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2016-12-09_REVISION - M1980244
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2016-12-09_REVISION - M1980244
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Entry Properties
Last modified
12/12/2020 4:16:45 AM
Creation date
12/9/2016 2:03:14 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1980244
IBM Index Class Name
Revision
Doc Date
12/9/2016
Doc Name
Adequacy Review Response #2
From
CC&V
To
DRMS
Type & Sequence
AM11
Email Name
TC1
AME
ERR
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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MEMORANDUM At <br /> Adrian Brown <br /> To: Gabe Racz, Vranesh and Raisch, LLP <br /> Gene Riordan, Vranesh and Raisch, LLP <br /> CC: Margaret Burt, Newmont Mining Inc. <br /> From: Adrian Brown, P.E., Adrian Brown Consultants, Inc. <br /> Re: Additional Information Request—Natural Water Level <br /> Date: August 11, 2016 <br /> Groundwater Flow in the Cripple Creek Diatreme <br /> The groundwater flow regime in the Cripple Creek diatreme is dominated by geology.The diatreme is located on <br /> a hill, and receives precipitation of approximately 20 inches per year(ABC, 2015).The volcanic rock in the <br /> diatreme is of moderate to low permeability, and in general approximately 6 inches per year of that incident <br /> precipitation infiltrates to the diatreme,with the balance evapotranspiring (ABC, 2015). However, small surface <br /> runoff occurs in some areas of the diatreme during high precipitation or thaw events, which results in a modest <br /> reduction in the amount of infiltration and evapotranspiration within the diatreme. The diatremal rock is <br /> surrounded by low permeability Precambrian gneiss, schist,granite, and granodiorite,which serves as a <br /> container for the groundwater in the diatreme (Lindgren and Ransome, 1906). The geology of the Cripple Creek <br /> mining district is shown in Plate 1. <br /> The extent of the diatreme is presented in Plate 2. The diatreme comprises three steep-sided eruptive centers, <br /> at the north,west, and south, where upwelling volcanic matter was ejected. In addition,there is a gently <br /> thinning volcanic rockmass to the east,where volcanic material flowed after being discharged from the volcanic <br /> centers.This overflow apron is generally devoid of economic gold. <br /> Historic (Pre-Mining) Groundwater Elevation <br /> The elevations of groundwater in the Cripple Creek mining district prior to the inception of mining were <br /> obtained in the pioneering study of the (then) 277 underground mines in the district performed by Lindgren and <br /> Ransome(1906).The district and the mines they inspected are shown in Plate 3. <br /> During the study of the mines Lindgren and Ransome carefully recorded the hydrogeology of the "wet" mines in <br /> the district, collecting information relating to the water level prior to and during operation,which is reported in <br /> detail in Chapter XII—Underground Water.This information is summarized on Plate 4,taken from Pages 240- <br /> 241 of Lindgren and Ransome (1906). In addition, Lindgren and Ransome provide a diagram showing this <br /> information,which is presented in Plate 5 of this memorandum.At the base of Plate 5 is a summary of the <br /> name, location, pre-mining water elevation estimate, and first water encountered. <br /> The pre-mining water level data that is presented in Plate 5 is plotted on a map of the diatreme in Plate 6.The <br /> following observations are made: <br /> Page 1 <br /> Adrian Brown Consultants, Inc. <br /> 130 W.4ch Ave., Denver CO 80223 <br /> 303-698-9080 www.abch2o.com <br />
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