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1.0 INTRODUCTION <br />The Site is comprised of several properties (Wiant, Gurule, Villano, Sasaki, Adams, Watada, and Yokooji) <br />located within parts of Sections 18 and 19 of Township 1 North, Range 66 West of the 6th Principal <br />Meridian. The project is located approximately 600 to 2000 feet east of the South Platte River and is <br />generally bounded by U.S. Highway 85 on the west, by Weld County Road (WCR) 6 on the south, and by <br />WCR 27 to the east in Weld County, Colorado, as shown on Figure 1. <br />SW TKO Joint Venture, LLC (the Owner) has applied for and received a 112 Reclamation Permit to mine <br />gravel on the Site. However, prior to start of activities that impact alluvial groundwater, the Colorado <br />Division of Minerals and Geology (DMG) has required that a groundwater Sampling and Analysis Plan <br />(SAP) be established. The goal of the proposed SAP is to document the mechanism by which groundwater <br />quality in the local alluvial aquifer will be monitored and evaluated as to whether impacts occur as a result of <br />mining. <br />2.0 SITE CONDITIONS <br />The average land slope is 0.1 percent and the groundwater is typically 25 feet below the surface during <br />most of the year. The Site is surrounded by primarily agricultural land with domestic wells and irrigation <br />wells to the north, south and east. The Site slopes north, northwest toward the South Platte River and is <br />underlain by the Broadway Alluvium and the DenvedArapahoe Formation claystone (Colton, 1978). The <br />alluvial deposit underlying the Site is primarily composed of the Broadway Alluvium. The alluvium is <br />classified as sand and gravel deposited by the South Platte River and its tributaries. The deposit ranges in <br />thickness between approximately 30 to 50 feet, but averages approximately 40 feet. The deposits extend <br />well above the groundwater table to typically within three feet of the ground surface, creating an unconfined <br />aquifer of relatively homogeneous material (Colton, 1978). The Broadway Alluvium is underlain by Denver <br />and Arapahoe bedrock with outcropping of these formations located a couple of'miles east of the Site on the <br />ridge (located near the Fulton Ditch and Brighton Ditch Lateral). Refer to the Site Map shown on the <br />attached Figure 2. <br />The site groundwater is directly connected to the South Platte River and is therefore generally associated <br />with water quality that does not currently meet drinking water standards for several parameters, including <br />nitrates and fecal coliform due to the extensive use of septic systems in the area. Degrading sources to the <br />local groundwater other than the relatively low water quality in the river include: 1) feedlots; 2) local septic <br />systems; 3) pesticidesmerbicides associated with the current agricultural use; 4) petroleum hydrocarbons <br />associated with the existing oil and gas facilities; and 5) other potential sources as identified in the project <br />Environmental Site Assessments including a former county landfill that is located southwest of Pond 2. <br />3.0 PROPOSED PROJECT <br />The proposed project includes open surface mining of the shallow alluvial aggregate for direct sale or for <br />use in concrete and asphalt hatching. The sand and gravel processing area and a batch plant will be <br />installed in the southern portion of what will be Pond 2 (Figure 2). The southern and northern portions of the <br />site will be used for silt storage and will be mined in the first two years of the project. Water quality data will <br />be collected from the area near the northem silt storage area to establish baseline water quality for this area <br />where domestic wells are nearest the proposed mining activities. Following is an estimated schedule of <br />operation for each respective Recharge Site (RS-A through RS-D): <br />Groundwater Sampling and Analysis Plan November 2005 <br />Lupton Lakes Project -1- <br />