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6.4.9 Exhibit <br /> Soils Information <br /> A Custom Soil Resource Report for Costilla County, specific to this site, is attached for <br /> review. The site is composed of Kibin fine sandy loam. <br /> Kibin fine sandy loam is a well-drained soil type characterized by its fine sandy loam <br /> texture, deep profile, and formation from fine-loamy alluvium over outwash derived from <br /> granite,gneiss, and mica schist. It's typically found in areas with low precipitation (8-12 inches <br /> annually) and moderate temperatures (around 417). It is often found in cropland with slope of <br /> 0 to 3 percent. <br /> Key Characteristics: <br /> • Texture: Fine sandy loam, indicating a balanced mix of sand, silt, and clay particles. <br /> • Drainage: Well-drained, meaning water moves through the soil relatively easily. <br /> • Parent Material: Formed from fine-loamy alluvium (sediment deposited by flowing <br /> water) over outwash (material deposited by melting glaciers). <br /> • Depth:Very deep, meaning the soil extends 40 deep below the surface. <br /> • Climate: Adapted to areas with low precipitation and moderate temperatures. <br /> Other Relevant Information: <br /> • Typical Location: Often found in cropland with slopes of 0 to 3 percent. <br /> • Associated Vegetation: Native vegetation might include grasses, shrubs, and trees <br /> adapted to the local climate and soil conditions. <br /> • Potential Uses: May be suitable for agriculture, depending on specific local conditions <br /> and management practices. <br /> Smith Pit Amendment Application <br /> pg. 12 <br />