~~Planetary physical properties (My game called star system generator)
Geosphere chemical composition types:
-Ferrinian: Entirely iron and nickel.
-Selenian: Silicate rocks and/or oxygen rich volatiles, but core of iron/nickel.
-Oxycarbean: Silicate/carbonate/carbide rocks, but core of iron/nickel.
-Carbean: Silicon/titanium carbide rocks with small amounts of carbonates, but core of iron/nickel/carbon.
-Glacian: Fluid types in solid state, but mantle of rocks and core of metals.
-Gasean: Gases of theoatmon and togun, but mantle of rocks and core of metals.
-Customidian: Artificially dyed by extraterrestrials with chemical dyes are natural and artificial, determining why planetary composition challenges planetary origin and formation.

Traits:
-Terramare: Also known as land-sea planets, planets have lands and seas on its surface.
-Cytherean: Foggy planets are completely cloaked by clouds and supercritical fluids of fluid types, resembling Venus.
-Europan (for Glacian planets): Planets have subsurface oceans.
-Chthonian (for non-Gasean planets): Former Gasean planets lost envelope of theoatmon and togun.
-Artificial: Artificial planets are constructed.
-Cryotholian (for Gasean planets): Below temperature zone, Gasean planets have permanent non-cloud (haze or smoke, soot, dust, snow, etc.) of tholinyls and aerosol types, but losing temperature, never raining or snowing. Cryotholian planets have diverse types, except other Azurians beyond CryoAzurian. Other Azurians will becomes Cryotholian CryoAzurian when it ejected.
-Sideropean: Planets lack metallic cores.
-Hothouse: Planets have runaway greenhouse effect.
-Airless: Planets lack atmosphere

Hydrosphere fluid types (Surface and subglacial), cultural name to scientific name:
-Water (Dihydrogen monoxide)
-Ahych (Ammonia)
-Fyesh (Methane)
-Azote (Nitrogen)
-Oambr (Neon)
-Jatule (Oxygen)
-Togun (Helium)
-Theoatmon (Hydrogen)

Biosphere:
Cellular
-Protocellular
-Unicellular
-Multicellular
Biome
-Marine
-Terrestrial
-Aerial
-Subglacial

Atmosphere:
Density
-Superdense
-Dense
-Medium
-Sparse
-Trace
-Airless
Chemical composition
-Noble gases
-Carbon dioxide
-Sulfur dioxide
-Vapors of fluid types

Aerosol chemical composition types of clouds/hazes over thick atmosphere of theoatmon and togun (for Gasean planets):
-Letter - Demonymic name (Hex color): H, He, aerosol chemical composition.
-A - Azurian
--CryoAzurian (#c4eeff): CH4, hydrocarbons.
--MesoAzurian (#41d9d9, turquoise coloration from sulfur and organic compounds): CH4, simple hydrocarbons.
--PyroAzurian (#0077a6): CH4.
--HyperPyroAzurian (#0047ab, what does cloudless Frigidian look like, color can't be seen because higher temperature, but glows redder): Fires of H and He, hotter version of Frigidian.
-B - Frigidian (#f2f4ff, #f5f6fc): Clear, pristine, opaque clouds/hazes of H and He.
-C - Oambrean (#fff2f4, #fcf5f7): Ne.
-D - Azotulean (#fff5ff, #f5f5ff, #f4f2fc but #ffefd9 from tholin discoloration): N2, CO, O2.
-E - Fyeshian (#ebfffb): CH4, C2H6, Ar.
-F - Tholinian (#805026, #ffca80): Tholin.
-G - Sulfurian (#fff2ba): H2S, NH3, (NH4)HS, HCl, SO2.
-H - Ahychian (#ffe1ba): NH3, (NH4)HS, (NH4)2S, H2O, CO2.
-I - Waterian (#ffffff): H2O.
-J - Acidian (#fff8e6): H2SO4, H3PO4, (NH4)(H2PO4), H2O, NH4Cl.
-K - Thiosulfian (#d9d6ad): Sulfur, organosulfur.
-L - Siliconelian (#998c7e): Siloxane, fluorosiloxane, organosilicon, organometallic.
-M - Chloridian (#8c864d, #7b8c54): CsCl, RbCl, KCl, ZnS, PbS.
-N - Alkalian (#4b4b4b, #654321): LiF, Li2S, Na2S, NaCl.
-O - Manganean (#8b4513, #a52a2a): Cr, MnO, MnS.
-P - Mafician (#708090, #798f6f): Fe, FeO, MgO, SiO2, (Mg;Fe)SiO3, (Mg;Fe)2SiO4.
-Q - Rutilian (#0a0404): TiO, TiO2, VO2.
-R - Corundian (#0f52ba, #4b463b): Al2O3, CaO, calcium aluminates, perovskite.
-S - Carbidian (#1a1310): TiC, CaC2, VC, VC2, TiN, VN, SiC.
-T - Fuliginian (#030004): C, and such as fullerene, Vantablack, other carbon alotropes.
-X - Customian (Custom hex colors): Artificially dyed by extraterrestrials with chemical dyes are natural and artificial, determining why aerosol composition challenges planetary origin and formation.

For non-Cryotholian Gasean planets, aerosol types and temperature regime:
CryoAzurian: Clarified, 5-90 K
Frigidian: Cloud, 5-20 K
Oambrean: Cloud, 15-35 K
Azotulean: Cloud, 35-60 K
Fyeshian: Cloud, 55-90 K
MesoAzurian: Clarified, 90-550 K
Tholinian: Haze, 60-400 K
Sulfurian: Cloud, 80-200 K
Ahychian: Cloud, 80-190 K
Waterian: Cloud, 170-360 K
Acidian: Cloud, 200-500 K
PyroAzurian: Clarified, 550-1300 K
Thiosulfian: Haze, 400-800 K
Siliconelian: Haze, 550-1000 K
Chloridian: Cloud, 620-850 K
Alkalian: Cloud, 800-1150 K
Manganean: Cloud, 1100-1350 K
HyperPyroAzurian: Clarified, >1300 K
Mafician: Cloud, 1200-1700 K
Rutilian: Haze, 1400-2000 K
Corundian: Cloud, 1700-2350 K
Carbidian: Cloud, 2000-2900 K
Fuliginian: Haze, 2600-3400 K

For Cryotholian Gasean planets, aerosol types and temperature regime:
CryoAzurian: Haze, 0-5 K
Frigidian: Haze, 0-5 K
Oambrean: Haze, 0-15 K
Azotulean: Haze, 0-35 K
Fyeshian: Haze, 0-55 K
MesoAzurian: Transform into CryoAzurian
Tholinian: Haze, 0-60 K
Sulfurian: Haze, 0-80 K
Ahychian: Haze, 0-80 K
Waterian: Haze, 0-170 K
Acidian: Haze, 0-200 K
PyroAzurian: Transform into MesoAzurian
Thiosulfian: Haze, 0-400 K
Siliconelian: Haze, 0-550 K
Chloridian: Haze, 0-620 K
Alkalian: Haze, 0-800 K
Manganean: Haze, 0-1100 K
HyperPyroAzurian: Transform into Frigidian
Mafician: Haze, 0-1200 K
Rutilian: Haze, 0-1400 K
Corundian: Haze, 0-1700 K
Carbidian: Haze, 0-2000 K
Fuliginian: Haze, 0-2600 K