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1987-12-01_PERMIT FILE - C1981017 (100)
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1987-12-01_PERMIT FILE - C1981017 (100)
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Last modified
1/4/2021 12:34:29 AM
Creation date
5/15/2012 8:35:32 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981017
IBM Index Class Name
PERMIT FILE
Doc Date
12/1/1987
Doc Name
Operation Plan-Permit Area
Section_Exhibit Name
Chapter IIB
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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Chapter II <br /> have been designated A, B, C, D, E, F and G and are depicted on maps <br /> 11-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. Description <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 /> 17 <br />
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