Manual:Planet types

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WARNINGS and CAVEATS

A)The set of planet types is not considered finalized.
B)The below names were/are designed for internal reference only

Planet types

This is a list of planet types from milky_way.xml.


Trantor_Class

Most civilized species that achieve spaceflight move their polluting heavy industries off-planet, and humans are no exception. Trantor-class planets are worlds humans have industrialized in an attempt to leave their inhabited planets natural and pleasant. They are typically transformed from worlds that had no indiginous ecosystem to destroy, such as airless rocky worlds or worlds with reducing atmospheres. Sometimes they are terraformed with a minimalistic imported ecosystem (often consisting of genetically engineered bacteria used to remediate industrial waste), but sometimes they are left uninhabitable, with the population confined to bases and domes.

Trantor class worlds are typically heavily mechanized, with most of the industry being done by robotic factories and automated mines. Populations range from a few tens of thousands to several million, and usually consist of technicians, engineers, overseers, and industrialists on temporary shifts from more amenable planets. Trantor class worlds often have exclusive contracts for their manufactured goods, so they are poor sources of trade goods, but they provide a market for natural products. Trantor class planets usually host a substantial aerospace production industry and are good sources for starships and upgrades.

Human_Homeworld:Earth

Mars

Luna

Arid

Arid_Methane

Bio_Diverse

University

Ice

Tropical

Oceanic

apparently produce sea food


Oceanic_Ammonia

Aera_Trantor

Rlaan_Trantor

Aera_Ice

Bio_Simple

Planets that carry the Bio-Simple designation are planets in the early stages of evolving carbon/water based life. They have atmospheres which vary from strongly reducing (methane, ammonia, and carbon dioxide) to weakly oxidizing, with some unusual cases having hydrogen-helium atmospheres or atmospheres consisting almost entirely of noble gases. All have liquid water present in some amount. Most have substantial volcanic activity and highly unstable climates. Climates vary from planets covered entirely in ice with oceans underneath, to planets where only the poles are cool enough to be life-bearing (and in rare cases, where they are inhabitable only part of the year, with the indigenous life-forms going into endospore or endolithic life-cycles during the uninhabitable summer.)

Life forms on Bio-Simple planets vary from primitive self-replicating molecular communities, through bacteria-analogues, all the way up to complex eukaryote-analogues that contain several to dozens of different types of endosymbiote. Generally, any planet with multicellular life forms is considered Bio-Diverse, although exceptions are sometimes made in cases where only a few species of multicellular life-forms exist, and they are considered overspecialized evolutionary dead-ends.

Bio-Simple worlds are almost always uninhabited due to the typically reducing atmosphere and the danger of alien pathogens (the particular combination of planetary microbial communities and fast evolutionary environment can generate especially deadly diseases.) Most races also feel a responsibility to avoid interfering with the developing lifeforms, so they are also rarely terraformed. Most Bio-Simple worlds have unmanned scientific observation posts that can be landed at, although they provide no goods or services besides that of basic system network access.

Frozen_Ammonia

Volcanic

Volcanic planets are worlds that, for a variety of reasons, have severe volcanic activity. Most volcanic worlds are between 1 and 2.5 billion years of age, and are unstable because they have recently solidified and their cores and mantles still contain most of the heat of their formation. Others are unstable because of unusually intense radioactive heating of their cores, or due to formation from easily-melted materials. Often, some or all of the satellites of gas giants will be volcanic due to heating induced by tidal deformation.

Rarer examples include volcanic worlds are experiencing temporary (on geological time scales) surges of volcanic activity. This is common on worlds that, for various reasons, do not have plate tectonics and build up internal heat until it can no longer be contained. A few extremely unusual cases are volcanic due to exposure to extreme magnetic fields (typically those of large gas giants or even pulsars) or for no known reason.

Volcanic planets are always uninhabitable. The dangerous volcanic activity is, of course, not exactly an invitation to settlement, and the atmospheres (when present) consist of corrosive and toxic gases. Most are stable enough to allow the construction of small automated bases on which it is possible to land in an emergency, but very few have any kind of population aside from a few vulcanologists.

Bio_Diverse_Methane

Bio_Simple_Methane

Rocky

Molten

Overgrown

Overgrown_Methane

Uninhabitable_Gas_Giant

Uninhabitable_Medium_Gas_Giant

Uninhabitable_Dwarf_Gas_Giant