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<br /> <br />by slow minersl westhering (yery similar to <br />the pattern Whitmore had previously found for <br />overland flow). Based on measurements of <br />dissolved salts and sediment, a linear <br />predictive equation for salt load was de- <br />veloped. Good results were obt.ained; <br /> <br />l"V <br />o <br />CJ1 <br />W <br /> <br />however, the equation is of limited practical <br />apflication because sediment load is a <br />di ficult independent va,iable to measure or <br />predict. He concluded that lImicrochannels <br />contribute 3.4 percent of the total salt load <br />of the Price River at Woodside." <br /> <br /> <br />l <br /> <br />10 <br />