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PERMFILE124956
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PERMFILE124956
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Entry Properties
Last modified
8/24/2016 10:22:27 PM
Creation date
11/25/2007 1:16:54 PM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1982079
IBM Index Class Name
Permit File
Doc Date
4/8/1982
Doc Name
LIMITED IMPACT 110 & SPECIAL TEN-DAY 111 PERMIT APPLICATION FORM
Media Type
D
Archive
No
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<br />u <br />3-62 ~ <br />cREi;Lr~ sE~clEs <br />These are well drained, moderately coarse textured, terrace soils <br />developing in moderately coarse textured, calcareous, stratified water <br />lain materials which have been derived from a variety of parent rocks, <br />buried subsoils often occur. <br />These soils occupy the level to gently sl.opng high terraces, the "fan- <br />li.ke" areas at tho mouth of small draina~~e ways and occur on the moderately <br />coarse textured flood plains of the larLer intermittent streams of the <br />uplands. <br />The Greeley soils a.re moderately productive soils. They have a moderate <br />crater holding capacity; are easily tilled over a wide range of moisture <br />content and are moderately rapid in permeability. <br />SOIL PROFILE <br />Surface Soil <br />0-8 inches, grayish brown fine sandy loam. Very friable, with <br />fine granular structure; non calcareous. <br />,,~ Subsoil <br />. 8-29 inches, grayish brown and brown sandy loams. Friable when <br />i' moist, with coarse prismatic and blocky structure, <br />usually calcareous. <br />Parent Material <br />29 inches plus, pale brown sand loam which grades to a sand <br />at depths below 36 inches, usually calcareous. <br />Variations <br />There is considerable variation in the parent material part of the <br />profile in regard to texture and depth. <br />Mappln2 Units <br />S of <br />Generalized Description <br />72, 892 (Field Sheet) Deep and moderately deep, sandy terrace <br />18 (Published Map) soils with loamy sand surface soils and <br />sandy loam subsoils underlain by a light <br />colored, lifrp~ sandy loam water lain parent <br />material. Occupying ........... <br />~n <br /> <br />
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