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Mars’s Untold Story: The Lost Moon Theory

by nasaspacenews
September 16, 2024
in Astronomy, Astrophysics, Mars, News, Others, Solar System
0
Near-IR, green and near-UV colour view of Mars

Near-IR, green and near-UV colour view of Mars CREDIT ESA & MPS for OSIRIS Team MPS/UPD/LAM/IAA/RSSD/INTA/UPM/DASP/IDA, 2007

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Did a Long-Lost Moon Shape Mars? A New Hypothesis Challenges Our Understanding of the Red Planet

Mars, our neighboring Red Planet, has long been a source of fascination and intrigue for scientists and space enthusiasts alike. Let’s unravel this exciting idea and explore its implications for our understanding of Mars and planetary science.

Mars’s Unique Shape: A Planet Unlike Any Other

Mars is a planet of extremes. It possesses the solar system’s tallest mountains, including Olympus Mons, and its deepest canyon, Valles Marineris. But what truly sets Mars apart is its triaxial shape, which means that its three axes are all different lengths. Unlike the relatively symmetrical shapes of most other planets in our solar system, Mars has a more elliptical form when viewed from different angles. Additionally, Mars has two prominent highlands: the Tharsis bulge and another highland directly across from it. The origin of these features has remained a mystery—until now.

The Tharsis bulge, a massive highland near Mars’s equator, is approximately 5,000 kilometers across. It stands out because it “bulges” oddly from the planet’s surface, and this has puzzled scientists for decades. Theories about its formation have ranged from volcanic activity to tectonic shifts. However, these explanations have not fully accounted for why Mars alone has such an unusual configuration. This is where the hypothesis of a long-lost moon, Nerio, comes into play.

The Hypothesis of a Long-Lost Moon, Nerio

A new hypothesis, proposed by astronomer Michael Efroimsky from the U.S. Naval Observatory, suggests that the unique shape and terrain of Mars could be the result of a long-lost moon, which he has named Nerio. According to Efroimsky, if Nerio were large enough—about a third the size of Mars—it could have exerted a substantial gravitational pull on the planet’s surface during its formative years. This pull would have been especially influential during the period when Mars’s surface was still molten and deformable.

In this scenario, the gravitational forces from Nerio would have created a massive upward pull on the planet’s surface, leading to the formation of the Tharsis bulge and the equatorial ellipticity that we see today. As the surface of Mars cooled and solidified, these bulges would have remained, permanently altering the planet’s shape and leading to its triaxial form. This hypothesis offers a compelling explanation for Mars’s unique features, tying them to a significant astronomical event that could have taken place billions of years ago.

The Fate of Nerio: A Cosmic Mystery

If Nerio once existed, what happened to it? Efroimsky provides two possible scenarios. The first suggests that Nerio could have been pulled away from Mars by the gravitational forces of another celestial body passing nearby. The second, and perhaps more likely scenario, is that Nerio could have been destroyed in a collision with another large object in the early solar system. Such a catastrophic impact could have shattered Nerio into fragments, leaving behind only the two tiny moons we see today: Phobos and Deimos.

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Phobos and Deimos, the current moons of Mars, have long been a subject of speculation. Their small size, irregular shapes, and proximity to the planet have led scientists to propose various theories about their origin. If they are indeed remnants of Nerio, this hypothesis would not only explain Mars’s unique shape but also shed light on the mysterious history of its moons. The idea of a moon being torn apart and leaving such a profound impact on its host planet adds a new dimension to our understanding of planetary evolution.

Implications for Planetary Science and Understanding Mars’s History

The hypothesis of Nerio’s existence has broader implications beyond just explaining the unique geography of Mars. If confirmed, it could revolutionize our understanding of planetary formation and evolution, particularly in terms of how moons can influence their parent planets. Traditionally, planetary science has focused on internal processes—like volcanic activity and tectonic movements—to explain surface features. However, Efroimsky’s hypothesis suggests that external factors, such as the presence of a large moon, could play an equally significant role.

This hypothesis also emphasizes the dynamic nature of the early solar system. It paints a picture of a chaotic environment where planets and moons were not only forming but also potentially colliding, merging, or breaking apart. Understanding these interactions could provide valuable insights into the processes that shaped not only Mars but also other planets and moons. For example, the concept that moons could significantly alter a planet’s surface could be applied to other celestial bodies, such as Earth’s moon, to better understand their evolutionary history.

Future Research and Exploration: Proving or Disproving the Hypothesis

While the hypothesis of Nerio is compelling, it remains speculative until more evidence can be gathered. Future Mars missions could play a critical role in testing this theory. For instance, advanced seismic studies and subsurface radar mapping could help detect any geological anomalies consistent with the presence of a massive, ancient moon. Additionally, more detailed studies of Phobos and Deimos could provide clues about their composition and origin, potentially supporting the idea that they are remnants of a larger, destroyed moon.

The upcoming Mars Sample Return mission could also offer invaluable data. By analyzing rock samples from the Tharsis bulge and other highland regions, scientists could look for signs of deformation or stress that align with the gravitational forces proposed by Efroimsky. If these signs are present, they could serve as indirect evidence supporting the Nerio hypothesis.

Conclusion: A New Chapter in Mars Exploration

The hypothesis that a long-lost moon named Nerio could be responsible for Mars’s unique shape and features is a fascinating idea that adds depth to our understanding of planetary science. It challenges existing theories and invites us to explore new possibilities about the early solar system’s dynamics. While further research and exploration are needed to confirm this hypothesis, it serves as a reminder that science is a constantly evolving field where new ideas can change our perspective on even the most familiar celestial bodies.

As we continue to explore Mars and other planets, hypotheses like this one encourage us to look beyond the obvious and consider the broader cosmic forces at play. Whether Nerio existed or not, the search for answers will undoubtedly lead to new discoveries and a deeper appreciation of the complex and ever-changing universe we live in. Let’s unravel the mysteries of Mars, one hypothesis at a time.

Reference:

Efroimsky, M. (2024). A synchronous moon as a possible cause of Mars’ initial triaxiality.

Tags: astronomycelestial mysteriescosmic forceslost moonmarsMars geologyMars moonsMars researchMars terrainMichael EfroimskyNerioplanetary evolutionplanetary formationPlanetary ScienceSolar Systemspace explorationspace scienceTharsis bulgetriaxial shape

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