My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
REP46268
DRMS
>
Back File Migration
>
Report
>
REP46268
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/25/2016 12:49:22 AM
Creation date
11/27/2007 10:51:29 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1980005
IBM Index Class Name
Report
Doc Date
7/15/1992
Doc Name
GROUND WATER HYDROLOGY AT SENECA II PEABODY C-80-005
From
MLRD
To
SHAWN SMITH
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.
/
5
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
III IIIIIIIIIIIII III ~ ~ <br />STATE OF COLORADO <br />MINED LAND RECLAMATION DIVISION of ~o~ <br /> <br /> <br />Department of Natural Resources <br />~~,_. <br />~ <br />C-1-- \ <br />Nr3 <br />~ <br />$ <br />1313 Sherman SL, Room 215 <br />Denver <br />CO 80203 ~ i1 <br />, <br />303 866-3567 '+ra7e++ <br />FA%:303 832-8106 <br /> Roy Romer, <br /> Gwemor <br /> Mmnael B. Long, <br /> Division Director <br />TO: Shawn Smith, Reclamation Specialist <br />FROM: Jeff Martin <br />DATE: July 15, 1992 <br />SUBJECT: Ground water hydrology at Seneca II, Peabody C-80-005 <br />Seneca II Hvdrolooic Environment <br />The geohydrology of the Seneca II mine is extremely complex due to <br />lenticular sedimentary rock formations which have been folded and <br />irregularly thickened coal seams due to differential compaction <br />during deposition. <br />The permit area is virtually bisected by the Tow Creek anticline, <br />a ground water recharge area. Water entering recharge areas on the <br />west side of the anticline moves westward and northwestward to the <br />Hayden syncline structural low. Ground water flow on the east side <br />of the anticline moves southward and southeastward initially along <br />the plunging axis of the Twentymile Park syncline and eventually <br />into the Hayden syncline. A portion of the latter mentioned ground <br />water flow enters the Trout Creek aquifer several miles <br />downgradient from the permit area and may resurface in Trout Creek. <br />Surface water falling on the west and east sides of the Tow Creek <br />anticline moves laterally to the topographically low basins of <br />Grassy Creek and Fish Creek respectively. <br />Peabody Monitoring at Seneca II <br />Peabody Coals Inc. monitors a total of 43 wells in and around the <br />Seneca II mine, 20 of which are used to determine water quality on <br />a biannual basis (two wells had insufficient flows for sampling). <br />Each well is monitored in full compliance with Peabody's monitoring <br />plan. <br />Peabody compares ground water quality at the mine site to both <br />irrigation and livestock standards as set by the Colorado <br />Department of Health. Ground water in the area surrounding Seneca <br />II is not being pumped for either irrigation or stock watering. <br />Only well GW-S5-TC, the Seneca II shop well is used for domestic <br />purposes and as is later discussed, is not impacted by mining <br />activities. <br />
The URL can be used to link to this page
Your browser does not support the video tag.