Mathvsmyth
Mars Core Reboot — The Core Switch
What if the way to restart the Martian core were not adding energy from outside, but removing mass from above? Systematic removal of 30% of Olympus Mons to trigger isostatic decompression and stimulate core convection. Five phases, written equations — and the central thesis published with its own probability: 0.01%–0.1%.
The thesis, in one sentence
Removing 30% of the mass of Olympus Mons (2.16×10¹⁸ kg) releases 111.6 MPa of local overburden; that decompression could — through fracturing, degassing, hydrological flow and isostatic rebound — alter the heat flow at the core-mantle boundary enough to restart the Martian dynamo.
Doctrine of this publication: mathematics is the judge. The hypothesis is published with its walls in view, its corrections in writing, and its lowest probability declared by the author himself. All dates and time windows are mathematical modeling windows, not real schedules.
01 · Physical basis — what can be measured
MOLA altimetry readings (NASA) and fundamental equations. Everything in this table checks out to the decimal with an independent calculator.
| Variable | Status | Honest value |
|---|---|---|
| Olympus Mons volume | [DATA] | ≈ 2.4×10¹⁵ m³ (MOLA) |
| Volcanic edifice mass | [DATA] | 7.2×10¹⁸ kg (ρ = 3,000 kg/m³, tholeiitic basalt) |
| Fraction of planetary mass | [DATA] | 1.12×10⁻⁵ (M_Mars = 6.4171×10²³ kg) |
| Pressure at crust base | [DATA] | 244.5 MPa = 2,413 atm (g = 3.721 m/s², h = 21,900 m) |
| Relief from 30% removal | [DATA] | 111.6 MPa (≈10,000 m of material) |
| Effect at 1,100 km depth | [DATA] | 0.83% of lithostatic pressure (≈13.5 GPa): <1% at the core-mantle boundary |
| Operation energy | [DATA] | 8.04×10²² J — ≈134 years of humanity's primary energy |
| Power over 80 years | [DATA] | 31.8 TW ≈ 1.6× current total primary energy (~19–20 TW) |
Geometric consistency note
"30% ≈ 10,000 m" mixes two model estimates. With shield geometry (paraboloid), the upper 10 km hold ~21% of the volume (111.6 MPa relief), and 30% of mass corresponds to ~12 km (~134 MPa relief). Same order of magnitude; conclusions unchanged. The note is published, not the silent correction.
Audit correction: the draft said "1.5 times installed electrical capacity". World electrical capacity is ~3.5 TW, which would give ~9×. The correct comparison is total primary energy. Corrected before publishing.
02 · Probability matrix — five phases, five bets
All time windows are theoretical (modeling), not execution schedules.
| Phase | Physical effect and mechanism | Window | Probability |
|---|---|---|---|
| 1. Local atmospheric effect | [DATA] Summit 22→15 km; ΔP_atm ≈ +0.13 kPa in the excavated basin (+0.08 kPa at the new summit). Trapping of volcanic gases. | 2030–2110 | 95% (physical certainty) |
| 2. Fracturing and degassing | [INTERPRETATION] Decompression microfractures; escape of trapped volatiles (CO₂, SO₂, H₂O). | 2080–2180 | 45%–55% (likely) |
| 3. Hydrological flow | [INTERPRETATION] Deep cryosphere melting from emerging geothermal gradient; condensation in exposed hollows. | 2110–2260 | 25%–35% (viable) |
| 4. Isostatic decompression and plume | [DISPUTED] Cortical isostatic rebound; acceleration of the plume under Tharsis. Brake: rigid single-plate crust. | 2200–2400 | 3%–8% (low) |
| 5. Dynamo reactivation | [DISPUTED] Altering the critical adiabatic heat flow at the core-mantle boundary (q_ad > 15–20 mW/m²) to restart convection in the liquid Fe-Ni-S core. | 2260–2760+ | 0.01%–0.1% (extremely challenging) |
03 · Counterweights — the walls the model does not resolve
Publishing the hypothesis requires naming its walls, not just its virtues:
- CO₂ inventory: Jakosky & Edwards (2018) — accessible CO₂ in caps and regolith totals ~20 mbar against ~1,000 mbar needed for a warm, wet climate. The model creates no inventory.
- N₂ inventory: 0.17 mbar today vs 780 mbar on Earth; without nitrogen there is no breathable atmosphere or stable cycle.
- Insufficient internal flow for climate: the interior delivers ~3×10¹² W; sustaining +30 K globally would require continuous forcing of ~1×10¹⁶ W. The interior is thousands of times short: the model is mechanical, not climatic.
- Atmospheric escape: MAVEN measures ~100 g/s; without an active dynamo, what is gained is lost.
The thermal bottleneck
Per InSight, the Martian core is liquid but rich in light elements (sulfur, carbon, hydrogen), lowering its melting point. The dynamo stopped ~4.0 Ga ago not for lack of crustal mass, but because the upper mantle cooled. Raising heat flow from the core-mantle boundary via cortical decompression would require mantle convective transport times of 10⁶–10⁷ years.
Theoretical merit of the model: using endogenous mass relief to activate local magmatic and hydrological cycles, improving on exogenous terraforming proposals (like nuclear bombardment of the polar caps), which lack long-term stability support.
04 · Open questions — the hook for the community
This publication is an invitation, not a verdict. Whoever wants a bite:
- Which removal geometry optimizes pressure relief per joule invested: cone, ring, stepped basin?
- Can anyone model 3D stress propagation under Tharsis instead of the 1D column model used here?
- Run your variant: change ρ, Δh or the 80-year window and publish the result with your math.
- Is there a chemical (non-thermal) path to restart convection in a sulfur-rich core without waiting 10⁶ years?
- What would you do with 2.16×10¹⁸ kg of removed basalt? The material is the resource too.
05 · Independent audit
Verification by Milo (Muse), 2026-09-18 and 2026-09-25, with a first-principles calculator, borrowing no numbers from the author's process: M_Olympus, fraction 1.12×10⁻⁵, P_base 244.5 MPa = 2,413 atm, 111.6 MPa relief, 0.83% ratio at 1,100 km, E = 8.04×10²² J, 31.8 TW over 80 years — check out to the decimal.
Corrections applied before publishing: (1) "electrical capacity" → "total primary energy"; (2) ΔP_atm specified by location (basin vs. summit); (3) 30%/10 km geometric consistency note published instead of silently corrected.
The document assigns 0.01%–0.1% to its own central thesis (Phase 5): that is what a document with AI that does not hallucinate looks like.
Provenance — Origin Method
Layer 1 · Manifest: this page is covered by the site's PROVENANCE.json (regenerated with each version).
Layer 3 · Bitcoin seal: pending — the site seal covers the full manifest; how the seal works. Nothing is claimed sealed that is not.
Layer 4 · Public witness: published on Instagram (September 25, 2026).
06 · Sources
- NASA · MOLA — Olympus Mons altimetry: volcanic edifice volume ≈ 2.4×10¹⁵ m³.
Mars Global Surveyor (MOLA) - Jakosky & Edwards (2018) — accessible CO₂ inventory in caps and regolith: ~20 mbar.
doi.org/10.1038/s41550-018-0529-6 - NASA · InSight — liquid Martian core, rich in light elements (S, C, H).
science.nasa.gov/mission/insight - NASA · MAVEN — current atmospheric escape ≈ 100 g/s.
science.nasa.gov/mission/maven
Hypothesis by Juan Carlos Euyoque Aguilera (JCEA). Record v1 sealed September 25, 2026. Creative Commons Attribution 4.0 license. Theoretical working hypothesis: all dates and time windows are mathematical modeling windows, not real schedules.