My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2019-10-18_REPORT - M1978208
DRMS
>
Day Forward
>
Report
>
Minerals
>
M1978208
>
2019-10-18_REPORT - M1978208
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/18/2025 6:57:01 AM
Creation date
10/18/2019 12:32:06 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1978208
IBM Index Class Name
REPORT
Doc Date
10/18/2019
Doc Name Note
Unofficial Report/Maps
Doc Name
Annual Fee/Report/Map
From
Elk Creek Sand & Gravel, LLC
To
DRMS
Email Name
ECS
MAC
Media Type
D
Archive
No
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
228
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
Strike Dip Joint Designation Remarks <br /> N33W 35NE J-f Foliation (Primary) <br /> N58W 74NE J-1 Secondary <br /> N54E 75SE J-2 Secondary <br /> N38W_ _ _ 77SW _J-3 _ Secondary <br /> N54e 76NW J-4 Secondary <br /> N27W 41SW 1-5 Tertiary <br /> N20E 40NW J-6 Tertiary <br /> Stability evaluations for proposed highwall slopes were preformed using the average joint orientations <br /> listed above. There were based mainly on the primary foliation and secondary steeply dipping joints, <br /> but also considered the tertiary daylighting joint sets. Because the tertiary joint sets are not very <br /> common or persistent,the two sets were averaged into one westerly dipping orientation for the <br /> analyses. Also because of the lack of occurrence and persistence of these tertiary features,they are <br /> considered to be relevant only to individual highwall,and not overall slope,stability. <br /> The stereonet analysis and summary included in Attachment D shows potential; sliding plane and wedge <br /> failures. These all assume continuous,through-going joint features,which is a conservative assumption <br /> for this rock mass. Analysis shows potential slope failures if the slope were steepened to 1:4 from <br /> originally proposed 1:2 configuration, but acceptable slope conditions for a quarry development if <br /> steepened to 1:3 as Elk Creek is presently proposing(12 ft benches by 35 ft highwalls= 1:2.9). <br /> For slope failures to occur, planar or wedge failures must first be kinematically(geometrically) possible <br /> or admissible. In addition,for given possible planar or wedge failures mode,the material strength <br /> properties of the rock must be low enough for these failures to be mechani9cally possible or admissible. <br /> Such analyses were run for all kinematically admissible planes and wedges for both weathered and <br /> unweathered rock using internal friction angles of 30 degrees and 40 degrees, respectively. <br /> For the proposed 1:3 slopes, our analyses indicate that sliding failure is kinematically admissible only on <br /> the averaged westerly dipping joint set, but that this is mechanically admissible only in the upper <br /> weathered rock. Toppling failure is not kinematically admissible for any of the six joint sets analyzed. Of <br /> five wedge failures modes identified in the analyses,three are kinematically and mechanically <br /> admissible in the upper weathered rock, but not in the general rock mass. Two of the wedges might <br /> require spot bolting, but limited individual wedge failure in final highwalls is usually considered <br /> acceptable in quarry operations. As an example, DMG permitting for the Morrison Quarry in a similar <br /> rock mass assumed up to 15 to 20 percent such failures to be acceptable. The upper weathered rock <br /> should be laid back to 1:1 for long term stability. <br /> Part of the slope stability analyses included interpretation of rock mass classification and therefore, <br /> strength properties. Summaries of estimated rock mass properties based on rock mass classification <br />
The URL can be used to link to this page
Your browser does not support the video tag.