10-18-2004 Planning Packet - Laserfiche WebLink

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RANCI-: IN CHARACTKRISTICS: Solum ihicknc^s and depth to tree carbonates range trom 24 to 54 inches CoaiM.* fragments of mi\ed lithology compiise 2 to S pcrccri of the volume of the control section The A horizon has hue of lOYR. value of 2 or 3. and chroma ol I or 2 Tttc Ap horizon has value of 4 or 5 and chroma of I or 2 and value of 6 when dry The E hotizon has hue of lOYR. value of 4 or 5. and chroma of I or 2. The A and E horizons tvpicallv are loam, silt loam, sandy loam, or fine sandy lo.im. but include clay lo.iin. if eroded They are ncutial to medium acid The Bt horizon has hue of lOYR m e upper part and lOYR or 2 5V' in the lower p.trt. value of 4 or 5. and chroma of 3 through 5. Mottles arc present m the lower subhorizons in some pedons It typically is clay loam or loam, but sandy clay loam is in parts in some pedons. The argilhc horizon has IS to 35 percent clay and 30 to 45 percent sand It is slightly acid to strongly acid. Some pedons have a BC horizon. The C horizon has a hue of lOYR or 2.5Y, value of 4 or 5. and chroma of 3 through 6. It IS loam or clay loam. It lacks mottles in some pedons. It has 15 to 25 pcrcrnl calcium c.»rbonaie equivalent and is mildly or moderately alkalikne COMPETING SERIES: These arc the Amanda. Bclrnom . Belmoie. C-hj-muU. CM. Coggon . Conestoga. Douds . F.l Para. Gallman. Grcllton . Hebron. Hickory. High G,i_r. Hollinger . Kalam.izoo. Kanawha. Kend.allvillc. Kidder. Kosciusko . LcRcy. l,etog. Lindiev. McHcnrv. Mandcvillc. .Maitinsville. Miam.i. Mifflin. Military. ^’^Ime. Ocklev. Owoss o. Pecatonica. Pnneeton . Rawson. Relay. Rgnova. RicJjlir.d. RuM5. Rockbridge . Roseville. Sisson . Strawn. Stitr.mitville. Tcanawav. Theiesa. Wa_w^ee. Westville. Whalan. and Woodbine soils in the same family Amanda horizon soils have more illitc in the B and C horizon; Belmont soils have redder hue in the B horizon. Belmore. Chili. Kalamazoo, and Ocklcy soils formed in glacial oatwasn and have sandy or sandy-skeletal 2C horizons. Chcnault soils have chert fragments in the solum and arc underlaid by limestone bedrock. Coggon. Gallman. Hickory. Pecatonica. Renova. Riddles. Summiiville. and Wcsivillc soils have thicker sola. In addition. Coggon soils have low chroma mottles in part of the B2 horizon. Conestoga. Kendallville. Lctort. Richland, and Rockbridge soils have more coarse fragments Douds. El Dara. Kidder, Sisson, and Wavvasee soils have less clay and more sand or silt in the lower p.irt of the B horizon and in the C horizon. High Gap. Hollinger. .Mandcvillc. .Mifflm. Military. Norden. Roseville. Whalan. and Woodbine soils have bedrock bcginnmg between depths of 20 and 60 inches. Grcllton. Hebron. Lindlcy. and Raw-son soils have more silt or clay or both in either the lower part of the B honzon or C horizon or both. Kanaw ha soils are formed in alluvium from acid shale and arc in an area of higher rainfall. LeRoy and Strawn soils have thinner sola. McHenry and Miami soils have more silt or clay, or both in the upper part of the solum. Maninsville soils have redder hue in the B horizon and formed in stratified o iiw ash or lacustrine sediments Nodine soils have thicker sola which is more stratified and leached of free carbonates to greater depths. Owosso soils have more sand and less silt or clay in the upper part of ihcir sola. Pnneeton soils formed in aeolian sediments and have siraiified C horizons Relay soils have hue of 2.5Y or 5Y in all parts of the B horizon. Teanaway soils have firm sandy clay loam C horizons with ^______________i