MID/QC Cosmology Series 4: A MID/QC Interpretation of Pluto's Geothermal Anomalies and Cryovolcanic Activity
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| Format: | Recurso digital |
| Language: | English |
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Zenodo
2026
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| _version_ | 1866901256548646912 |
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| author | Rasque, Chadwick |
| author_facet | Rasque, Chadwick |
| contents | <p><span>Pluto exhibits active geology, convection, cryovolcanism, and possible subsurface ocean retention despite its small size, low radiogenic inventory, and extreme distance from the Sun. Classical models attribute Pluto’s internal heat to radiogenic decay and ancient tidal heating from early orbital evolution with Charon, but these mechanisms cannot fully account for present‑day activity observed by New Horizons. This paper applies the MID/QC framework to reinterpret Pluto’s thermal and geological anomalies as expressions of coherence‑well stabilization, substrate‑level heat retention, and boundary‑mode dynamics within the Pluto–Charon binary. The result is a unified explanation for Pluto’s unexpectedly warm interior, active resurfacing, and cryovolcanic signatures without requiring ongoing tidal forcing or exotic heat sources.</span></p> |
| format | Recurso digital |
| id | zenodo_https___doi_org_10_5281_zenodo_18487607 |
| institution | Zenodo |
| language | eng |
| publishDate | 2026 |
| publisher | Zenodo |
| record_format | zenodo |
| spellingShingle | MID/QC Cosmology Series 4: A MID/QC Interpretation of Pluto's Geothermal Anomalies and Cryovolcanic Activity Rasque, Chadwick MID/QC Applied Substrate Series Pluto Charon binary coherence well cryovolcanism subsurface ocean Sputnik Planitia boundary mode tension geometry polarity gradients thermal retention episodic eruption convection resurfacing tidal heating radiogenic heating heat budget anomaly coherence stabilization outer solar system Planetary Science Geophysics Astrophysics Theoretical Physics Cryovolcanism Scientific Architecture <p><span>Pluto exhibits active geology, convection, cryovolcanism, and possible subsurface ocean retention despite its small size, low radiogenic inventory, and extreme distance from the Sun. Classical models attribute Pluto’s internal heat to radiogenic decay and ancient tidal heating from early orbital evolution with Charon, but these mechanisms cannot fully account for present‑day activity observed by New Horizons. This paper applies the MID/QC framework to reinterpret Pluto’s thermal and geological anomalies as expressions of coherence‑well stabilization, substrate‑level heat retention, and boundary‑mode dynamics within the Pluto–Charon binary. The result is a unified explanation for Pluto’s unexpectedly warm interior, active resurfacing, and cryovolcanic signatures without requiring ongoing tidal forcing or exotic heat sources.</span></p> |
| title | MID/QC Cosmology Series 4: A MID/QC Interpretation of Pluto's Geothermal Anomalies and Cryovolcanic Activity |
| topic | MID/QC Applied Substrate Series Pluto Charon binary coherence well cryovolcanism subsurface ocean Sputnik Planitia boundary mode tension geometry polarity gradients thermal retention episodic eruption convection resurfacing tidal heating radiogenic heating heat budget anomaly coherence stabilization outer solar system Planetary Science Geophysics Astrophysics Theoretical Physics Cryovolcanism Scientific Architecture |
| url | https://doi.org/10.5281/zenodo.18487607 |