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y- .~ <br />• • <br /> <br />,7p <br />The Haplaquolls soil is very deep and very poorly or <br />( poorly drained. It formed in alluvium. The surface layer <br />is grayish brown sandy loam, loam, ar clay loam 7 to 22 <br />inches thick. The underlying material is gray stratified <br />sand, loamy sand, sandy laarn, loam, clay loam, or clay. In <br />Borne places sand or er,tremely gravelly sand is at a depth of <br />16 tc~ 6u inches. <br />PermeaCility of the Haplaquolls soils is moderate to <br />rapid. AvailaGle water capacity is low to high. Effective <br />ray?ting depth is erg inches or more for water-tolerant plants <br />ar~d lCr tc~ ZCr i aches f~?r p I ants sensitive to a h i gh water <br />taGle. Runoff is slaw ar- paraded, and the hazard of water- <br />erasion is slight. The hazard of sail Clawing is slight.. A <br />high water- taG l e i s at c. r• near- the surface dur i rig the spring <br />{• and ear I y surnrner. Ire Borne areas the water- tab I e remains <br />aG~~ve a depth of 1 foot thr-ougFiout the year- wh i I e i r~ otF~er <br />areas the water- tats I e i s at a deptF~ of 1 to _: feet dur i rig <br />late summer, fall, ar~d winter. The hazard .?f flooding is . <br />frequent. <br />This unit is used far livestoc4; grazing ar~d wildlife <br />habitat. <br />Native vegetation an this unit varies from area.to area <br />but consists mainly of rushes, sedges, cattails, and <br />willows. <br />This map unit is in capability subclass VIw. <br />r! <br />l~ <br />-~ <br />