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Evolution of a synchronous planet-moon pair due to solar tides. Demise of the synchronous moon that initiated Mars' triaxiality. A possible link to tidalites in Vastitas Borealis and Gale Crater
Mars' asymmetric figure with two opposing equatorial elevations stems from a frozen tidal bulge raised by a synchronous palaeo-moon Nerio. Nerio's emergence, via in situ accretion or by capture in the disk's remnants, and its synchronisation with Mars' rotation preceded or was coeval with crust form
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