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2.0 GENERAL SITE CHARACTERISTICS <br />As part of model development, 149 groundwater wells were identified, 88 well logs were <br />reviewed and 10 cross - sections were constructed. Based on the analysis of this data the <br />following general interpretations were made for the Tamarack modeling area: <br />• An old river channel is evident on the west site of the model area. This channel is <br />located south of the current South Platte River below the Sand Hills. At the east <br />end of the study area this old river channel aligns with the current South Platte <br />River. Figure 2.1 provides simplified cross - sections highlighting the basic <br />channel configuration. <br />• The alluvial aquifer can be divided into two layers; 1) the top layer consisting <br />primarily of sands; and 2) the lower layer consisting primarily of gravels. The <br />base of the aquifer is easily identified either as clay, brule or shale on the geologic <br />logs. <br />Figure 2.1- Schematic Cross - Sections of Tamarack SWA <br />Based on these general site characteristics the model area was divided into three <br />hydrogeologic zones as shown on Figure 2.2: <br />River Floodplain — Area near the current South Platte River. Typically the depth to <br />water in this area is less than 3 meters (10 feet). <br />Paleo - Channel - An old river channel is evident from the geologic logs. This channel is <br />located south of the current South Platte River below the Sand Hills. At the east end of <br />the study area this old river channel aligns with the current Platte River. Figure 2.1 <br />provides simplified cross - sections highlighting the basic channel configuration. <br />• <br />Page 3 of 8 <br />