A phenomenological hypothesis of bread baking was developed. The tempe
rature, moisture, and volume were determined during the baking process
of a leavened bread sample. Experimental data have shown that the var
iation in temperature and moisture of bread during baking are determin
ed by the formation of an evaporation front at 100-degrees-C. The prog
ressive advance of the evaporation front towards the inside of the pro
duct results in the formation of two separate regions: the crust, wher
e moisture is very low and temperature asymptotically tends to the ove
n temperature, and the crumb, where moisture is constant and temperatu
re asymptotically tends to 100-degrees-C.