Gray to greenish-gray, medium-bedded quartzose sandstone, generally fine-grained, calcareous, finely micaceous, probably more than 500 m thick; contains abundant yellow-orange limonitic spots and commonly contains conspicuous cross beds and ripple marks; beds are up to 2 m thick and interbedded with gray silty micaceous shale and, locally, with thin silty limestone. Locally contains massive, thick-bedded, white to light-gray-weathering pebble conglomerate, which contains matrix-supported white quartz and black and gray chert pebbles to 2 cm diameter. Unit was mostly deposited on a marine shelf (Mull and others, 1994). Conformably overlies Hunt Fork Shale. Conformably underlies Ear Peak Member of the Kanayut Conglomerate). Thickness ranges 0 to 560 m. Contains late Late Devonian (middle Famennian) marine megafossils, including brachiopods, gastropods, pelecypods, and echinoderms, and trace fossils such as Skolithos (Nilsen and others, 1985). As mapped here, includes a unit informally described as wacke sandstone and quartzite members of the Hunt Fork Shale (Nelson and Grybeck, 1980; Brosgé and others, 1979). This unit was described as grayish green, brown, and black micaceous manganiferous clay shale and shaly siltstone that contains interbedded thin- to medium-bedded, fine- to medium-grained, limonitic quartzitic quartz-chert wacke that weathers orange and brown; green fine-grained wacke; and minor amounts of gray quartzite and calcareous sandstone. Wacke is composed of fragments of quartz, chert, muscovite and biotite schist, and minor amounts of plagioclase feldspar. Ferruginous lenses contain brachiopod coquina and pebbles of chert and shale and ironstone (Brosgé and others, 1979; Kelley, 1990a). Nelson and Grybeck (1980) reported brachiopods, gastropods, pelecypods, echinoderms, other mollusks, plants, feeding tracks, and trails. Brosgé and others (2000) mapped dark-gray wacke and brown calcareous sandstone containing coquina lenses as part of this unit. As mentioned above, unit is much more widely exposed than shown here because it is commonly mapped as a unit within the Kanayut Conglomerate