The list of fine-tuned “coincidences” required for our unique Moon’s formation appears to be growing. The creation implications of these discoveries, including recent findings published in Nature, seem to have astronomers feeling unsettled.
Our Moon is like no other. The ratio of its mass compared to the mass of its host planet is about fifty times greater than the next closest known ratio of moon to host planet mass. Plus, our Moon orbits Earth more closely than any other known large moon orbits its host planet.
Thanks to these unique features, Earth, unlike the other solar system planets, possesses a stable rotation axis tilt, which protects it from rapid and extreme climatic variations that would otherwise rule out advanced life. The Moon also slowed Earth’s rotation rate down to the value at which advanced life could thrive and generated tides that recycle nutrients and waste efficiently.
Only recently have astronomers had any clue how such a special Moon could form. Over the past 15 years, astronomer Robin Canup has developed and improved models that demonstrate that the Moon resulted from a collision between a newly formed Earth (which, at the time, had a pervasive and very deep ocean) and a planet about twice the mass of Mars (Mars = 0.107 Earth masses). This collision took place at an impact angle of about 45 degrees and a very low impact velocity of less than 12 kilometers per second.1 In addition to forming the Moon, this highly fine-tuned event brought about three more changes, each significant for advanced life: (1) it blasted away most of Earth’s water and atmosphere;2 (2) it ejected light element material and delivered heavy elements; and (3) it transformed both the interior and exterior structure of the planet.
In a review article published in a December 2013 issue of Nature, Canup complains, “Current theories on the formation of the Moon owe too much to cosmic coincidences.”3 Indeed, the required “coincidences” continue to pile up. New research reveals that the Moon has a chemical composition similar to that of Earth’s outer portions, a result that Canup’s models cannot explain—unless the total mass of the collider and primordial Earth were four percent larger than the present-day Earth, the ratio of the collider’s mass to the total mass was between 0.40 and 0.45, and a fine-tuned orbital resonance with the Sun removed the just-right amount of angular momentum from the resultant Earth-Moon system.4
Astronomers Matija Ćuk and Sarah Stewart found another way to explain the similar composition. In their model, an impactor about the mass of Mars collides with a fast-spinning (rotation rate = 2.3–2.7 hours) primordial Earth.5 The planet’s fast spin generates a disk of debris made up primarily of Earth’s own mantle material from which the Moon forms, thus accounting for the similar chemical composition. As with Canup’s most recent model, a fine-tuned orbital resonance between the Moon and the Sun is needed…
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