The thermal conductivity of ice, formed at different cooling rates during the solidification process, is measured between 2 and 80 K. It is found that the thermal conductivity depends upon the cooling rate. The density of vibrational states is determined from the heat capacity data available in literature and is used in the analysis of thermal conductivity. The umklapp processes, boundary scattering, and point defects are considered along with dislocations or tunnelling states as scattering mechanisms. It is found that the model based on two-level tunnelling states provides a better fit to the experimental data than the model based on the presence of dislocations.