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Mr. Rick Siebel, Regional Director -6- May 16, 1995 <br />Office of Surface Mining <br />Western Region Coordinating Center <br />(a) Establish or restore <br />meandering pattern with <br />approved by the Division; <br />the channel to approximate its natural <br />a geomorphically acceptable gradient as <br />(b) Allow the drainage channel to remain in dynamic equilibrium with <br />the drainage basin system without the use of artificial structural controls <br />unless approved by the Division; <br />(c) Establish or restore the stream to include a diversity of aquatic <br />habitats (generally a series of riffles and pools) where appropriate, that <br />approximates the premising characteristics; and <br />(d) Restore, enhance where practicable, or maintain natural riparian <br />vegetation on the banks of the stream in accordance with the require- <br />ments of 4.15. <br />The Starkville Gulch, an ephemeral dry drainage with little vegetation, was diverted in 1980. <br />The Division believes the 2275-foot-long permanent diversion, including the 675-foot section <br />comprised of the eight-foot-diameter culvert, meets both hydraulic and regulatory requirements <br />for permanent retention, for the following reasons: <br />(a) The culvert does not contribute to a diminution of downstream water rights. The culvert <br />is designed to pass 465 cubic feet per second, the flow associated with the 100-year, <br />24-hour precipitation event and, as such, does not serve as an impediment to any <br />appropriated or non-appropriated flow. <br />(b) The average stream gradient has been maintained with a stable longitudinal profile. The <br />upstream end of the permanent diversion is installed at the level of original channel. The <br />outlet of the permanent diversion discharges into the original bedrock-lined stream channel <br />at the west end of the permit boundary. The original overall gradient through this section <br />of the stream bed is estimated to be no steeper than 4.35 %, based on the current 100-foot <br />difference in elevation between the culvert inlet and the permanent diversion discharge <br />point, and the 2300-foot horizontal distance measured between the two points on Map 12 <br />from the permit. The overall gradient of the 2275-foot permanent diversion is 3.4%, with <br />one 675-foot section lined by the culvert, and one 750-foot section lined by riprap designed <br />to maintain the channel bottom stable up to the 100-year, 24-hour precipitation event. The <br />third section, the center one, has no armoring, as it has been designed flat enough that <br />armoring is not required. The reconstructed channel gradient of 3.4%, as compared to the <br />estimated premising gradient of 4.35%, is a difference of less than 1%. We believe this <br />difference falls within the regulatory criteria of "approximate premising configuration." <br />(c) The channel has been established to approximate the natural meandering pattern with a <br />Division-approved, geomorphically acceptable gradient. The natural steep channel gradient <br />