The Soils of Elgin County - Agriculture and Agri-Food Canada

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Tab_ le 2. Correlation of major soils andElgin Countyland units with physiography and surficial geology inSoil Typeor Land UnitNatural DrainagePhysiography andUsual TopographySurficial GeologyGlacial TillMuriel (MU) Moderately well Till moraines and till Silty clay to clay tillGobles (GO) Imperfect plains ; nearly level to on end and groundKelvin (KE) Poor very strongly sloping moraines (Port StanleytopographyTill)Bennington till Moderately well Till moraines and till 40 to 100 cm of loamyphase (BNJ) plains; nearly level to lacustrine depositsTavistock till Imperfect gently sloping overlying clayeyphase (TA.T) topography glacial till (Port StanleyMaplewood till Poor Till)phase (MA.T)Bookton till Well Sand plains, deltas, and 40 to 100 cm of sandyphase 030.7) till plains, nearly level lacustrine, fluvial,Berrien till Imperfect to gently sloping or eolian depositsphase (BE.T) topography overlying clayey glacialWpPoor till (Port Stanley Till)Lacustrine Gravels or Gravelly SandsKin" (KT) Rapid Beaches and shorecliffs; Gravelly beach andHighgate (HI) Imperfect nearly level to gently nearshore deposits, andMuirkirk (MK) Poor sloping topography well to poorly developedraised shorelinesLacustrine SandsFox (FX) Rapid Sand plains, spillways, Sandy lacustrine,Brady (BY) Imperfect deltas; nearly level to fluvial, outwash,Granby (GY) Poor gently sloping topographyFrome (FR)Very poorand deltaic depositsWattford (WF) Well Clay and sand plains ; Lacustrine deposits,Normandale (NO) Imperfect nearly level to very fine and very fine sandsSt. Williams (SW) Poor gently sloping topography predominate; surfaceChurchville (CH) Very poor may be eolian-modifiedLacustrine SiltsBrant (BT) Well Clay plains ; nearly level Lacustrine deposits,Tuscola (T[J) Imperfect to,gently sloping silt and very fineColwood (CW) Poor topography sand predominateWalsher (WA) Well Sand and clay plains, 40 to 100 cm of sandyVittoria (VI) Imperfect deltas; nearly level to lacustrine depositsSilver Hill (SL) Poor very gently sloping overlying loamytopographylacustrine deposits
Table 2.Correlation of major soils andElgin County (continued)land units with physiography and surficial geology inSoil Typeor Land UnitNaturàl DrainagePhysiography andUsual TopographySurficial GeologyLacustrine Silty ClaysBrantford (BF) Moderately well Clay plains; nearly Lacustrine deposits,Beverly (BV) Imperfect level to gently sloping clay and siltToledo (TO) Poor topography, occasionally predominateSouthwold (SO) Very poor dissected with stronglysloping topographyBennington (BN) Moderately well Clay plains; nearly level 40 to 100 cm of loamyTavistock (TA) Imperfect to gently sloping lacustrine depositsMaplewood (MA) Poor topography overlying clayeylacustrine depositsBookton (BO) Well Sand plains, deltas, and 40 to 100 cm of sandyBerrien (BE) Imperfect clay plains ; nearly level lacustrine, fluvial,Wauseon (WU) Poor to gently sloping or eolian depositstopographyoverlying clayeylacustrine depositsMelbourne (ME) Moderately well Clay plains ; nearly level Lacustrine heavy clayEkfrid (EK) Imperfect to gently sloping depositsStrathburn (ST) Poor topographyFluvial DepositsBurford (BU) Rapid Spillways, deltas, older Gravelly fluvial outwashBrisbane (BI) Imperfect (higher) terraces along depositsThames River, creeks andtheir major drainagechannels; nearly level tovery gently slopingtopographyCaledon (CA) Well Spillways, deltas, older 40 to 100 cm of sandyCamilla (CM) Imperfect (higher) terraces along deposits over gravellyAyr (AY) Poor Thames River, creeks and fluvial outwashdepositstheir major tributaries; and occasionallynearly level to verygravelly ice-contactgently sloping topography stratified driftEolian DepositsPlainfield (PF) Rapid Sand plains, duned sand Eolian-modifiedWalsingham (WA) Imperfect plains; nearly level to lacustrine sand depositsWaterin (WN) Poor gently sloping topography and eolian duned sandSpringwater (SP) Very poor deposits
Page 1 and 2: The Soils ofElgin CountyVolume 1Min
Page 3 and 4: ACKNOWLEDGEMENTSThe completion of t
Page 5 and 6: Southwold Soils (SO) . . . . . . .
Page 7 and 8: LIST OF FIGURES1 . Soil map index f
Page 9 and 10: 5. More detailed information for a
Page 11 and 12: Table 1 .Climate data for Elgin Cou
Page 13: Figure 4.Generalized geologic map o
Page 17 and 18: Figure 6.Schematic landscape cross-
Page 19 and 20: HOW THE SOILS WERE MAPPED AND CLASS
Page 21 and 22: of soil profiles and horizons which
Page 23 and 24: GENERAL DESCRIPTIONS OF THE SOILSSo
Page 25 and 26: Table 3.Soils and land units mapped
Page 27 and 28: Figure 11 .Soil textural groups and
Page 29 and 30: phase (BN.T) soils were mapped in c
Page 31 and 32: underlying fine textured materials
Page 33 and 34: atings for selected special crops a
Page 35 and 36: Conservation tillage practices, par
Page 37 and 38: clay. The Ap horizons commonly have
Page 39 and 40: Gobles soils were frequently mapped
Page 41 and 42: Kelvin soils are susceptible to com
Page 43 and 44: Soil Moisture CharacteristicsMiddle
Page 46 and 47: soils which occur in the eastern po
Page 48 and 49: Bluish gray or gray gley colours ar
Page 50 and 51: Stanley till, Tavistock till phase
Page 52 and 53: to neutral in the Ap horizons, to m
Page 54 and 55: tillage practices, particularly no-
Page 56 and 57: Organic (OR)Organic land units usua
Page 58 and 59: eference and also Publication No .
Page 60 and 61: Procedure :1) Locate the symbols 'B
Page 62 and 63: Table 4.Agricultural alnd capabilit
Page 64 and 65:
Soil Suitability ClassesDescription
Page 66 and 67:
Procedure:1) Locate the symbols 'BV
Page 68 and 69:
Table 6.Agricultural land suitabili
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Table 6 .Agricultural land suitabil
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Table 6. Agricultural land suitabil
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erosion losses will occur . Potenti
Page 108 and 109:
the average annual soil loss using
Page 110 and 111:
Table 9 . Mean K values, K ranges a
Page 112 and 113:
Table 10.LS values for different co
Page 114 and 115:
Table 13.C values for common field
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Table 14 . C values for some field
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Table 16.C values for some common c
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GLOSSARYAlluvium materialBlanketCal
Page 122 and 123:
ProminentmottlesRaised shorelineSoi
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4. Schut, L.W. and W.G. Stevens . 1
Page 126 and 127:
APPENDIX 1Generalized Soil Informat
Page 128 and 129:
BERRIEN SOIL TILL PHASE (BE.T)GENER
Page 130 and 131:
BURFORD SOIL (BU)GENERALIZED PROFIL
Page 132 and 133:
CAMILLA SOIL (CM)GENERALIZED PROFIL
Page 134 and 135:
GOBLES SOIL (GO)GENERALIZED PROFILE
Page 136 and 137:
KELVIN SOIL (KE)GENERALIZED PROFILE
Page 138 and 139:
MAPLEWOOD SOIL - TILL PHASE (MA.T)G
Page 140 and 141:
NORMANDALE SOIL (NO)GENERALIZED PRO
Page 142 and 143:
STRATHBURN SOIL (ST)GENERALIZED PRO
Page 144 and 145:
TOLEDO SOIL - COARSE PHASE (TO.C)GE
Page 146 and 147:
WATTFORD SOIL (WF)GENERALIZED PROFI
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APPENDIX 2Field Identification of S
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5. Proceed to Figure 13 and determi
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Figure 13 : Field Site Key To Ident
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Figure 14 :Field Site Key To Identi
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A iFigure 15 :Field Site Key To Ide
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Figure 16 : Field Site Key To Ident
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The Soils of Elgin County - Agriculture and Agri-Food Canada

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