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SUMMARY AND CONCLUSIONS <br />There were 14 ponds and springs located and photographed during the summer of 2014. <br />Of these 14 ponds and springs, six contained water and eight were dry at the time of the <br />survey in June. <br />Of the 14 ponds and springs identified, the following 25 appear to hold water or run <br />throughout the summer during a normal year: P -74, P -93, P -44, HDCS, P -23, P -24 and P- <br />95. The following three out of the 38 listed appear to contain the greatest volume of <br />water: P -74, P -23, and P -95. <br />Little to no difference in structural stability between the 2013 and 2014 field seasons was <br />observed. The minor changes that have occurred are most likely due to natural changes in <br />seasonal and daily precipitation and temperature. Many of the ponds contained more <br />water in 2014 which is a result of a higher snow pack than the preceding winter and a <br />seasonal rainfall. When comparing the 2013 and 2014 photos, vegetation has increased in <br />areas due to more water present in the soil. Overall, no effects from subsidence were <br />observed at any of these 14 ponds and springs. <br />19 <br />