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inches of sandy, graveh alluvial detxrsits I lacking signilie:mt humus and clay "tines') in ttx <br />subsoil, txneath I to I!5 t~et of the deuritxJ surface soils. fire ,ruh-surface soil furs no <br />significant content of prrHdercd caliche. topsoil is confined to atxrut a foot to u halt=lirot of <br />silty clay loam. '.SlaB' Afesn C'Jat' Loam occurred in a small north portion of the site helirrr <br />it vvas completely remoccd in prior gravel retraction operations, and is therefore no longer of <br />consideration here. for this operation. onlc ttx top portions of the Shavarw Mesa occurring <br />in A1Gf soils shall br stripped anJ rxcavuted for gravel extraction. 'afaC" :Nock grarcllt• <br />clot' lua-n S-l0°o. 'Ru' Rough hrr,krn lrrnrl, 'Rr' Rock orucrnp and Rough broken land, <br />',NaB' .flack clop loam 1-S°n, and ':11aC' :Hack c!u}' loam 5-111°o u~ils are talis and r<xk <br />outcrop un the nresa sideskrpes ucrr the rim ul the mesa and only invoked in the prcrFxrud <br />operation as a possible alternative access roure. -their depth descriptions are not relx+ncd and <br />thou soils arc not recmrrahle tier plant gnnvTh medium. Their depths are then of rxr <br />pragmatic value here. 'M!8' Mese Clav Loam 2-SYe and ',1faB' :1feh~a C7aP Lrrone a urring in <br />cast ofthe permit area are not to t+e involved with ttx permitted operation. <br />l~he prcviuusly submitted reproduced portion of the Ucln- :14unrrnsc Arco. (7) .sheer .~'urnhcr 3.i <br />of the Natural Keu+urccs Conservation Service soil map shows the location of the described soils. <br />E 1 MontroeoCo 13hsvanoGrav l AmondADDI t Ezhl <br />+a++ro~ <br />