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ty�:aw <br />UILDING rr b <br />60 ROW f <br />'50' BUFFER ° <br />l FROM LINE <br />- / 5 BUFFE <br />jf <br />..- <br />° 1�ERMI7= fl1JNACt <br />pip <br />f'] <br />�r °� a• <br />f �, a` Q � <br />} 0 <br />L,P <br />C4 0 <br />#= p�Q0 <br />'1+; R'C � t'3"',' 'k- �'�£7_4' -4„ -i1�iF � ,��r w:F °+ r� �✓ <br />"=sue+ . ' ,�• ' ';� `�C,�.'i �� �', •" ,i +� ' ^st ?� " 1` '' ^�,, . 1J � � <,�> �� �' <br />eV <br />V <br />Q Q C) L <br />k <br />i + �' <br />MW <br />„_� -. Pr - r `i4 - - ,cy'. `"`yam A.`,• <br />'�-"'� - �' _`'� -' -3 - .� �" -`�,r - °firer i„�.,;a: . $c... `-.r`- `�x'�. '� �° '��s'� �•_'� - - - ,±'��ks.{k-•�� <br />NORTH <br />600 0 600 1200 1800 <br />�.r <br />{ IN FEET) <br />1 inch 600 ft. <br />- LEGEND a " <br />PERMIT BOUNDARY Q <br />_ _acct— ���► o �, —3 ow - EXISTING ROAD — — — — — — — <br />EXISTING STRUCTURE <br />BUFFER <br />t` >• Via. <br />ROM UNE ;, Y; .,. ;a - Ca <br />Cascajo soils and gravelly Z <br />land <br />HaC Harvey loam 1 to 9 percent i <br />°rt` ,• i;,; . slopes <br />WEB Wilid silt loam, 0 to 3 percent <br />slopes W <br />- - �'�` °;'' W�^:,• :r�;� <br />m rn <br />, <br />SOIL NOTES: w <br />a = ,;.. <br />M1. fii`, <br />�,;'. " =yt•`,, ;,•,!Y 1. Co– Cascajo Soils and Gravely Land. This series consists of <br />.j i "n'' ;' "• .., deep, excessively drained soils on terrace edges, breaks, fan <br />terraces, and sandy, calcareous alluvium. Slopes range from 5 <br />to 15 percent. The natural drainage class is excessively drained J <br />and water movement in the most restrictive layer is moderately <br />w.,a,p high to high. There is no zone of water saturation within a O <br />♦ //'//' ), a depth of 80 inches. This soil series is not considered prime <br />farmland. <br />2. HaC– Harvey loam. 1 to 9 percent slopes. This units parent <br />LL:,,,; :' ' material consists of calcareous loam eolian deposits. Depth to <br />Y P P Z <br />* '` ,: 7 :, _ a root restrictive layer is greater that 60 inches. The natural p <br />' „s drainage class is well drained and water movement in the most Z a) <br />i” '` restrictive layer is moderately high. There is no zone of water Q j <br />%rl <br />.r .4" saturation within a depth of 72 inches. Organic matter content 3 in the surface horizon is about 2 percent. U Q F-- <br />3. W113–Wiley silt loam. 0 to 3 percent slopes. Components of this <br />unit are plains soils. The parent material consists of loess. J LL <br />r <br />-`_• - ,b��,�`;� ,j.�• °•" ; , �_ =, �_ :'`�E #= Depth to a root restrictive layer is greater than 60 inches. The O- J <br />< -•'- -., e" natural drainage class is well drained and water movement in Q W <br />X > OJ <br />'' F= ,�n'a =. `" *;: q, the most restrictive layer is moderately high. There is no zone <br />of water saturation within a depth of 72 inches. Organic � R <br />� 4;' ,j.��G•' � +r,x.,'f�s'� matter content in the surface horizon is about 1 percent. �G/ p yj <br />} <br />5 Z) <br />�' , VEGETATION NOTES: a Z U- <br />LU <br />C�;; w <br />_ fk,:i I^ 1. Proposed permit area is currently used for rangeland. Z O m <br />2. Existing vegetation on the site is typical of the high arid plains. = p' <br />y• Ground cover is primarily composed of pasture grasses such as W W <br />�?' wt, "' blue grama. Low growing shrubs such as Skunkbrush Sumac or W H <br />3' 0 � w , �;, 1�{,' - ;F;i,��;� yucca may also be present, especially in ravines and drainages. � <br />Aux <br />LL C1 <br />IN+' <br />" "4•, _P `q: , W <br />, _ _ <br />