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Table 3 . -- Classification of Soils and Parent Materials in the Shuswap Lakes Area .Soil Subgroups and SeriesOrthicPeatyGleyed Carbonated Regosol Peaty Carbonated RegoOrthic Orthic Mull Rego Rego to Rego Regc Rege HumicParent Materials Regosol Regosol Regosol Gleysol Gleysol Gleysol Gleyscl Gleysol GleysolGlacio-lacustrineSiltsGrierHeubnerAlluvial-ColluvialFansGrindrod - Schindler - Niowitch - Gardom Heubner BessetteRiver and Stream Falkland Rumball Bolean Apalmer - Mable Complex Gardom - BessetteDepositsYardBeach DepositsCelista
Table 3 .-- (Continued)Soil Subgroups and Seriesarent MaterialsOrthicHumicGleysolOrthicBlackOrthicDarkGrayGleyedOrthicDarkGrayOrthicBrownWoodedDegradedBrownWoodedOrthicAcidBrownWocdedOrthicGrayForestedGleyedGrayWoodedGlacial Till - Armstrong Bluespring - Grizzly HillGravelly Outwash orSlopewash over TillHillcrestMorainal Gravels - Nahun - - - MoultonGravelly Stream andDeltaic TerracesSa.ndy Stream andDeltaic TerracesLarch Hill Glenemma SauffGrandview - - 0'Keefe Pillar Banshee StepneyGlacio-lacustrineSiltsNeskain - - - - EnderbyShallow Colluviumover BedrockEquesis - Pari - HobbsAlluvial-ColluvialFansRiver and StreamDepositsririsconlith - Gulch - Lumby Broderick - ChumWhit eNisconlith - - Kosta - - - IdaWallenstein
Page 2 and 3: SOIL SURVEY^f theSHUSWAP LAKES AREA
Page 4 and 5: A. ii .PageBrown Wooded Soils .....
Page 6 and 7: 1- iv -PageL - Canoe Point Climatic
Page 8 and 9: - 2 -HOW TO USE A SOIL SURVEY REPOR
Page 10 and 11: The school population is accommodat
Page 12 and 13: pectively) the gradient between the
Page 14 and 15: - 8 -ground is not snow-covered . T
Page 16: - 10 -small flocks of sheep . Light
Page 19 and 20: It was observed that the surface so
Page 23: Forested, Gray Wooded, Acid Brown W
Page 27 and 28: DESCRIPTIONS OF SOILSREGOSOL SOILSR
Page 29 and 30: -23-HorizonDepthInchesDescriptionAp
Page 31 and 32: -25-DepthHorizon Inches Description
Page 33 and 34: - 27 -DepthHorizon Inches D escript
Page 35 and 36: -29-Land UseThe Celista soils are d
Page 37 and 38: Rumball-Nisconlith sandy loam to lo
Page 39 and 40: -33-The Schindler soils were classi
Page 41 and 42: - 35-Bolean-Nisconlith silt loam co
Page 43 and 44: -37-Peaty Rego Gle,ysolSoilsThe soi
Page 45 and 46: -39-and scattered spruce and cedar
Page 47 and 48: cover, typical of the Orthic Regoso
Page 49 and 50: -43-DepthHorizon Inches Description
Page 51 and 52: -45-DepthHorizon Inches Descrip tio
Page 53 and 54: - 47 -HorizonDepthInchesDescription
Page 55 and 56: -49-Gleysol . The native vegetation
Page 57 and 58: structure . The underlying C horizo
Page 59 and 60: -53-graphy . Two small arable areas
Page 61 and 62: -55-GRANDVIEW SERIESThese soils occ
Page 63 and 64: -57-The soils have developed under
Page 65 and 66: -59-HorizonDepthInchesDescriptionCk
Page 67 and 68: DepthHorizon Inches DescriptionCk 3
Page 69 and 70: -63-ArableNonarabl eGulch loam to g
Page 71 and 72: -65-GleTed Orthic Dark Gray SoilsKO
Page 73 and 74: - 67 -when cropped . Under dry farm
Page 75 and 76:
-69-HorizonDepthInchesDescriptionBC
Page 77 and 78:
HorizonDepthInchesDescriptionL-H 1
Page 79 and 80:
-73--HorizonDepthInchesDescriptionL
Page 81 and 82:
-75-HorizonDepthInchesDescriptionII
Page 83 and 84:
-77-scattered areas were cultivated
Page 85 and 86:
-7gcareshould be taken to avoid bri
Page 87 and 88:
- 81 -ArableNonarabl eGlenemma grav
Page 89 and 90:
- 83 -The parent material is sandy
Page 91 and 92:
-85-HorizonDepthInchesDescriptionL-
Page 93 and 94:
- 87 -The parent material is compos
Page 95 and 96:
- 89 -terraces . Minor areas of mor
Page 97 and 98:
Under natural conditions the Banshe
Page 99 and 100:
-93-The Orthic Acid Brown Wooded Ho
Page 101 and 102:
-95-HorizonDepthInchesDescriptionL-
Page 103 and 104:
-97-The Enderby soils were mapped i
Page 105 and 106:
-99-ArableNonarabl eChum loam 51 -
Page 107 and 108:
IDA SERIESThe main areas of the Ida
Page 109 and 110:
- 103 -G1e,y ed__Gra,y Wooded Soils
Page 111 and 112:
- 105 -DepthHorizon Inches Descript
Page 113 and 114:
- 107 -On the Broadview area northe
Page 115 and 116:
- 109 -SALTWELL SERIESThis series o
Page 117 and 118:
Associated soils derived from till
Page 119 and 120:
grass . A profile in forest, about
Page 121 and 122:
HorizonDepthInchesDescriptionAe 0 -
Page 123 and 124:
DepthHorizon Inches DescriptionCk2
Page 125 and 126:
HorizonDepthInchesDescriptionC 39 -
Page 127 and 128:
DepthHorizon Inches DescriptionCgjk
Page 129 and 130:
- 123 -Land UseAt the time of the s
Page 131 and 132:
- 125 -1,800 to 2,800 feet . A tota
Page 133 and 134:
- 127 -HorizonDepthInchesDescriptio
Page 135 and 136:
- 129 -The Brunisolic Gray Wooded C
Page 137 and 138:
SYPHON SERIESIn the mapped area the
Page 139 and 140:
- 133 -ArableNonarabl eLeonard grav
Page 141 and 142:
-135-Bisequa Gray Wooded SoilsHOBSO
Page 143 and 144:
-137-DepthHorizon Inches Descriptio
Page 145 and 146:
- 139 -HorizonDepthInchesDescriptio
Page 147 and 148:
feet depth . Surface and subsoil te
Page 149 and 150:
-143-The Canoe soils erode easily .
Page 151 and 152:
- 145 -The parent material consists
Page 153 and 154:
-147-gravel and stones . Scattered
Page 155 and 156:
-149-DepthHorizon Inches Descriptio
Page 157 and 158:
The Gray Wooded Solodized Solonetz
Page 159 and 160:
- 153 -The Broadview soils are suit
Page 161 and 162:
- 155 -DepthHorizon Inches Descript
Page 163 and 164:
-157-Land UseA small acreage is cul
Page 165 and 166:
-159-Deep__Muck Soils (calcareous P
Page 167 and 168:
DepthHorizon Inches DescriptionH2 3
Page 169 and 170:
-163-CLASSIFICATION ACCORDING TO SU
Page 171 and 172:
- 165 -Table 4 (Continued)Irrigable
Page 173 and 174:
Table 4(Continued)IrrigableLand Cla
Page 175 and 176:
-169-Table 4(Continued)IrrigableLan
Page 177 and 178:
Table 4(Continued)SoilsIrrigable_La
Page 179 and 180:
- 173 -Table 4(Continued)SoilsIrrig
Page 181 and 182:
-175-Table 4(continued)IrrigableLan
Page 183 and 184:
- 177 -Table 4(Continued)IrrigableL
Page 185 and 186:
- 179 -Table 4(Continued)SoilsIrr i
Page 187 and 188:
of available moisture use, and crop
Page 189 and 190:
- 183 -used as a guide tosoils :est
Page 191 and 192:
- 185 -Exchangeable Cati onsMilli-e
Page 193 and 194:
Table 5 : -- Chemical Analyses of 6
Page 195 and 196:
Table 5(Continued)Exchangeable Cati
Page 197 and 198:
Table 5 (Continued)Exchangeable Cat
Page 199 and 200:
Page 201 and 202:
Table 5(Continued)Depth pHHorizon I
Page 204 and 205:
Page 206 and 207:
Page 208 and 209:
Page 210 and 211:
Table 5 (Continued)Exchangeable Cat
Page 212 and 213:
- 206 -Tabe 6(Continued)FarmNo .Soi
Page 214 and 215:
-- 208 -16 . Bremner, J . M . Deter
Page 216 and 217:
Table A (Continued)YearJan .Feb .Ma
Page 218 and 219:
Table E : IYIoNTE CREEK-MONTHLY AND
Page 220 and 221:
Table G (Continued)Year Jan . Feb .
Page 222 and 223:
Table I :TAPPEN-MONTHLY AKD ANNUAL
Page 224 and 225:
Table J (Continued)Year J Feb . Mar
Page 226 and 227:
Table M- ENDERBY-iJIONTHLY AND ANNU
Page 228 and 229:
Table 0 : SPRING AND FALL FROSTS AN
Page 230 and 231:
Table Q :SAILiVIONARM-HOURSOF BRIGH
Page 232 and 233:
- 226 -GLOSSARYAlluvium - All mater
Page 234 and 235:
-228-C - A mineral horizon or horiz
Page 236 and 237:
- 230 -Extremely acid ~ pH 4 .5Very
Page 238:
- 232 - j;Talus - Rock fragments an
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