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The i\ or Ap ho►•izons have hue of I OYR. 4alue of? or 3, and chrama of l or 2. T}ie E
<br /> f�orizon �vhere present, has value of 3 to �, and chroma of l to 3. Tf�e A �nd E horiz�ns
<br /> are lo�m o�•clay� loam, but sandy loam, tine sa�ld�� loam,or silt loam is �vithin tlle ►•an�e.
<br /> They range ti•oin rnaderately acid to neutral.
<br /> I�he Bt horizon lias hue of I OYR or 2.�Y, value ot�-4 or 5, anc� chroma of 3 �r=�. It is clay
<br /> loam or loam and has 2-4 to 3� percent clay and 30 to-1� percent sand. The B/A clay
<br /> ratios range fraui I.? to I.�. It is stron,ly acid to slightly acid in the upper paE•t ancl
<br /> moclerately acid to neutral in the lo�ver part. A Bw horizan is sometimes present belo�v
<br /> the Bt.
<br /> The E3k horizon has hue oF lOYR or?SYR, value ot�or �, and chrorna of 3 to 6, The Bk
<br /> horizon is loam or clay loam. [t is slightly alk�line or moderately alkaline. Itelict
<br /> redoximocphic features are present in sorne pedons.
<br /> The C horizon has hue of 2.�Y or 1 QYR, value of� to 6, �xnd chcottla of 3 to 6. It is loam
<br /> or clay� loam. (t is slightly alkaline oc mocierately alkaline. Relict redoYimarpltic f'eatuces
<br /> are present in some pedans.
<br /> COI�d'FTING S�RI�S: These are the ,Ai�_�u.,, ��\i�s�I�, kialti�nui�:, !3<<�,s4tt, lll�_����inin�.
<br /> l ,I�.I�, �)����;i'I;1�. �)Ui1fi�1'I��L'�, t�illlt. ���:�C��IIt�, � ;{Ul�lllll�, � ��I1�'���j,, �.:c�l���. ������l;lAV��.
<br />��ti�'t�J. ��1ltiVI1141`. 1111.'1�7, (�IIV`,��n��. ���1CI�1.� ��[V����(, `��'�'�(��'�, �sl+3f�l, �� :lU�t�lll:l. c"il1C�
<br /> _ _ _ _
<br />�� inu��,l�i�_I. soils in th�sa���e farnily. Angus and S�bbo soil h�ve sat�n•ation in t1�e lo�ver
<br /> third of the series control section. Ar�yle, Baltimore, anc! Oneca sa[ls ha��e B f�orizons
<br />�vith 7.�YR or redder hue. B�ssett sails are very stro►�gly acid to moderatel} acid irl the
<br /> upper part of the Bt horizon. Blaoming and Racine soils have l� to 3� percent sand in the
<br /> upper part oFthe pacticle-size c�ntrol section. Caleb soils have some subhorizons that
<br /> have t��ore than �� percent in the lo���er part of the contcol sectiorl. vu�vagiac and Koronis
<br /> soils have less than 24 percent clay in the lo�ver one thii•d af the particle-size control
<br /> section. Dunbridge, �Vaucoma, Ne�vcomer and `Vinneshiel:soils ha��•e sola terminated by
<br /> bedrock at depths above b0 inches. Gara sails avera�e less than `_' percent roek fi•agments
<br /> in the c�ntrol section. Longlois, Lydic, anci Neda soils have more than 3 percent rack
<br /> fragments in some subhorizon of the control section. La�u•amie soils have more than��
<br /> pet•cent sanci in somc subhorizon in tlie ►niddle part of tlte control secti�n. �lc�ha�4k soils
<br /> have a hi�her content of silt and have dark colors in the B harizon ��hich apparently are
<br /> iniieritzd from dark sha(e. O�tivood soils have no rock fi•agments in the pa��ticle-size
<br /> control section. Razort soils have less ih�n 30 percent sand in the control section.
<br /> GEOGRAPHIC S�TTING: These sails have conve� slope5 on moraines and till plains.
<br /> Slope gradients r�nge from � to 70 percent. They formed in calcareous, loamy glacial till
<br /> of late W'isconsinan AQe. l�I�iill aI111U�I t�I17E7�C1�UCZ l'1Il�TeS tfQEll �� CIZ,rees to �2 degrees
<br /> F. �tean annual precipitatian ran�es t�rom 2> to 33 inches. Frost fi•ee da}s raii�e ti•om 12,i
<br /> to (65. Flevations ran¢e t�ra►n 700 to f 60O Fect.
<br /> GEOGI2APHICALLY ASSOCIATED 5{�ILS: "Chese incluc(e the t ��r�l���..�, 1����r_I;t�.,
<br />( I��!I���'.'. ��;illl�'�. ��i�{I '�I�'-.�Ii. ��.�t1`,�,I1�1`t � �' 17f�lli�. ��lI���C:�,.1� Gt�ll� �.i.�t�'� $���$. I O�l��
<br /> . _ .. . .._.. .v. . ._. . _ _ _. ._ ��
<br /> drained Cordova and some�vhat poorly and poorly drained Dund�s soils are on flats and
<br /> uppei•draina;�ways tivith a higli seasonal �vater table. Very poorl��drained Glencoe,
<br />
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