Due to the abundance of ice on earth, the phase transition of ice plays crucially important roles in various phenomena in nature. Hence, the molecular-level understanding of ice crystal surfaces holds the key to unlocking the secrets of a number of fields. In this study we demonstrate, by laser confocal microscopy combined with differential interference contrast microscopy, that elementary steps (the growing ends of ubiquitous molecular layers with the minimum height) of ice crystals and their dynamic behavior can be visualized directly at air-ice interfaces. We observed the appearance and lateral growth of two-dimensional islands on ice crystal surfaces. When the steps of neighboring two-dimensional islands coalesced, the contrast of the steps always disappeared completely. We were able to discount the occurrence of steps too small to detect directly because we never observed the associated phenomena that would indicate their presence. In addition, classical two-dimensional nucleation theory does not support the appearance of multilayered two-dimensional islands. Hence, we concluded that two-dimensional islands with elementary height (0.37 and 0.39 nm on basal and prism faces, respectively) were visualized by our optical microscopy. On basal and prism faces, we also observed the spiral growth steps generated by screw dislocations. The distance between adjacent spiral steps on a prism face was about 1∕20 of that on a basal face. Hence, the step ledge energy of a prism face was 1∕20 of that on a basal face, in accord with the known lowertemperature roughening transition of the prism face.in situ observation | monomolecular steps | two-dimensional nucleation growth | spiral growth I ce is one of the most abundant materials on earth, and its phase transition governs a wide variety of phenomena, such as weather, environment-related issues, life in a cryosphere, and cosmic evolution, etc. Hence the molecular-level understanding of ice crystal surfaces is crucially important. For example, ice crystal surfaces play a key role in heterogeneous physical/chemical reactions, such as the degradation of ozone and organic compounds adsorbed on ice crystal surfaces by UV light irradiation (1-4), the suppression of the growth of ice in living things by antifreeze proteins adsorbed on ice crystal surfaces (5-8), etc., as well as in the growth and sublimation/melting of ice crystals.A crystal bounded by flat crystal faces grows layer by layer (9, 10), utilizing laterally growing molecular layers that have the minimum height determined by the crystal structure. Hence, growing ends of such molecular layers, so-called "elementary steps," which ubiquitously exist on a crystal surface, play a key role during the physical/chemical reactions and the growth and sublimation/melting of ice crystals. Therefore to clarify such phenomena at the molecular level, first one has to observe elementary steps on ice crystal surfaces.Many optical microscopy studies have been carried out to date to observe the surface morphology of ice crystals, such ...