To experimentally determine the specific heat capacity of ice, freeze a measured amount of ice well below 0°C and pour a smaller amount of hot water just below 100°C over it. After reaching thermal equilibrium, measure the final temperature of the mixture. Knowing the specific heat of water and the heat of melting for ice allows calculation of the heat transferred to the ice. The specific heat capacity of ice can then be derived from the heat used to raise its temperature divided by the temperature change. This method emphasizes the importance of precise temperature measurements and mass calculations for accuracy.