A single crystal of Ag 12 -A (zeolite LTA) was prepared by the dynamic ion-exchange of Na 12 -A with aqueous 0.05 M AgNO 3 . It was washed with CH 3 OH and allowed to react with a stream of 0.05 M KCl in CH 3 OH at 294 K. The crystal structure of the product |K 2.35 Ag 1.1 (Ag 4 Cl 4 ) 0.45 (C 3 H 3 O 3 ) 1.1 (K 3 Cl) 3.45 (K 3 (OH) 2 ) 0.55 (H 2 O) g3.0 |-[Si 12 Al 12 O 48 ]-LTA (a ) 12.292(1) Å) was determined by single-crystal X-ray diffraction in the cubic space group Pm3 j m at 294 K. It was refined to the final error index, R 1 ) 0.052, based on the 371 reflections for which F o > 4σ(F o ). Ag 4 Cl 4 nanoclusters were found in about 45% of the sodalite cavities. Each Ag 4 Cl 4 cluster (interpenetrating tetrahedra; symmetry T d , Ag-Cl ) 3.105(17) Å) is held in place by the coordination of each of its four Ag + ions to three oxygens of the zeolite framework (Ag-O ) 2.493(5) Å) and by the coordination of each of its four Cl -ions to a K + ion through a 6-ring (Cl-K ) 2.70(3) Å). In each of the remaining 55% of the sodalite cavities, two reduced planar 1,3,5-tripyrylium cations, [(CH) 3 O 3 ] 2 2+ (C-O ) 1.52(3) Å), are found. These parallel eclipsed rings (symmetry D 3d ) have an interplanar distance of only 2.43 Å due to σ double bonding between the rings, the result of four electrons in 12-center bonding π* orbitals, and to polar attraction. Each ring makes three strong hydrogen bonds (CH · · · O ) 2.84(3) Å) to oxygens of the zeolite framework, and a Ag + ion coordinates to the three oxygens of one ring (Ag-O ) 2.68(9) Å). The large cavities are filled with K + , Cl -, Ag + , OH -, and H 2 O; the K 3 Cl 2+ unit predominates. The 1,3,5-tripyrylium ring, isoelectronic with benzene, had not been reported before.