Laserfiche WebLink
O TETRA TECM <br />The original North Quarry Reservoir Plan was included in the fifth amendment to permit M-1973- <br />021. The reservoir plan defines a high water line between elevations 6020 and 6080 with a bottom at <br />elevation 5770. The reservoir was designed below the 6455 elevation and, therefore, was planned to <br />have 80 feet highwalls and 40 feet benches (Figure 1) <br />Quarry development is controlled by a default slope of 1:1 (H:V) unless a geotechnical evaluation of <br />the rock being mined indicates competent rock that can be mined at a steeper slope. The 80 feet <br />highwalls with 40 feet benches required geotechnical evaluation clearance to be developed per the <br />mine permit. <br />GEOTECHNICAL EVALUATIONDATA <br />In accordance with an agreement with the Colorado State Division of Reclamation and Mining <br />Safety (DBMS), AI contracts a geotechnical evaluation to be performed every year. This <br />geotechnical report is prepared as an addendum to the Morrison Quarry Annual Report submitted <br />every year to the DBMS. The report contains rock mechanics data based on field observations and <br />measurements of the rock being mined at the quarry. The data in the report is used to define the rock <br />mass as either "competent" or "poor". Competent implies minimal stability issues are present in the <br />rock mass and allows the default slope to be steeper than 1:1. Poor indicates a potential for rock mass <br />instability through features such as faults, shear zones, or unfavorable foliation and/or joint <br />combinations and may allow the default slope to be steeper than 1:1, however, typically the default <br />slope value is retained in these areas. <br />2001 GEOTECHNICAL ADDENDUM <br />The 2001 geotechnical addendum indicates mining in the North Quarry was completed on the north <br />and east sections of benches to approximately elevation 6,595. The mine slopes were recorded as 60 <br />feet highwalls with 40 to 70 feet benches. <br />The rock described in the report was granitic gneiss with mafic and felsic intrusions (felsic dikes and <br />pegmatites). Joints in the rock mass were described as closed with slight to moderately weathered <br />surfaces and spacing of approximately Y2 to 2 feet. Foliation orientations vary greatly due to the <br />folding of the rock with an average dip to the west. The rock mass was defined as primarily <br />competent with the following exceptions defined as poor: <br />• A shear zone, 6 feet wide, dipping 50-60 degrees SE <br />• A wedge failure, 20 feet wide <br />• A shear zone, 2-10 feet wide <br />• A shear zone, undulating and continuous <br />• An intrusive dike, 6 feet wide <br />-2- <br />