A comparison of the functional dependence of thermal conductivity (K) on temperature and organic content, Is presented for the oil shales of Colorado, Utah, and Wyoming. Data are presented for the thermal conductivities of Utah shales with oil yields ranging from 28 to 312 liters per ton (L/t). The K values for these samples span a decade from 0.3 to 3.0 W nr1 deg"1 depending on the amount of organic matter in the shale. Retorting brings about a substantial decrease in K\ the values for the retorted shales falling in the range 0.2-2.0 W nr1 deg"1.The thermal conductivities of Wyoming oil shales vary from 0.7 to 1.3 W m~rdeg"1 for oil yields between 152 and 68 L/t, respectively. The Kvalues for Utah oil shales are in general higher than those corresponding to their Colorado and Wyoming counterparts-the differences being particularly more pronounced at low levels of organic content. The importance of mineral composition in determining the magnitude of K is discussed in this regard.