The velocity decrease at the injector has now increased to -20% on average in the interval. The pressure front appears to be intact. The steam zone seems not to have expanded outward much, but has intensified in place (Figure 32). The migrated profile and time slice of Figure 36 and 39 seem to support this conclusion since the steam reflections have increased in amplitude, but not much in diameter. The steam leak seems to have penetrated nearly down to the top of the P formation at this point, as visible in the migrated profile image. The temperature observation wells of Figure 42 show that the heating has increased to the west, but still nothing has arrived at the eastern observation well, which is supported by the seismic results.