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SUMMARY AND CONCLUSIONS <br />There were 51 ponds and springs located and photographed in June 2013. Of these 51 <br />ponds and springs, 24 contained water and 27 were dry at the time of the survey in June. <br />Of the 51 ponds and springs identified, the following 25 appear to hold water or run <br />throughout the summer during a normal year: SLP -1, P -19, P -22, P -18, P -96, Sly Spring, <br />P -69, P -70, P -55, P -56, P -57, P -81, P -62, P -25, P -29, P -36, P -37, P -74, P -93, P -44, <br />HDCS, P -23, P -24, P -95, LCCS. The following 10 out of the 38 listed appear to contain <br />the greatest volume of water: P -55, P -57, P -22, P -29, P -74, P -23, P -25, P -37, P -95, and P- <br />18. <br />Little to no difference in structural stability between the 2012 and 2013 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 2013 which is a result of a higher snow pack than the preceding winter. When <br />comparing the 2012 and 2013 photos, vegetation has increased in areas due to more water <br />present in the soil. Overall, no effects from subsidence were observed at any of these 51 <br />ponds and springs. <br />55 <br />