To the north, the Tiago Macheira Subbasin contacts the Tassajara Formation, with which no groundwater exchange occurs. Groundwater flow in the subbasin is generally from southeast toward the northwest or north, corresponding to the slope of the regional terrain and water table surface. Uncontained shallow groundwater occurs within 25 feet (8 m) of the surface, while deeper confined water has levels that occur at various depths from 75 feet (20 m) to 150 feet (50 m) below the surface.
This subbasin is in the vicinity of the seismically active Greenville Fault associated with the Diablo Range. In fact the name of the second segment of the Greenville Fault (starting from north to south) is the Arroyo Mocho Segment.[4] The Arroyo Mocho Segment is generally considered to be more well developed and not as youthful as traces delineating the Marsh Creek-Greenville Segment, for example.
^State of California Department of Water Resources, 1974
^[1] Thomas L. Bonnie, ‘'What are the projected impacts of injecting reclaimed, reverse osmosis water into the Livermore-Amador Groundwater Basin?'‘ (2000)