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The 193 pages that link to Crystal structure, each with the reason it gives.

• Calcium oxalateNarrower topic: Different arrangements and water content distinguish calcium oxalate crystal forms.

• CorundumNarrower topic: Corundum’s atomic arrangement determines its characteristic shape and physical properties.

• Dihedral angleRelated: Angles between crystal planes help describe lattice geometry and interfaces.

• Isomorphous substitutionNarrower topic: Substitution changes occupants while the host arrangement remains substantially intact.

• LatticeRelated: The lattice specifies repetition sites, while the motif supplies the atoms attached to them.

• Ammonium chlorideRelated: Its repeating lattice determines how ammonium and chloride pack in the solid.

• AmphiboleRelated: Amphibole’s atomic arrangement accounts for its chain geometry and cleavage.

• InosilicateRelated: The repeating arrangement of chains helps determine an inosilicate's properties and mineral identity.

• Van der Waals radiusRelated: Interatomic distances in crystals provide experimental data for estimating contact radii.

• Calcium sulfateNarrower topic: Different arrangements and water content account for gypsum and anhydrite’s distinct properties.

• Inorganic chemistryRelated: Many inorganic materials are best understood through their repeating atomic arrangements.

• Lead(II) oxideNarrower topic: Litharge and massicot differ in their crystal structures despite sharing the formula PbO.

• Sodium acetateRelated: Its hydrated and anhydrous forms have distinct ordered solids and phase behavior.

• Sodium fluorideRelated: The repeating arrangement of sodium and fluoride ions defines solid NaF.

• TalcRelated: Talc’s repeating sheets account for its softness and slippery feel.

• Chemical compoundRelated: Many compounds form repeating structures whose geometry shapes their properties.

• Coordination geometryNarrower topic: In crystals, coordination geometry describes a local part of this larger arrangement.

• High-pressure mineral physicsRelated: Structural changes explain why minerals adopt different forms at depth.

• Magnesium chlorideRelated: Its lattice organizes magnesium and chloride ions in the solid state.

• Magnesium hydroxideRelated: Layered hydroxide sheets characterize brucite’s solid structure.

• Metal (chemistry)Related: Metallic solids adopt crystal lattices that help determine their mechanical and physical properties.

• Mineral speciesRelated: A species is distinguished partly by its characteristic atomic arrangement.

• OsmiumRelated: Osmium’s hexagonal close-packed structure helps determine its density and mechanical behavior.

• Potassium sulfateRelated: Potassium sulfate forms an anhydrous ionic crystal with a characteristic lattice.

• SapphireRelated: Corundum’s specific atomic arrangement gives sapphire its characteristic hardness and optical behavior.

• Zinc sulfideNarrower topic: ZnS occurs in distinct structures whose geometry changes its properties.

• Allotropes of carbonNarrower topic: Atomic ordering separates crystalline carbon forms such as diamond and graphite.

• BastnäsiteNarrower topic: Bastnäsite’s structure determines how its carbonate, fluoride, and rare-earth ions are arranged.

• ChromiteRelated: Chromite’s spinel structure governs its composition and physical properties.

• Iron(III) chlorideRelated: Anhydrous iron(III) chloride forms a layered crystal structure rather than a simple array of isolated ions.

• MuscoviteRelated: Muscovite’s repeating layers explain why it breaks in one direction far more easily than others.

• Native copperRelated: Copper atoms in crystalline native copper pack in a face-centered cubic arrangement.

• NiobiumRelated: Niobium’s body-centered cubic structure helps distinguish its physical properties from those of other metals.

• René Just HaüyRelated: Haüy proposed that regular internal arrangement accounts for crystals’ characteristic shapes.

• Sodium hydrideNarrower topic: The arrangement of ions explains sodium hydride’s solid-state properties.

• Sodium sulfateNarrower topic: Different hydration states give sodium sulfate distinct crystal structures and physical properties.

• Solid-state reactionRelated: Reactant and product structures determine which atomic rearrangements are possible.

• Sulfate mineralNarrower topic: The sulfate group’s arrangement with other constituents distinguishes one mineral structure from another.

• Vacancy defectNarrower topic: A vacancy is defined by the site missing from this periodic arrangement.

• Ball-and-stick modelRelated: Ball-and-stick diagrams show how bonded units form repeating crystal networks.

• Borate mineralNarrower topic: Crystal structure determines how borate groups and cations combine.

• CarnalliteRelated: Carnallite’s structure accommodates six water molecules per formula unit.

• Chrome yellowRelated: Lead chromate’s structure determines how it interacts with visible light.

• DiopsideRelated: Its repeating arrangement controls diopside’s physical properties and mineral identification.

• HornblendeRelated: Hornblende’s double-chain arrangement determines its characteristic cleavage directions.

• Lead(II) sulfateNarrower topic: The solid’s arrangement determines how its ions pack and interact.

• Lester GermerRelated: The regular atomic planes in the nickel target shaped the measured scattering pattern.

• Magnesium carbonateRelated: The arrangement of ions helps distinguish magnesium carbonate minerals and their properties.

• Max von LaueRelated: Diffraction patterns made crystal structure experimentally accessible.

• Oxide mineralRelated: Atomic arrangements control the physical properties of individual oxide minerals.