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2009-03-04_PERMIT FILE - C1981008A
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2009-03-04_PERMIT FILE - C1981008A
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Last modified
8/24/2016 3:44:05 PM
Creation date
5/19/2009 10:09:24 AM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981008A
IBM Index Class Name
Permit File
Doc Date
3/4/2009
Section_Exhibit Name
Section 2.04.9 Soils Resource Information
Media Type
D
Archive
Yes
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too greater than 72 inches with a mean depth of 53 inches. These deposits have stabilized and <br />formed cambic horizons and in some places weak argillic horizons. Additionally, they have <br />developed secondary accumulations of carbonates. The accumulation of carbonates is reflected <br />in a higher pH in the Bk and Btk horizons. The pH in A, Ap, ABt, Bw and Bt horizons (Lift A) <br />averages 7.7 and in the Bk Btk and C horizons (Lift B) averages 8.2. Soil in this map unit is used <br />primarily for irrigated pasture and hay crop. Barx soil is the second component (30 percent) in this <br />map unit. Barx/Darvey is a prime farmland soil in San Miguel County; Colorado if the soil is irrigated <br />by an adequate and dependable water supply. Attachment 2.04.9-6 is a letter from the Montrose <br />County NRCS stating that Barx/Darvey soil in the survey area does not have an adequate or <br />dependable water supply for irrigation. Barx/Darvey soil was therefore not considered prime <br />farmland soil in the survey area during mining until a revised assessment was made by the NRCS <br />in February 2008 (Attachment 2.04.9-10). As of February 15, 2008, the entire field south of BB <br />Road and west of 2700 Road containing this unit is considered prime farmland since it is more than <br />67% prime farmland soil type, and is being handled as such by the Western Fuels - Colorado LLC. <br />This property is entirely owned by Morgan. <br />Map unit 98F occurs in natural drainage areas that eventually form shallow valleys on the mesa and <br />on the floodplain of Tuttle Creek. Depth to bedrock varies widely in this map unit. Haplargids with <br />varying depths to bedrock form on drainage side slopes. Endoaquepts are formed where irrigation <br />water has accumulated in drainage bottoms. In a few naturally occurring areas of water <br />accumulation Endoaquolls have formed. <br />Eolian sands are intermixed with Cretaceous Dakota and Burro Canyon Formations in map unit <br />98G. Soil is generally moderately deep with significant inclusions of shallow soil on convex slopes. <br />Soil salvage in this map unit may yield slightly less than predicted. <br />Map unit 98H occurs on mesa side slopes that are not as steep as those found in map unit 98B. <br />Hardness of bedrock varies depending on the underlying strata. Wahweap soil has the same <br />physical and chemical properties as those soils similarly named in the survey area. Wahweap is <br />outside the range of characteristics compared to the survey area, in that it occurs in an area of 7 <br />inches mean annual precipitation. <br />(Revised June 2008) 2.04.9-19
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