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<br />Ctoneham Series <br />The Stoneham series consists of well-drained. nearly <br />level to moderately sloping soils on uplands. These soils <br />formed in loamy, old alluvial material. <br />In a representative profile (fi:. 11). the surface layer <br />is li_ht ~nvish-brown loam about 5 inches thick- It is <br />noncalcareaus. Tile stlbsai] is brown sandy clay loam <br />about 9 inches thick. It is noncalcareous. The underlyiil~ <br />material is light-„moray sandy loam and ^nvelly ]oam <br />that is hi_hlp calcareous, :\t a depth of RO inches. it is <br />pale-brown gravelly sandy loam that is hi_hly cal- <br />careous. It ettends to a depth of about fi4 inches. <br />Stone]am soils absorb water at a madentc rate. and <br />the available water capacity is madentc. Permeability <br />is moderate, and the entire sail is suitable for roots. <br />Representative profile of Stoneham loam. 3 to J pef•- <br />cent slopes, in an area of grass. 170 feet, south and ~0 <br />feet east of the northwest corner of section `?l. T. 3 S.. <br />R. 59 tiV.: <br />dl-0 to 5 inches. Ilght ;ravish-brown (lOYR 0/_) loam, dolt <br />grayish brown (lOYIi a/_) when moist; weak, med- <br />ium. granular sttvcture: soft. friable: [nany dbrous <br />roots; noncalcareous; neutral; clear. smooth baua- <br />dary. <br />D=[~ to 13 inches, brown (lOYR 5/31 sandy clay loam. darlt <br />brown (lOTR i!3) when moist; moderate, medium. <br />prismatic structure parting Co weak to madente <br />subaagular bloc!tp structure; thin clay films on pMS <br />faces: hard. [rmble: noncalcareous: mildly alltaline: <br />gradual. smooth boundary. <br />C1ca-13 to ^_0 inches, li~hr-msy (lOYR i/.1 sandy loam. <br />pale brown (lOYR G/31 when moist: weak. medium. <br />suoangular blocky structure; hard. friable: calcare• <br />ous and canmins lime in splotches and disseminated: <br />moden Cely alkaline: Clear. smantlt boandary. <br />IIC.ca-?0 [0 30 inches. lizht ,eay (lOYR '/^_1 gncellp <br />loam, pale brown (lOYR 8/3) when moist: massive: <br />hard. friable: 15 percent gavel: calcareous and <br />contains rnmmnn, medium and caatse. lime mottles <br />(lOYR 9/.1 and disseminated lime; moderately alkn- <br />line: dear. smooth boundary. <br />IIC3-30 [n 60 inches. pale-brown llOYR fil31 gnvellS sandy <br />Inam. brown f10YR 5/3) when moist: massive: <br />sli[h[ly hard. very friable: 19 percent ;ravel: cal- <br />careous and conmins disseminated lime; moderately <br />alkaline: clear, wavy 6onndary. <br />The 3 horizon rances Irnm 3 to ~ inches in thickness. from <br />grayish brown to pale brown in color. and from heavy due <br />sands loam to lnnm in testate. The B horizon nnaes from <br />5 to 18 inches in thickness, CMnt brown to Iisht brown in <br />color- and Crnm lleht clay Inam to coarse sandy loam in tez- <br />tnre. Depth to calcareous material wages from 3 to 15 inches. <br />Stoneham loam, 3 to 9 percent slopes IS[DI.-This soil <br />has the profile described as representative for the series. <br />It is on uplands near major stream channels in scattered <br />areas throughout the county. The areas are uniform in <br />shape and range from 50 to 90 acres in size. Runoff is <br />generally medium but is rapid if the soil is unprotected. <br />The hazards of water erosion and soil blowing are severe <br />in cultivated areas. Gullies form in draina~eways in some <br />places. Included in mapping are small areas of sand <br />and gavel deposits and a fe~v small areas of Ascalon <br />soils. <br />,1Lost areas of this soil are cultivated. but some areas <br />have a cover of native gt~ss. Capability unit VIe-1, non- <br />irri_~ated; Loam_v Plains range site; tree planting suit- <br />ability group 1. <br />