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REV98642
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REV98642
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Entry Properties
Last modified
8/25/2016 3:22:41 AM
Creation date
11/22/2007 12:19:58 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1988112
IBM Index Class Name
Revision
Doc Date
1/10/1996
Doc Name
ESTIMATED FLUID TRAVEL TIMES IN THE SATURATED PORTION OF THE SANTA FE FORMATION FROM THE TAILINGS
From
BATTLE MOUNTAIN GOLD CO
To
DMG
Type & Sequence
TR15
Media Type
D
Archive
No
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~II ~I~~II~I~~~~~~I~ <br /> <br />BATTLE <br />ANNE C. BALDRIGE <br />DIR ELTOR OF ENVIRONMENTAI. <br />ANO GOVERNMENTAL AFFAIRS <br />January 10, 1996 <br />• s,~ <br />94i1LE MOUNWN <br />GGOOILD COMPANY <br />DE':~Aiauaa~A.' Pendleton <br />Mr. James C. Stevens <br />Colorado Division of Minerals and Geology <br />1313 Sherman Street, Room 215 <br />Denver, Colorado 80203 <br />-~.~LS <br />Subject: Estimated Fluid Travel Times in the Saturated Portion of the Santa Fe <br />Formation from the Tailings Facility to the Closest Existing Monitoring <br />Well, San Luis Project, Costilla County, Colorado. <br />Dear Messrs. Pendleton and Stevens: <br />Based on comments received from the Division in our meeting on December 8, 1995, <br />we were requested by Battle Mountain Resources, Inc. (BMRI) to evaluate fluid travel <br />times in the saturated portion of the Santa Fe Formation from beneath the tailings <br />facility to the closest existing Santa Fe Formation monitoring well (M-14), assuming a <br />hypothetical release from the tailings facility and instantaneous travel to the saturated <br />portion of the Santa Fe Formation. <br />The fluid travel times estimated herein are based on a range of actual data and a set <br />of hypothetical assumptions proposed by Jim Pendleton of the Division that are <br />judged to bracket fluid travel times under the set of hypothetical assumptions. <br />To make the estimate of fluid travel time, we reviewed the existing data base and <br />made several assumptions based on our discussions in the December 8 meeting. <br />The data and assumptions used in this analysis are as follows: <br />(1) Fluids were assumed to be entering the ground water talple directly <br />beneath the centroid of the existing pond, which produced a lateral <br />distance to the nearest monitoring well of 1,400 feet. <br />5670 GREENWOOD PLAZA BLVD., SUITE 106 ENGLEWOOD, CO 80111 (703)721-0427 FAX (707) 721-6813 <br />GOLD COMPANY <br />
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