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2004-08-19_REVISION - M2003037 (4)
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2004-08-19_REVISION - M2003037 (4)
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Last modified
6/15/2021 2:52:09 PM
Creation date
11/21/2007 6:33:58 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M2003037
IBM Index Class Name
Revision
Doc Date
8/19/2004
Doc Name
Part 2 Exihibit L Addendum 1
From
Haldorson and Sons Inc.
To
DMG
Type & Sequence
AM1
Media Type
D
Archive
No
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m~ ~~~ ~~~i~f~$ <br />CONSULTING GEOTECHNICAL ENGINEERS AND MATERIALTESTING <br />Greg Lewicki and Associates <br />11541 Warrington Court <br />Parker, Colorado 80138 <br />Attention: Mr. Greg Lewicki <br />Subject: Haldorson Property near <br />Montrose, Colorado <br />Mr. Lewicki: <br />February 24, 2004 <br />PN: M04030GE <br />This letter summarizes some geotechnical engineering comments <br />regarding the subject property. The comments are based on our <br />experience with numerous geotechnical engineering studies in the <br />area. <br />It is our opinion that the proposed property is generally <br />hydraulically isolated from the groundwater source and conditions <br />of the Spring Creek Mesa area to the south and west by an exposed <br />ridge of Mancos Shale and to the east by a deeply incised <br />drainage channel, referred to as Mexican Gulch. <br />The Mancos Shale typically has low permeability which resists <br />groundwater movement except along fractured zones which are <br />typically small and isolated. The general location of the Mancos <br />Shale ridge is shown on the attached figure. <br />Mexican Gulch is deep and completely penetrates the sand and <br />gravel cap of Spring Creek Mesa. The sand and gravel cap is <br />generally the permeable material which stores and transmits <br />groundwater. <br />The general trend of the area is down to the northeast. This <br />leads to the likelihood of potential water sources north of the <br />site to flow to the northeast and away from the site. <br />Because the gravel layer is discontinuous to the east the <br />ground water is not able to travel to the site from the east. <br />The Mancos Shale to the south and west of the site resists <br />groundwater movement to the site from the south and west. The <br />only likely source of groundwater charge is from irrigation very <br />local to the site, such as the irrigation water applied directly <br />on the surface of the site and the small agricultural area <br />immediately adjacent to the site. It is not likely that <br />sufficient water is applied to the site or the area adjacent to <br />the site to result in significant groundwater on the site. <br />P. 0. BOX 3986 P. O. BOX 0045 214 BODO DR. <br />GRAND JUNCTION, CO 81802 MONTROBE, CO 8140Y DURANGO, CO 81301 <br />(aro)z4s-ssas (s7a>s4a-slsa (aTO)zsa-soas <br />
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