My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2008-02-25_GENERAL DOCUMENTS - M1974004
DRMS
>
Day Forward
>
General Documents
>
Minerals
>
M1974004
>
2008-02-25_GENERAL DOCUMENTS - M1974004
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 3:23:15 PM
Creation date
8/18/2008 10:25:52 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1974004
IBM Index Class Name
GENERAL DOCUMENTS
Doc Date
2/25/2008
Doc Name
Structural Geology Evaluation Specification Aggregates Quarry 2008 Annual Report
From
Lafarge West, Inc.
To
DRMS
Permit Index Doc Type
Gen. Correspondence
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.
/
52
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
5.0 Analysis of Structural Discontinuities <br />The stability of the rock mass that forms the highwalls of the quarry is mainly controlled <br />by the discontinuities. Discontinuities create the surfaces that sliding can occur upon <br />and the intersections of multiple discontinuities define the boundaries of wedges or <br />blocks that have the potential to slide. As observed throughout the quarry, the <br />discontinuity sets all have a range of dip and dip direction, and therefore it is possible <br />that discontinuity orientations in a specific location of the quarry deviate from the <br />general discontinuity orientations assumed for the analyses presented in this report. <br />5.1 Evaluation of Discontinuity Measurements <br />As the database for discontinuity measurements has increased, various methods have <br />been utilized to efficiently analyze the new acquired geologic data. The analysis of the <br />discontinuity data was conducted using Dips 5.1 (Rocscience, 2006), which is an <br />interactive program for the analysis of discontinuity orientations based on geological <br />data inputs. For this study, the data were evaluated with stereographic plots using a <br />combination of contour analyses and cluster analyses to determine representative dip <br />directions and dip angles for the predominant discontinuity sets. <br />The contour analysis of the entire dataset (i.e., 3036 points) resulted in a plot of density <br />contours, which facilitated our determination of the general discontinuity orientations <br />across the entire facility (Figure 4). The cluster analysis has helped to further refine the <br />data by utilizing an iterative approach to group the data measurements into <br />representative clusters. The nucleus of each cluster represents the concentration <br />center for a given data set as is shown for the cumulative dataset in Figure 6. The <br />differences between each of the individual year's analyses can best be seen on a <br />stereographic presentation showing each of the concentration poles for the clusters for <br />each annual analysis (Figure 7). A combination of the clusters from Figure 6 and the <br />results of the contour and cluster analysis of the entire dataset (Figure 7) were used to <br />define the discontinuities and their orientations for use in this year's analysis. These <br />t poles are summarized in Figure 8 and are presented in further detail in Table 2 below. <br /> <br />- 11 -
The URL can be used to link to this page
Your browser does not support the video tag.