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<br />0018J3 <br /> <br />Two major alpine glaciations occurred in the higher mountains ofIdaho with the last <br />major alpine glaciation occurring during the Pinedale Substage. Minor glaciation occurred <br />during the Temple Lake Substage about 4,000 years ago which probably affected higher <br />elevations in the Bitterroot Range and Sawtooth Range (Ross and Savage, 1967). Higher <br />mountains throughout the central Idaho mountains and the Seven Devils mountain range were <br />glaciated during the Pleistocene by alpine glaciers (USDA Forest Service Draft Upper Columbia <br />River Basin EIS, 1997). Pan of the Valley Creek watershed has upland valley deposits. <br />commonly derived from alpine glaciation (Bond and Wood, 1978) . <br /> <br />United States' Expert Report Disclosing Me1hodologieS fer Quantification of Organic Act Claims Consolidated Subcase No, 63-25243 <br /> <br />19 <br />