ACROSS THE BREVARD FAULT ZONE: THE CHATTAHOOCHEE INTERCEPTOR TUNNEL, COBB COUNTY, GEORGIA
Detailed geologic mapping within the alignment corridor identified sixteen different lithologic/geotechnical units. Each lithologic/geotechnical unit was evaluated on the basis of mineralogy, texture, weathering characteristics, structure, and the presence, nature and abundance of discontinuities, including lithologic contacts. This data relates to rock strength, breakage characteristics, type and relative depth of weathering, rock mass classification, and groundwater infiltration potential. Evaluation of this data allowed preliminary estimation of tunneling conditions and served as a guide for the location of vertical and angled exploratory core holes; as well as the location of 6-inch air-rotary drill holes to address depth of weathering and areas with the potential of large-volume groundwater movement that might be encountered during tunnel construction.
Lithologic/geotechnical units identified during surface mapping were correlated with subsurface data from rock-core and air-rotary drilling. Additionally, the surface units are currently being correlated with subsurface exposures during shaft excavation (access and pumping) and initial drill and blast portion of the tunnel; and will continue during the tunnel boring operations.