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2020-02-07_REVISION - M1977211 (14)
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2020-02-07_REVISION - M1977211 (14)
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Entry Properties
Last modified
6/15/2021 5:44:29 PM
Creation date
2/10/2020 8:17:00 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977211
IBM Index Class Name
Revision
Doc Date
2/7/2020
Doc Name Note
Exponent Reort
Doc Name
Adequacy Review Response
From
Continental Materials Corp.
To
DRMS
Type & Sequence
AM4
Email Name
TC1
Media Type
D
Archive
No
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1100318 R0T0 0811 JRW1 10 <br />reclamation before completion of the bench to minimize local bench instability is also discussed <br />in the amendment and shown in Figure 6. <br />The 1994 Amendment defines an “Area H” as seen in Figure 3. The “H” stands for “Hole.” <br />The length of Area H shown in the 1994 Amendment and 2000 Amendment is 1,859 feet in a <br />north-south direction. According to the amendment, the area defines the limits of excavation to <br />be created at the base of the quarried slope; the excavation of this area allowed removal of the <br />aforementioned undisturbed land at the north end of the quarry from the Mining Plan.19 <br />Figure 7 through Figure 11 show the Mining Plan Map, cross sections, and Reclamation Plan <br />Map associated with the 1994 Amendment. <br />As a further part of its engineering and geologic evaluation and design, the 1994 Amendment <br />discusses slope stability of Area H with particular reference to the west side of the area and <br />considers four factors: 1) historical sliding and instability arising from the presence of clay <br />zones (seams) in the Manitou Formation, 2) increasing the slope gradient within Area H, 3) <br />limestone bedding plane dip, and 4) dimensions of Area H.20 With respect to historical sliding, <br />the amendment discusses two slope failures that occurred in the mid-1970’s and one that <br />occurred in January 1993.21 All three failures reportedly occurred on clay zones within Manitou <br />Formation limestone and occurred as translational sliding block failures.22 Figure 12 shows the <br />evolution of the risks associated with the presence of clay beds. The 1994 Amendment states <br />that to increase slope stability, the upslope areas with strata containing the clay zones (Area MV <br />in Figure 3) would be mined prior to mining Area H, thereby significantly reducing the hazard <br />of massive landslides. With respect to the slope grading and bedding factors, the 1994 <br />Amendment stated that prior stable performance of the quarry did not indicate these were <br />substantial stability issues. As discussed in subsequent sections of this report, the <br /> <br />19 Application for Permit Amendment Pikeview Quarry, Permit Number M-77-211, received by Colorado <br />Division of Minerals and Geology on June 2, 1994, page 8 (Appendix 12) <br />20 Application for Permit Amendment Pikeview Quarry, Permit Number M-77-211, received by Colorado <br />Division of Minerals and Geology on June 2, 1994, page 19-24 (Appendix 12) <br />21 Mark A. Heifner, Submittal of six annual reports for Castle Concrete Company, May 21, 1993 (Appendix 23) <br />22 Application for Permit Amendment Pikeview Quarry, Permit Number M-77-211, received by Colorado <br />Division of Minerals and Geology on June 2, 1994, page 20 (Appendix 12)
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