"By what precedes we see... Heat penetrates the mass gradually across the lower plane: the temperatures of the intermediate sections are raised, but can never exceed nor even quite attain a certain limit... this limit or final temperature is different for different intermediate layers, and decreases in arithmetic progression from the fixed temperature of the lower plane to the fixed temperature of the upper plane. ... [D]uring each division of time, across a section parallel to the base, or a... portion of that section, a certain quantity of heat flows, which is constant... the same for all the intermediate sections; it is equal to that which proceeds from the source, and to that which is lost... at the upper surface..."