This document summarizes the geology and construction of excavations for the UC Berkeley Stanley Hall Replacement Project. Key points: - The project involved replacing an existing building with 3 basement levels extending to 75 feet deep in an urban environment near the Hayward Fault. - Geotechnical investigations identified complex subsurface geology including fill, sandstone, shale, mudstone breccia, serpentinite, and the Louderback Shear Zone fault. - Excavation required demolition, dewatering, micropile and conventional foundations, and soil nail shoring walls up to 40 feet high. - Detailed geologic mapping of the excavation faces during construction revealed differences from pre-construction interpretations