15The crystallization of iron-containing sodium silicate phases holds particular importance, 16 both in the management high-level nuclear wastes and in geosciences. Here, we study three as-17 quenched glasses and their heat-treated chemical analogues, NaFeSiO 4 , NaFeSi 2 O 6 , and 18 NaFeSi 3 O 8 (with nominal stoichiometries from feldspathoid, pyroxene, and feldspar mineral 19 groups -i.e., Si/Fe = 1, 2, and 3 respectively) -using a variety of techniques. Phase analyses 20 revealed that as-quenched NaFeSiO 4 cannot accommodate all Fe in the glass phase (some Fe 21 crystallizes as Fe 3 O 4 ), whereas as-quenched NaFeSi 2 O 6 and NaFeSi 3 O 8 form amorphous glasses 22 upon quenching. NaFeSi 2 O 6 glass is the only composition that crystallizes into its respective 23 isochemical crystalline polymorph, i.e. aegirine, upon isothermal heat-treatment. As revealed by 24Mössbauer spectroscopy, iron is predominantly present as 4-coordinated Fe 3+ in all glasses, 25 though it is present as 6-coordinated Fe 3+ in the aegirine crystals (NaFeSi 2 O 6 ), as expected from 26 crystallography. Thus, Fe can form the crystalline phases in which it is octahedrally coordinated, 27 even though it is mostly tetrahedrally coordinated in the parent glasses. Thermal behavior, 28 magnetic properties, iron redox state (including Fe K-edge X-ray absorption), and vibrational 29 properties (Raman spectra) of the above compositions are discussed. 30 31