2003-P06827 - new septic system - Laserfiche WebLink

Home Browse Search

1 �,y \w ' 1 1 places the slope is in several directions. Bec�usd because they loosen the soil and increase eros• this soil is eroded, the surface layer in culciv�ted This soil is well suited to hay and pasture �r��• ueas h u been mixed with the subsoil and is very which protect the soils. It is also well suit�' ' dark �rayish-brarn or dark grayisThy-,broIn Claces�the 1� buildin (sit�ility unit IVe-1; xoodland Qro� It is ouch li�ter colored when d p � group 5) brarnish subsoil is exposed. ' � Included in aapping were small patches of Dalbo Ha den cla loam 18 to :4 ercent s�o es t soils that have convex slopes. Also incladed rere (HcE2).--This steep soil occupies 2-acre to 10�� areas of poorly drained D�u�das and Cordova soils in areas on hillsides. Slopes are coa�nonly 50 to 0� narraw drainageways that cross t?►is soil and areu feet long. Slopes are broken by shallow downs�o� of Glencoe soils in scattered depressions. drainageways and occazional deep ravines. Beca�� ' The main liaitations are maintenance of tilth and this soil is eroded, the surface layer is clay•lo� � control of erosion. This soil is well suited to all that is a mixture of the ra ish-brown surface� the cmps co�only gro++n in the county. If the and the dark g y soil is well �anaged, rox c�rops can be grown on it Y�1Lowish-brown subsoil. In a g�wl�ctj areas the surface layer is dark brown and consists � ' , nearly every year. (Capability �mit IIe-1; roodland mainly of material from the subsoil. This soil hts f group 1; building site group S) a t}�inner surface layer and subsoil than the one described as t ical for the series. A few, saall, � Hayden clay loam, 6 to 12 percent slo es ercded � P . calcareous, olive-brown bald patches occur near Ne ' (NcC2) .--This rolling soil occupies 2-acre to 15- crest of slopes. This soil is lower in organie- acre, irregularly shaped areas on knolls and hill- matter content and is less friable than Hayden loa� sides. Slopes are commonly 75 to 125 feet long. Steepness of slopes severely limits the use of Because this soil is eroded, the surface layer is this soil for farming. This soil erodes rapidly in ' clay loan that is a mixture of the dark grayish- azeas where the vegetative cover is sparse. It is brown material from the original surface layer and better suited to p�sture or woodland or to recrea- the dark yellowish-brawn subsoil. 'Ihe color is much tional or wildlife uses than to most other uses. li�ter when dry. In places small patch es are ex- (Capability unit VIe-1; woodland group 1; building ' posed that consist mainly of the brownish subsoil. site group S) llzis soil contains less organic matter and is less _ _ friable than Hayden loams, Hayden and Lester loams, 24 to 35 percent s�lopes Included in aapping were small patches of Dalbo (HdF� . 'Ihese very steep soils occupy 2-acre tp 10- ' soils that occupy convex positions. Also included acie areas on hillsides, on sides af deep ravines, xere azeas of D�mdas and Cordova soils in shallw and on slopes adjacent to lakes and sloughs. $lopes - drainagexays. Snall, scattered depressions that aze�co�only 50 to 120 feet long. About 70 percent contain are as of Glencoe soils were also included. of this umit is Hayden loam, and 30 percent is ' 'lhis soil is good cropland and is suited to all Lester loam: 'Ihe surface layer of the Hayden loam the crops co�anly grown in the county. 'me hazard is thinner and lighter colored than that of the of erosion is severe. Good �anagement is needed to Lester loam. The Hayden and Lester loams have a contml erosion and runoff. (Capability im it IIIe-1; profile similar to that described as re�resentative ' woodland group 1; building site group 5) for their respective series, except that they have a thinner sur�ace layer and subsoil. • Hayden clay loam, 12 to 18 percent slopes, eroded Included in mapping were shallow downslope drain- (HcD2) .--This hilly soil occupies 2-acre to 15-acre ageways that contain poorly drained soils that have � az'eas on hillsides and knolls. Slopes are co�only a thick, dark surface layer. A few areas of gently 6Q to 125 feet long. 'Ihe slope is generally in rolling soils on hilltaps were included with this several directians. Because this soil is eroded, mapping iu►it in some places. Small sl�ps occur the surface layer is clay loam that is a mixtun of down slope. ' the dark grayish-brown material from the original Most areas of these soils woodland. The hazard surface layer and the dark yellowish-brown subsoil. of erosion is very severe. The very steep, short In places the sia face layer is mainly material from slopes comnonly limit the use of these soils to the dark-brown subsoii. The dry color is mucf� woodland, wildlife habitat, and enhancement of the ' lighter. This soil is lower in organic-matter can- natural beauty of the azea. (Capability �mit tent and is less friable than Hayden loams. VIIe-1; woodland group 1; building site group 5) Included in aapping were a few, calcareous, olive- brown, bald patch es near the crest of slopes. Included in convex areas wen small patches of Dalbo � Heyder Series ,_ soils. Areas of Dimdas and Cordova soils were in- cluded in the few shallow drainageways and drpres- The Heyder series consists of deep, welI-drained sions, soils that fox�ed in lo ' This soil is severely limited for cultivated �Y glacial till. These soils have convex slopes and are on knolls and hil:: crops because of th e steepness of slopes and the The hills and knolls are S to 200 aczes in size an� hazard of seve n erosion. Careful management is lie S to 80 feet above the surrounding drainagewa��s needed if inte n illed crops are grown. Corn should and depressions. Slopes range from 2 to 35 percen� be grown only occasionally. Soybeans are not suited, �d a�e 75 to 250 feet long. Stones and boulders ,' � 38 , � , .