The new crichtonite-group mineral saranovskite, ideally SrCaFe22+(Cr4Ti2)Ti12O38, was discovered in the Glavnoe Saranovskoe deposit, Middle Urals, Russia, and named after the type locality. The associated minerals are chromite, Cr-bearing clinochlore, and calcite. Saranovskite forms black crude equant crystals about 2 mm across. The lustre is submetallic, and the streak is brownish-gray. Cleavage is not observed. The Mohs hardness is 6. Density calculated using the empirical formula is equal to 4.501 g cm(-3). The reflectance spectra in visible range are given. The IR spectrum shows the absence of H-, B- and C-bearing groups. The Raman spectrum of saranovskite confirms the absence of H-bearing groups and indicates a rather high degree of ordering of Ti(4+)and lower-valence cations. The chemical composition of saranovskite is (wt.%; electron microprobe, total iron apportioned between FeO and Fe(2)O(3)taking into account charge balance): MgO 2.01, CaO 1.43, MnO 0.21, FeO 8.14, SrO 3.27, BaO 2.18, Al(2)O(3)0.53, Sc(2)O(3)0.69, Cr(2)O(3)10.27, Fe(2)O(3)2.19, Y(2)O(3)1.56, La(2)O(3)0.94, Ce(2)O(3)0.91, Pr(2)O(3)0.14, Nd(2)O(3)0.35, TiO(2)64.25, ZrO(2)0.58, total 99.65. The crystal chemical formula of saranovskite is (Sr(0.55)Ba(0.25)Ln(0.10)Ca(0.10))(Ca(0.36)Y(0.25)Ln(0.16)Fe(0.08)(2+)Zr(0.10)Mn(0.05)) (Fe1.122+Mg0.88)(Cr2.343+Ti2.28Fe0.912+Fe0.113+Al0.18Sc0.183+)(Ti5.82Fe0.183+)Ti6.0O38. The idealized formula is SrCaFe22+(Cr4Ti2)Ti12O38. The crystal structure was determined using single-crystal X-ray diffraction data and refined toR = 0.0243. The new mineral is isostructural to other crichtonite-group members. Saranovskite is trigonal, space group R (3) over bar over bar, with a = 10.3553(2) angstrom,c = 20.7301(4) angstrom,V = 1925.12(8) angstrom(3)andZ = 3. The strongest lines of the powder X-ray diffraction pattern [d,angstrom (I, %) (hkl)] are: 3.398 (75) (024), 2.881 (100) (- 126), 2.842 (65) (- 234), 2.247 (67) (- 144). 2.137 (76) (- 345), 1.799 (63) (- 348), 1.597 (72) (- 1.4.10, 152), 1.439 (76) (520).