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[FIGURE 1 OMITTED]GeologyThe surface features houses of the area under discussion listings (fig. 2) consist of montana the exposed core of the Cedar Creek Anticline. This structure houses marks the southwestern boundary of the Williston Basin, a major structural listings feature of the northern Great Plains. The anticline is an asymmetric montana fold with a strike of S. 30[degrees] E. and dips of from 4[degrees] to 40[degrees] southwest and less than 1[degrees] northeast (Clement 1986). The exposed section of the anticline crops out in an essentially straight line 145 miles long from northwest of Glendive, Montana, southeast to the Buffalo, South Dakota, area houses (Davis and Hunt 1956).
Generation 2 crystals listings show montana several interesting houses growth patterns. One of these is the creation of sceptered listings and montana specimens that initially form from several millimeters of new growth parallel to the a-axis on the {210} faces of a G1 crystal (fig. 9). After a continued houses growth on this addition, listings a G2 sceptered cap with a different termination morphology and color is created montana and houses on the G1 base (fig. 11). Growth hillocks and other microtopographic listings features (discussed in the G3 section) as montana well as doubly terminated crystals also appear.
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