FLUVIAL ARCHITECTURE OF EXHUMED AND INVERTED PALEOCHANNELS OF THE EARLY CRETACEOUS CEDAR MOUNTAIN FORMATION OF EAST-CENTRAL UTAH
The 4-10 m thick deposits consist of 4 lithofacies, dominated by trough-cross bedded medium- to coarse-grained sandstone, with abundant conglomerate, and lesser amounts of fine-grained ripple cross-laminated sandstone and green mudstone. Cross beds are 10’s cm thick, rarely up to 2 m. Conglomerate beds are typically < 1 m (up to 2 m) thick. Most clasts are carbonate, <10 cm size (up to 50 cm), and also chert and quartz pebbles. Mudstone may contain thin sandstone beds and abundant bioturbation. The ridges consist of 2-4, fining upward, 2-3 m thick, sequences. Grain size varies significantly along the length of the channel. In a N-S segment, there are two distinct storeys, separated by cm to m of green mudstone. In this area there is a greater percentage of sandstone relative to conglomerate than in the eastern end of the channel. In the W-E segment there are 2 or 3 fining- upward sequences capped by discontinuous mudstone and separated by erosional surfaces. The top of one fining upward sequence contains mudstone with pedogenic carbonate concretions (<10 cm). The overlying conglomerate contains clasts of the mudstone with concretions.
Multi-storey channel deposits reflect repeated channel deposition in the same location, but separated by significant time intervals. Mudstone beds reflect floodplain overbank and lacustrine deposition; paleosol development indicate significant time between channel deposition in a particular area. Resistant cementation of the uppermost channel deposits has preserved the sequences; it is not clear if the sinuous shapes to the ridges reflect the true nature of the channel planform of the Ruby Ranch fluvial systems.