realestate big hole vally montana

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[FIGURE 3 OMITTED]It realestate and big is important hole to note that there is a 7-10-foot-thick bentonite-capped, erosion-resistant bed overlaying the barite-containing concretion vally zone. The bentonite cap weathers to a dark montana gray, after realestate undergoing significant bloating, with the end product big a layer of gumbo soil, devoid hole of vegetation, vally with a "popcorn" surface characteristic of degraded bentonite (Gill and Cobban 1966). montana Color differences on weathered concretions can realestate also big be used as an indicator of barite-containing material. The barite-zone concretions often have hole a dull red tint in contrast to the gray surfaces of the layers above vally and montana and below the producing realestate and big zone.

CrystallographyThere are three well-crystallized mineral species present at Glendive. Because calcite and gypsum (var. selenite) are described in figure 4 and do not vary in crystal hole habit, they will not be mentioned vally in this section. All three forms typical of barite--pinacoids, montana and realestate rhombic prisms, and rhombic pyramids--are found in crystals from this area. Specimens, except for one occurrence of lamellar microcrystals in an ammonite fossil, show the most elongation parallel to the a-axis, forming prismatic crystals from several millimeters big and hole to 10 cm in length. This basic habit vally varies from squat bladelike individuals to acicular stellate groups and individuals montana and realestate with a tabular cross section. Some specimens exhibit sharp color big zoning that hole produces vally amber terminations on clear prismatic shafts, montana or sheetlike growths of amber realestate material, big typical of concentric hole zoning in crystals (Rakovan vally and Waychunas 1996), that form a rind on the prism montana faces of some specimens.

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

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realestate big hole vally montana

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