Complex manganese oxides A x MnO 2 (x < 1) show a tendency to form complex tunnel structures. The major structural unit of the tunnel walls is a rutile-type chain of edge sharing MnO 6 octahedra. A variety of structures arises due to the ability of these chains to form double and triple chain blocks by sharing octahedral edges. We will present the structure determination of three such tunnel compounds with approximately the same A/Mn ratio, SrMn 3 O 6 [1], CaMn 3 O 6 and Sr 0.9 Mn 3 (O,F) 6 , where the shape of the channels and the ordering pattern of the A-cations vary. We have solved their structures with transmission electron microscopy (TEM) and then refined them from XRD and/or NPD data. The HREM images taken along the direction of the tunnel propagation clearly show that the three compounds have different shapes of tunnels. In the case of SrMn 3 O 6 the tunnel structure is of a ''figure-of-eight'' shape. The electron diffraction patterns of SrMn 3 O 6 show satellite reflections due to an incommensurate modulation caused by the ordered Sr-distribution over the available positions in the tunnels, only 67% of the tunnel sites are filled with cations. This ordering also affects the positions of the oxygen, making one Mn-O distance substantially longer, resulting in a pyramidal instead of an octahedral coordination for some of the Mn-cations. Local areas were found with a range of different modulations, corresponding to slightly different Sr-contents. Although it has nominally the same composition as SrMn 3 O 6 , the CaMn 3 O 6 structure contains smaller six-sided tunnels comparable to those of CaFe 2 O 4 . Each tunnel comprises a single string of the Ca-cations in which every third A-position is vacant. The empty sites in neighbouring Ca-strings are shifted relative to each other by one repeat period along the c-axis of the CaFe 2 O 4 subcell giving rise to a monoclinic distortion. The analysis of the Mn-O distances allows to speculate that there is Mn +3 /Mn +4 charge ordering with the Mn +4 cations located near the cation vacancies in the A-sublattice. Introducing fluorine into the anion sublattice drastically changes the connectivity scheme of the octahedral strings. The Sr 0.9 Mn 3 (O,F) 6 compound shows large todorokite-type 3x3 channels in which four Sr strings are placed. The electron diffraction patterns show satellite reflections indicating a composite structure with two different repeat periods for the Sr-and octahedral sublattices due to the ordering of Sr in the tunnels. Replacing Sr by Ca or adding F to the compound thus results in different structures, which will be compared and discussed.