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ma}� have rnucky modi�iers, It is commc�nly neutra) but ranges from siightly �lkaline to
<br /> si��h<<y a���.
<br /> f1B horizon has colc�rs and textures similar to the f�and B; hori�ans.
<br /> The B� horiz�n h�s hue of�Y ur 2.SY, r•alue of 2 tt� �, and chronia oP l or ?. Dark
<br /> coic�red tongues from thG A hoeizon ran�e from f'ew to comm�n, It is (caa�t�, clay loam ar
<br /> silty cl�y loam. Near the center af sorne depressions, some p�dons ha��e B horizons that
<br /> have a sli�ht cl�y increase relativz to the A horizons. R is net�tral tu sli�htly alkalin�, but
<br /> in soine p�dons the tc�u�er��irt oFthe B horizon is slighdy all:�line with slight
<br /> et'��rvescence. The Bg horizon is absent in some pedons.
<br /> The Cg horizon has hue of�Y Qr 2.�Y, val��e uF�t to 6, an�i chroma of I to 4. lt is laarn,
<br /> clay� foam or siity cl�}� loam. It is slightly alkaline, �vith we�k ar st�ng�Efer��escence.
<br /> Calcium carbonate segregations ar� present in some pedans.
<br /> C01��1PETING S�RIES: Tf��s� are thc t�� :�i�-,l, [ ,��>>Ii�•�. I ���ll�!. (�i��<<,,�, .t��i���•C��ii��s��i�,
<br /> €��tl�li�, hi�tn�trrli,l�, ��; �n��, �ttl l.tti�, I'<<�,;, [:,1„in�l�, til�.i�i.�z��.�lnd l� ; �,i•, seCies. �
<br /> Coland and Comfrey soils do n�t hav� rock fraom�nts in their c�ntrol �ections. In
<br /> atldidon, Coland s�ils are de�per to tr�� carbonates. Delft soils are pc�orty drained, are not
<br /> in closed depcessions, havz prism�tic structure in subsail, and do not have tangues of the
<br /> A hori�on in the Bg hori�an. Gi�lo�4�, Jam�s Canyon. Keddie. Kimmerling, Konner,
<br /> I�1cClave, Pe�h, f�nc� W'enas soils are tlrier in the soil moisture cnncra( section during the
<br /> 1?Q days f'ollo��ing the surnmer s�lstici. Romnell sails e�ntain Appreciah(c amounts ot
<br /> gypsum in their sala. 5handep soils do not have tan�ues of tl horizon in the B� horizon
<br /> and have a coarse [4xtur�d 2C h�rizon.
<br /> �,EOGI2APII[C SETTIRG: Glencae s��i(s ty�pically arc in�Ic�s�d depressi�ns or la��
<br /> gradien[ s��-ales�a�itt�in the Des �icaines lc�b� of the Latc �t'isconsinan �laciation. '1'he
<br /> Glenc�e soils are formed in tvarny colluvial sediments and laamy glacial till. ;1�1r:an
<br /> annual temperattrre ranges frc�►n�� t� �2 degrets E. t��[ean z�nnual preci�itation ranges
<br /> f'rom 2� to 32 inches. I hc frost free days ran�e trom l2�#tn l 72. The elevation t�bove sea
<br /> level rang� from 700 t� I600 feet.
<br /> GEOGItAPHICALLY .45SOClATED 5(aILS: "t'liesc are the ( a«�����.�, ( I;��i ���, 1_i_s�l�ti,
<br /> `�i_�_,II��, and ���.<��:,�;� soils. Th� well drained Clarion soils Are on tl�e slopin� uplands.
<br /> 5omervhat poorly drainE:d Vicollet and the poorl�� drained Canisteo, 1�'ebster, and Hurps
<br /> sails are on nearfy Icvel tn �ently� undulating slopes. All the abor•e h�ve mollic epipedons
<br /> less tt�an 2�1 inches thick. [n addition, the Canisteo and Harps soily contain free
<br /> carbonates tliroug}u;�u[. The GEencoe soils also arc associaceci �victi the f I.►v��1��� and I,_�;,«�_
<br /> sails and their respecti4� topographic assvciat�s in some places.
<br /> QRA[NAGE AIYD PERVIEABtLITY: �'ery pcwrly draine�i. Surface runaR is
<br /> negli�ible. Permeability is m�erate or moderat�ty slu�v.
<br /> USE AND VEGETATION: '�tostly drained and cronpeei ta carn anct s�ybeans. 'Vative
<br /> ve�etatior� �a�as a wet sike planc communitrr•af the ta(1 �rass prairie plant fo�mati�n.
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