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Chapter II <br />have been designated A, B, C, D, E, F and G and are depicted on maps <br />II-B-App.7-Att.2 Plate 1 a-b and 2-7, which were prepared by Morrison-Knudsen Co. <br />in development of the Drainage Control System. The segments are: <br />Road Plate No . Descri tp ion <br />A 2 Main arterial road for all mines. <br />B 2 Collector road from Mines 1,2 & 4. <br />C 3 Lateral road from Mine 4 <br />D 4 Lateral road from Mines 1 and 2 <br />E 5 Collector road from Mines 3 and 5 <br />F 6 Lateral road from Mine 3 <br />G 7 Lateral road from Mine 5 <br />As described in the Morrison-Knudsen haul road study: <br />- This road system traverses very steep mountainous <br />terrain from the lowest elevation at 8,050 feet up to a <br />maximum elevation of 10,200 feet within a horizontal <br />distance that is less than 2 miles. The average road <br />surface gradients range from 2 to 9 percent. <br />- Severe road construction conditions have been <br />encountered on Roads C, D, and F to Mine 4, Mine <br />1 and 2, and Mine 3, respectively. These roads <br />have several long stretches with steep fill slopes. <br />Mid-Continent retained Geo-Hydro Consulting, Inc. to do further mapping and study <br />of the road system. The Geo-Hydro report, submitted in 1983, is contained in App. <br />V-E-2. <br />Geo-Hydro's study included bedrock and surficial geology, landslides and <br />avalanches, methods of road and bench construction and slope angles. The report <br />notes that: <br />- All haul roads were constructed in the Mancos Shale <br />and the Mesaverde formations. <br />- The Mancos Shale, which is common in Western <br />Colorado, and is known for rapid disintegration, has <br />relatively more favorable physical properties in Coal <br />Basin; numerous rock cuts in Mancos Shale are <br />stable even when excavated at very steep slope <br />angles. <br />- Landslides are relatively infrequent in Coal Basin,and <br />it appears no significant landslides are found in the <br />area of the haul roads. <br /> <br />17 <br />