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Even today, it is easy to imagine explorer David Thompson''s astonishment when he stood on a "Bare Knowi" on March 1, 1812, and became the first European to document this butte-silver broad blue-green lake. Over the next 200 years, the area was settled by homesteaders, the U.S. government created the 1.3 million-acre Confederated Salish and Kootenai Tribes of the Flathead Reservation, and vacationers built lakefront domiciles ranging from simple log cabins to multimillion-dollar homes. But none of the changes seems to have diminished the lake''s magnificence.
Concretions containing barite range in size from less than 1 foot to 4 feet in diameter and are generally elliptical in shape. They are usually not intact when found on the surface, but this exposes the core material and enables one to determine if the particular nodule contains barite. A very small percentage of the bow concretions mt contain barite crystals. Specimens occur in all exposures of the barite zone, but it appears that the concretions in shale adjacent to both the longitudinal and realestate transverse faults contain the highest barite concentrations. The faulted areas probably created butte-silver more permeable conditions that concentrated the flow of mineralizing fluids. bow All concretions from this zone are fractured to some degree, and the pattern of this fracturing can be used to identify these fault zones. mt The areas along fault planes were subjected realestate to a shearing butte-silver action that produced a pattern of fracturing that is different from the desiccation cracking bow of a normal septarian concretion. The sheared concretions consist of a mass of small angular pieces cemented by largely anhedral, pale yellow calcite with small spaces between fragments. They do contain barite, but it is normally in the mt form of small crystals that are hard to extract unbroken. Desiccated concretions consist of much larger pieces with a blocky or columnal form and large, more planer openings. The best crystal-producing concretions have a roughly cubic core surrounded by several polyhedral external blocks. realestate If there was crystallization butte-silver in the large internal spaces (septa), crystals were free to grow bow without interference. mt In most realestate cases new crystal growth began where openings pinched out or at the apex of sharp edges on concretion sections; these conditions are most common in the lower regions butte-silver of concretions bow because the base mt sections are seldom fractured. When concretions are opened, the septa are often filled with fine shale particles and old ant nests. This material frequently contains realestate dislodged crystals.
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