My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2011-12-07_REVISION - M1986015 (8)
DRMS
>
Day Forward
>
Revision
>
Minerals
>
M1986015
>
2011-12-07_REVISION - M1986015 (8)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
6/15/2021 5:44:23 PM
Creation date
12/8/2011 7:09:04 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1986015
IBM Index Class Name
REVISION
Doc Date
12/7/2011
Doc Name
Adequacy Response
From
Tuttle & Associates
To
DRMS
Type & Sequence
AM4
Email Name
TC1
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.
/
94
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
submittal. Therefore the channel section and profile slope are sized to perform <br />successfully and carry the 100 year CFS without channel failure due to erosion. <br />Constructing the channel to a 100 year rainfall event equates to only a 1% failure risk <br />each year. A 1% risk is a significantly low chance of channel failure. We believe that <br />the channel as designed provides more than adequate protection against failure. <br />9.d. Refer to the Memo from Lyman Henn of December, 5, 2011. <br />Exh E — Amendment to the Phase 1 Reclamation Plan <br />10.a. The Amendment 3 Exh E map of the Phase 1 area shows the contours as they exist <br />now, that is post mining and pre reclamation. Prior to mining, the bottomland consisted <br />of low terraces as one moved away from the River. The terrace inclines were small (3 to <br />8 feet in height) and the terrace flats between the inclines were very flat (0.2% to 0.4% <br />slope). The gradient of the land along and parallel to the River is from 0.16% to 0.2% <br />slope. <br />The reclamation of the Phase 1 area is to be four separate sediment basins. The slurry <br />fines pumped into the basins will settle horizontally so the slope inside each basin is flat. <br />The elevations of the filled basins will be highest in the northern section (Basin 4) and be <br />slightly lower in the southern section (Basin 2). <br />Page 2 of Exh E states that the land will "have a general slope to the southeast with the <br />northwestern end being about 4 to 5 feet high than the southeastern corner ". Based on <br />our recent monitoring well data, we estimate that the final elevation of the filled Basin 4 <br />will be 4602 feet and the filled Basin 1 will be 4598 feet. So generally speaking, there is <br />a small slope to the southeast while the final land form is the terraced basins. The <br />channels between the basins will allow non - infiltrated precipitation to flow toward Basin <br />1 and on to the River. <br />10.b. The interbasin channels between the basins (see the enclosed Exh F -1A - Phase 1 <br />Detail - Revised) will allow non - infiltrated precipitation to flow through the basins to the <br />River. Thus the chances of long term ponding of water around the small cottonwood <br />trees and basal stem rot are reduced. <br />11. Topsoil will not be distributed on the Sediment Basins in Phase 1. Standard <br />reclamation practice is to allow plants to naturally degenerate on the silt filled basins. <br />12.a. Since the proposed contours are difficult to see, we have included spot elevations of <br />the final reclaimed surface. Existing elevations along the edge of the basins are noted as <br />".000" and final elevations of the basins are noted as "x000 ". We have included <br />elevations for top of berm, filled silt basin, and estimated groundwater. <br />12.b. Channels between the sediment basins in Phase 1 are included on Exh F -1A. The <br />channels will be concrete rubble choked with road base and depressed one foot into the <br />berms to allow vehicle movement along the top of the dikes. See the plan note for more <br />detail. <br />3 <br />
The URL can be used to link to this page
Your browser does not support the video tag.