SOIL SURVEY
SOIL SURVEY SOIL SURVEY
-108-OL - Ottertail Soilscape GroupPhysiographic Setting (Figure 55, page 91 )This soilscape group occurs on morainal landforms below 1550 m a .s .l ., i nthe main valley bottoms, often as remnants and small pockets of what was probabl ymore extensive moraine .Landform and Parent Material sThe Ottertail soilscape group commonly occurs on morainal blankets overbedrock, but morainal veneers and deep morainal deposits are not uncommon . Theparent materials are compact, calcareous, medium textured till which may hav ebeen locally reworked by water . Small lacustrine pockets are often found as inclusion sin this till along the Kicking Horse Valley .EnvironmentThe Ottertail soilscape group occurs in the montane vegetative zone rangin gin elevation from about 1050 m a .s .l . at the western Park gate to about 1550 m a .s .l .Table 36 . Key criteria differentiating the Ottertail map units .Soilscape Coarse Fragment DrainageClassificationTextureMap Unit Content (%) Clas sOL 1 Degraded Eutric Brunisols silt loam 10-20% wel lOL2Gleyed Melanic and
Figure 73 . Degraded Eutric Brunisol soil chosen to characterize the 01 1map unit .
- Page 75 and 76: -57-Table 10 . Brief description of
- Page 77 and 78: ure 24 . This photo shows the huge
- Page 79 and 80: igure 26 . Site of the pedon chosen
- Page 81 and 82: -63-Figure 28 . Site of the pedon c
- Page 83 and 84: - 65-CLI.Figui 30 . Site of the ped
- Page 85 and 86: -67-Table 15 . Brief description of
- Page 87 and 88: L-69-r_ -, _ 1 4Figure 35 . Site of
- Page 89 and 90: Figure 37 . Site of the pedon chose
- Page 91 and 92: -73-Landform and Parent Material sT
- Page 93 and 94: -75-The silty surface texture, slow
- Page 95 and 96: -77-material and/or shallowness (of
- Page 97 and 98: Figure 44 . Site of the pedon chose
- Page 99 and 100: -81-HR1 Map Unit (Degraded Eutric B
- Page 101 and 102: -83-in the solum, but may exceed 50
- Page 103 and 104: -85-KI - Kicking Horse Soilscape Gr
- Page 105 and 106: -87-Silty surficial textures provid
- Page 107 and 108: -89-Wetness, texture, and potential
- Page 109 and 110: -91 -Table 27 . Brief description o
- Page 111 and 112: Site of the pedon chosen to charact
- Page 113 and 114: -95-Table 29 . Brief description of
- Page 115 and 116: -97-NI1 Map Unit (Lithic Orthic Eut
- Page 117 and 118: -99-Figure 62 . Site of the pedon c
- Page 119 and 120: -101 -EnvironmentThe Ogden soilscap
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- Page 123 and 124: -105-Table 34 . Brief description o
- Page 125: -107-Figure 70 . Site of the pedon
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- Page 131 and 132: -113-YpiFigure 76, Site of the pedo
- Page 133 and 134: -115-Figure 78 . Site of the pedon
- Page 135 and 136: -117-OP 1 Map Unit (Cumilic Regosol
- Page 137 and 138: -119-OT - Otterhead Soi Iscape Grou
- Page 139 and 140: ure 82 . Site of the pedon chosen t
- Page 141 and 142: -123-Table 44 . Key criteria differ
- Page 143 and 144: -125-SI2 Map Unit (Lithic Humo - Fe
- Page 145 and 146: -127-Landform and Parent Material s
- Page 147 and 148: -129-Table 47 . Brief description o
- Page 149 and 150: Figure 91 . Site of the pedon chose
- Page 151 and 152: -133-Environmen tzones .The Tocher
- Page 153 and 154: -135--The steep slopes and the rela
- Page 155 and 156: -137-Table 50 . Brief description o
- Page 157 and 158: Figure 97 .Site of the pedon chosen
- Page 159 and 160: -141 -EnvironmentThe Watchtower soi
- Page 161 and 162: -143-Table 53 . Brief description o
- Page 163: -145-The stoniness and periodic sno
- Page 166 and 167: Brief description of the pedon chos
- Page 168 and 169: -150-late snowmelt areas or streams
- Page 170 and 171: -152-The soils have been rated acco
- Page 172 and 173: -154-Table 58 . Guides for assessin
- Page 174 and 175: -156-Table 60. Guides for assessing
-108-OL - Ottertail Soilscape GroupPhysiographic Setting (Figure 55, page 91 )This soilscape group occurs on morainal landforms below 1550 m a .s .l ., i nthe main valley bottoms, often as remnants and small pockets of what was probabl ymore extensive moraine .Landform and Parent Material sThe Ottertail soilscape group commonly occurs on morainal blankets overbedrock, but morainal veneers and deep morainal deposits are not uncommon . Theparent materials are compact, calcareous, medium textured till which may hav ebeen locally reworked by water . Small lacustrine pockets are often found as inclusion sin this till along the Kicking Horse Valley .EnvironmentThe Ottertail soilscape group occurs in the montane vegetative zone rangin gin elevation from about 1050 m a .s .l . at the western Park gate to about 1550 m a .s .l .Table 36 . Key criteria differentiating the Ottertail map units .Soilscape Coarse Fragment DrainageClassificationTextureMap Unit Content (%) Clas sOL 1 Degraded Eutric Brunisols silt loam 10-20% wel lOL2Gleyed Melanic and