Three borehole tensor strainmeters (BTSM) installed near Parkfield and separated by more than 5 km have established a good baseline of data spanning the past eight years. A significant change in the accumulation rate of shear strain (0.5 and 1.0 microstrain per year at two of the sites) commencing approximately in mid-1993 and continuing to 1995 is evident in these data. Some supporting evidence for a change in the strain rate at that time is seen in dilatometer data, geodetic measurements, fault zone properties and microearthquake locations. There was also an increase in medium level seismic activity (M=4.7 on 10/20/92; M=3.9 on 10/26/92; m=3.5 on 3/13/93; M=4.4 on 4/3/93; M=4.8 on 11/14/93) in the Middle Mountain area. While a rainfall induced strain may have caused the observed strain anomaly, we propose a more likely explanation is that aseismic slip at depth on a section of the fault south of Middle Mountain produced the observed strain anomaly. This anomaly is unique in the current data set. ¿ American Geophysical Union 1996