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assumed. The total storage capacity of the Twentymile Sandstone aquifer over the area of the Twentymile Park <br />ground water basin underlain by this aquifer, about 35 square miles, is calculated to be about 336,000 acre -feet. <br />There are insufficient wells completed in the Trout Creek Sandstone aquifer within the Twentymile Park Basin to <br />construct a potentiometric surface for this unit. Consequently, ground water recharge and discharge cannot be <br />calculated using the flow net analysis technique. An approximate method of calculating recharge to the unit may be <br />made by examining the probably situation under which recharge occurs. It is believed that most of the recharge to the <br />Trout Creek Sandstone probably occurs in the vicinity of the unit outcrop in the southern margins of the Twentymile <br />TR13 -83 2.04 -27.1 11/03/14 <br />