Verri
User:The Minmus Derp (10/01/2025)
User:The Minmus Derp (10/01/2025)
~55,000 light-years
Nenar
Delnar b
Verrin
Icy
0.404 AU
0.637372 years
0.32
0.27472 AU
0.53328 AU
0 (reference plane)
1st
Vilni Group asteroids
0.083 Terrestrial Masses
3,592.56 km
2.5524 g/cm3
2.5598 m/s2
1.5% Iron/Nickel
80.1% Silicates
18.4% Ices
3,180 km
85 K
98 K
75 K
Liquid methane/ethane
Large lakes, rivers, and ponds
Water
890 m
89.4%
1.55 atm
Variable
Stratosphere:
- 97.4% N2
- 1.4% CH4
- 0.2% H2
- 1.0% He
Lower troposphere:
- 94.0% N2
- 4.9% CH4
- 0.1–0.2% H2
- 1.0% He
0.265
2.2 billion years old
15.88 days
27º
None
Single global landmass
Livai, Krali, Ontri
Antra Mons
Antra Mons (1,488 m)
River of Dawn
Kanjen Range
Desert sands
1.5%
Desert, polar lakes
Polar vortex
Equatorial deserts
Polar regions
Equatorial deserts
Polar regions
5
Miscellaneous captured asteroids
Millions
Verri Shipyards
Medium
Low-Medium
Solar Energy
The lone planet of the Delnar System, Verri is the homeworld of the Verna species, capital of the Delnar Empire, and a key world within the Vernarcan Federation. Verri is one of a few examples of a world possessing methane-solvent life, mostly found in its polar lakes, and is also arguably one of the smallest and driest worlds to support intelligent life with only 10.6% of its surface submerged.
Physical Characteristics
Verri is 3,592 km in radius, somewhat larger than the Verna colony world of Liratan and much smaller than the vast majority of habitable worlds known. Verri is the largest object within the Delnar System excluding Delnar itself, followed by its binary companion of Sil as well as the assortment of dwarf planets and asteroids nearby. With a bulk density of 2.5524 g/cm3, Verri's composition is roughly 80% silicates, with the rest composed of water ice and other materials.
Verri's physical structure is differentiated into distinct layers, with a ~5000 km diameter rocky center, surrounded by several layers composed of differing crystalline forms of ice and tidally melted liquid water. A liquid layer of 'magma' exists composed of water and ammonia between the ice I crust and deeper higher-pressure forms of ice, due to the heat flux coming from the planet's core. The planet's crust is completely decoupled from the interior, showing that this layer goes all the way around the planet.
Due to the near-complete lack of siderophile elements within Verri's structure, Verri also does not possess a substantial magnetic field beyond that formed by interactions between Delnar's barely-there solar wind and the upper haze atmospere.
Orbit and Rotation
Verri orbits Delnar once every 232.8 days, at a distance of roughly 0.4 AU from the star. Unlike most inhabited planets around red dwarves, Verri is not tidally locked due to its comparatively extreme distance, rotating once every 15 days and 22 hours. This also enables the stability of its binary companion Sil, which experiences a state of double tidal locking with it. It has an orbital eccentricity of 0.32, and its orbital plane defines the reference frame of the entire Delnar System at around 33 degrees inclined from Delnar's rotational axis. Both Verri and Sil hold an axial tilt at 27º from the binary pair's orbital plane.
Surroundings
Verri, as the largest object in orbit around Delnar, as a great affect on its surroundings, including the large binary companion Sil, the variety of captured asteroids surrounding the pair, and the various objects in orbital relationships with them orbiting Delnar itself.
Verri's sister world is nothing like it. Sil is an airless, pockmarked world which never had the smallest speck of native life outside of unfortunate bacteria. With a composition made almost entirely silicates, it is believed to originate much closer to Delnar than its current partner, being ejected from this position by long-term gravitational effects. Sil's surface is marked by substantial geologic activity and volcanism, which provides power to even many modern colonial installations on its surface.
In ages past, Sil could just barely be seen on the horizon through the ever-present haze of Verri, often seen as a distant mountain by the great civilizations at the poles and only revealed otherwise by interactions with the nomads of the equatorial deserts and explorations therein. The first space missions finally revealed the planet in its true glory, and its exploration and colonization was key to Verna expansion within the Delnar System. In the modern day, Sil's surface has been partly worldhoused and covered by great habitation domes of a variety of forms. Most of them are designed for Verna (and thus Pr'rana as well) habitation, but there are some enclaves of Ravoryl, Alorath, and other species found here.
Captured Asteroids
Delnar is a small star, and for such a small star 0.4 AU is a vast distance. Thus, Verri-Sil's sphere of influence is verri large. This means that some of the multitude of asteroids found within the Delnar System have been captured into long orbits around the planets. The asteroid Arik directly orbits Verri itself, but seven others orbit both worlds at a great distance. The largest of these is Anadel, home to the largest segment of the impressive San Ska Re Shipyards found throughout Verri's sphere of influence. Here, a massive number of starships of the Vernarcan Federation Space Force and many other organizations were all built, including the famous FSS Kareland.
Resonant Companions
Verri and Sil, being the largest mass concentration outside of Delnar in their solar system, have a great effect on the other objects within it. Most notably, the barely-spherical dwarf planet of Hygeras is locked in a 3:4 orbital resonance with Verri and Sil, orbiting three times every four times Verri-Sil orbits. Other objects exist in this resonance, but more commonly objects in the 3:2 and 2:1 resonances are found.
Atmosphere
Verri is endowed with an impressively thick atmosphere, with a surface pressure of 1.55 atm, and is one of the uncommon objects whose atmospheres are able to support clouds, hazes, and weather. Due to this extensive, hazy atmosphere, Verri's size was initially difficult to determine through visual means especially from afar. This haze also prevented Verri's surface from being seen on most wavelengths, making for disappointing views from the first Verna space missions.
Three elements make up the vast majority of Verri's atmosphere: nitrogen, methane, and hydrogen. Uniquely, the precise atmospheric composition varies wildly depending on altitude and latitude due to methane's constant cycling between a gas and liquid in the planet's lower atmosphere. Up in the stratosphere, methane makes up ~97.4% of the atmospheric content, decreasing to 94% nearer to the surface. Methane concentrations are conversely highest near the surface with a fairly constant 4.9% up until 8 km above the datum level. After that point, concentrations decrease as altitude rises, down to around 1.4% amid the haze layers. Methane can also be more commonly found near Verri's winter pole, caused by surface evaporation.
Compared to these fluctuating numbers, Hydrogen is much more consistently around 1 part per 1000, accompanied by trace amounts of other hydrocarbons like ethane, diacetylene, methylacetylene, acetylene, propane, cyanoacetylene, various things that aren't acetylenes I'm sure, and other gases like hydrogen cyanide, carbon dioxide and onoxide, cyanogen, argon, and around 1% concentration of helium caused by Verna industry following the invention of practical fusion reactors. These hydrocarbons are created in the upper atmosphere of Verri by the breakup of methane by Delnar's ultraviolet light, producing the thick orange haze which is the planet's most famous feature.
Methane on Verri is replenished over time by a variety of means. Delnar's energy should have converted all traces of methane in the atmosphere into more interesting hydrocarbons within 150 million years, much smaller than the 2.2 billion year existence of the planet. Some of this replacement is caused by cryovolcanism, releasing methane from the interior, but the majority is created by biological processes within Verri's ecosystem. Complex organic chemicals arise on Verri which likely provided the initial origin of Verrin life-forms, including polycyclic aromatic hydrocarbons in the upper atmosphere.
Climate
Verri's surface temperature averages approximately 93 K. At this temperature, the vapor pressure of water ice is extremely low, limiting what little water vapor there is to the stratosphere. Even without the famous haze layer, Verri is an extremely dark world with about 1% as much solar flux from Delnar as planets like Teralla and Erdath receive from their parent stars. But approximately 90% of even this meager amount is absorbed by the thick atmosphere, leaving under 0.1% of this amount.
The high quantity of methane in the atmosphere creates a greenhouse effect on Verri's surface, without which the planet would be substantially colder. Conversely, Verri's haze layers partly counteract this by absorbing sunlight and making its surface significantly colder than the upper atmosphere. Clouds cover around 1% of Verri's surface, although every so often this coverage can expand to as high as ten times this value. Clouds are generally formed when heightened levels of sunlight during each hemisphere's summer, resulting in convection, although unexplained formation does occur during mid-spring and fall.
Geography
The surface of Verri is highly complex and geologically young, greatly influenced by the presence of liquid hydrocarbons. Most of the planetary surface is between 100 million and a billion years old, at most less than half the age of the planet and the Delnar System as a whole. Cryovolcanic features are present across the planet, with highly viscous liquid water and ammonia serving as a lava stand-in. Windblown particles have created large-scale features that would be visible from space were it not for the haze. Few impact craters survive on Verri, with the single-digits numbers of them which remain all partially filled in by raining hydrocarbons or cryovolcanism. Topographical variation is generally no more than 150 meters in most places, with the highest of mountains at only 1,488 m above the datum level.
With the absence of large oceans separating landmasses and large variance in elevation, Verri's surface is thus defined by regions of bright and dark terrain. These include Eirnu, a large high-albedo region similar in size to Kastri on Teralla. Like much of the equator, Eirnu is extremely dry and cut with valleys, hills and chasms. It is crossed in several places by dark-colored ridges or crevices, representing alternately tectonic activity or liquid-formed channels from ages past.