My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE49324
DRMS
>
Back File Migration
>
Permit File
>
500000
>
PERMFILE49324
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:51:14 PM
Creation date
11/20/2007 1:59:06 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1984062
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
2.04 Information on Environmental Resources
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.
/
115
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
• characteristics by the II.S. Geological Survey, CYCC and independent <br /> consultants. Pump tests were conducted under various geologic <br />conditions and with the use of observation wells and continuous <br />water level and discharge recorders. The results of these teats are <br />listed in Table 27, Aquifer Characteristics. Data and analyses <br />derived from the pump tests are presented in Eahibit 19, Aquifer <br />Test Data. The overburden aquifer has an average permeability of <br />3.4 gallons per day per square foot (indicative of low yields), <br />storage coefficient of 1.12 a 10'5 (in the range of typical <br />confined, Artesian aquifers with low porosity) and an average yield <br />of 5.5 gallons per minute (suitable for small stockvater or domestic <br />supply). Due to low permeability and Limited yield, the overburden <br />could only be considered an aquifer for the specific use of loin <br />• yielding wells for small demand. <br />Ground Water Recharge Characteristics <br />The proposed permit and adjacent area is Located in a semi-arid <br />climate, with average annual precipitation of about 16 inches. Moat <br />precipitation is lost to runoff, evapotranspiration and sublimation, <br />minimizing the amount available for ground water recharge. The <br />unconfined alluval aquifers are recharged in the spring when the <br />snowmelt eater infiltrates through the alluvium. The confined <br />overburden aquifer is recharged predominantly by infiltration in the <br />. outcrop area delineated on Map 4, Mine No. 3 Hydrology. <br />2.04-40 <br />
The URL can be used to link to this page
Your browser does not support the video tag.