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Coulson Excavating Company, Inc. -Stroh Gravel Pit <br />Exhibit I -Soils Information <br />Soils present in the permit area were determined from the Soil Survey Map of Larimer <br />County Area, Colorado, 1980: United States Department of Agriculture Soil <br />Conservation Service and Forest Service - in cooperation with Colorado Agricultural <br />Experiment Station. (Soil Survey of Larimer County Area, Colorado, 1980) <br />The permit area for Stroh Gravel Pit contains the following soils (See Exhibit C): <br />• Fluvaquents (33), nearly level; <br />• Loveland Clay Loam (64), 0 - 1% slopes; <br />• Paoli Fine Sandy Loam (81), 0 - I% slopes; and <br />• Table Mountain Loam (105), 0 - 1% slopes. <br />Fluvaquents consist of variable layers ranging from sandy loam to clay loam, stratified <br />with thin layers of sand or clay. Underlying material is sand and gravel. Usually, a water <br />table exists at a depth of less than 12 inches. Here runoff and the hazard of erosion are <br />small. This soil is matched to pasture or native grasses. <br />Loveland series soils are classified as deep and poorly drained. The surface layer is <br />described as mottled dark grayish-brown or grayish-brown clay loam, approximately 15 <br />inches thick. Underlying material is grayish-brown clay loam on top of sand, gravel and <br />cobbles, approximately I7 inches thick. Native vegetation is made up of blue grama, <br />bluegrass and sedges. The permeability ranges from moderately slow above 32 inches to <br />very rapid below 32 inches. Water capacity ranges from medium to high. These soils are <br />most suitable for imgated and dry-farmed crops. The hazard of water erosion is small and <br />runoffis slow. <br />Paoli series soils are classified as deep and well drained. The surface layer is an <br />approximate 42-inch thick dark brown fine sandy loam. Underlying material consists of <br />brown fine sandy loam. Native vegetation consists of blue grama, bluestems, needlegrass <br />and a few forbs and shrubs. Paoli soils have a moderately rapid permeability and high <br />water capacity making them suitable for irrigated crops. Here runoff is slow and the <br />hazard of water erosion is minor while wind erosion is moderate. <br />Table Mountain series soils aze classified as deep and well drained, The surface layer is a <br />grayish-brown loam approximately 36 inches deep. Underlying material includes a 10- <br />inch thick layer of brown fine sandy loam and a 5-inch thick layer of yellowish-brown <br />fine sandy loam. Sand and gravel exist below the underlying material. The native <br />vegetation consists of blue grama, bluegrass, bromegrass and a few forbs and shrubs. <br />Table Mountain series soils have moderate permeability and high water capacity making <br />them suitable for irrigated and dry-farmed crops. In this case, runoff is stow and the <br />hazard of water erosion is minimal. <br />Based on these depths, the average depth of the topsoil over the permit area is <br />approximately 1.93 feet. The northern and southern mining zones contain a total of <br />approximately 286,348 yd' of topsoil, which will be removed and stockpiled and then re- <br />spread during reclamation. <br />H:\Stroh\word\DMG\Exhibit Ldoc <br />