My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP44711
DRMS
>
Back File Migration
>
Report
>
REP44711
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:47:13 AM
Creation date
11/27/2007 10:22:25 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981022
IBM Index Class Name
Report
Doc Date
4/1/2005
Doc Name
2004 Annual Hydrology Report
From
Oxbow Mining, LLC
To
DMG
Annual Report Year
2004
Permit Index Doc Type
Hydrology Report
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.
/
84
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
4.0 SEEP AND SPRING INFORMATION <br />Two spring monitoring points, SP-8 and SP-9 aze monitored and the results compared with <br />baseline and historic monitoring data. A significant change in the quality or quantity of flow <br />from these springs and seeps after retreat mining might indicate that the mine might be impacting <br />these water resources. <br />The data collected from Oxbow's groundwater monitoring stations, along with the results of <br />~.:~,.,. laboratory analyses are presented in Exhibit 2 -Groundwater Information <br />Spring SP-8 <br />Based on the quality and location of spring SP-8, it was determined that the source of the spring <br />was the abandoned Oliver Mine. Until 1999, flows from this spring were been relatively <br />consistent. No flows were recorded during any of the 2001, 2002, 2003 or 2004 monitoring <br />events. Based solely upon coincidence, Oxbow believes that water from the Oliver Mine may <br />have drained into the Sanborn Creek mine at the time of the 1999 mine fire event. Since this <br />event occurred, no flow from spring SP-8 has been recorded. <br />Spring SP-9 <br />• Spring SP-9 is a seep located at the base of a landslide feature in the Unnamed Gulch. <br />Historically, flow had been nearly continual, but at very low rates. The source of the spring <br />appears to be a shallow perched water zone dischazging from the toe of a surface slide feature. <br />During 2004 the spring SP-9 did not flow. <br />• <br />
The URL can be used to link to this page
Your browser does not support the video tag.