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pit location was left nearly level. The surface of this backfill is not finished and will <br /> need to be configured in a compatible fashion to adjacent backfill areas. <br /> D. Deviation from original elevation for new backfilled land-Although the resulting <br /> land has a lower elevation than it formerly did, the configuration of the backfilled land <br /> is similar to and compatible with adjacent lands in a similar topographic setting with <br /> respect to drainage patterns and lesser erosional features. <br /> 3. Processing facilities- Nothing has changed here. <br /> 4. Access corridors- No change in access corridors. <br /> 5. New soil and overburden stockpiles- No changes occurred other than to add some material <br /> to the existing topsoil stockpiles and remove material from the overburden stockpile for <br /> backfilling. Locations are still the same as in previous years. <br /> RECLAMATION ACTIVITY IN THE LAST YEAR: <br /> 1. Climatic summary of previous year- The following four pages of graphs show the climatic <br /> patterns for 2012 and the first half of 2013. These data are for KDEN,the weather station at <br /> Denver International Airport (DIA). As has been previously determined, the Coal Creek site, <br /> on average tends to be somewhat cooler and wetter than DIA,but the overall pattern at DIA is <br /> largely applicable to the specific Coal Creek area. Past examinations showed that the stations <br /> surrounding Coal Creek(Bennett, Parker, and Cherry Creek Dam)were about 5 to 10 percent <br /> wetter and a couple of degrees cooler, on average, than DIA. However, consistency in the <br /> differences is often lacking on the annual scale with the three nearby stations showing more <br /> variation between themselves than the average of the three stations vary from DIA. Also, <br /> because recent records from those stations are often not continuous the data set itself for each <br /> station shows high variance. <br /> The 2013 set of graphs show that from June until early September precipitation was below <br /> normal and temperature was above average. Thus, the summer of 2013 was unusually dry and <br /> hot. Vegetation was undoubtedly stressed by the lack of moisture and the high temperatures <br /> and, in fact, grass dormancy set in a bit earlier than usual resulting in a fairly brown prairie <br /> through the summer. <br /> On September 10 this pattern very abruptly changed with higher than normal precipitation and <br /> normal to slightly below normal temperatures. September was also the month that Colorado <br /> experienced a huge flood event primarily to the northwest of this area. Nevertheless, Coal <br /> Creek ran high several times, but not nearly to the extent of streams and rivers that begin in <br /> the mountains. After September temperature rose back to somewhat higher than normal and <br /> precipitation declined back down to a pattern similar to the summer. Please look at the graphs <br /> for individual months rather than the annual graph to see this pattern. The annual graph tends <br /> to be cumulative and therefore the higher than normal precipitation in September carves <br /> Status report for 2014 due July 15, 2014 Page 5 of 10 <br />