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<br />. <br /> <br />. <br /> <br />. <br /> <br />Ol\1l~e;3 <br /> <br />at the gage is significantly affected by these diversions. This gage is used by <br /> <br /> <br />the Water Commissioner for administration of water rights and is not reliable <br /> <br /> <br />for use in the calculation of virgin stream flows. The gaging stations on the <br /> <br /> <br />Mancos River near Johnson Canyon have a relatively short period of record <br /> <br /> <br />and, therefore, are not useful in estimation of streamflow for the 1951 through <br /> <br /> <br />1980 study period. The Johnson Canyon gages were used in the estimation of <br /> <br /> <br />river losses, as discussed in Part X. <br /> <br />-7- <br /> <br />" ,,;< <br />