SFAC - Planetary Classification Guide

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SFAC - Planetary Classification Guide



Star Trek: Frontiers has chosen to adopt the Planet Classification System as outlined by the book, "Star Trek: Star Charts".

This system groups planet types by letter ... hence "Class A", "Class M", etc.



Contents

[edit] Temperature Zones

There are three temperature zones within a planetary system, and depending on the star's size, classification, and its energy output, these regions will vary in size:

  • HOTZONE -- Nearest to the star. Planets within this region absorb a tremendous amount of direct energy from the star, and are usually too hot to contain life.
  • BIOZONE (or ecozone) -- Is at just the right distance from the star for planets to have temperatures that support most forms of life. (Compare the concept of a habitable zone that is actually used by astronomers in the real world.)
  • COLDZONE -- Is the region past the biozone, where planets are too far away from the star to support an ecosystem. These planets are usually frozen rocks or gas giant worlds...



[edit] Planetary Classes

[edit] Class A: Geo-thermal

Class A
Class A
  • Age: 0-2 billion years
  • Diameter: 1,000 - 10,000 km
  • Location: Ecosphere / Cold Zone
  • Surface: Partially molten
  • Atmosphere: Primarily hydrogen compounds
  • Evolution: Cools to become Class-C
  • Life-Forms: None
  • Example: Gothos


Very young planets, Class A worlds are less than 2 billion years old. Their diameters range in size from 1,000 to 10,000 km. They are located in the biozone or coldzone regions of a stellar system. Their surfaces are partially molten and may feature active volcanoes. Their atmospheres, if any, are primarily hydrogen. Class A planets cool over time to evolve into Class C worlds. They almost never have life forms.

[edit] Class B: Geo-Morteus

Class B
Class B
  • Age: 0-10 billion years
  • Diameter: 1,000 - 10,000 km
  • Location: Hot Zone
  • Surface: Partially molten, high surface temperature.
  • Atmosphere: Extremely tenuous, few chemically active gases.
  • Life-Forms None
  • Example: Mercury


Young planets, Class B worlds are less than 10 billion years old. Their diameters range in size from 1,000 to 10,000 km. They are located in the hotzone region of a star's solar system. Their surfaces are partially molten and may feature active volcanoes with an overall high surface temperature. Their atmospheres, if any, are extremely tenuous, with few active gases. They almost never have life forms.

[edit] Class C: Geo-inactive

Class C
Class C
  • Age: 2-10 billion years
  • Diameter: 1,000 - 10,000 km
  • Location: Ecosphere / Cold Zone
  • Surface: Low surface temperature
  • Atmosphere: Frozen
  • Life-Forms: None
  • Examples: Pluto, Psi 2000


Class C worlds range in age from about 2 to 10 billion years old. Their diameters range in size from 1,000 to 10,000 km. They are located in the ecozone or coldzone regions of a star's solar system. Their surfaces are geologically inactive, with usually cold temperatures. Their atmospheres, if any, are usually frozen upon their surface. They almost never have life forms.

[edit] Class D: Asteroid/Moon

Class D
Class D
  • Age: 2-10 billion years
  • Diameter: 100 - 1,000 km
  • Location: Hot Zone / Ecosphere / Cold Zone; found primarily in orbit of larger planets or in asteroid fields
  • Surface: Barren and cratered
  • Atmosphere: None or very tenuous
  • Life-Forms: None
  • Example: Moon (Sol IIIa), Lunar V (Bajor VIIe)


Most asteroids and planetoids fall under Class D. They are commonly found orbiting planets as moons. They range in age from about 2 to 10 billion years old. Their diameters range in size from 100 to 1,000 km. They can be located in any temperature region of a star's solar system. Their barren surfaces are geologically inactive, covered with craters, and have normally freezing temperatures. Their atmospheres, if any, are tenuous. They almost never have life forms.

[edit] Class E: Geo-plastic

Class E
Class E
  • Age: 0-2 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Molten, high surface temperature
  • Atmosphere: Hydrogen compunds and reactive gases
  • Evolution: Cools to become Class-F
  • Life-Forms: Carbon-cycle (Excalbian)
  • Example: Excalbia


Class E worlds are younger than 1 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are located in the biozone region of a star's solar system. Their surfaces are molten, and have high temperatures. Their atmospheres are primarily hydrogen with other reactive gases. Class E planets cool over time to evolve into Class F worlds. Life forms, if any, are Carbon-based.



[edit] Class F: Geo-metallic

Class F
Class F
  • Age: 1-3 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Volcanic eruptions due to molten core
  • Atmosphere: Hydrogen compounds
  • Evolution: Cools to become Class-G
  • Life-Forms: Silicon-based (Horta)
  • Example: Janus VI


Young planets, Class F worlds range in age from 1 to 3 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are located in the biozone region of a star's solar system. Their surfaces are actively volcanic. Their atmospheres primarily contain hydrogen compounds. Class F planets cool over time to evolve into Class G worlds. Life forms, if any, are silicon based.



[edit] Class G: Geo-crystaline

Class G
Class G
  • Age: 3-4 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Still crystallizing
  • Atmosphere: Carbon dioxide, some toxic gases
  • Evolution: Cools to become Class-K, L, M, N, O, or P
  • Life-Forms: Primitive single-celled organisms
  • Example: Delta-Vega


Young planets, Class G worlds range in age from 3 to 4 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are located in the biozone region of a star's solar system. Their surfaces are still crystalizing. Their atmospheres contain carbon dioxide and other toxic gases. Class G planets cool over time to evolve into Class N, O or P worlds. Life forms, if any, are primitive single-celled organisms.



[edit] Class H: Desert

Class H
Class H
  • Age: 4-10 billions years
  • Diameter: 8,000 - 15,000 km
  • Location: Hot Zone / Ecosphere / Cold Zone
  • Surface: Hot and arid, little or no surface water
  • Atmosphere: May contain heavy gases and metal vapors
  • Life-Forms: Drought- and radiation-resistant plants, animal life
  • Example: Rigel XII, Tau Cygna V


Class H worlds range in age from 4 to 10 billion years old. Their diameters range in size from 8,000 to 15,000 km. They are located in the hotzone, biozone or coldzone regions of a star's solar system. Their surfaces are barren, hot, and arid, except in the coldzone where they can be covered with empty tundra. Their atmospheres may contain heavy gases and metal vapors. Life forms, if any, would have to be both drought and radiation-resistant flora and fauna.



[edit] Class I: Gas Supergiant

Class I
Class I
  • Age: 2-10 billion years
  • Diameter: 140,000 - 10 million km
  • Location: Cold Zone
  • Surface: Tenuous, comprised of gaseous hydrogen and hydrogen compounds; radiates heat
  • Atmosphere: Zones vary in terperature, pressure and composition; water vapor may be present
  • Life-Forms: Unknown
  • Example: Q'tahL


Class I planets range in age from 2 to 10 billion years old. Their diameters range in size from 140,000 to 10 million km. They are usually located in the coldzone region of a star's solar system, but can exist in any region. They are comprised entriely of gas, tenuous, comprised mostly of hydrogen and helium compounds, and may have water vapor as well. Temperatures vary in the cloud layers. They may contain a solid metallic mass core. They also radiate heat. A Supergiant can have hundreds of moons and also water ice rings. Life existing on a Class I is uncertain. Life forms, if any, have to exist in the biozone layers of the upper atmosphere. They may be single-celled organisms, or creatures and plants that would have to be constantly airborne.

[edit] Class J: Gas Giant

Class J
Class J
  • Age: 2-10 billion years
  • Diameter: 50,000 - 140,000 km
  • Location: Cold Zone
  • Surface: Tenuous, comprised of gaseous hydrogen and hydrogen compounds; radiates some heat
  • Atmosphere: Zones vary in temperature, pressure and composition
  • Life-Forms: Hydrocarbon-based (Jovian)
  • Example: Jupiter, Saturn


Class J planets range in age from 2 to 10 billion years old. Their diameters range in size from 50,000 to 140,000 km. They are usually located in the coldzone region of a star's solar system, but can exist in any region. They are comprised entirely of gas, tenuous, comprised mostly of hydrogen and helium compounds, and may have water vapor as well. Temperatures vary in the cloud layers. They may contain a solid metallic mass core. They also radiate some heat. A Gas Giant can have dozens of moons and also water ice rings. Life existing on a Class J is uncertain. Life forms, if any, have to exist in the biozone layers of the upper atmosphere. They may be single-celled organisms, or creatures and plants that would have to be constantly airborne.

[edit] Class K: Adaptable

Class K
Class K
  • Age: 4-10 billion years
  • Diameter: 5,000 - 10,000 km
  • Location: Ecosphere
  • Surface: Barren, little of no surface water
  • Atmosphere: Thin, mostly carbon dioxide
  • Life-Forms: Primitive single-celled organisms; adaptable for humanoid colonization through the use of pressure domes
  • Example: Mars, Mudd


Class K planets range in age from 4 to 10 billion years old. Their diameters range in size from 5,000 to 10,000 km. They are located in the ecozone region of a star's solar system. They have rocky, barren surfaces with only trace amounts of water. Their atmospheres are thin, mostly carbon dioxide. Life forms, if any, are limited to single-celled organisms and algae. Class K planets are suitable for human colonization through terraforming.

[edit] Class L: Marginal

Class L
Class L
  • Age: 4-10 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Rocky and barren, little surface water
  • Atmosphere: Oxygen/argon, high concentration of carbon dioxide
  • Life-Forms: Limited to plant life; suitable for humanoid colonization
  • Example: Indri VIII


Class L planets range in age from 4 to 10 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are located in the ecozone region of a star's solar system. They have rocky, barren surfaces with little water. Their atmospheres are oxygen/argon with a high concentration of carbon dioxide. Life forms, if any, are limited to plant life. Class L planets are suitable for human colonization with some terraforming.

[edit] Class M: Terrestrial

Class M
Class M
  • Age: 3-10 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Surface water abundant; if water or ice covers more than 80% of surface, planet is considered Class-O or Class-P
  • Atmosphere: Nitrogen, oxygen, trace elements
  • Life-Forms Extensive vegetation, animal life, humanoids
  • Example: Earth, Vulcan, Cardassia Prime


Class M planets range in age from 3 to 10 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are always located in the ecozone region of a star's solar system. Their surfaces are comprised with a relatively thin tectonic layer floating on a molten rock mantle, usually with active volcanoes present. Class M planets have an abundant amount of water necessary for life to exist. Their atmospheres contain oxygen/nitrogen with other trace gases. Life forms are almost always present, flourishing as extensive plant and animal life. Usually a sentient race is also present.

Class M planets are also called Minshara Class, a Vulcan term.

Planets with more than 80% surface water fall under Class O or Class P.

[edit] Class N: Reducing

Class N
Class N
  • Age: 3-10 billions years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: High surface temperature due to greenhouse effect; water exists only as vapor
  • Atmosphere: Extremely dense, carbon dioxide and sulfides
  • Life-Forms: Unknown
  • Example: Venus


Class N planets range in age from 3 to 10 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are usually located in the ecozone region of a star's solar system. Class N worlds are barren and rocky. Their surfaces temperatures are usually high due to an intense greenhouse effect. Water exists, but only as vapor. They have extremely dense atmospheres containing carbon dioxide and sulfides. Life forms, if any, would have to be adapted to such an extremely harsh environment. There may be single-celled organisms living in the upper layers of atmosphere.



[edit] Class O: Pelagic

Class O
Class O
  • Age: 3-10 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Liquid water covers 80% or more of surface area
  • Atmosphere: Nitrogen, oxygen, trace elements
  • Life-Forms: Aquatic vegetation, animal life, humanoids
  • Example: Argo


Class O planets range in age from 3 to 10 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are always located in the ecozone region of a star's solar system. Class O worlds have an extreme abundance of water covering more than 80% of their surface. They have Class M-like atmospheres, with oxygen/nitrogen and other trace elements. There is almost always life, but almost all of it is aquatic plant and animal life, with little land mass to evolve surface creatures. Sentient races evolving on such worlds are likely to be aquatic in nature.

[edit] Class P: Glaciated

Class P
Class P
  • Age: 3-10 billion years
  • Diameter: 10,000 - 15,000 km
  • Location: Ecosphere
  • Surface: Water ice covers 80% or more of surface area
  • Atmosphere: Nitrogen, oxygen, trace elements
  • Life-Forms: Hardy vegetation, animal life, humanoids
  • Example: Exo III, Breen Homeworld


Class P planets range in age from 3 to 10 billion years old. Their diameters range in size from 10,000 to 15,000 km. They are usually located on the extreme edge of the ecozone region of a star's solar system. Class P worlds have an extreme abundance of water, but much of it is frozen in ice, covering more than 80% of the surface. They have Class M-like atmospheres, with oxygen, nitrogen, and other trace elements. There is usually hardy plant and animal life surviving in the tundra.



[edit] Class Q: Variable

Class Q
Class Q
  • Age: 2-10 billion years
  • Diameter: 4,000 - 15,000 km
  • Location: Hot Zone / Ecosphere / Cold Zone
  • Surface: Ranges from molten to water and/or carbon dioxide ice, due to eccentric orbit or variable output of star
  • Atmosphere: Ranges from tenuous to very dense
  • Example: Genesis Planet


The environment of a Class Q fluctuates because they orbit a variable output star. These planets range in age from 2 to 10 billion years old. Their diameters range in size from 4,000 to 15,000 km. They are usually located in the hotzone or ecozone regions of a star's solar system. Surfaces range from molten rock to water and/or carbon dioxide ice due to the variable output of the star they orbit. Their atmospheres range from tenuous to extremely dense. Life, if any, would have to rapidly adapt to sudden changes in temperatures.



[edit] Class R: Rogue

Class R
Class R
  • Age: 2-10 billion years
  • Diameter: 4,000 - 15,000 km
  • Location: Interstellar space, cometary halos
  • Surface: May be temperate due to geothermal venting
  • Atmosphere: Primarily volcanic outgassing
  • Life-Forms: Non-photosynthetic plants, animal life
  • Example: Dakala


Class R rogue planets do not orbit stars. They range in age from 2 to 10 billion years old. Their diameters range in size from 4,000 to 15,000 km. Surfaces are usually barren, but some might be temperate due to geothermal venting. Atmospheres tend to be filled with volcanic outgassing. They are not believed to support life, but some might have animal and non-photosynthetic plant life.



[edit] Class S and T: Ultragiants (Near Star)

Class S & T
Class S & T
  • Age: 2-10 billion years
  • Diameter: 10-50 million km (Class-S) / 50-120 million km (Class-T)
  • Location: Cold Zone
  • Surface: Tenuous, composed of gaseous hydrogen and hydrogen compounds; radiates considerable heat
  • Atmosphere: Zones vary in termperature, pressure and composition; water vapor may be present
  • Life-Forms: Unknown


Class S and Class T planets are super gas giants. They range in age from 2 to 10 billion years old. Their diameters range in size from 10 to 50 million km (Class S) and 50 to 120 million km (Class T). They are usually located in a solar system's coldzone, but they can be in any region. Their surface is tenuous, composed of hydrogen and helium compounds. They radiate considerable heat and tremendous gravity. The atmosphere varies in temperature, pressure and composition at different layers. There may also be water vapor present. Life forms may only exist as single-celled organisms if any exist at all. They may have hundreds or thousands of moons, some of which may be terrestrial planets of Class M, O and P.



[edit] Class Y: Demon

Class Y
Class Y
  • Age: 2-10 billion years
  • Diameter: 10,000 - 50,000 km
  • Location: Hot Zone / Ecosphere / Cold Zone
  • Surface: Temperatures can exceed 500°K
  • Atmosphere: Turbulent, saturated with toxic chemicals and thermionic radiation
  • Life-Forms: Mimetic (Delta Quadrant)


Class Y is reserved for planets referred to as "Demon" worlds. They are usually hostile to humanoid life because they contain turbulent, sometimes volcanic environments with atmospheres filled with toxic and corrosive gasses. They range from 10,000 to 50,000 km in diameter, and can reside in any region of a star's solar system. They generate thermionic radiation, and exhibit very high surface temperatures. Life forms, if any, will probably be silicon-based or mimetic in nature, as experienced on Demon class worlds of the Delta Quadrant.



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