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<br /> <br /> <br />. <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />- <br />{ A- <br />L!LGJ <br /> <br />I~ <br />~ <br /> <br />Comanche Creek and Wolf Creek Floodplain Study <br />Adams County, Colorado <br /> <br />4 Miles <br />J <br /> <br />3 <br />1 <br /> <br />Scale 1: 126.720 <br />1 2 <br />1 <br /> <br />o <br />LJ <br /> <br />1 <br />I <br /> <br />GENERAL SOIL MAP <br />ADAMS COUNTY, COLORADO <br /> <br />U. S. DJJ'[lRTMENT OF AGRICUl.TURE <br />SOIL CONSERVATION SERVICE <br />COLORADO AGRICULTURAL EXPERIMENT STATION <br /> <br />I <br />104020' <br /> <br />\!V <br />UID6 <br />40 <br />287 <br /> <br />COUNTY <br /> <br />I <br />104030' <br /> <br />@ <br />-~ <br /> <br />I <br /> <br /> <br /> <br /> <br />'(1 <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />Plafner-Ulm-Renonill association: Nearly level fa sfrongly sloping, well-drained, <br />loamy soils formed in old a lIuvium on interbedded sha Ie and sandstone; on uplands <br /> <br /> <br />Jr <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />3 <br /> <br /> <br /> <br /> <br /> <br /> <br />St["8~~11'!r\ <br /> <br />- <br /> <br />36131 <br /> <br />( <br /> <br />3 <br /> <br />~ <br /> <br />r <br /> <br />UNION <br /> <br />PACIFIC <br /> <br />3 <br /> <br /> <br />1 <br /> <br />1 <br /> <br />.~.... <br /> <br />~.. <br />:: <br />t:; <br /> <br /> <br />............'.....'./.'........................ <br />. ... .... .. .... <br /> <br />( <br /> <br />~ <br />;-yrG <br /> <br /> Compiled 1972 <br />~ J H= ,. <br />ill' '\ .1'/ <br />'\ 1 <br /> :t> <br /> <br />111 <br /> <br />/; <br /> <br /> <br />J <br /> <br />*Texture refers to the surface layer of the mojor soils unless otherwise stated. <br /> <br />Arvada-Heldt-Nunn association: Nearly level, well drained, loamy and clayey soils <br />formed in alluvium; on (erraces and fans <br /> <br />~~) <br />ft <br /> <br />1 <br /> <br />Terry-Renohill-Tassel association: Gently sloping to steep, well-drained and some- <br />what excessively drained, loamy soils formed in materials from soft sandstone and <br />shale; an uplands <br /> <br />Bloke land-Va lent-Terry association: Undulating to hilly, somewhat excessively <br />drained, dominantly sandy soils; on uplands . <br /> <br />iJ <br /> <br /> <br />Nunn-Satanta association: Nearly level, well-drained, loamy soils formed in alluvial l <br />materials that ore underlain by grovel in same places; on terraces and fans <br /> <br /> <br />/# <br /> <br />Alluvial land association: Nearly level, poorly drained to well-drained, loamy and <br />sandy soils formed in stream and river deposits; on flood plains <br /> <br />R.62W. <br />R.63W. COUNTY ~ <br />I WELD <br /> <br />T-~--v? <br />H) <br /> <br /> <br />Ascalon-Vona-Truckton association: Nearly level to stra{lgly sloping, well-drained <br />and somewhat excessively drained, loamy and sandy soils formed In wind-laid <br />deposits; on uplands <br /> <br />\J ) \ <br />" <br /> <br /> <br />- i ~Samsil-Shingle association: Sloping to steep, excessively drained, clayey and <br />.. . loamy soils formed in materials from soft shale and sandstone; on uplands <br /> <br />\. <br /> <br />Weld-Adena-Calbyassociation: Nearly level to steep, well-drained, loamy soils <br />formed in wind-laid deposits; on uplands <br /> <br />1 <br /> <br />I{I/ 1/ <br />SOIL ASSOCIATIONS* <br /> <br />-~3-~(J <br /> <br />---, <br /> <br />R. 61 W. <br /> <br />R. 64 W. <br /> <br />---...- <br /> <br />----- <br /> <br />- - .. <br /> <br />- -- <br /> <br />- -- <br /> <br />~ <br />~ <br /> <br />""- <br /> <br />~ <br /> <br />G> <br />c: <br />n <br />:7 <br /> <br />) <br />19 <br /> <br />::::::::=t~._ <br /> <br />Ii <br /> <br />; <br />