Beach north of La Jolla, California, record a deep-water channelized slope system of an Eocene forearc basin. The outcrop exposure, which is approximately 100 m (330 ft) high by 1.7 km (~1 mi) long, offers insight into reservoir distribution and connectivity within coarse-grained, confined, deep-water channel systems. To use this outcrop as a quantitative subsurface analog, a detailed two-dimensional lithologic model was constructed from measured sections and interpreted photopanels. Elastic rock properties, including compressional-wave velocity, shear-wave velocity, and density typical of shallow offshore west African reservoirs were used to construct an impedance model. This model was convolved with 15-, 25-, and 50-Hz quadrature-phase Ricker wavelets to generate near-and far-angle stack one-dimensional and two-dimensional synthetic seismic reflection models. Because deep-water lithofacies have distinct amplitude-variation-withoffset behaviors and the interpretation of surfaces is intimately coupled with predicting lithofacies, simple bed interface models of conglomerate, sandstone, interbedded sandstone and mudstone, and muddy sandy debrite were used to build a template for successful interpretation.Interpretation of these forward seismic models demonstrates (1) the limits of and uncertainty associated with the interpretation of seismic data at different frequencies commonly encountered in the exploration, development, and production of deep-water reservoirs; and (2) how the combination of near-and far-angle seismic data can be used to interpret channel-fill lithofacies and Lisa Stright is an assistant professor of hydrocarbon geosciences in the Department of Geology and Geophysics at the University of Utah. She leverages her combined engineering and geology background to couple quantitative observations from outcrop analogs and subsurface data sets to build more predictive geocellular and flowsimulation models. She works specifically in siliciclastic reservoir characterization and modeling. is W. J. and M. L. Crook Professor and associate dean of Academic Affairs, School of Earth Sciences, Stanford University. His research foci include the tectonics of sedimentary basins, basin and petroleum systems modeling, and deep-water siliciclastic depositional systems. He is a recipient of AAPG's Sproule Award and Grover E. Murray Memorial Distinguished Educator Award.