Cenozoic rocks include about 15,000 feet of continental sedimentary and volcanic rocks of Oligocene age. Volcanic rocks consist of ignimbrite flows, plugs and dikes, lavas, and air-fall tuffs. Ignimbrite plugs and dikes fill vents from which some of the surrounding ignimbrite sheets were probably discharged. Plug rocks have vitroclastic textures and textures transitional between vitroclastic and flow banding. Dike rocks have vitroclastic textures and show various stages of vesiculation. Ignimbrites forming the basal sheet are crystal-rich rhyodacites, and have less silica and alkalies than the rhyodacites forming the top sheet. The ignimbrite plugs are more siliceous and alkalic than their surface-equivalent ignimbrite sheets. These plugs are modally and chemically “stratified”; their upper parts are crystal-rich rhyodacites and contain less silica and alkalies than the basal, moderately crystal-rich rhyolites. The origin of these variations is not well understood, but available data suggest that the basal portion of a differentiating magma chamber may have been tapped, so that the magma became progressively more siliceous and alkalic; continued pulses of increasingly more siliceous material may account for the “stratification” of the plugs. Cognate crystals in the ignimbrite plugs, dikes, and sheets were broken prior to extrusion; some were broken during compaction and welding. Most of the vesiculation took place prior to extrusion. Fluidization of the constituents may account for the mobility of the ignimbrites. Chemical compositions and textures have been modified in most sheets after they were emplaced. Secondary sanidine of a devitrification origin locally crystallized to a more sodic sanidine, and the replaced potassium may be accounted for by the K-feldspar rims on cognate crystals. Textural changes include welding, devitrification, and vapor-phase crystallization. The ignimbrite plugs and thick ignimbrite sheets are welded and devitrified from base to top. Thin sheets are welded only in their middle portions, and devitrification is confined to their upper zones. Ignimbrite plugs and their equivalent ignimbrite sheets contain vapor-phase minerals from base to top in vesicles that formed after welding. These ignimbrites were probably richer in volatiles than those in which vapor-phase crystallization was confined to the upper zones.