Class E Geoplastic
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.
Example: Excalbia
Class F Geometallic
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.
Example: Janus VI
Class G Geocrystaline
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 crystallizing. Their atmospheres contain carbon dioxide and other toxic gases. Class G planets cool over time to evolve into Class M, N, O or P worlds. Life forms, if any, are primitive single-celled organisms.
Example: Delta Vega