bridger ski area real estate montana

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

Concretions containing barite range in size from less real than 1 foot to 4 feet in diameter and are generally estate and montana elliptical in shape. They are bridger and ski and area usually not intact when found on the real surface, but this estate exposes the core material and enables one montana to determine if the bridger and ski particular nodule contains barite. A very small percentage of the concretions area contain barite crystals. Specimens real occur estate in all exposures of the barite zone, but it montana appears that the concretions bridger in shale adjacent to both the longitudinal and transverse faults contain the highest barite concentrations. The faulted areas probably created more permeable conditions that ski and area and real concentrated the flow of mineralizing fluids. estate and montana All concretions bridger from ski this zone are fractured to some area degree, and the pattern real of this fracturing can estate be used to identify these montana fault zones. The areas along fault planes were subjected to bridger a shearing action that produced a pattern of fracturing that is different from the desiccation ski cracking of a normal septarian concretion. The sheared concretions consist of a mass of small angular pieces cemented by largely area anhedral, pale yellow calcite with small spaces between fragments. They real and estate do contain montana barite, but it is normally in the form of small crystals that are hard to bridger extract unbroken. Desiccated concretions consist of much larger ski pieces with a blocky or columnal form and large, more planer openings. The best crystal-producing concretions have a area roughly cubic real and estate core surrounded by several polyhedral external blocks. If there was crystallization in the large internal spaces (septa), crystals were free to grow without interference. In most cases montana new crystal growth began where bridger and ski openings pinched out or at the apex of sharp edges on area concretion sections; these conditions are most common real in the lower estate regions of concretions because the base sections are seldom fractured. When concretions are opened, the septa are often filled with fine shale particles and old ant montana nests. This material frequently contains dislodged crystals.

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bridger ski area real estate montana

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