My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2010-07-27_HYDROLOGY - C2009087 (2)
DRMS
>
Day Forward
>
Hydrology
>
Coal
>
C2009087
>
2010-07-27_HYDROLOGY - C2009087 (2)
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 4:16:49 PM
Creation date
7/28/2010 1:26:48 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C2009087
IBM Index Class Name
HYDROLOGY
Doc Date
7/27/2010
Doc Name
Review Letter
From
DRMS
To
Peabody Investments Corporation
Permit Index Doc Type
Correspondence
Email Name
TAK
DIH
JDM
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.
Page 1 of 1
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
STATE OF COLORADO <br />-DIVISION OF RECLAMATION, MINING AND SAFETY <br />Department of Natural Resources C Z 00'J' 0'9 1 <br />1313 Sherman St., Room 215 Co r/ej <br />Denver, Colorado 80203 4r?7 'a J DC O L O R AN OF <br />Phone: (303) 866-3567 I RECLAMATION <br />FAX: (303) 832-8106 MINING <br />July 27, 2010 SAFETY <br />Bill Ritter, Jr. <br />Mr. John Cochran Governor <br />Manager Environmental Hydrology Mike King <br />Peabody Investments Corporation Executive Director <br />3001 West Shamrell Boulevard, Suite 110 Loretta E. Pifieda <br />Flagstaff, AZ 86001 Director <br />Re: Peabody Sage Creek Mine (C-2009-087) <br />Isotopic dating of ground water report (your letter of July 9, 2010) <br />Dear Mr. Cochran: <br />The Division of Reclamation, Mining and Safety has reviewed the above-referenced <br />letter and report in which you request that an additional baseline Wadge overburden well <br />not be required for a potential expansion of underground mine workings northwest of the <br />currently approved mine plan. <br />A hydraulic barrier is not needed to explain the difference in age between ground water <br />in deeper confined conditions (> 1.15 million years) and in the near-surface outcrop area <br />(65 years). The age difference probably results from shallow ground water not reaching <br />the deeper areas because shallow ground water exits to the surface through springs before <br />flowing to the deeper areas where ground water is nearly stationary. The deeper ground <br />water is nearly stationary because it does not discharge to the surface. The greater <br />circulation near the surface results in the shallow ground water being much younger than <br />the deeper ground water, even though the two ground waters are hydraulically connected. <br />An additional baseline well is needed for adequately determining the attitude of the <br />potentiometric surface so that potential impacts from mine subsidence can be evaluated. <br />Please contact me if you have you would like to discuss this further. <br />Sincerely, <br /> <br />Tom Kaldenbach <br />Environmental Protection Specialist <br />cc (via email): Dan Hernandez, DRMS <br />Jason Musick, DBMS <br />Office of Office of <br />Mined Land Reclamation Denver • Grand lunction • Durango ArtivP and Inartiva Minnc
The URL can be used to link to this page
Your browser does not support the video tag.