2003-P06845 - new septic system - Laserfiche WebLink

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� rnickness of Ne �olum nn�d� Prom 20 to J8 � cli�• loani ��Qil are exposed in cultivated :�;res buc is co�wonlr 2a to 36 inche�. The Ap ' fields. �ri:on is very dark tray to dark trayish �ra+n. In Ixluded in �appieQ were a few patc�e� of Dalbo y�iiv�ced arva� N• A1 Aori:on i� 3 to S incAu �oils. i1►ere are are�u of Dundu and �ordova �oil� ' ��,;k snd is Dlack or wry dask �ray. '1A� A2 hori- in s.��llow draina�eway�, Areas of Clencoe �oils p,,, Mhera present, is 3 to � inche� thick and is re:e uso included in the few scattered depre»ions. ��, a�rk trar to jrqisA Drcva, Zh� SZ Aori:on lbst areu of chi� ��oil �are in per�a�ent putua� �1 �rner�llr i� dazk r�llovisA �rown but is y�llouish or Moodland. This soil i� �ood cropland and is �uiUd ' .�n �nd olive Ora+n in places. 'ifi� S2 horiton has to ill crop� co�■onlr Qrown in Ns cowty. Th� hasard , .�rked incr�u• in elsy cont�nt aa co�pared to th� of erosion i� severe. Good sana e�ent i� re ,�e rsn�es h�o■ 22ntotSS�xt�d part o! th� S hori- to :educ� erosion and nmoff. (Capability �iti� �ilr �a to 33 perceat clap� Sand2contentiran�es IIIc-1; roodland �roup 1; buildin� �ite �roup S) • �30 to �S percenc� riN 2S to 50 percent o! th�- H�den loau. 12 to 18 percent �1_ o_p` (�p�,._�is . tiy�d Eraction coarser Nan fia� sand. 'ih� C Aorison hili• soil occup es 2-acrs to 1 -acre, irre�ululr ��cains la to 24 percent elsp and �35 to SO perceat shaped areas en hillsi'des ir�d knolls. Slo es ars �od. : Hi�h-chroaa �ottles m ea�on throu out the P ' � typiulir 60 to 125 feet lon�. Sooe areas are on eeciortsn. In�the•eistern areteof thercounxide�e� �e side slopes of low hills, and slope i� mainlr ; p tY. in aoe direction. Slopes are in several directioas, s i IIC horizon of reddish-Drown Toa�y or sandy hovevez, in most areas. This soil hu a ro a�terial at a depth of � to 20 feet. 'Ihe A horizon siai:u to that described as npresentative for�the . u sli�htly acid to neutni. The 8 horizon is aedi- ser_a� except that the surface layer is dark �ray_ � uid to neutnl. ish brarn and is �ch lighter colored rhen dry, Hayden soils are not so fine textured as the There are a few scattered exposures of the dark_ siulu Erin soils. . fiey ae finer textured throu�h- brora clar loam subsoil. The surface layer ud the mc the profile thaa the usxiated Heyder soils. lt�rden soils are not aottled in the B2 horizoa as subs°il ue c°°aonly thinner than those in the pro- w the assxiated I�lessel soils. 'Ihey are g�r file �mbed as representative for the series, tutured ar�d lwer in contmt of Yravel and �obble_ �lnded in �apping were s�all patches of Dalbp - • ' �tonea than the siailu Cin 1 soils that occupy convex positions. Areas of Qmaas �s ey soils ar�d have a and Cordova soils occupy shallow drainageMays snd ' li�tbr colond Ap horizon thsn the associated depmsions. Later soils. . ' ' � - _ lbst aeas of this soil are in persanent past�e Hayden loa�, 2 to 6 �ercmt sl °r r0°��• 'The hazaYd of erosion severely liaits - �ntlr ia►dulating soil occupies y-�acrsettoel5-acres �e ase of this soil for cultivated crops, ig Irre;nlarly �sha ' CO� �8e�nt practices are used, intertilled ' P� u'�zs on lrml ls and hillsides. �� ld be grown only'occasionallr• This soil Slopes are 75 to 125 feet lon:. The slope in mcst _ is better suited to hay and pa.sture than to most , ►lues is in several directioas. This soil haa the o�� s, (Capability tmit IVe-1; xoodland �ro�p Ro�ile described as represenutive for the series, 1; bnilding site group 5) ' Included in aappin� wen a few, small, eroded MLcAes of soils that have a surface iayer of dark-- � clay loaa. Aiso included rere i fer atches ��n loam. 18 to 24 percent slopes (IibE) ,__� - 1 Dalbo soils thst hsve cvavez slopes. Inpcluded in st� s°11 °�cupies 2-acre to 10-acre areas on hill- �� °nuve drzinaQe+tars rere areas of the r_ sida. Slopes are coaonly SO to 100 feet lon� aad � h Qrained Amdss md �.d�a soils. A fex scattered �e �t� by shallow downslope drainageways, lh� ' - 4Pressions contain areis of Qencoe soils, soil hu a thinner surface layer and subsoil than � �� sain aanaYeaent needs ae control of erosion �ose described u representative for the series, 'tl �intenaace of tilth. T}ie hazard of erosion is I'rluded in mappin� were a few, ssall, 2-acre to ��rate. This soil is vell suited to all crn s 3 a�' nntle crests and side-slope benches. �°�0^lY �'arn in the caun p Most ueas of this soil are in peimanent puturt ��lj soil is suited to roM czops n�=1ye�e�i�e�d, or roodland, Sterpness of slope severely liaits iu ��bility �it IIe-1; woodland �Q f0f ��on fars crops. If not protected by �dt� Ro� S� ��p 1; buildinY plant corer, this soil erodes rapidly. It is difH- cult to operate uchinery on the steep slopes. TAis i den loa� 6 to 12 percent slopes }� soil is �ost groductive wAen sana`ed for �razi� � y+in ( n .--This , or roodlsad or saintained in its natural stste tor �� sail occupies 1-ur� to 15-acre� irrejularlr =,e�T�tional �ue and for wildlifs habisat. ' �r�zs on hillsides md knolls. Slopas ar• ;tr �it Yfe-1; roodland �roup 1; buildin� siG�il- E~°^lY 75 co 125 feet lont. In wst plues th� y� �s in several directions. TAis soil his s ��P s� `�� siular to thac descztbed as representative Hrden cla loaai, 2 to 6 ercent slo es, ezoded ��'• series, ex��p� that Ltie surface la er is r y p p Raylsh brovn and is �c1 li r (Hca., . i1�is �ently �dulatinQ soil occupies 2-atr� � �� scaccered pa�ches of darkeyella+ish-Drorn to 13•ure, irre�ularlr s�aped areu on knolls and � hills:dcs. Slopes are 75 to 12S feet lon�. In �ost 37 � � � . ' , ' t • • r