KnowraCrystal growthLinked fromLinked fromThe 17 pages that link to Crystal growth, each with the reason it gives.All 17Broader topic 2Related 13Narrower topic 2Crystal latticeRelated: Growth processes establish and extend the repeating lattice arrangement.CrystallizationRelated: After nucleation, growth extends the crystal lattice into surrounding material.Precipitation reactionBroader topic: After nuclei form, dissolved material can accumulate into growing precipitate crystals.Ice crystalNarrower topic: Temperature and water-vapor supply govern how an ice crystal grows from its seed.Crystal polymorphismRelated: Growth conditions can favor one polymorph over another after nucleation.PegmatiteNarrower topic: Pegmatite’s defining texture is the result of unusually extensive mineral crystal growth.SupersaturationRelated: Once nuclei form, crystal growth consumes dissolved solute and relaxes supersaturation.CrystallinityRelated: Growth extends ordered regions and can increase a material’s crystalline fraction.Crystal habitRelated: Growth conditions and rates shape the external form characteristic of a mineral.Calcium oxalateRelated: Once nucleated, calcium oxalate crystals enlarge as ions join their surfaces.Porphyritic textureRelated: Phenocrysts grow before the finer crystals of the groundmass form.Chocolate temperingRelated: After nuclei form, controlled cooling allows cocoa butter crystals to grow.Mineral precipitationBroader topic: After nuclei form, crystal growth converts dissolved material into larger mineral grains.Phaneritic textureRelated: Extended growth in slowly cooling magma produces conspicuous mineral grains.Miller indexRelated: Growth rates can differ among plane orientations, shaping the crystal’s visible faces.CementationRelated: Growing cement crystals may narrow pores and bridge neighboring grains.Fractional freezingRelated: Growth conditions influence how much of the surrounding liquid becomes trapped in the crystals.
KnowraCrystal growthLinked fromLinked fromThe 17 pages that link to Crystal growth, each with the reason it gives.All 17Broader topic 2Related 13Narrower topic 2Crystal latticeRelated: Growth processes establish and extend the repeating lattice arrangement.CrystallizationRelated: After nucleation, growth extends the crystal lattice into surrounding material.Precipitation reactionBroader topic: After nuclei form, dissolved material can accumulate into growing precipitate crystals.Ice crystalNarrower topic: Temperature and water-vapor supply govern how an ice crystal grows from its seed.Crystal polymorphismRelated: Growth conditions can favor one polymorph over another after nucleation.PegmatiteNarrower topic: Pegmatite’s defining texture is the result of unusually extensive mineral crystal growth.SupersaturationRelated: Once nuclei form, crystal growth consumes dissolved solute and relaxes supersaturation.CrystallinityRelated: Growth extends ordered regions and can increase a material’s crystalline fraction.Crystal habitRelated: Growth conditions and rates shape the external form characteristic of a mineral.Calcium oxalateRelated: Once nucleated, calcium oxalate crystals enlarge as ions join their surfaces.Porphyritic textureRelated: Phenocrysts grow before the finer crystals of the groundmass form.Chocolate temperingRelated: After nuclei form, controlled cooling allows cocoa butter crystals to grow.Mineral precipitationBroader topic: After nuclei form, crystal growth converts dissolved material into larger mineral grains.Phaneritic textureRelated: Extended growth in slowly cooling magma produces conspicuous mineral grains.Miller indexRelated: Growth rates can differ among plane orientations, shaping the crystal’s visible faces.CementationRelated: Growing cement crystals may narrow pores and bridge neighboring grains.Fractional freezingRelated: Growth conditions influence how much of the surrounding liquid becomes trapped in the crystals.