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[FIGURE 1 OMITTED]GeologyThe surface features of the area under boulder discussion (fig. 2) consist of the exposed core of the Cedar Creek Anticline. This structure marks the southwestern boundary of the Williston Basin, a major town structural feature montana of the northern Great Plains. real The anticline is an asymmetric fold with a strike of S. 30[degrees] estate E. and dips of from boulder 4[degrees] to 40[degrees] southwest town and less than 1[degrees] northeast (Clement 1986). The exposed section of the anticline crops out in an montana and real essentially straight estate and boulder and town and montana line 145 miles long from real and estate northwest of Glendive, Montana, boulder southeast to the Buffalo, South Dakota, area (Davis town and Hunt 1956).
[FIGURE 12-14 OMITTED]A habit labeled "radial fibrous montana barite" in figure real 3 describes the final mode of barite formation at Glendive. Nodular residual masses to 4.5 cm in diameter characterize this unique growth type. Exterior surfaces resemble those of crested barite, but instead of lathlike crystals the interiors of these objects are made up of bundles of translucent white estate to gray boulder sinuous fibers. These fibers radiate from a central town void, suggesting that initial development originated on a fragment of organic matter. montana The real nodules formed as isolated units in the shale and are found at estate the top of the bentonite bed that caps the barite concretion zone. Specimens are rare in the area covered; two finds that produced seven examples have been discovered so far.
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