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2008-03-20_APPLICATION CORRESPONDENCE - C2008086
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2008-03-20_APPLICATION CORRESPONDENCE - C2008086
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Last modified
8/24/2016 3:25:23 PM
Creation date
3/24/2008 12:16:28 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C2008086
IBM Index Class Name
APPLICATION CORRESPONDENCE
Doc Date
3/20/2008
Doc Name
Preliminary Draft Environmental Impact Statement
From
DRMS
To
BLM
Section_Exhibit Name
Red Cliff Mine Project
Email Name
SB1
Media Type
D
Archive
No
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Ms. Catherine Robertson <br />Mazch 20, 2008 <br />Page 3 <br />The narrative on page 3.2-20 needs to be amended to clarify that the <br />proposed coal waste disposal area will be located within the northern section <br />of the project area, not the southern section. In addition, we would <br />recommend that the proposed coal waste disposal location be included on <br />Figure 3-7. <br />The groundwater discussion in Section 3.2.5 provides an analysis of bedrock <br />groundwater occurrence and water quality. Based on our review of the well <br />completion information and available water level data there appears to be <br />insufficient information to infer that the estimated bedrock flow direction is to the <br />sough. Three wells were constructed and monitored, two wells monitor <br />groundwater within and below the Cameo coal zone (8-2-8 and 8-3-10), one well <br />more than a mile to the northeast monitors groundwater in the overburden (7-34- <br />7). The overburden well has better water quality and exhibits a substantial head <br />difference. The potentiometric level in the overburden well is significantly above <br />the screen interval whereas water levels in the coal zone wells aze at or below the <br />constructed screen interval. There is not sufficient data to determine a hydraulic <br />connection between the water-bearing zone encountered at we117-34-7 and the <br />Cameo coal zone. Rather than assuming that the three wells constructed and <br />monitored are hydraulically connected and represent a water table condition, it is <br />more probable that the water encountered at we117-34-7 is a perched aquifer or <br />saturated zone. The groundwater flow direction in this perched zone is more <br />likely to be to the northeast following the regional dip of the bedrock. <br />Additional monitoring wells would be required to fully characterize bedrock <br />groundwater occurrence and movement in the project study area. The <br />DRN~IS recommends the following minor modifications to the bedrock <br />groundwater discussion on page 3.2-29. <br />In the third paragraph on page 3.2-29 the following sentence: "The hydraulic <br />con~tection between the water-bearing zone and the Cameo coat zone that is <br />approximately 570 feet is also unclear."needs to be clarified and the reference <br />to 5'10 feet needs to be explained. We recommend that the last two sentences <br />of the third paragraph on page 3.2-29 be deleted from the text. <br />4. A couple of typographical errors were noted in Section 3.2.6 and 4.2.6. If <br />appropriate please revise the following pages accordingly. On page 3.2-35, in <br />the i~rst paragraph, third sentence the text should read high-quality water as <br />opposed to "high-quantity water': On pages 4-82 and 4-83 references to well <br />locations is given as Figure 3-9, USGS Stations This is incorrect and the <br />reader should be referred to Figure 3-8 for well locations. <br />5. Groundwater inflow to the mine is only briefly discussed in Chapter 3, Affected <br />Environment and in Chapter 4, Environmental Consequences and Mitigation. <br />Potential impacts from the inflow are described only with regard to groundwater <br />
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