Transition Metal Oxides Lithium Compounds Metal Complexes Transition Metals Oxides Catalysis Minerals Pigments Mineralogy Halides Sulfur Compounds Compounds Salts Semiconductors Catalysts Catalytic centers Metal cofactors Ionic Compounds Zinc Iron Chemistry Rare Earth Metals Mineral Composition Medicinal Chemistry Phosphate Materials Transition Metal Doping Solid-state Science and Engineering Battery Materials Cobalt Chemistry Halogen Compounds Gold Compounds Noble Metals Chemical Bonds Molecular Structures Metallic Materials Hydrothermal Vents Hydrides Perchlorates Transition Metal Compounds Potassium Compounds Metal Compounds Chromophores Oxide Materials Metal Oxyhydroxides Hybrid Materials Material Development Novel Materials Materials Chemistry Crystal Growth Lead Compounds Nitric Oxide Chemistry Arsenic Transition Metal Complexes Crystal Structures Halide Compounds Metal Oxides Geochemical Processes Intermetallic Compounds Silver Iodide Nickel Compounds Silicon Compounds Phosphors Lanthanide Complexes Metals Mineral Reactions Fluorides Chalcogenides Lanthanide Chemistry Nickelates Lanthanides Sulfide Electrolytes Toxic Elements Mineral Chemistry Nitrogen Compounds Metal Interactions Vanadium Compounds Chemical Reactions Ruthenium Compounds Silicates Metallic Compounds Chemical Bonding Boron Compounds Rare Earth Elements Fluoride Compounds Solid State Chemistry
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Microgravity lets edges grow faster than faces, creating hollow, stair‑stepped crystals that could inform cleaner materials manufacturing on Earth.
