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<br />ABSTRACT <br /> <br />The Uinta Mountains include 13,620 Km2 of land above 2,135 m. The <br />range includes 26 peaks that rise above 3,965 m. Over 1.8 Km3 of sur- <br />face runoff water originates annual on the range. <br />The commonest rock type in the interior of the Uintas is Uinta <br />quartzite, a hard rock that produces infertile soils on weathering. The <br />higher elevation, least fertile soils are dominated by coni,ferous for- <br />~ <br />ests. Lodgepole pine is the commonest conifer and dominates over 60% of <br />the coniferous forest area. Engelmann spruce is also common at higher <br />elevations. Most coniferous forests on the range are open and have low <br />productivity. The Uintas produce about 1.41 x 105 m3 of timber per <br />year: lodgepole contributes about 59% of that total and Engelmann <br />spruce about 31%. <br />The Uintas furnish about 119,709 animal unit months (AUMs) of <br />grazing for domestic livestock. Cattle account for 52% and sheep 46% of <br />the AUMs. The range and water impoundments around its edges furnish <br />about three million days of recreation annually. Camping, fishing, <br />hiking artd big game hunting account for 33, 20, 13, and 10% respectively <br />of the visitor days. <br />Most of the land (66%) is managed by The U.S. Forest Service. <br />Private interests control another 24% of the area above 2,135 m. <br />This report will consider the impact of late lying snow on the <br />lodgepole pine, subalpine meadow, spruce-fir, and alpine herbland eco- <br />systems. The linkage between snowpack and streamflow is considered. <br />Background levels of silver in plants and soils are reported and the <br />vegetational monitor design for the study is evaluated. The use of <br />satellite photos for monitoring snowpack retreat is also discussed. <br /> <br />2 <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />