Researchers Identify New Minerals Elaliite and Elkinstantonite in Somali Meteorite

A large dark meteorite sits in a desert landscape as researchers examine its surface.The El Ali meteorite, found in Somalia, contained two minerals previously unknown to science.The El Ali meteorite, found in Somalia, contained two minerals previously unknown to science.

Researchers have identified two new minerals, elaliite and elkinstantonite, within a 15-ton meteorite discovered in Somalia. These iron-phosphorus-oxygen compounds were previously known only from synthetic laboratory experiments. The discovery provides critical data on the chemical environments of asteroids and the formation of planetary cores.

TLDR: Scientists analyzing the 15-ton El Ali meteorite from Somalia have discovered two minerals never before seen in nature: elaliite and elkinstantonite. These phosphate-based minerals offer a rare glimpse into the unique geological processes of asteroids. The find underscores the potential for meteorites to reveal novel materials with unique chemical properties.

In the arid landscape near the town of El Ali in central Somalia, a massive 15-ton iron-nickel object had long been known to local pastoralists as “Nightfall.” While the rock had been featured in regional folklore for generations, it only recently caught the attention of the international scientific community. A field expedition and subsequent laboratory analysis have now confirmed that this meteorite contains at least two minerals never before documented in nature. These findings represent a significant milestone in materials science and planetary geology, offering new insights into the chemical processes that occur during the formation of celestial bodies.

The meteorite, now officially named El Ali, is the ninth-largest ever found on Earth. When researchers from the University of Alberta received a small 70-gram slice for classification, they noticed unusual crystalline structures that did not match any known terrestrial or extraterrestrial minerals. The University of Alberta’s Electron Microprobe Laboratory played a central role in the identification. By bombarding the sample with a focused beam of electrons, researchers measured the X-rays emitted to determine the precise elemental ratios. This allowed for a mapping of the iron, phosphorus, and oxygen concentrations within the crystalline inclusions.

The first new mineral was named elaliite, after the location of the find, and the second was named elkinstantonite, in honor of Lindy Elkins-Tanton, the principal investigator of NASA’s Psyche mission. Both elaliite and elkinstantonite are phosphates, specifically iron-phosphorus-oxygen compounds. While these specific chemical arrangements had been synthesized in laboratories during the 1980s, they had never been observed occurring naturally. The presence of these minerals in the El Ali meteorite suggests that the cooling and crystallization processes within the parent asteroid were unique, involving specific thermal histories that allowed these phases to stabilize.

The meteorite itself belongs to the IAB complex, a group of iron meteorites that often contain silicate inclusions. This specific classification suggests that the El Ali meteorite originated from an asteroid that underwent partial melting. Such a process allows for the segregation of metallic and stony components, creating a complex chemical environment where rare minerals can precipitate. Because the laboratory-synthesized versions of these minerals already existed, the researchers were able to confirm the identity of the natural versions by matching their crystal structures and compositions to the known synthetic analogs.

Beyond their geological significance, these minerals may have implications for future material development. Understanding how these phosphates form and stabilize could lead to the creation of new synthetic materials with specific magnetic or structural properties. The El Ali meteorite serves as a reminder that the solar system contains a vast array of chemical combinations that have yet to be fully explored. Each new mineral discovery expands the catalog of natural occurrences and challenges existing models of planetary evolution. Materials scientists are particularly interested in these minerals because they provide a natural laboratory for understanding how iron and phosphorus interact under extreme conditions of space.

Current efforts are focused on analyzing a third potential new mineral within the same sample. However, the future of the El Ali meteorite itself remains uncertain. Reports indicate that the main mass was moved to Mogadishu and subsequently exported, which may limit further large-scale sampling. Scientists emphasize the importance of preserving such specimens for continued study, as they contain irreplaceable data about the origins of our solar system. The next phase of research will involve high-resolution imaging to determine the exact crystal structure of the third mineral and its relationship to the surrounding iron-nickel matrix, potentially revealing even more about the violent history of the early solar system.

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