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SUMMARY AND CONCLUSIONS <br />There was one pond and two springs that were photographed in 2016, all of which contained water at the <br />time of the survey and appear to hold water throughout the summer during a normal year. <br />Little to no difference in structural stability between the 2015 and 2016 field seasons was observed. The <br />minor changes that have occurred are most likely due to natural changes in seasonal and daily <br />precipitation and temperature. Overall, no effects from subsidence were observed at any of these water <br />resources. <br />8 <br />