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Additional Pages <br />2006 Annual Report RECEWEiD <br />Pueblo East Pit NOy 13 <br />M-1986-015 p~l~O"~R ~ <br />Transit Mix of Pueblo Minin9and ~. <br />Anniversary Date: November 12 <br />Overview of Permit Year: The 2005-2006 permit year was eventful, to say the least. The operation was <br />practically shut down fox the second half of the summer due to severe flooding on the Arkansas River. As a <br />result of these problems, the amount of disturbed land was expanded a bit more rapidly than was initially <br />expected, but is now returning to a more normal pattern. Work on preparing the amendment fox Phase 2 was <br />nearly completed by the end of the permit year and the amendment is nearing the point of being submitted. <br />Annual Report Maps: The annual report map prepared fox this year is based on the Phase 1 mining plan map <br />and contains a bit more detail than has been provided in other annual reports. This is largely the result of the <br />major impacts of the floods on the operation. <br />Affected Lands: During the first half of the year, up until July, the operation proceeded as had occurred in <br />the past. That is, a slow and steady expansion very closely following the permitted plan. Dewatering continued <br />to be a growing problem with volumes of discharge reaching hlghex and higher levels. But everything remained <br />quite manageable and work proceeded according to plan. <br />During the summer of 2006, especially in July and August and into mid-September, the monsoonal <br />moisture was quite intense with the Colorado Springs-Pueblo-Cation City triangle being hit very hard by intense <br />rains, often day after day. This was a relief from the extremely dry winter and spring earlier in the year when <br />precipitation was almost non-existent. Unfortunately, the amount of moisture received created a series of flood <br />events that peaked in two major floods. The first was the largest flood since the floods at the end of April 1999. <br />River flow in the first flood adjacent to the pit was estimated at between 17,000 and 20,000 cfs. Although the <br />April flood which was about 12,000 to 13,000 cfs caused more damage due to its long duration, the floods of <br />2006 were more of a flash flood character -quick but very intense. The second flood was somewhat smaller, but <br />still larger than the 1999 peak volumes. It too was a flash flood type. Although prolonged flood events often <br />create more damage, flash floods create extreme damage where the circumstances are ideal for damage to occur. <br />Although nobody witnessed the breaching of the pit wall, it is suspected, based on the resulting damage, <br />that it occurred rather quickly in a series of two events. As the river rose it is suspected the initial water flowed <br />in from wetlands just south of the south end of the pit. Across-channel in the meander to the south carried this <br />water and normally it is discharged into the river on the east side of the meander. But the volume was so great it <br />flowed down small rivulets, cut under the protective berm and poured into the pit at one location. It is not <br />known if this was the fast event or the second in the sequence. <br />The main event was caused by the river making its way around some in-channel sand bars that had <br />developed over the past few years on the downstream side of the meander. Prior to the flood the river bank was <br />stable and well vegetated, but during the flood the water was forced into the bank by a sand bar in the middle of <br />the channel. This probably began to undercut the bank thinning the 100 foot setback. As the river tore higher <br />and reached a peak flow the river appears to have overflowed the bank and poured into the pit. Headwaxd <br />erosion quickly cut through the thinned and weakened wall until the river could pour into the pit and quickly fill <br />the pit creating a lake that covered about 30 to 40 acres. During the breaching process the initial break rapidly <br />widened to about 300 feet. Once the pit was full the breaching process stopped. Thus the size of the breach was <br />probably a function of the time it took to fill the pit with water and stabilize the inflow. A smaller pit would <br />have had a smaller break, but if the pit had been larger the break would have likely been even larger. <br />Transit Mix of Pueblo 2006 Annual Report M-1986-015 Pueblo East Pit Page 1 of 3 <br />