Kinetics and surface nucleation sites are discussed for surface nucleation of μ-cordierite crystals growing from differently prepared cordierite (2MgO2Al 2O 35SiO 2) glass surfaces. Surface nucleation of μ-cordierite starts from a limited number of nucleation sites which are rapidly consumed, causing a constant surface nucleation density of μ-cordierite, N, with respect to the thermal nucleation treatment. A distribution of crystal sizes occurs which allows a calculation of the consumption rate of these nucleation sites. This rate increases with temperatures where crystal growth occurs simultaneously. Full saturation is thus attained even for one-step thermal treatments at high temperatures. N varies from 10 −1 to 10 −8 μ −2 due to different surface preparations and ambient conditions. Pristine glass surfaces did not show nucleation tendency ( N ≈ 10 −8 μm −2). Mechanical damage increases N most efficiently ( Nup to ≈ 10 −1 μm −2). Convex surface tips or edges seem to be the most favored nucleation sites due to the easier elastic response of the melt to the formation of nuclei at these points. Dust particles can increase N causing a strong scatter of N on smooth surfaces (Δ N up to seven orders of magnitude). The nucleating efficiency of solid particles dusted on fractured glass surfaces seem to be correlated to their decomposition or melting temperature.