| OCR Text |
Show 767 Toroweap Formation (Permian): Brady Canyon Member: 3. Limestone, yellowish gray (SY7/2); weathers very pale orange (10YR8/2); thick-bedded to thin-bedded; sandy; silty; clastic grains subangular to subrounded; some lenses stone; poorly lithified; to conformable contact silt weathers fossils; lacks slope; form lower of 1. 22 •••...••.. (4 ) 2. 87.17 (286) Limestone, yellowish gray (SY7/2); weathers pale yellowish brown (10YR6/2); thick-bedded; to weathers well form erous, fossils crinoid do fossilif disarticulated are broken columnals, rounded that ribbon nodules, lithified; massive cliff; chert rounded chert; and brachiopods and bryozoans weather out of not the contact rock; lower gradational........................ 36.S8 (120) 1. yellowish Dolostone, (SY7/2); (10YR6/2); chert; thick-bedded; ribbon nodules; chert rounded gray pale yellowish weathers brown lithified; well SO.60 (166) weathers cliff; Tossiliferous, fossils are braciopods, to form and bryozoans, that broken are crinoid columnals and rounded and by dolomit been destroyed ization; lower contact disconformity have .•••••..•••..•.....•• Total thickness of Brady Canyon Member Toroweap Formation Seligman 6. weathers ........•..... (Permian): light brown (SYR6/4): yellowish orange dark (lOYR6/6); 8084 (29) the Member: Siltstone thin-bedded; S2.42 (172 ) 41. 76 (137) |
