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2008-04-30_REPORT - M1973021 (3)
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2008-04-30_REPORT - M1973021 (3)
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Last modified
8/24/2016 3:28:56 PM
Creation date
5/8/2008 8:30:55 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1973021
IBM Index Class Name
REPORT
Doc Date
4/30/2008
Doc Name
Geotechnical Addendum/ 2007 Annual Report
From
Tetra Tech
To
DRMS
Permit Index Doc Type
Annual Reclamation Report
Media Type
D
Archive
No
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Figures 3 and 4 are a photo documentary of the features observed in Bench D. <br />3.3 South Quarry <br />Geotechnical data was collected for the areas mined in 2007. As mining in this expansion to <br />the quarry only started this year, the primary activity for the expansion included overburden <br />stripping and building haul roads. One highwall has been completed (Bench 1, approximate <br />elevation 7000 feet above MSL); however the related bench has not been completed yet being <br />approximately 120 feet wide at the time of the survey. The highwall orientation is <br />approximately north-south and likely represents the average highwall development orientation <br />for the upcoming mining. <br /> The type of rock encountered in the highwall is consistent with rock found in other areas of the <br /> quarry. The rock of the highwall was fine to medium grained biotite gneiss. No intrusions were <br />• observed in this highwall survey. <br /> The gneiss observed in the highwall was moderately to highly weathered, likely due to the <br />• proximity to the original ground surface. The highwall generally displays two prominent joint <br />• sets and a foliation surface. Joint spacing ranges from approximately '/4 inch up to 3 feet. Joint <br />ed <br />l <br />t <br />l <br /> . <br />os <br />o c <br />y open <br />surfaces generally are slightly smooth to slightly rough and are moderate <br /> When joint surfaces are open or exposed, the joint faces are typically moderately to highly <br />. weathered and display iron staining. The joints generally do not contain any infill material. <br /> Foliation spacing ranges from less than one inch up to 2 feet. Foliation surfaces generally are <br /> slightly smooth to slightly rough and are moderately open. Across the highwall, the foliation <br /> displays relatively similar orientations with anticlinal folding. The anticlinal axis is <br />into <br />in <br />di <br />ti <br />li <br />f <br />h <br />i <br /> g <br />pp <br />on <br />a <br />o <br />n t <br />e <br />approximately the same orientation as the highwall, which results <br /> the highwall in areas and out of the highwall in other areas. When foliation surfaces are open <br />• or exposed, the aperture is up to one inch and the foliation faces are typically moderately <br />l <br />i <br /> ; <br />a <br />weathered with iron staining. The foliation generally does not contain any infill mater <br /> however in some cases minor clay infill was observed. <br />• The highwall observed was dry and seepage through the rock is not anticipated. Average <br /> RMR values calculated for the rock exposed in the highwall of Bench 1 range from 38 to 55 <br /> indicating poor to fair rock. Joint orientation field data and RMR spreadsheets for the <br />• highwalls are included in Appendix A. <br />~' The Bench 1 scanline was approximately 200 feet long and was separated into 4 discrete <br />~ sections. <br />Stations 0+00 through 0+50 consisted of biotite gneiss displaying an anticlinal trend. <br />The strike of the foliation ranges from 0 to 10 degrees. Foliation dips range from 28 to <br />38 degrees. The average spacing of the foliation was approximately 12 to 18 inches <br />and the foliation displays slightly smooth, wavy apertures that are open up to 0.5 <br />inches. The primary joint set strike ranges from 145 to 150 degrees and generally dips <br />from 65 to 75 degrees. The secondary joint set strike ranges from 210 to 220 degrees <br />and generally dips from 72 to 80 degrees. Joint set 1 average spacing was 7 inches and <br />-5- <br />• F:\3919_038\Anmial_Repod_2007\Gcotech_Addcndum_2007Wnnual_Report_2007_Gcotcch.doc <br />• <br />• l _ - - <br />Apri12008 <br />
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