My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PERMFILE121331
DRMS
>
Back File Migration
>
Permit File
>
300000
>
PERMFILE121331
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
8/24/2016 10:19:44 PM
Creation date
11/25/2007 9:15:36 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
C1981035A
IBM Index Class Name
Permit File
Doc Date
12/11/2001
Section_Exhibit Name
2.04.7 GENERAL HYDROLOGY DESCRIPTION
Media Type
D
Archive
Yes
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
9
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
2.04.7 page 3 <br />• CLIFF HOUSE SANDSTONE <br />This unit comprises the caprock to the dip slopes of the area. Based on in1 <br />provided by the Menefee Land Company exploration drilling program for a propc <br />bordering the King Coal Mine, the sandstone is not saturated and is above the po <br />surface in the immediate project vicinity. No water was encountered in any drill t <br />program at a level above or in the Menefee seams. All wells in this unit were dry <br />House formation. The nearest water wells completed in this wut or the two units <br />below are as follows: <br />W-1 (#186332) -Ted Compton; .17 miles south of permit bounda: <br />W-3 (#199059) -Gary Etheridge; .43 miles south of permit bounda~ <br />W-9 (#077395) -Curtis Beyer; .42 miles south of permit boundai <br />U <br />• <br />MENEFEE FORMATION <br />The upper part of this formation contains the coal seam being mined at the <br />Mine. Fifty years of mining has not encountered any ground water in this formatie <br />Number 1, which is drilled in and draws water from the Quaternary alluvium, has ~~ <br />leve176 feet below ground level. Ground level at that point is at an elevation of 7, <br />sea level. The coal seam being mined is at an elevation of 7,450 feet. Thus, the m <br />located at least 136 feet above the potentiometric level. There is no indication tha <br />will be affected by the King Coal Mine. <br />An exploratory core drill hole located in the SE14 NW/4 of Section 32 (See <br />driven from the surface through all the overburden strata to the base of the Curren <br />upper Menefee coal seam. No water was encountered. A well core hole was drive <br />the mine bench near the water tank to a depth of ninety feet. The well was dry. T] <br />well is below the upper Menefee seam outcrop. These two holes along with the pr <br />mentioned active water wells indicate that the overburden strata, and strata at leas <br />twenty feet below the lower Menefee coal seam contain no aquifers. _ <br />-- The best evidence ts, owever, of no disturbed aquifers or no aquifers and r <br />water seepage in the mine workings themselves, except for the aforementioned "pe <br />aquifers. Water must be pumped into the mine from Weils # 1 and # 2 for dust a <br />This is a normal need for operating coal mines. Intake water used inside the mine <br />pumped out or discharged. <br />POINT LOOKOUT SANDSTONE <br />The Point Li~okout Sandstone is below the formation to be mined and will ~ <br />disturbed during.the mining process. The upper 100 to 140 feet is a massive sands) <br />or may not contain significant amounts of ground water. Wells have recently been <br />this unit for new real estate developments (Rafter J.) approximately eight miles ea <br />project area. Small amounts (max. pump rate of 30 gpm) of water were encounter <br />locations. <br />coal mine <br />e during this <br />'the Cliff <br />King Coal <br />n. Well <br />static water <br />390 feet above <br />ne will be <br />t the aquifer <br />ap C-3) was <br />mined <br />in 1978 on <br />collar of the <br />to a depth of <br />ground <br />fire control. <br />typically not <br />t be <br />to which may <br />filled into <br />of the <br />in some <br />August 2000 <br />
The URL can be used to link to this page
Your browser does not support the video tag.