planet is regular in composition, a molten ball of silicon, nickel, and other such metals. This core is nearly half the mass of the Earth, and it makes up 47.6% of the planet, which means that this core is larger on average. It however does not spin that fast, and it produces less successful magma plumes then what is expected of it, and while the amount of large active volcanoes may seem like alot, the expected amount is nearly double that of what is seen.  The inner core is surprisingly larger then the outer core, and  it has a slightly higher amount of nickel in it then the outer core. The inner core makes up a staggering 67.8% of the core, and said inner core seems responsible for a great deal of the activity found in the core. This molten ball also does not have as definite of a boundary with the mantle, or with itself, which creates a sort of blob like core. The reasons for this are unknown, but it may have come from a primordial impactor, as seen with the mantle and a bit with the crust. 
==== Mantle ====
The mantle here is quite average, it has a similar enough composition to the core that it surrounds, most likely because it does not have any real boundary with that core, and it has a slightly higher strength then the Earth’s mantle, not allowing for as many mantle plumes to come out of it. This mantle is mostly round, and it shares a definite boundary with the crust above it, and the currents which go through the mantle are faster then what is found on the Earth, which leads to more tectonic activity, as reflected in the volcanic activity and geography. This mantle has a large weak spot, with most of the volcanoes coming from this area, and thus where most of the successful magma plumes come from. This weak spot has a strength 27.9% less then the Earth’s, and the reason for it is believed to be from an old impactor 8 - 7 billion years ago during the formation of the planet. It would have been similar in mass and size to the young planet, and it would have impacted with a great strength, enough that most of the mantle that it impacted would have been ejected out into space, which would explain this weak spot, which also has a lesser density then the rest of the mantle around it. An imprinted bulge of material which is not consistent with the rest of the mantle is also observed here, though faintly. 
==== Crust ====
The crust here is weak and more fluid with its movement. This means that the tectonic activity here is higher than the Earth’s, and it is around 29% higher than the Earth’s in speed. This is reflected in the geography. Because the crust is smashing and submerging underneath itself faster than our planet’s speed and what is expected of this world, the number of cracks, rifts, faults, etc. is higher. High enough that new land is regularly formed from exposed rifts opening wide, sometimes miles wide in the most extreme cases. The mountains that form on this crust are taller on average, having an average height just a bit shorter than the Himalayas, and the trenches here follow a similar trend, with a few even being deeper than the marina. While the crust is described as being more fluid and active, this does not mean that it does not have a definite boundary with the mantle below it. The reason for this is unknown, but the densities of the two are different, the materials and their density are different (the crust has a higher content of silicon and similar metals and alloys), and the layers of the two follow a different structure, which is different enough that going between the two would be very noticeable.
=== Geography ===
==== Northern hemisphere ====
The northern hemisphere of this planet has a large amount of land, around a 75/25 split of land and ocean. The northern hemisphere has not that many islands, and the islands that do exist are small, volcanic shreds of could have been supervolcanoes and small sand banks with some amount of grounding vegetation. The northern hemisphere’s lands are connected to each other in a similar manner to the ones in the southern hemisphere, as in through thick land bridges connected what would have been disconnected continents. The northern hemisphere has less water than the southern hemisphere, and this water has formed into 2 large seas, with only a few small lakes following from them. The lands which surround these 2 oceans have lots of swirly peninsulas which follow great and soft curves with lots of smaller peninsulas of loosely connected sand banks and seamounts following off of them. The land in the northern hemisphere is more solid then the southern hemisphere, only a few areas in the northern hemisphere appear to be not solid / fractured, and those areas are the mentioned loosely connected sand bank peninsulas. That or land bridges which are currently sinking. 
==== Southern hemisphere ====
The southern hemisphere is much like the northern hemisphere and has much of the same geography except for these key differences. The southern hemisphere has way more water, and while this water has formed into 2 oceans, both of which are double the size of their northern counterparts, and a few hundred lakes, which may seem small compared to what we have on Earth, but it is a massive difference between it and the northern hemisphere. The southern hemisphere has way more islands too compared to the northern hemisphere, and these islands are not sand banks or volcanic scraps, but larger and more well formed, speaking of form, the islands here follow archipeligoes, well defined ones too, as opposed to the ones in the north, which are not well defined or large. The north has little pebbles compared to the south when it comes to islands. 
The south also has more dynamic coastlines. While the north has maybe a fractured bay of sorts in which it stores most of its islands, the south’s coastlines go in all sorts of directions, jabbing and bending in what would be seen as nonsensical directions by the north’s view. Another thing to note is the continents in the north and south. As opposed to the north, the south has more continents, or more specifically, more well-defined ones. The continents in the north are all connected by land bridges and while this remains true for the south, the land bridges in the south are thinner then the north’s and are more likely to split. The south also has an independent continent, something the north does not, and that is in the form of a polar continent which splits off whenever a certain set of rivers overflow, which is quite often throughout the year.
=== Climate ===
The planet has a temperate climate, with this climate being a slightly sub-humid one, and the weather activity in this climate is low. This climate’s ability to form weather and weather patterns that stay consistent over time is 0.7789% less than the Earth’s climate. (Weather is defined here as patterns that are not just clear.) This temperate climate produces partly cloudy and light showery weather, with the high end of this weather being light tropical cyclones and the low end being plain clear weather. This climate also has a moderately low wind speed of around 8.1009 meters per second. This planet’s climate is considered a global climate; in other words, this climate has little variation from north to south. The polar climate is only marginally colder than the equatorial climate, and the only real difference between the polar and equatorial climates is the amount of weather, which drops a bit from the equator to the pole. 
This climate seems to be an "age-climate." A long-lasting climate that defines the planet for a long span of time and then transitions, either quickly or slowly. This climate is a “dune-age” climate, a hot climate that is the opposite of an ice age, which has no ice caps and is infested with deserts. This climate seems to have only settled in recently, and the ice caps melting might have set back desertification by a little bit, with the humidity in the air preventing airdiness from arising. The humidity in the air here is only a little lower than the Earth’s humidity; this is predicted to change though, getting lesser and less until it is around 4.335% less than the current humidity. The signs of desertification are already present in random patches of desert in places where they shouldn’t be.
=== Biosphere ===
==== Landsphere ====
===== Terrestrialanimalia =====
Most creatures on land are low lying quadrupeds which have large underbellies, and lerger noses. While most animals take a variation on this, with some going their own way as little fox/wolf-like animals that graze as well, most of them have that form. Most animals graze on large fields and tend to be nomadic in their nature. They are all vegetarians, no omnivores or carnivores found, which is odd considering how massive the market would be, and they are all short-haired, meaning they have fur on their skin, its just very short. These creatures have evolved over time to have larger and more efficient sweat pores, and they have also developed a sense of smell for water, which is also the thing they mostly stick to. Most of these animals live near the subpolar regions and poles, primarily in shaded plains, with the unique members of this biosphere taking up the mantle at the equator and deep forests / jungles. 
Those unique members tend to live isolated in their own communities and are less nomadic. They are smaller on average then their average cousins, but they are also more water efficient, especially the equatorial ones, which would thrive in any modern desert today, with a reuse system for water and a heightened smell to water, building off of their brothers up north and south. They also have developed a faster speed, and are less likely to just graze, which is opposed to the polar and subpolar animals which take a long time to graze and are typically very slow. The creatures here generally move in herds, (except the ones in the deep forests, who also have abandoned a smell for water), and thees herds tend to follow a decentralized “communal network” which means that there is no leader, but group decisions are held by a vote. Quite an advancement for vegetarian herd species which are much like camels and sheep. The grazing pastures for these animals tend to be very large as well, and there is little species variation besides the equatorial and forestal regions. 
===== Terrestrialplantia =====
The plants here are generally short, have a yellowish-green tint, and are very spreadable, able to grow anywhere except for cold and hot deserts. There are no flowering plant species, there are no carnivorous plant species, and the way in which they spread is via seeds embedded in their leaves. It would be like if grass has deeds in it. They are little dark pellets and are able to germinate anywhere, except for the deserts. This also means that the land plants can sometimes grow in the oceans, but these plants don’t live for long and typically don’t even reach above the water level. These grasses are thick, and have a similar thickness to that of a kale. The plant part of the land biosphere is homogeneous and not that interesting to see, but it is scenic. Oh, I almost forgot, the forests, but they are much the same too, just now with short trees who are spread out from each other, unless they are deep in the forest, then they grow a bit taller and get closer, but not too close, 3 7’0” men could fit in the gaps between those trees with their arms stretched out, and said trees also grow thick roots which are around 14 inches wide sometimes. 
== ~000~ ==