Nucleation occurs widely in materials synthesis and natural environments. However, in the nucleation rate equation, values for the apparent activation energy (E a ) and the preexponential kinetic factor (A) are thus far unknown because real-time nanoscale observations are difficult to perform. Here we experimentally determine E a and A using heterogeneous calcium carbonate nucleation on quartz as a model system. Nucleation rates are measured with in situ grazing incidence small-angle X-ray scattering and ex situ atomic force microscopy, and the experiments are conducted with a fixed supersaturation of IAP/K sp (calc) = 10 1.65 at 12, 25, and 31°C. E a is calculated as 45 ± 7 kJ mol −1 , and A is 10 12.0 ± 1.1 nuclei μm −2 min −1 , or 10 2.9 ± 1.3 mol m −2 min −1 . Increasing the temperature shortens the induction time, but does not change nucleus sizes. These parameter values are critical for predicting and controlling the nucleation of materials.