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The marine Pierre Shale beds above and below the barite concretion zone produce a diverse assemblage of Late Cretaceous marine fossils that are legal to collect if montana found on BLM land. Most specimens are contained ennis and realestate in concretions and are preserved only because the concretions formed around them. Rare occurrences of poorly preserved molds of animals are also mls found in the shale. Commercial collectors montana and hobbyists ennis are most interested in a variety of ammonites belonging to the genera Baculites, Hoploscaphites, Jeletzkytes, Ponteixites, and Rhaeboceras. In addition, one genus realestate of nautiloid, Eutrophoceras, occurs here. and mls and montana Found along with the cephalopods are gastropods, pelecypods, ennis echinoderms, and vertebrate bones. A vertebrate specimen in realestate the collection of North Dakota State University, in Fargo, consists and mls of a Hadrosaur bone with a shark tooth embedded in it (James Grier, pers. com., 1998). Petrified wood of Paleocene age, including some montana monocot stem sections, can be found in the bed of Cedar Creek, which flows along the axis of the anticline.
Crop ennis and realestate Revenue Coverage (CRC) premium rates went up by as much as 20% for corn this mls year. montana At press time the rates for winter wheat weren''t out, but Barnaby thought they might go up in some areas, as well."Don''t just buy what you ennis and realestate did in the past," he says. "It may have been cheaper a year ago to buy CRC on winter wheat, but it may not be in 2004."
AccessTo get mls to the anticline, take 1-94 exit 215 (City Center), the easternmost interchange serving Glendive, and proceed montana south on Merrill Avenue through town past, not under, the ennis railroad underpass realestate to Marsh Road, which is an extension of Merrill Avenue. Follow Marsh Road south out of town for about 9 miles to where the surface turns to gravel. This is the beginning of the productive Pierre Shale and the public land abutting the anticline. Proceed on the gravel up and over a large hill (composed of Fox Hills sediment) and under a set of power lines to the bed of Cedar Creek. After crossing the bridge over the creek, take the first left, mls turning east, onto a dirt road that will lead to the barite-containing outcrops.
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