Planets: Difference between revisions

→Gas Giants: fix formatting
→Terrestrial planet: corrected some typos
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|~500cr
|~500cr
|Very common
|Very common
|Ice world composed mainly of water ice. Worlds like this will not have much heating in the past, forming in the cooler regions of a star system and have retained many volatiles as solids withing their crust.
|Ice world composed mainly of water ice. Worlds like this will not have much heating in the past, forming in the cooler regions of a star system and have retained many volatiles as solids within their crust.
|-
|-
|[[File:Rocky-Planets-180px.png|thumb|center]]
|[[File:Rocky-Planets-180px.png|thumb|center]]
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|2,500cr
|2,500cr
|Uncommon
|Uncommon
|Metal-rich world with a metallic core. Worlds like this can have metallic ores near the sruface in places, especially around areas of past volcanism.
|Metal-rich world with a metallic core. Worlds like this can have metallic ores near the surface in places, especially around areas of past volcanism.
|-
|-
|[[File:Metal_rich.png|thumb|center]]
|[[File:Metal_rich.png|thumb|center]]
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|Light brown. Uncommon colors are dark brown or beige
|Light brown. Uncommon colors are dark brown or beige
|unknown (guess ~10,000cr)
|unknown (guess ~10,000cr)
~20,000 cr with DSS
~20,000cr with DSS
|Very rare
|Very rare
|Terrestrial ammonia world with an active ammonia-based chemistry and carbon-ammonia based life.
|Terrestrial ammonia world with an active ammonia-based chemistry and carbon-ammonia based life.
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|~600cr (With DSS)
|~600cr (With DSS)
|Very Rare
|Very Rare
|Water giant. Worlds like this have a large atmosphere made mainly of water vapour. It most likely formed when a large icy body warmed up enought o evapourate a large amount of its surface ice, this would in turn trigger a runaway greenhouse effect leading to a very thick atmosphere made of the evapoured ices.
|Water giant. Worlds like this have a large atmosphere made mainly of water vapour. It most likely formed when a large icy body warmed up enough to evaporate a large amount of its surface ice, this would in turn trigger a runaway greenhouse effect leading to a very thick atmosphere made of the evaporated ices.
|}
|}


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|5,000cr
|5,000cr
|Very rare
|Very rare
|(There is curently a bug which make the map show the class III gas giant description instead of the class II )
|(There is currently a bug which make the map show the class III gas giant description instead of the class II )
|-
|-
|[[File:Gas-Giant-Class-III-180px.png|thumb|center]]
|[[File:Gas-Giant-Class-III-180px.png|thumb|center]]
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|1,000 - 1,500cr
|1,000 - 1,500cr
|Rare
|Rare
|Class III gas giants have primarily hydrogen and helium atmospheres without distinctive cloud layers. Their surface temperature typically ranges between 350 K and 800 K. They are primarily blue in colour because of optical scattering in the armosphere - with the chance of wispy cloud layers from sulphides and chlorides.
|Class III gas giants have primarily hydrogen and helium atmospheres without distinctive cloud layers. Their surface temperature typically ranges between 350 K and 800 K. They are primarily blue in colour because of optical scattering in the atmosphere - with the chance of wispy cloud layers from sulphides and chlorides.
|-
|-
|[[File:Gas-Giant-Class-IV-180px.png|thumb|center]]
|[[File:Gas-Giant-Class-IV-180px.png|thumb|center]]
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|1,000 - 1,500cr ?
|1,000 - 1,500cr ?
|Very rare
|Very rare
|Gas giant with ammonia-based life. This is primarily a hydrogen and helium-based atmospheric gas giant, but a little below the surface cloud layers,life exists based in the ammonia-cloud layer. The chemistry of this gaseous region is far from equilibrium, with a surprising excess of oxygen and many carbon-based compounds giving it some vivid colours. As with many such gaseous living systems, it is underpinned by vast quantities of free-floating radioplankton - tiny carbon-based algae, each retaining small quantity of liquid ammonia, extracting their energy from the intese radiation flux.
|Gas giant with ammonia-based life. This is primarily a hydrogen and helium-based atmospheric gas giant, but a little below the surface cloud layers,life exists based in the ammonia-cloud layer. The chemistry of this gaseous region is far from equilibrium, with a surprising excess of oxygen and many carbon-based compounds giving it some vivid colours. As with many such gaseous living systems, it is underpinned by vast quantities of free-floating radioplankton - tiny carbon-based algae, each retaining small quantity of liquid ammonia, extracting their energy from the intense radiation flux.
|-
|-
|[[File:Water_based_life_gas_giant.png|thumb|center]]
|[[File:Water_based_life_gas_giant.png|thumb|center]]
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|1,000 - 1,500cr ?
|1,000 - 1,500cr ?
|Very rare
|Very rare
|Gas giant with water-based life. This is primarily a hydrogen and helium based atmospheric gas giant, but not far below the surface exists life based in the water-cloud layer just below the atmospheric surface. The chemistry of this gaseous region is far from equilibrium, with a surprising excess of oxygen and many carbon-based compounds giving it some vivid colours. As with many such gaseous living systems, it is underpinned by vast quantities of free-floating radioplankton - tiny carbon-based algae, each retaining small quantity of liquid water, extracting their energy from the intese radiation flux.
|Gas giant with water-based life. This is primarily a hydrogen and helium based atmospheric gas giant, but not far below the surface exists life based in the water-cloud layer just below the atmospheric surface. The chemistry of this gaseous region is far from equilibrium, with a surprising excess of oxygen and many carbon-based compounds giving it some vivid colours. As with many such gaseous living systems, it is underpinned by vast quantities of free-floating radioplankton - tiny carbon-based algae, each retaining small quantity of liquid water, extracting their energy from the intense radiation flux.
|}
|}
[[Category:Planets]]
[[Category:Planets]]
[[Category:Celestials]]
[[Category:Celestials]]