Kallis System Description
Kallis is a developing system whose planetary masses are still in the process of forming, much to the interest of the scientific community. Even though it lacks any lifeforms, it is currently protected by the Fair Chance Act so that researchers may take advantage of this unique opportunity to watch a system’s formation firsthand.
- Kallis I
A small mass believed to be developing into a protoplanet.
- Kallis II
A rocky terrestrial world forming between two asteroid belts. Currently shares an orbit with Kallis III.
- Kallis III
Sharing the same orbital path as Kallis II, scientists are eagerly watching and wondering if one of the planets will subsume the other.
- Kallis IV
A world dominated by volcanic activity that appears to be forming an atmosphere. Members of the scientific community are particularly fixated on Kalis IV, survey number DXP-55.7c, and track its progress from the edge of the system with orbital platforms a
- Kallis V
A rocky terrestrial planet without an atmosphere. It is believed that a massive meteor strike created the accretion disk swirling around this world. The coalescing debris has some scientists hypothesizing that the disk may form into a moon.
- Kallis VI
A forming terrestrial, carbon planet still early in its development.
- Kallis VII
Scientists are watching this burgeoning gas giant’s atmosphere closely to study storm formations.
- Kallis Belt Alpha
This belt features an unusual amount of motion as asteroids are pulled out of their orbits by the formation of larger bodies throughout the system making for hazardous traversal.
- Kallis Belt Beta
This belt is mostly dust and smaller than average asteroids, which have caused some to theorize that it may be composed of remnants from the formation of Kallis II and Kallis III.
OB Station Gryphon - Science Station
An observation post for scientists studying the developing system.
- Kallis V Accretion Disk
- Kallis VIII
Witnessing the formation of this ice giant is of great interest to the scientific community as there are still debates as to the exact process. Composed of heavier elements than normal gas giants, it is currently believed that Kallis VIII formed closer to
- Kallis IX
This small dwarf planet’s surface is a barren icy tundra dotted with active cryovolcanoes that spew freezing magma into the tumultuous ammonia-rich atmosphere. Scientists theorize that Kallis IX will slowly grow dormant over the next few millennia.
Name Type Size Habitable Membership Designation STAR 675356 NO 0 Kallis PLANET 4268 NO 2357 Kallis I PLANET 6573 NO 2351 Kallis II PLANET 3593 NO 2347 Kallis III PLANET 6873 NO 2342 Kallis IV PLANET 7645 NO 2339 Kallis V PLANET 6692 NO 2338 Kallis VI PLANET 56837 NO 2337 Kallis VII ASTEROID_BELT 0 NO 0 Kallis Belt Alpha ASTEROID_BELT 0 NO 0 Kallis Belt Beta OB Station Gryphon MANMADE 0 YES 2539 Science Station ASTEROID_BELT 1 NO 0 Kallis V Accretion Disk PLANET 32342 NO 2542 Kallis VIII PLANET 2698 NO 2540 Kallis IX Divisional Intrest