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rnickness of the solum range� from 20 to 48 cla�• loam subsoil are exposed in cultivated ' ,��1,es but is conaonly 28 to 36 inches. The Ap ' fields. �ati:on is very dark �ray to dsrk �rayish broan. In Included in mapping were a few patches of Dalbo • ��civated areas the A1 horizon is 3 to S' inch es soils. There are areas of Dundas and Cordova soil� � L�l�k and is black or very duk yray. The A2 hori- in sl�sllow drainageway3. Areas of Glencoe soils p�, where present� is 3 to 8 inches thick and is were also included in the few scattered depressions. ,�ry dark �ray to �rayish brovn. The 82 horizon Nost areas of this soil �are in permanent pasture � �nerally is dark yelloxish brown bUt is yella+ish or �+oodland. This soil is good cropland and is suited ' .n.,n and olive brown in places. The 82 horizon has to all crops co�mnonly grown in the county. The hazard � a�rked increase in clay contant as compared to the of erosion is severe. Good management is nquired ,� 1ori:on. The finest textured part of the B hori- to reduce erosion and nrnoff. (Capability unit ;� ranges froa 22 to 35 percent clay but is typi- IIIe-1; woodland group 1; building site group 5) ' ulty 28 to 33 percent clay. Sand conteni ranges �� 30 to 45 percent, with 25 to SO percent of the- Hayden loam, 12 to 18 percent slopes (HbD) .--'lhis �nd fraction coarser than fine sand. 'Ihe C horizon hill� soil occupies 2-acre to 15-acre, irregularly contains 18 to 24 percent clay and 35 to 60 percent shaped areas on hillsides and knolls. Slopes are y�, , High-chroma mottles are common throughout the typiully 60 to 125 feet long. Some areas are on 1 �hori=on. In some areas then are iron oxide con- the side slopes of low hills, and slope is mainly ' cetiorts. In the eastern pazt of the county, there in one direction. Slopes are in several directions, u a IIC horizon of reddish-brown loamy or sandy however, in most areas. This soil has a profile ' terial at a depth of 4 to 20 feet. The A horizon similar to that described as representative for the � zcidhtoYneutralo neutral. The B horizon is medi- series, except that the surface layer is dark gray- ish brown and is much lighter colored when dry. Hayden soils are not so fine textured as the 'm en are a few scattered exposures of the dark- iular Erin soils. _ They are finer textured throug}t- brown clay loam subsoil. The surface layer and the aut the profile than the associated Heyder soils. subsoil are co�only thinner than those in the pro- den soils are not mottled in the B2 horizon as file described as representative for the series. the associated Nessel soils. 'lhey are finer Included in mapping were small patches of Dalbo tured and lawer in content of gravel and cobble- soils that occupy convex positions. Areas of Dundas stoaes than the similar Kingsiey soils and have a and Cordova soils occupy shallow drainageways and ' �t�r colored Ap horizon than the associated depnssions. ' s ter soils. . Nost areas of this soil are in pe�anent pasture or xoodland. The hazard of erosion severely limits Hayden loam, 2 to 6 percent slopes (HbB).--'Ihis the ase of this soil for cultivated crops. If etly imdulating soil occupies 2-acre to 15-acre, co�on management practices are used, intertilled � rregnlarly shaped areas on Imolls and hillsides. crops shwld be grown only �occasionally. 'Ihis soil � lopes are 75 to 125 feet long. The slope in m�st _ is better suited to hay and p�.sture than to most ptices is in several directions. This soil has the other crops. (Capability unit IVe-1; woodland group file described as representative for the series, 1; buiiding site group S) Included in mapping were a few, small, eroded tches of soils that have a surface layer of dark-- Hayden loam, 18 to 24 ercent slo es HbE lrwn clay loan. Also included were a few atches p p � � ' -�13 Dalbo soils that have convex slo es. Included in steep soil occupies 2-acre to 10-acre areas on hill- , P sides. Slopes are co�monly 50 to 100 feet long and n'a+, concave drainageways rere areas of the poor- aze broken by shallorr downslope drainageways. This drained D�mdas and Cordova soils. A few scattered soil has a thinner surface layer and subsoil than �Pzessions contain areas of Glencoe soils. those described as representative for the series. TMe main management nee�s tre control of erosion Included in mapping were a few, small, 2-acre to �aintenance of tilth. The hazard of erosion is 3-acn, gentle crests and side-slope bench es. rate. This soil is well suited to all crops hbst areas of this soil are in pe�anent pasture �only gr�,n in the county. If management is good, or xoodland. Steepness of slope severely limits iu 11s soil is suited to row crops nearly every year. tise for comnon farm crops. If not protected by �ability i.mit IIe-1; xoodland group 1; building plant cover, this soil erodes rapidly. It is diffi- t, �� S� cult to operate machinery on the steep slopes. This soil is sost productive when managed for grazin� �den loam, 6 to 12 percrnt slopes (HbC� .--This or woodland or maintained in its natural state for l�ne soil occupies 2-acre to 15-acre� irregularly �creational use and for r+ildlife habitat. (Capabil- areas on hillsides and knolls. Slopes ue ity imit VIe-1; woodland group 1; building site nly 75 to 125 feet long. In most places the group S) u0� ls in several directions. This soil has a tlle similar to that described as representative Ha7den clay loam, 2 to 6 percent slopes eroded N� series, excepc that 2.he surface layer is (NcB� .--This gently �mdulating soil occupies 2-acre � Rayish brown ar.d is w ch lighter colored when• to 15-acre, inegularly shaped areas on knolls and ' � f�4 scattered patches of dark yellowish-brown hilisides. Slopes are 75 to 125 feet long. In most 37 � � . r � -