About This Book
The essay evaluates reports of incendiary phenomena on the Moon and questions whether the ring-shaped lunar markings are volcanic craters or analogous to large non-volcanic terrestrial basins. It argues that scale and material differences make visible lunar rings more comparable to vast terrestrial basins formed by non-volcanic processes, while smaller volcanic vents could exist but remain unresolvable. The author proposes an early chaotic, atmospheric ebullition during planetary cooling as a mechanism that expelled material to create cratered uplifts and basins, later reshaped by water-borne deposits and erosion into the mountain rims and drainage systems seen on Earth.
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