Laserfiche WebLink
Ad& <br />RMR spreadsheets for the highwalls are included in Appendix A. Scanline descriptions are <br />MW included below: <br />Aft <br />The Bench 6880 scanline was approximately 400 feet long and was separated into 5 discrete <br />Imk sections. The approximate orientation of the highwall is 340 degrees (north 20 degrees west). <br /> • Stations 0+00 through 0+75 consisted of granitic gneiss. The foliation strike varies in <br /> this area due to minor folding and ranges from 15 to 25 degrees. Foliation dips were <br />• 15 to 20 degrees southeast, parallel or slightly out of the highwall, with average <br /> spacing of approximately 4 inches and foliation apertures were closed and smooth. <br /> The primary joint set strike ranges from 315 to 325 degrees and generally dips from 85 <br />Ah to 90 degrees northeast. A secondary joint set is evident in this area and exhibits a <br />A& strike of 85 to 90 degrees with dips of 75 to 85 degrees southeast. The spacing of joint <br />set one averaged approximately 36 inches and the spacing of joint set two averaged <br />approximately 20 inches. Joint apertures were closed with slightly rough faces. <br />Stations 0+75 through 1+05 consisted of granitic gneiss. The foliation strike in this <br />area varies due to a local syncline and ranges from 340 to 360 degrees with dips of 32 <br />to 38 degrees northeast out of the face. Foliation spacing averages approximately 16 <br />inches and foliation apertures were closed and smooth. The primary joint set strike <br />ranges from 120 to 130 degrees and generally dips from 65 to 75 degrees southwest. <br />The secondary joint set strike ranges from 15 to 20 degrees and generally dips 85 to 90 <br />degrees southeast. Joint set spacing averages approximately 24 to 36 inches and joint <br />apertures were generally closed and rough. The synclinal nature of the foliation in this <br />area creates a minor potential for a plane failure of rock blocks sliding out of the face <br />on the foliation joint. However, the "bowl" created by the foliation is cut off at 1+05 <br />creating a partial interlock to the remainder of the highwall. Blocks from this area are <br />anticipated to be limited in size and should be retained on the bench below the <br />highwall. <br />Stations 1+05 through 1+25 consisted of mixed granitic and biotite gneiss in a shear or <br />slough zone. Foliation and joint orientations were indistinct due to the very close <br />spacing of joints combined with the amount of slough material covering the highwall. <br />The rock displays moderate iron staining and is assumed to be disintegrated under the <br />sloughed material due to weathering from localized shear. Blocks observed in this area <br />were generally less than 6 inches diameter due to the disintegrated nature of the rock. <br />Raveling from this zone is anticipated to cause only local operational delays. <br />Stations 1+25 through 2+20 consisted of massive granitic gneiss with planar jointing. <br />The foliation strike ranges from 5 to 15 degrees and dips range from 10 to 25 degrees <br />southeast, parallel or slightly into the highwall. Foliation average spacing was 36 <br />inches and apertures were slightly rough and generally closed. The primary joint set <br />strike ranges from 330 to 335 degrees and generally dips from 75 to 80 degrees <br />northeast. The secondary joint set exhibits a strike of 55 to 60 degrees with dips of 85 <br />to 90 degrees southeast. The average joint spacing was 30 inches and both joint sets <br />exhibited moderately open to closed, slightly rough faces. <br />-4- <br />Morrison Quarry Annual Report 2008 February 2009 <br />F A3919_038\Annual_Report _2008\Geotech_Report _2008\Annual_Report_2008_Geotech.doc