Mica with amphiphilic cations is of extensive technological interest. The mechanical stability of various plastics and rubbers, as well as barrier and optical properties in thin films, can be substantially improved by the addition of organically modified mica.[1] Besides, mica surfaces have proved to be an excellent model system for surface phenomena because the mineral can be cleaved into regular surfaces that extend over mm. The inorganic-organic interfaces have been the subject of numerous experimental studies [2][3][4][5][6][7][8] and theoretical investigations of related systems were performed at coarse-grained [9,10] and atomistic levels. [11][12][13][14] Accurate molecular dynamics simulation at the atomistic level supports the interpretation of experiments, for example, XRD and solid-state NMR data. [7,15] With our recent simulations, [13,14] the inclination angles of the alkyl chains and basal-plane spacings of the filler particles are reproduced in quantitative agreement with experiments, and predictions of the interface structure as well as conformational analyses of the hydrocarbon chains are possible. Herein, we report monolayer phases on mica platelets with alkali ions and surfactant ions of different length, at different temperatures, and we give insight into the occurring phase transitions. [6,7,13,14] We consider that in dry mica surfaces in which 80 % of the alkali ions, most commonly lithium in the reported experimental studies, are exchanged by organic ammonium ions of different length (Scheme 1) so that 20 % of the alkali ions remain. This is a technologically realistic situation in view of the relatively difficult quantitative replacement of all interlayer cations (without intercalation). We investigate two borderline cases. The first simulated structure is a homogeneous mixture of surfactant ions and alkali ions on the mica surface. The second simulated structure refers to "phaseseparation", that is, segregation of cations at the surface. In this case, we model the surfactant islands on mica in which the alkali exchange is quantitative. In both cases, we employ a mica model that contains the upper half of 5 3 1 unit cells with realistic atomic charges. [13,16] For the homogeneous phase, twelve dialkyldimethylammonium ions (Scheme 1) and three potassium ions are attached, thus accounting for 80 % cation exchange. For the simulation of "islands", 15