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2013-04-09_REVISION - M1977215 (4)
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2013-04-09_REVISION - M1977215 (4)
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Last modified
6/15/2021 2:28:23 PM
Creation date
4/29/2013 3:39:17 PM
Metadata
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Template:
DRMS Permit Index
Permit No
M1977215
IBM Index Class Name
REVISION
Doc Date
4/9/2013
Doc Name
SUBMITTAL OF COMPLETENESS ITEMS
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OPERATOR
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DRMS
Type & Sequence
AM1
Email Name
RCO
Media Type
D
Archive
No
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• <br />4 <br />have a moderately water storage <br />II <br />terials would hay. <br />These treatment should be moderate. <br />capacity. Permeability but mixing would tend <br />high natural fertility vigorous <br />moderately hig E <br />and revegetation is discounted as <br />have m Supplemental fertilization t© insure vlg <br />These soils h slightly. <br />to lower fertility <br />suggested• €easible <br />growth is economically an an <br />dressing susceptible <br />If t ©p scheme, some other method of stabilizat <br />are very to <br />be <br />treatment since fine ter gravel surfacing <br />to o sinc d water'xerosion. Chemical stabilizers or g <br />to both wind and <br />are viable alternatives- volcanic <br />deep soils derived from welded ashflow <br />. <br />Area Qom ,, g captains shallow to Gulch formation. This poorly moderately . ro d uce well. °drained, i <br />bedrock, weathered by mechanical action to P ► <br />land disruption tuff has weathered largely to ventilation <br />coarse textured soils. <br />lan s road <br />the vent travels o ls ; <br />lion in Area B will be an access roe <br />t <br />The major depth of 2 feet. <br />orough Actual production acres lost exceed a a thin veneer <br />p portions, soils seldom ,. covered by only slabs w P n occur as shallow as 4 only evidence y only <br />of development <br />slabs organic c ater a h trees. surface layer w elop <br />n <br />is a mcturiaa anchored organic by matter in the natur ally, the <br />small accumulation of of clay i the subsoils• largely by depth. <br />occasional a ht concentration zmited <br />bility of these to supply nutrients is 1� <br />ability of these materials <br />productivity the small <br />consequently site p ark are ity incre asel s i n the sofand <br />clay <br />Soil depth and conseq <br />The stable soils in eboX lls�• Organic s`atthasphorus <br />exhibit n A B C profile sequence (Cry en and P <br />accumulations an A- <br />accumoletrond increase availablehforpplant growth- <br />depth and therefore nitrogen <br />are more readily <br />t -apes <br />cold, thin' well - drained soils on steep sides <br />lopes. <br />large percentage of the area where <br />Rock g consists of 2-4" large p slopes have high runoff <br />s outcrops and in slides 4" tick. <br />arches �-'� elation due to lack of soil. <br />hazard d and only storage patches <br />of water for vegetation due to due s o lack <br />hazard and Poor a <br />essential to help control runoff and erosion. <br />Revegelation efforts will be slow and costly <br />of topsoil -, but essential disturbance <br />equipment and confine mast <br />The v evere stop he more gradual to Soils in these more stable <br />slopes will limit the use of oboral €s- <br />to the slopes. deep Cry <br />s ope p moderately ryoborat accumulation of <br />slope have are well long enough to exhibit a significant supplies of <br />lop enoug to retain notable moderate to <br />clay have been horizon, gyoung enough Fertility nanotable <br />is <br />primary rn min r B is and yet <br />primary minerals and available plant nutrients. <br />high. <br />- 39 - <br />
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