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2009-06-12_ENFORCEMENT - M1977211 (2)
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2009-06-12_ENFORCEMENT - M1977211 (2)
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Last modified
8/24/2016 3:47:39 PM
Creation date
6/15/2009 9:23:40 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977211
IBM Index Class Name
ENFORCEMENT
Doc Date
6/12/2009
Doc Name
Board Order
From
DRMS
To
Castle Concrete/Continental Materials- Mac Shafer
Violation No.
MV2009013
Email Name
BMK
Media Type
D
Archive
No
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before the Board at the April, 2009 Board meeting. The Operator requested that the hearing <br />be moved to the May 13, 2009 Board meeting. <br />11. The site is located in a geologically structurally complex zone where five <br />faults are mapped near, and within, the mine boundary. The site geology consists primarily <br />of Manitou limestone, with Saguache sandstone underlying, and Pikes Peak granite forming <br />the base. Complex faulting resulted in the strata being uplifted and tilted at a steep angle. At <br />the west boundary of the quarry the strata dips east at about 70 to 80 degrees. Erosion over <br />many millennia has exposed the Manitou Limestone outcrop, which is the aggregate being <br />mined. The CGS issued a report ("CGS Report") by Jon White, and TC Wait, on January 7, <br />2009, drafted at the Division's request and after CGS engineering geologists visited the site <br />and reviewed the 1994 Mine Permit document, a 1986 slope stability evaluation by MSHA <br />("1986 Slope Stability Memo"), and a 2001 Decision Notice by the National Forest Service <br />that permitted the removal of granite on forest lands above the quarry wall. The CGS Report <br />states "[b]rittle deformation features are abundant within the Precambrian granite, sandstone, <br />and limestone outcrops in the vicinity of the fault zone (e.g. slickensides, altered zones, <br />fractures, and fault gouge), which indicate additional numerous, small unmapped fault and <br />shear zones within the mine area." The CGS Report on p. 10 concludes that the quarry <br />rockmass is inherently weak "caused by the abundant discontinuities related to the Rampart <br />range fault zone."2 <br />12. On May 8, 2001 the Division approved the Operator's Amendment #2 to <br />permit number M-1977-211. Condition 41 of the approval for Amendment 42 ("the <br />Condition") provided that the Operator would provide a geo-technical report when the <br />underlying granite rock formation was exposed. The Condition states in part "No portion of <br />the quarry high wall will be constructed (mined) to slope angles steeper than the granite east <br />joint dip without prior approval by the Division." The Condition required the Operator to <br />report to the Division "as soon as the granite is exposed, the east joint dip and bench high <br />wall slope angle for each cliff (bench high wall) at approximately the north and central ridge <br />location." The Operator was to report the dip and slope angle "at these two locations for <br />each new bench high wall until the final granite portion of the high wall configuration is <br />completed." <br />13. The Condition required the report to be prepared and signed by a registered <br />geotechnical engineer or other qualified engineer, and was to include an analysis of the <br />stability of the cliff (bench high wall) as it related to the overall stability of the amendment <br />area quarry high wall. If the expert analysis revealed potential high wall stability problems, <br />then the Operator was to propose a modification to the mining plan to eliminate the <br />instability problem. <br />14. The Division testified and the Operator did not contest that granite was <br />exposed and the Division did not get a report. The report required by the Condition was not <br />z The causes of the slope failure and the resulting violations are discussed in a separate Board Order for MV-2009- <br />012. <br />Continental Materials <br />Pike View Quarry, M-1977-211 <br />MV-2009-013 3
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