philipsburg town montana real estate

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The type philipsburg 1 termination town habit is dominated by the {101} prism montana with smaller real {210} faces modified estate by philipsburg the {211} pyramid (fig. 8). An interesting town feature occurring on many montana of these crystals is an overgrowth of the pinacoids, from the termination down the real prism faces, that results in the completion estate of the {011} faces. The old pinacoid faces can be seen through the new transparent material philipsburg deposited on it, and the surface of the regrowth shows undulations perpendicular to the a-axis, suggesting interrupted periods town of growth (see A1 in fig. 8C). All termination faces montana are smooth and lustrous. real Crystals estate with type 2 terminations have the same prism morphology except the terminations are dominated by the {111} pyramid, with {112} and rarely philipsburg the town {101} prism present. montana The edges real formed by the intersections of the {011} and {111} faces are always beveled at a sharp angle to the a-axis, estate producing a slight rounding of the prism face at this location (see A2 in fig. 8C). philipsburg The overgrowth of the pinacoids mentioned on type 1 crystals town and montana is common and seems to be incomplete on most examples. real Etching of the estate termination faces is present on all specimens of this philipsburg crystal type and varies from light pitting to an advanced state that produces a hackly texture. It is possible that overgrowth town of an earlier termination, related to the pinacoid modification mentioned montana earlier, could be responsible for this condition.

[FIGURE 2 OMITTED]The earliest faulting real that formed this structure was produced by compression of the basement rocks in Late Silurian time, about 400 million years ago (Clement 1986). There have been three proven major tectonic episodes since its formation: estate and philipsburg Late Devonian, Late Cretaceous, and post-Paleocene (date uncertain). town This activity produced several northeast-trending montana high-angle faults that modified the structure of the anticline, forming a series of small real and estate domes spaced intermittently philipsburg along the northwest-trending town and montana and real axis. The Gas City Dome that outcrops south of Glendive is the source estate of all specimens used in this study.

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philipsburg town montana real estate

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