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NEPA--Environmental Assessment

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ENVIRONMENTAL CONSEQUENCES<br />

Alternative 1<br />

Under this alternative, the visible trails from the high number of sheep grazed in the early 1900’s<br />

would eventually revegetate, though it would be very slow, and use from deer and elk would hinder<br />

this revegetation. This would reduce soil movement from uplands into streams.<br />

Under this alternative any contribution of nitrate or fecal coliform from sheep manure would be<br />

discontinued, though the existence or amount of any current impacts is unknown.<br />

Under this alternative, heavy metals contributed to streams from sheep grazing on mineralized soils<br />

would be eliminated. It is likely that extensive sheep grazing in the past has decreased the vegetative<br />

ground cover in mineralized areas and accelerated erosion and exposure of oxygen and water to<br />

metal sulfide bearing substrates. This weathering and erosion of metal-bearing rock and soil is a<br />

portion of the undifferentiated background metal load documented in the Use Attainability Analysis<br />

(Simon, 2001). Under a “no grazing” alternative, whatever portion is attributable to grazing would be<br />

eliminated.<br />

Alternative 2<br />

Under this alternative, natural revegetation of historic sheep trails would continue, but at a slower<br />

rate than in Alternative 1. Sheep use on historic trails likely keeps them from recovering as quickly<br />

as they would if there were no sheep.<br />

The existence or amount of nitrate or fecal coliform from sheep grazing is currently unknown,<br />

though it would continue at a similar amount with the continuation of current grazing<br />

Continued contribution of metals in streams from grazing on mineralized areas may continue.<br />

About 119 acres on the Gladstone allotment and 687 acres on the Red Mountain allotment are in<br />

areas suitable for sheep grazing overlapping with highly mineralized areas (Bove, 2007).<br />

Additionally, 635 acres of the West Lime allotment overlap with mineralized areas and would remain<br />

available for possible future re-stocking, for a total, of approximately 1,441 acres of overlap. In the<br />

past, most of these areas were grazed, though recently not as much use has been made of the<br />

mineralized areas.<br />

Alternative 3<br />

Under this alternative, natural revegetation of historic sheep trails would continue, at a slower rate<br />

than in Alternative 1, but a faster rate than in Alternative 2. . The heavily used area and new trails<br />

between Spencer Basin and Highland Mary Lakes would be improved because of the actions<br />

specified for the Deer Park Allotment.<br />

Any impacts from nitrates or fecal coliform would be similar to Alternative 2, because there is no<br />

need for particular actions to address these constituents.<br />

Under this alternative, impacts of grazing on mineralized soils would be reduced almost to the level<br />

of Alternative 1. The proposed action of “excluding grazing south of Ohio Peak on the Red<br />

Mountain allotment and excluding grazing south of Ohio Gulch west of Cement Creek and south of<br />

Hancock Gulch east of Cement Creek on the Gladstone allotment” significantly reduces the acreage<br />

of mineralized soil available for grazing. This reduces the amount of mineralized soil likely to be<br />

grazed in the Red Mountain allotment from 687 to 93 (an 86% reduction) This also reduces the<br />

amount of mineralized soil likely to be grazed in the Gladstone allotment from 119 to 76 (a 36%<br />

reduction). Since the West Lime Allotment would be closed, this removes an additional 635 acres of<br />

mineralized soil in suitable grazing from areas that have been grazed at some time in the past, for a<br />

total of approximately 169 acres of overlap. The proposed action in this document removes a total<br />

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