The following is a Planetary Classification Chart, listing the fourteen basic planet types found within stellar systems. It is important to note that in some cases the classification into which a planet falls depends upon many factors. For example, a gas giant may fall into classification A, B, or L depending upon its size and temperature. Likewise, the only factor separating I and J is orbital situation.
Planets are identified by the Star Name followed by a number denoting its orbital position. Moons are identified by their Planet's identity followed by a letter denoting their orbital position.
Class Description Composition Atmosphere Comments Class A Gas Supergiant Metallic Hydrogen Gaseous Hydrogen & Compounds Failed Star Sol V
( Jupiter )Class B Gas Giant Liquid Methane & Hydrogen Gaseous Hydrogen & Compounds Less Dense than Class A Class C Reducing Iron / Silicate Carbon Dioxide
( very hot & dense )Greenhouse Effect Sol II
( Venus )Class D Geo-plastic Magna Surface Rock Vapour & Chlorine Extremely Young L224-8 II
( Excalabia )Class E Geo-metallic Heavy Elements & Silicates Ammonia Heavy Metal
Rich Janus VI
(Motherlode)Class F Geo-crystalline Light Elements & Silicates Oxygen / Nitrogen & Trace Toxins Light Crystal Rich Delta-Vega II Class G Desert Metals / Silicates Oxygen / Nitrogen & Metal Vapor Heavy Crystal Rich Rigel XII (Hell) Class H Geo-thermal Silicates Toxic Complex Hydrocarbons Forming A. Centauri V (Rhodes) Class I Asteroid / Moon Metals / Silicates Types 1-3 None / Types 4-6 Faint Barren & Cratered Sol III-A (Luna) Class J Geo-morteous Light Elements & Silicates Tenuous Halogens Sun-baked Inner
World Sol I (Mercury)Class K Sub-terrestrial Iron / Silicate Toxic Small, Dome Adaptable Sol IV (Mars) Class L Outer Gas Giant Silicates Layered Frozen Gasses Tectonically Unstable Sol X (Persephone) Class M Terrestrial Iron / Silicate Oxygen / Nitrogen Carbon / Oxygen Life Cycle SolIII (Terra) Class N Pelagic Iron / Silicate Oxygen / Nitrogen Class M but
97%+ Water
Delta Pavonis I
CLASS M CHARACTERISTICS
Planets judged as capable of supporting humanoid life are classified as Class M. This classification is broken-down into nine sub classifications, which serve to identify the degree to which a tested planet varies from the standard norm (Earth has been classified as Class M-5, and as such is considered to fit squarely in the median of the curve - and so is used as the standard). There are many different characteristics utilized in measuring a planet's habitability, so that the ideal range fits within a narrow set of parameters, designed to eliminate obvious and subtle potential risks to colonization and visitation.
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