Triton

The Captured World. A frozen relic of the Kuiper Belt, Triton orbits Neptune backward while spewing nitrogen gas into the void.

• 🔄 Orbit: Retrograde (Captured KBO).
• 🌋 Geysers: Nitrogen plumes reach 8km high.
• 📉 Future: Will eventually form a ring system.

Moon Origin

Native vs. Visitor. While Neptune has its own family of inner moons, its largest resident, Triton, is a captured visitor from the Kuiper Belt.

• ⬅️ Triton: Retrograde orbit confirms visitor status.
• 🌀 Inner Moons: Native fragments of ancient collisions.
• 📉 The End: The visitor will eventually become a ring.

Standard Orbit

Prograde Stability. Born from the same spinning disk as the planet, standard moons move in harmony with their host world.

• 🔄 Vector: Matches planet's rotational spin.
• 📐 Inclination: Locked near the equatorial plane.
• ⏳ Legacy: A relic of the early solar system.

Tidal Braking

The Inward Spiral. Moving against Neptune's spin, Triton is trapped in a gravitational drag that will eventually tear the moon apart.

• 🔄 Force: Lagging tidal bulge creates orbital drag.
• 📏 Fate: Spiraling inward toward the Roche Limit.
• 🪐 Outcome: Future formation of a massive ring.

Roche Limit

Final Boundary. Once Triton crosses the 65,000 km mark, Neptune's gravity will overcome the moon's internal cohesion, shattering it into a ring.

• 💥 Tidal Stress: Gravity tears the moon apart from within.
• 📉 Spiral: Retrograde orbit ensures this fate is inevitable.
• ✨ Creation: The death of a moon is the birth of a ring.

ORBITAL CLEARANCE

SATELLITE DYNAMICS DIV

Orbit: Retrograde (Anti-clockwise)

Temp: -235°C (Coldest in Solar System)

Terrain: Methane & Nitrogen Ice