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Prior to pond construction, a similar assessment of the site was also made. The early <br />photographs show there was no evidence suggesting that this location of the pond would not <br />be appropriate. Failure of an internal perimeter pond slope simply could not have been <br />predicted. We will also show that most of the failed slope was pre-existing debris rather than <br />~ topsoil and that the slide would have likely occurred regardless of the presence of the topsoil <br />stockpile. Since the pond embankment itself is not in jeopardy we believe the repair of the <br />pond perimeter slope more appropriately falls under Rule 4.05.919) which provides for <br />maintenance rather than necessitating an enforcement action. <br />Our operating record clearly shows that while Colowyo readily accepts the <br />responsibility to remediate damage to regulated structures occurring from naturally occurring <br />events we strongly believe that SMCRA did not intend that the mere occurrence of such <br />events must require enforcement actions. Since the Regulations clearly provide for <br />maintenance of regulated structures we believe this would have been the more appropriate <br />course of action to address remediation of the slide area. The issuance of the NOV was <br />clearly not justified in this situation and amounts to an arbitrary, inconsistent and excessive <br />use of the Division's enforcement authority. For these reasons we respectfully request that <br />the NOV C-95-005 be vacated. <br />SPECIFIC COMMENTS <br />Our specific comments relating to the slide area are as follows. Please refer also to <br />the attached photographs accompanying this information for additional insight into our <br />comments. <br />11 Landslides are naturally occurrinG in the area. As we noted above, landslides <br />~"~ ~ ~ are a naturall occurrin but un redictable henomenon of the area. Photo ra hs 1 and 2 <br />(` .. ` ~lul~ Y 9 P P 9 P <br />Q , ; ~ show the areas immediately north and south of the pond area and show typical examples of <br />~~\, landslides in the center of each photograph. <br />_ 2) Prior to construction the topsoil stockpile area showed no signs of instability. <br />!,~,1 ~, Photograph 3 shows the future pond location and the future topsoil stockpile location before <br />,~n3~ur construction. The elevated area to the right of the picture (look for the motorgrader) was a <br />stable, reasonably flat area appearing quite suited for a small topsoil stockpile. There was no <br />~~~ ~ indication of any evidence suggesting that this location was anything but a stable surface <br />area. <br />3) The slide area is a function of a series of shallow, perched water zones in the <br />General area. Photographs 4, 5 and 6 show the relationship of the slide area to the zone of <br />~~ ~h`iS!~' springs located further to the east. In addition, out of sight within the West Pit Fill subdrain <br />~r ~ ~~ structure are two lateral french drains constructed to provide free flowing channels to de- <br />~.. <br />water the perched water zones encountered at this lower level during subdrain construction. <br />We believe that the water flowing from this lower zone is also saturating the debris below the <br />topsoil stockpile, resulting in the landslide. <br />41 To increase protection of the topsoil stockpile. the stockpile was set back from <br />the edoe of the pond. To further protect the topsoil, we did not want the stockpile perched <br />directly above the edge of the pond. Rather, to provide for enhanced protection of the <br />stockpile, we had taken extra measures to locate it away from the pond edge a distance of <br />