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rnickness of the solum�ranges from 10 to S8 cls�• loam subsoil are exposed in cultivated :,,�es but is comnonly 28 to 36 inches. The Ap ' fields. �a�i:on is very dark �ray to dark �rayi�h brown. In Included in mapping aere a few patches of Dalbo � ,,ltivaced areas the A1 horizon is 3 to S inches soils. Thare are areas of Dundas and Cordova soil� � ��l�k and is black or very dark �ray. 'ihe A2 hori- in slallow drainageways. Areas of Glencoe soils ,�� Mhere present, is 3 to 8 inches thick and is were aiso included in the �ew scattered depressions, ��, d�rk gray to �rayish brwn. The B2 horizon tbst areas of this 'soil �are in permanent pasture � �Cnerally is dark yelloxisA Drvwn but is yella+ish or voodland. This soil is good cropland and is suited ' �n.,n and olive bravn in places. The B2 horizon has to all crops commonly grown in the county. The haiard jairked incre u e in clay content as compared to the of erosion is seva n. Good management is required � kori.�on. The finest textured part of the B hori- to reduce ero�ion and ninoff. (Capability unit :o� ranges from 22 to 35 percent clay but is typi- IIIe-1; woodland group 1; building site group 5) ' u�ly 28 to 33 percent clay. Sand content ranges �� SO to 45 percent, with 25 to SO percent of the- Hayden loam, 12 to 18 perc2nt slopes (HbD) .--'ltiis y�nd fraction coaner than fine sand. '!he C horizon hillv soil occupies 2-acre to 15-acre, irregularly contains 18 to 24 percent clry and 35 to SO percent shaped areas on hillsi'des and knolls. Slopes are ' �, High-chroma mottles are coaim�n throughout the typically 60 to 125 feet long. Some areas are on � hori�on. In some areas there are iron oxide con- the side slopes of lorr hills, and slope is mainly ' csetiorts. In the eastern part of the county, there in one direction. Slopes are in several directions, � a IIC horizon of reddish-brawn loamy or sandy hoaever, in most areas. 'Ihis soil has a profile ' a�terial at a depth of 4 to 20 feet. The A horizon similar to that described as representative for the slightly acid to neutral. The B horizon is medi- series, except that the surface layer is dark gray- acid to neutral. ish brown and is much lighter colored when dry. Hayden soils are not so fine textured as the 'Ihen are a few scattered exposures of the dark- �iular Erin soils. , They are finer textured throug}L- brown clay loam subsoil. The surface layer and the t the profile than the associated Heyder soils. subsoil are commonly 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. 'Ihey are finer Included in mapping were small patches of Dalbo textured and la+er in content of gravel and cobble- soils that occupy convex positions. Areas of D�mdas tones than the similar Kingsley soils and have a and Cordova soils occupy shallow drainageways and ' t!►t�r colored Ap horizon than the associated depnssions. = ' s ter soils. . t�bst areas of this soil are in permanent pasture or woodland. The haza'rd of erosion severely limits Hayden loam, 2 to 6 percent slopes (HbB).--1his the use of this soil for cultivated crops. If ` ntly imdulating soil occupies 2-acre to 15-acre, coimon management practices are used, intertilled rregnlarly shaped azeas on }aolls and hillsides. crops shwld be grown only -occasionally. This soil � Slopes are 75 to 125 feet long. 'Ihe slope_in most _ is better suited to hay and pasture than to most lues is in several directions. This soil has the other crops. (Capability unit IVe-1; woodland group file described as representative for the series, 1; building site grwp S) Included in napping rvere a few, small, eroded �atches of soils that have a surface layer of dark-- Hayden loam, 18 to 24 ercent slo es HbE lrarn clay loan. Also included xere a few atches p p � ) •--'�is P steep soil occupies 2-acre to 10-acre areas on hill- Dalbo soils that have convex slopes. Included in sides. Slopes are commonly SO to 100 feet long and ='z'a+, concave drainageways rere areas of the poor- �e broken by shallox downslope drainageways. This drained D�mdas and Cordova soils. A few scattered soil has a thinner surface layer and subsoil than �Pressions contain areas of Glencoe soils. those described as representative for the series. n►e main management needs are 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 benches. rate. This soil is well suited to all crops Abst areas of this soil are in permanent pasture �only groMn in the county. If management is good, or woodland. Steepness of slope severely limits its js soil is suited to row crops nearly every year. �e for coimnon farm crops. If not protected by �ability �a►it IIe-1; woodland group 1; building plant cover, this soil erodes rapidly. It is diffi- t, �� S� cult to operate machinery on the steep slopes. This �den loam, 6 to 12 soil is �ost productive when managed for grazinQ llin Aercent slopes (HbC� .--This or woodland or maintained in its natural state for t soil occupies 2-acre to 15-acre� irre�ularly recreational use and for wildlife habitat. (Capabil- areas on hillsides and knolls. Slopes are ity imit VIe-1; woodland group 1; building site �0n1Y 75 to 125 feet long. In most places the group 5) °P� is in several directions. This soil has a �� similar to that described as representative Hsyden clay loam, 2 to 6 percent slopes, eroded ` �� series, except thac �tie surface layer is (HcBn .--This gently �mdulating soil occupies 2-acre * �'�Yish brown and is nuch lighter colored .when• to 15-acre, i negularly shaped areas on knolls and �' A f�M scattered patches of dark yellowish-brown hillsides. Slopes are 75 to 125 feet long. In aost 37 � � � r � - ,�