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<br />o North Fork is an ephemeral drainage, based on monitoring <br />data from Well 2. An ephemeral drainage does not qualify <br />as a potential alluvial valley floor based on water <br />availability for natural subirrigation. <br />t} <br />,~ o The potential for flood irrigation agricultural activi- <br />ties does not exist within the Bolton Draw watershed. <br />This is also discussed in Chapter III of the TEA. <br />On the basis of this evidence, the applicant is requesting a neg- <br />ative alluvial valley floor determination for the North Fork of <br />Bolton Draw. The means used to derive this evidence is discussed <br />in more detail in Chapter III of the TEA. Regardless of the AVF <br />finding, most of the identified subirrigated area along North <br />Fork will not be physically disrupted by mining. Of 5.4 acres, <br />only 0.67 acres will be thus impacted. The unnamed alluvial soil <br />unit which includes the subirrigated area constitutes 14.4 acres, <br />of which 6.0 acres will be physically disrupted by mining opera- <br />tions. <br />The applicant has acknowledged that Bolton Draw itself is a <br />potential AVF. (Vol. 1, p. 116 of the permit application). This <br />finding agrees with previous evaluations of that stream presented <br />in the Marr Strip Mine Technical and Environmental Analysis, and <br />the Canadian Strip Mine Technical and Environmental Analysis, <br />July 21, 1980. This determination is based on the following con- <br />siderations: <br />o Bolton Draw exhibits a channel along its entire length <br />and is underlain by alluvial deposits ranging from 100 to <br />400 feet in width (p. 108, Vol. 1 of the permit applica- <br />tion and p. 53 of the July 21, 1980 Canadian Strip Mine <br />TEA). The stream is also characterized by active flood- <br />plain deposits. <br />o Monitoring Well 2 in the Bolton Draw alluvium indicates <br />that groundwater is held in those deposits. <br />-43- <br />