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PERMFILE138996
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PERMFILE138996
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Entry Properties
Last modified
8/24/2016 10:39:46 PM
Creation date
11/26/2007 8:14:19 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1977129
IBM Index Class Name
Permit File
Doc Name
APPLICATION FOR MINING AND RECLAMATION PERMIT
Media Type
D
Archive
No
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' • • EXAIBIT I/J (Cont'd) <br />dark mineral grains; 67 to 70 percent basalt gravel; 'risible <br />' secondary calcium carbcnate, costly finely divide3; calcium <br />' carbonate eaui-ra_].ent a_rro~:inately <br />alkaline; gradual wavy boundary. <br />IIC3ca 28-60"--Sand, gravel, and cobble with <br />' mostly basalt; common dark mineral <br />soya accumulated secorda_~-y calcium <br />3J percent; noderataly <br />:oarse fragments being <br />:,rains; calcareous, with <br />carbonate on the underside <br />' of sand and pebbles. <br /> The Al horizon is gravelly sandy loa= or gravelly 1c~3. <br />1 <br /> 3~-c <br /> Elacs ton stony lose, 3 to 25 percent s_opes (Btn).--ibis gently <br /> <br /> sloping to steep soil occurs on high terraces an3 benches. It has <br /> the profile described as typical for the series. Included in mapping <br /> is up to 10 percent of litalire and Avalon soils. Also included in <br /> some places are small areas along terrace edges that have shale or <br /> sandstone bedrock at depths of 36 inches. <br /> Surface runoff is moderate to rapid a~3 th_ erosion hazard is <br />' moderate. <br /> The soil is used mostly for graying and as a source of gravel. <br />' G <br />3 b <br />'1 <br />it <br /> rave <br />p <br />s an <br />orrow areas are co~~on. <br />1 <br /> (Capability unit VIe-1; range site, loamy salt desert.) <br />' 2 <br />Ri <br />0 <br />t <br />( <br />' <br /> percen <br />verwash <br />to <br />slcpes <br />/~,, <br />{r Rd <br /> This is a miscellaneous land type consisting of fine sand, gravel, <br />1 cobblestones, and water-worn stones. It occurs along the Gunnison <br /> and Colorado Rivers and is subject to occasional partial overflow <br /> because it lies cnly 4 to & feet above the normal water level of <br />1 the streams. A.s a rile, the deposits at the higher levels have <br /> somewhat hummocky relief and consist mainly of sand, loamy fine <br /> sand, an3 fine sand with a few strips or patches of gravel in <br />' places. alt lower levels, the gravelly and cobbly materials are <br /> 33 <br /> <br />
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