2003-P06845 - new septic system - Laserfiche WebLink

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�� � � • • , ' • places che slope is in �everal directions. lec�uss because they loosen the soil and increase thi� soil is eroded, tAe surface layer in cultiv�ted This soil is well suited to har and pascur� �r � �reas �u baen aix�d with tha subsoil and ls v�ry which protect the �oils. Ic i� al�o we11 i�L�A, ' dark �rayisA-Drarn or dark ;rayisA;b�rovn c!4 loaa• to trae�, It is tu1� li�t�r eolored wAen dYy. In l�c�s N� ��=P�bilitr �it IVe-1; woodland �� brovnish suDsoil i� exposed. p 1: buildin� �ite rs�oup S) � � Included in a�ppin� were s�all patchas oE Da1Do soils that hav� conv��t �lopes. Also inclod�d Nr� �N H? d°p �la loaie 18 to 2� ercent slo q ` . ueu of poorly drain�d O�a�du and Cordcva soils in ' s �teep soil occupies Z-acr� to � . narrw draina=e�rsys that czoss t?►is soil and arus arau onthillsipes. Slopes are co�aonlr SQ to.�� of Glencoe soils in scattered depressions, feQt lon Slo es are broken br shallov d� • 1?�e �ain liaitations ue �intenance of ti1tA and dr�ina`erars and occuional deep ravines. D�a�e , . cont�l of erosion. This soil is well suited to all �is soil is eroded� the surface layer is elaX•lo�, the cro s co�onl that is a vixture of the Yrayish-brown surfact•� p Y �ro�+n in the countr, If tAe aad Ne dark - soil is vell nlu�ed. row crops car� be �rown a� it Ye1lAwish-brown subsoii. In a tw �`� r �, r��, ueu the surface layer is dark brown and coyi�t3 , nearl eve (Capability �it IIe-1; rood�and rinlr of eaterial fros the subsoil. This soi� A �'oup 1; buildin� sitd �roup S) a thinner_surface layer and subsoil than the o�� � Nsyden clay loas, 6 to 12 described as typical for the series. A fex percent slopes. ercded cslcareous, olive-brown bald patches xcur nearaV,� . (HcC2). This mllin� soil occupies 2-acre to 15- ure� irre�ularlr shaped areas en knolls and hill- crest of slopes. This soil is lower in or sides. Slopes ue comsonly 7S to 125 feet lo °�tter content and is less friable than H�deneloa� Because tAis soil is eroded, the surface 1 a u Steepness of slopes severely linits the vse of clay loaa that is a aixture of the duk � U►is soil for fanning. This soil erodes rapidly in broi+n aaterial fros the original surfaceYlryer1md �� hei° the vegetative cover is sparse. It is �' better suited� to pasture or woodland or to recrei_ d►e darfc yellovish-brown subsoil. The color is �uch tiorial or wil�life tises than to �ost other usea. li�hter rrhen �►, In places saall patches sre e=- posed that camsist aainly of the brownish subsoil, site�ility unit VIe-1; roodland Yroup l; build�A= This soil coatzins less organic aatter snd is less �p s� - � friable t}►aa Hsyden loass. Included in aapping rere s'all patches of Daibo H�'den and Lester loass, 24 to 35 percent sio a t soils that occup�► conoex positions. I11so incladed �d� �►ese very steep soils occupy 2-acre tp 10- _ w�re ireas of D�mdas and Cordova soils in shaliar �r� �� °n hillsides, on sides af deep ravines, ' dralnsgerrys. S�all, �scattered de ssions t�t �d °n slopes adjacent to lakes and sloughs. $lope� � as'e co�only SO to 120 feet long. �Ibout 7p pe�.cent contain areas of Glencoe soils xere also inclnded. of this �.mit is Hayden loaa, and 3p per�ent is . This soil is �ood cropland and is suited to all Lester loam: 'Ihe surface layer of the Hayden loam the crops coaoouly grawn in the county, The hasa� is ��er �d lighter colored than that of the , of erosion is severe. Good management is needed to Lester loan. 'Ihe Hayden and Lester loaa�s have-a ��lderosion and nmeff. (Capability tmit IIIe-1; p�file similar to that described � resentative �'oup 1; building site �roup S) for their res ective series, except that they hsve • - N den clsy loas, 12 to 18 percent slopes, esoded a �inner sur�ace layer aad subsoil.- (t1cD2). This hilly soil occupies 2_acre to �� Included in Dapping xere shallov downslope dnir.- areas an hillsides ar�d knolls. Slo s ue i�iys �at contain poorly drained soils that have ' 6Q to 125 feet lon�. 'ihe slo e is � �Ir a uick� dark surface larer. A fex areas of �entl� stveral directions. Because Lhis soilQisleroded ='0llin� soils on.hilltops xen included with this • the surfue 1 ' �=PPin� �it in some places. Ssall sliaps occtia �e �� rr is clry loas that is a si:tvre of down slope. �rsyish-brown ssterial fros the oripiaai Ubst anas of these soils woodland. The haurd surface lryer snd the dark yellowish-brown subsoil. of erosion is very severe. The very steep, shon In places the siaface layer is aainly esterial fzv� slopes co�only liait the use of these soils to the duk-b mvn subsoil. The dry color is aud► woodland, wildlife habitat� and enhancement of the li�Ater. This soil is lower in orYanic-uttez caa- natural beauty of the uea. (Capability ta►it ter�t and is less friable than Hayden loaat, Included in aappin� rere a fer, calcareous, oliw- �Ie-1; woodland �roup 1; buildinY site �roup S) bra+n. bald patch es near the crest of slopes. Ineluded in conve: ueu were s�all patches of Daibo � _ soils. Areas of O�a�dts and Cordova soils werc ia_ He�'d�r Series eluded in the fe+r shallor drainaQevays and depre�- The Heyder series consists of deep. velI-draine� sions, This soil is severely liaited for cultivated soils that fotaed in loary Ylacial till. Thes� crops because of tAe steepness of slo es and �� soils have canvex slopes and are on knolls and hil: hazard of severe erosion. Careful sanaQement is The hills and knolls are S to 200 acres in size anc • needed if in�e r,illed cro s are lie S to 80 feet above the surroundin� drainajeva��s P er°�n• Corn shauld ar�d depressions. � Slopes ranee fro� 2 to SS percen: . be �rorn onlr occu ionally. Soybeans are not suited, �d ue 75 to 250 feet lon�. Stones and boulders �a a. • ' ' .