My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2006-12-12_REPORT - M1974004
DRMS
>
Day Forward
>
Report
>
Minerals
>
M1974004
>
2006-12-12_REPORT - M1974004
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 3:16:32 PM
Creation date
12/29/2010 7:13:41 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
REPORT
Doc Date
12/12/2006
Doc Name
2006 Geotechnical Report
From
Lafarge North America
To
DRMS
Email Name
ACS
Media Type
D
Archive
No
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
58
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
<br />' addition, as discussed in the previous section, an east-west striking unnamed <br />fault zone is mapped in the northwest corner of the main pit. With the <br />combination of faulting and discontinuities on the north walls, the potential <br />impact on the slope stability should be closely monitored as mining continues. <br /> 6.2.3 West Walls <br /> No mayor stability issues currently exist for the west walls of the main pit or <br />' middle level of the quarry. Previous analysis indicated that the west highwalls <br /> have approximately the optimum orientations for stability. Two west wall <br /> orientations were analyzed in this study. The first had a dip direction of 091 °, <br /> and using this orientation the stereonet plot (Figure 13) indicated two plunges of <br />' line intersections less than the angle of the slope face, and one intersecting set <br /> of discontinuities that is within the failure envelope. Two of the intersections <br /> were at angles lower than the critical friction angle and indicate that sliding along <br /> these surfaces is possible but unlikely. For the set that is within the failure <br /> envelope (i.e. P-1 and P-6) sliding is assumed to occur because the plunge of <br /> the line of intersection slightly exceeds the 33° angle of friction. <br /> <br /> The second western wall analyzed in this study, has a dip direction of 120° <br />t (Figure 13). The results for this analysis yielded fairly comparable results, with <br /> two intersecting planes falling outside the failure envelope and one set mapped <br />' within. The intersection of discontinuities F-1 and P-2 fall just within the shaded <br /> region and sliding is assumed to occur as the plunge of the line of intersection <br /> exceeds the 33° angle of friction. <br />6.2.4 South Walls <br />As with the north wall and west wall, the southern wall has also been subdivided <br />into separate slopes for analysis: two southwest walls and a southeast wall <br />orientation were selected based on the proposed Lafarge mine plan (Lafarge, <br />2003). This approach is the same as was used for the 2004 annual report, in <br />-21 -
The URL can be used to link to this page
Your browser does not support the video tag.