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2010-04-14_GENERAL DOCUMENTS - C1981008 (2)
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2010-04-14_GENERAL DOCUMENTS - C1981008 (2)
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Last modified
8/24/2016 4:03:56 PM
Creation date
4/15/2010 12:07:23 PM
Metadata
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Template:
DRMS Permit Index
Permit No
C1981008
IBM Index Class Name
General Documents
Doc Date
4/14/2010
Doc Name
1998 Jim Irvine Order I Soil Survey
From
Greg Lewick and Associates, PLLC
To
DRMS
Permit Index Doc Type
General Correspondence
Email Name
MLT
SB1
Media Type
D
Archive
No
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order I Soil Survey, New Haracm Mire <br />�I <br />MAP UNIT; 98D — Bowbac ® Bowdish complex, 0 to 3 punt slopes.. <br />MAP UNIT SETTINGS <br />Slope Range: it to 3 percent <br />Elevation Range: 56100 to 5760 feet <br />Aspect: All <br />Landform: Mesa <br />Parent Material: Eolian deposits over residuum <br />Mate Geologic Symbol: Qe — Eclian Sand over Kdb p Dakota and Burrs <br />Canyon Formations <br />COMPOSITION <br />66 percent Bowbac sail <br />26 percent Bowdish sail <br />Contrasting Inclus <br />8 percent Progresso sail <br />2 percent shallow sail on <br />INTERPRETATIONS <br />aver hard sandstone <br />convex slopes <br />Lift Layers: <br />Lift Layer I Average Depth: 12 inches <br />Lift Lager 2 Average Depth: 17 inches <br />Total Lift Layer Average Depth: 2 inches <br />Other C onsiderations: Hardness of bedrock varies from weathered shales, <br />mudstones and sil #stones to some hard sandstone. Bowbac differs from Bowdish <br />as follows: Bowbac has a weak argillic horizon, Bowdish has a Iambic hnr17on. <br />Both have secondary accumulations of carbonates. Bowbac occurs over soft <br />weathered shades, siltstones and sandstones. Bowdish occurs over hard <br />sandstone. <br />Page: 7 of 43 Date: DEP 1198 <br />
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