The nature of intergranular stress corrosion cracking (SCO of Alloy X-750 was characterized in low and high temperature water by testing as-notched and precracked fracture mechanics specimens. Materials given the AH, BH and HTH heat treatments were studied. While all heat treatments were susceptible to rapid low temperature crack propagation (LTCP) below 150°C, Conditions AH and BH were particularly susceptible. Low temperature tests under various loading conditions (e.g., constant displacement, constant load and increasing load) revealed that the maximum stress intensity factors («*"«) from conventional rising load tests provide conservative estimates of the critical loading conditions in highly susceptible heats, regardless of the load path history. For resistant heats, Kfw provides a reasonable, but not necessarily conservative, estimate of the critical stress intensity factor (K,) for LTCP. Testing of as-notched specimens showed that LTCP will not initiate at a smooth surface or notch, but if a crack-like defect is present it readily occurs. Comparison of the cracking response in water with that for hydrogen-precharged specimens tested in air demonstrated that LTCP is associated with embrittlement of grain boundaries by hydrogen generated by the corrosion reaction at the crack tip. Equivalent activation energies for Stage II LTCP rates (11.3 kcal/mol) and hydrogen diffusion (11.5 kcal/mol) indicate that hydrogen diffusion to the peak stress regions ahead of a crack is the rate controlling process. Auger analysis showed that heat treatment and heat-to-heat variability was associated with phosphorus and sulfur segregation to grain boundaries. Above 150°C, rapid cracking does not occur due to an increase in fracture resistance and decrease in the degree of hydrogen enrichment. SCC initiation and growth does occur in high temperature water (>250°C), but crack growth rates are orders of magnitude lower than LTCP rates. The SCC resistance of HTH heats was far superior to that for AH heats as crack initiation times were two to three orders of magnitude greater and growth rates were one to two orders of magnitude lower.