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PERMFILE105032
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PERMFILE105032
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Entry Properties
Last modified
8/24/2016 9:58:06 PM
Creation date
11/24/2007 11:50:09 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1983142
IBM Index Class Name
Permit File
Doc Date
7/19/1983
From
PARAGON ENGINEERING INC
To
MLR
Media Type
D
Archive
No
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i , • • <br />1 <br />~; r~ <br />f <br />1~SA GRAVELLY CLAY LOAM, 2 to 5 percent slopes, Class IIIe Land (Me) <br />This soil is derived from old alluvium consisting mainly of materials <br />weathered from acid igneous and mixed igneous rocks, largely granite <br />and basalt, but includes smaller quantities of material from sand- <br />stone and shale. The alluvial mantle, for the most psrt,i ranges <br />from 5 to 8 feet deep but it is deeper in places. <br /> The 8- or 10-inch surface soil in cultivated fields is light brown <br />' when dry and brown when moist; its organic-matter content is very lou. <br /> the subsurface layer is light-brown or pale brown clr,~ loam containing <br />~ ' a considerable amount of cobblestones, rounded pieces of gravel, and <br /> chert fragments. Beginning at depths below 12 to 14 inches the sub- <br />' soil is very pale brown to reddish yellow and shows a considerable <br /> amount of white lime splotching. Lime encrustations appear on the <br />~, ' lower sides of the pieces of gravel, cobblestones, and stones that <br />laces the cobbl <br />ak <br />a <br />e <br />b <br />t <br />f th <br />il <br />I <br />t <br />0 <br /> p <br />y <br />m <br />e up a <br />ou <br />percen <br />e so <br />m <br />ss. <br />n som <br />5 <br />o <br /> material is more abundant than the gravelly, but in others smaller <br />' cobblestones and gravel are more abundant. In a few places the sub- <br /> soil material is weakly c•<mented into s semihardpan. Generally, <br />' however, it is permeable enough to permit the downward growth of <br /> deep-rooted plants. <br />' <br /> Surface runoff is medium, and underdrainage is adequate. The excess <br />' of gravel, cobblestones, and stones makes workability less favor- <br /> able than on Mesa clay loam soils. Saline areas occur only in a <br />t very few places bordering shale soils. <br /> Soil limitations are classified as severe for sanitary land fill <br />' (poor bank stability, rapid permeability), and sewage lagoons <br /> (rapid permeability belo~a 14"). <br />1 <br />..... <br /> <br />T <br />
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