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The gate across the entrance will be closed and secured at all times except during hours of <br /> construction activity. <br /> Topographically the original Signal Reservoir No. 1 and the proposed expansion are located <br /> atop a natural drainage divide and as such are not situated in the headwaters of a natural <br /> drainage, do not have a natural source of water supply, and receives negligible natural <br /> precipitation from surrounding areas. The reservoir has not overflowed and does not provide a <br /> natural source of water to any adjacent drainage. <br /> The planned expansion entails excavating a portion of the bottom of the existing reservoir. Any <br /> precipitation received during the construction period will be contained within the reservoir <br /> basin and subsequently be pumped into the adjacent Signal Reservoir No. 2 for containment. <br /> TCVMD owns all of the water rights associated with property comprising the permit area and <br /> has sufficient water and storage rights to support the planned expansion of the Signal Reservoir <br /> No. 1. <br /> The U.S. Department of Agriculture (USDA) Web Soil Survey (USDA 2017) indicates that the <br /> reservoir is underlain by the Ulm clay loam (UIC) and Platner loam (PIC) soil types Exhibit B-1 <br /> Soils Map. The USDA maps label the area comprising the permit boundaries as (W) indicating <br /> water. This recognizes the traditional and long-term use of the reservoir containing the permit <br /> area as a water storage facility. Soils <br /> The Ulm series is described as very deep, well drained soils that formed in calcareous alluvium <br /> derived from sedimentary rock. Ulm soils are on relict terraces, alluvial fans, fan remnants, <br /> plateaus, ridges, hills and footslopes. Slopes are 0 to 18 percent. The soils formed in fine and <br /> medium textured alluvium derived from interbedded shales and agrillaceous sandstone. <br /> The Platner series is defined as very deep well drained soils that formed in pedisediments of <br /> Ogallala or similar age, and are found on broad table lands and plains. <br /> No soils defined as topsoil are present within the planned permit area. <br /> TCVMD engaged Earth Engineering Consultants, LLC. (EEC), 4693 Greenfield Drive, Windsor, <br /> Colorado to examine subsurface conditions in the area to be excavated in the planned , <br /> expansion. Seventeen (17) holes, ranging in depth from twenty five (25) to forty(40)feet, were <br /> drilled within and immediately adjacent to the area to be excavated. The drilling and sampling <br /> were directed and supervised by an EEC field engineer. The report prepared by EEC concluded <br /> that: <br /> "The subsurface materials encountered beneath the relatively thin surficial layer generally <br /> consisted of a zone of sandy lean clay, lean clay with sand, sandy fat clay and/or clayey sand <br /> Signal#1 Reservoir Expansion-111 Special Operations Permit Application <br /> March 22,2018 8 <br />