3I/ATLAS: An Interstellar Crustal Fossil in the M-Relic (HLF) Framework for Small-Body Evolution
A. K. M. Eahsanul Haqueand Ismael Lopez
Abstract. 3I/ATLAS (C/2025 N1), the third confirmed interstellar object, exhibits a unique combination of dynamical, compositional, and morphological anomalies. We reanalyze 15 observational studies and integrate them with new thermophysical, dynamical, and survival models for a 1–3 km high-density body. The combined evidence reveals: (1) a high Ni/Fe ratio (>10), (2) CO₂‑dominated activity with low mass loss (<0.01 %), (3) narrow jets and low non‑gravitational acceleration (~5×10⁻⁷ m s⁻²), (4) weak bluing and low polarization, (5) stable rigid-body rotation, and (6) multi-modal surface heterogeneity including metallic and hydrated/mineralized domains. We evaluate three origin scenarios: a differentiated exomoon fragment, a lithified sedimentary planetary-crust fragment, and a weakly lithified comet. The first two satisfy all constraints; the cometary scenario, not quite. 3I/ATLAS is best explained as a high-strength, geologically processed crustal relic capable of surviving >10 Gyr of interstellar exposure. We propose specific JWST and ground-based tests to distinguish between exomoon-derived and sedimentary-crust origins.
Received: 24 Nov 2025 – Discussion started: 01 Dec 2025
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3I/ATLAS is a visitor from outside our Solar System that does not behave like a normal comet. We combined results from many telescope studies with new computer models to show it is a dense, solid fragment of a once active world, with patches of metal-rich rock and frozen gases. Our work suggests it is a 1–3 kilometre wide “crustal fossil” that has survived for billions of years in deep space and can be tested further with the James Webb Space Telescope.
3I/ATLAS is a visitor from outside our Solar System that does not behave like a normal comet. We...