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PERMFILE134411
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PERMFILE134411
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Entry Properties
Last modified
8/24/2016 10:35:06 PM
Creation date
11/26/2007 2:16:01 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1987171
IBM Index Class Name
Permit File
Doc Date
11/4/1987
Doc Name
SUBMITTAL OF FOUNTAIN COLONY PIT APPLICATION
From
MARK A HEIFNER
To
MLR
Media Type
D
Archive
No
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MININ6 PLAN <br />• <br />the Life of the operation. Of course, the projected volumes could be lower which <br />might reduce the lifespan by perhaps 25°x. Demands might be considerably higher, <br />as has been the experience in past years in the Colorado Springs and other areas, <br />and this could cut the life span by 50~. Therefore, as a range, it is projected <br />that each phase will last from two to ten years and the life of the operation will <br />be between 10 and 50 years. <br />We realize that this is quite a broad range, but in our experience and in <br />• <br />discussions with other companies in the Colorado Springs area, a 5:1 range ratio <br />is not unreasonable. <br />CHARA('I'F:RT$TTCwS ~ ~ (~$$`7E[, DEPOSIT: An exploratory program which was conducted <br />prior to preparation of this permit defined the gravel deposit. The gravel <br />generally seems to be somewhat thicker on the northern half to one-third of the <br />site. In some places, there are several feet of overburden on top of the gravel. <br />This is generally most true on areas along the western perimeter of the site. As <br />the edge of the mesa is approached, the gravel is much closer to the surface and <br />in places is essentially on the surface with no overburden. <br />The depth of the gravel ranges from about 5 to 10 feet thick on the south end <br />of the site to about 30 to 90 feet deep on the northern end of the site. This <br />depth tends to vary from place to place. An average figure for the whole site is <br />about 20 feet, plus or minus 5 feet. <br />Underneath the gravel is a shaley material which is related to or derived <br />from the Pierre Shale. Actual rock seems to outcrop considerably below the bottom <br />of the gravel. It is presumed that the material under the gravel which is related <br />to the shale is a weathered zone of material created during the period of time <br />between the time the shale was exposed and the gravel deposited. In some places <br />page 8 of 10 Exhibit D <br />
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