Laserfiche WebLink
with total extent of approximately 2.75 acres. A well defined scarp with a height of 10 to 15 feet extends from a <br /> diversion ditch along the west perimeter of the disturbed slope, for a distance of approximately 300 feet to the <br /> east. A less defined scarp, along with associated cracking and bulging extends another 250 to 300 feet. Minor <br /> cracks also extend from the west side perimeter ditch for a short distance to the west, across a portion of the <br /> slope that was not regraded in 2007. Bulging is evident along the toe of the slide, including the southwest corner <br /> of the toe, which extends into Pond 12. <br /> The total topsoiled acreage affected by the slide is approximately 1.75 acres(the southwestern portion of the <br /> failure zone had not been topsoiled). It is likely that recovery of a significant quantity of soil will be possible prior <br /> to remedial grading, but some topsoil will likely be lost due to safety considerations adjacent to the scarp, and <br /> some quantity of soil has been lost due to rill and gully erosion on the slope. <br /> Heavy snowpack and associated high soil moisture level is presumably a major factor in the slope failure. <br /> However, occasional heavier than normal snowpack is an environmental factor that must be taken into account, <br /> and the repeated slope failures that have occurred in this location indicate the need for more intensive remedial <br /> measures. <br /> SUPPORTING EVIDENCE FOR NOV CV-2008-001 <br /> Pond Discharge Sample 082-012-1645 <br /> On arrival at the Pond 012 location at approximately 8:50 am, 4/22/08, 1 observed that there was a heavy flow <br /> from the primary spillway discharge culvert, and that the discharge water was somewhat turbid. I had left my <br /> sample bottles in my vehicle at the Seneca Mine office, and informed Roy Karo that I wanted to obtain a sample <br /> of the discharge, and would need to return to the site later in the day or the following day to do so. I did return to <br /> the site the afternoon of 4/22/08, and obtained a sample at 4:45 pm. I offered to obtain a sample split for the <br /> operator, which was declined. The discharge appeared to be heavier and darker in appearance than when <br /> observed earlier in the day. The flow stream filled approximately 1/3 of the 24"culvert outlet. I collected the <br /> sample by passing a 1 liter untreated plastic sample bottle back and forth through the discharge stream until full <br /> (after first rinsing the bottle with the discharge). I recorded the sample in my field book as#082-012-1645. 1 <br /> marked the sample bottle with this number using a Sharpie permanent marker, obtained a photo at the sample <br /> location, and placed the sample in a cooler, which I packed with snow at the site. <br /> I kept the cooler in my possession, until I returned to Grand Junction, and hand delivered the sample to Cynthia <br /> Bauer at Grand Junction Laboratories at 9:15am on 4/24/08. Settleable Solids analysis was run at 11:00 to <br /> 12:00 on 4/24/08, well within the applicable 48 hour holding time for the parameter. See Chain of Custody Form, <br /> "PH General Report Sheet"for Settleable Solids, Lab#6189, and the analysis report dated 4/28/08, attached <br /> (Lab#6189, Sample ID 082-012-1645), which indicates total suspended solids (TSS) level of 952 mg/I and <br /> settleable solids (SS) level of 0.9 ml/I. Because snowmelt was in progress and was the major source of inflow to <br /> Pond 012 when the sample was collected, the TSS limit was not in effect. Unless the operator demonstrates that <br /> the runoff was in excess of the 10-year, 24-hour event,the settleable solids limit of 0.5 ml/I does apply, and was <br /> exceeded. <br /> 4122108 Digital Photos <br /> I took a number of digital photos depicting site conditions relevant to the enforcement action, which are included <br /> and described on the following pages. <br /> 4 <br />