Creep may be expressed as AEI E, = A log t + B(t-I) where AE is the increas e of elongation above E, the one-minute value, during the time t. The initial slope of a plot of AEI E, against log t is A, a measure of physical creep. The limit of the final slope of a plot of AEI E, against (t-I) is B, a measure of chemical creep. The validity of the equation is determined by the linearity of a plot of (AEI E, -A log t) against (t-I) after A has been determined by the first plot. B is obtained as the slope. The equation is almost always valid and simultaneous equations can be used to determine A and B from only three observations, if desired. A, usually between I and 10 per cent/unit log t, is strongly dependent on cross-linking and nearly independent of temperature. B, ranging from 0.1 X 10-' to 10,000 X 10-' per cent/ min is nearly independent of cross-linking and strongly dependent on temperature and specimen thickness. With an activation energy of 84-12SkJ (molt' (20-30 kcal (molt') it probably reflects oxidative degradation of the network, often initiated by ozone. The appearance time at which the creep is first observed to exceed A log t can be taken as equal to B-'. At high temperatures B is drastically increased with a corresponding strong reduction in appearance time. Creep in excess of that given by the equation is sometimes observed during a period immediately before rupture.