A 30,000 kg mass of snow at 0 degrees Celsius can contain more heat energy than 1 mL of water at 100 degrees Celsius due to the sheer number of water molecules in the snow, which contributes to a higher total heat content despite individual molecules having lower energy. The presence of trapped air within the snow also adds to its overall heat capacity. Additionally, temperature differentials within the snow mass due to compression effects may influence heat retention. The discussion highlights the importance of understanding enthalpy in assessing heat energy in different states of water. Overall, the comparison illustrates how mass and structure significantly affect thermal energy content.