The lower? and middle Eocene Raging River Formation is the oldest Tertiary stratigraphic unit exposed in the east-central Puget Lowland, Washington, and provides key information for reconstructing regional paleogeography and tectonic history. Three informal stratigraphic units (designated 1 to 3 from base to top) are here recognized in the Raging River Formation based on distinctive sedimentary facies and lithologies. A fourth unit (unit 0) might either represent the lowest exposed part of the Raging River Formation or semi-lithified Quaternary(?) colluvium. Unit 1, approximately 230 m thick, consists of interbedded sandstone, mudstone, and conglomerate of inferred nonmarine (lower part) and transgressive shallow-marine (upper part) origin. Unit 2, approximately 185 m thick, consists of interbedded conglomerate, sandstone, and mudstone, and is inferred to be of mainly alluvial origin. A significant transgression is recorded by Unit 3 (about 300 m thick), which consists of gray silty mudstone and lesser sandstone, and was deposited in a marine shelf (lower part) and bathyal slope (upper part) setting. This transgression reflects local tectonism and not fluctuating eustasy. The Raging River Formation is overlain by prodelta(?) marine shelf deposits in the lower part of the Tiger Mountain Formation. The Raging River Formation may provide a surface analog for conductive rocks that underlie a large part of the southern Washington Cascade foothills.Three sandstone petrofacies were identified in the Raging River Formation and lower part of the Tiger Mountain Formation. These petrofacies reveal an upward evolution in sediment source from Mesozoic basement rocks of oceanic affinity (petrofacies 1), to lower Tertiary volcanic rocks (petrofacies 2), to a mixed provenance including Mesozoic oceanic rocks, lower Tertiary volcanic rocks, and more distal plutonic or crystalline rocks (petrofacies 3).