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2.04.9 <br />to 99 percent. The effective rooting depth is 40 inches. Depth to water table is more <br />than 80 inches. The soil is not flooded or ponded. Available water capacity is low. <br />MR157 & 158 - The Herm - Fughes complex and the Herm - Fughes - Kolob family complex <br />are well drained soils found on mountains. They are derived from interbedded <br />colluvium derived from sandstone and shale and /or interbedded residuum <br />weathered from sandstone and shale. The slopes range between 5 to 40 percent. <br />The effective rooting depth for the Herm component is greater than 60 inches. The <br />Fughes component has a restrictive layer of paralithic bedrock at 40 -60 inches and <br />contains up to 15 percent large stones. The Kolob component is very stony <br />containing up to 70 percent large stones. These soils are not flooded or ponded. <br />Susceptibility to water erosion is low to moderate. <br />MU -166 - The Leroux -Seitz complex (MU166) are moderately to well drained soils found on <br />valleys and mountains. They are derived from residuum weathered from basalt <br />and /or interbedded residuum weathered from sandstone and shale and /or colluvium <br />derived from basalt and /or interbedded colluvium derived from sandstone and shale. <br />Slopes range from 5 to 40 percent. The soil is not flooded or ponded; however, a <br />seasonal zone of water saturation in the Leroux component is at 30 inches during <br />April, May, June, and July. <br />MU 185 - The Shawa- Sandia family - Kolob family complex are well drained soils found on <br />mountains slopes and benches. The soil is derived from interbedded colluvium <br />derived from sandstone and shale and /or interbedded residuum weathered from <br />sandstone and shale. The slopes range between 5 to 40 percent. The effective <br />rooting depth is more than 40 to 80 inches. Depth to water table is more than 80 <br />inches. The soil is not flooded or ponded. Available water capacity is moderate. <br />MU186 - The Shawa- Sandia family - Kolob family complex are well drained soils found on <br />mountain slopes and benches. They are derived from interbedded residuum <br />weathered from sandstone and shale and /or interbedded colluvium derived from <br />sandstone and shale. The slopes range from 40 to 65 percent. The Sandia soil has <br />a restrictive layer of paralithic bedrock at 40 to 80 inches. The Kolob component is <br />very stony containing up to 70 percent large stones. This mapping unit is not flooded <br />or ponded. Available water capacity of the Shawa and Kolob family is moderate and <br />the Sandia Family is low. <br />PR -14 2.04-113- 06/14 <br />