Ecological Land Classification of Mount Revelstoke and Glacie r ...

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Wildlife features of Cutbank (CT) Ecosites 133Definitive features of Griffith (GF) Ecosites 135Wildlife features of Griffith (GF) Ecosites 138Definitive features of the Glacier House (GH) Ecosection 139Wildlife features of Glacier House (GH) Ecosites 140Definitive features of the Heather (HE) Ecosection 140Wildlife features of Heather (HE) Ecosites 142Definitive features of Hermit (HR) Ecosites 143Wildlife features of Hermit (HR) Ecosites 147Definitive features of Jade (JD) Ecosites 149Wildlife features of Jade (JD) Ecosites 151Definitive features of the Jonas (JN) Ecosection 153Wildlife features of Jonas (JN) Ecosites 154Definitive features of the Kuskanax (KX) Ecosection 155Wildlife features of Kuskanax (KX) Ecosites 156Definitive features of the Lookout (LK) Ecosection 157Wildlife features of Lookout (LK) Ecosites 15 8Definitive features of Lauretta (LR) Ecosites 15 8Wildlife features of Lauretta (LR) Ecosites 16 0Definitive features of Nordic (NC) Ecosites 16 1Wildlife features of Nordic (NC) Ecosites 16 5Definitive features of Redoubt (RD) Ecosites 167Wildlife features of Redoubt (RD) Ecosites 170Definitive features of the Stoney (SN) Ecosection 170Wildlife features of Stoney (SN) Ecosites 17 1Definitive features of the Witch Tower (WR) Ecosection 17 2Wildlife features of Witch Tower (WR) Ecosites 173v
PLATE S1 .2 .3 .4 .5 .6 .7 .8 .9 .10 .11 .12 .13 .14 .15 .16 .17 .Subdued topography of recessive Horsethief Creek Group bedrock in the Purcell Mountains(right) contrasting with the rugged topography of resistant Hamill Group bedrock inthe Selkirk Mountains (left) . The Beaver River valley (Purcell Trench) divides the tw ophysiographic units .Areas underlain by Lardeau Group bedrock (foreground) have more subdued topograph ythan areas of Hamill Group bedrock (background and right) .Moraines along the forest edge are the boundary of AB1 landscape below Beaver Glacier .Sampled Orthic Dystric Brunisol of the AB1 Ecosite .Steeply sloping AB1 sample site with sparse vegetation .Sampled Orthic Humo-Ferric Podzol (lithic phase) of the AK1 Ecosite .Sampled Orthic Humo-Ferric Podzol of the AK5 Ecosite .Subalpine fir-mountain hemlock/heather-luetkea (020) is the dominant v .t . of AK1, AK2and AK4 .Steep, rocky slopes with subalpine fir-whitebark pine-(Engelmann spruce)/tall bilberry-heather(022) open forest typify AK6 .AK5 tract with fleabane-valerian (H16), one of several avalanche v .t .s in the Upper Subalpine.Sampled Orthic Humo-Ferric Podzol of the BU1 Ecosite .Sampled Ortstein Humo-Ferric Podzol of the BU2 Ecosite .Mountain hemlock-subalpine fir/rhododendron-tall bilberry (C47) forest dominates all BUEcosites .Sampled Rego Gleysol of the CE1 Ecosite .Willow (S15) v .t . on CE1 in central MRNP .Sampled Orthic Ferro-Humic Podzol which is an accessory soil of CM2 . Characteristicsoils have similar humus-enriched profiles and include Orthic Dystric and Sombric Bruni -sols and Orthic Humo-Ferric Podzols .CM2 along upper Connaught Creek on a fluvial fan with green alder/fern (S13) vegetationand small patches of the sedge (H21) v .t .vii
Page 1: Alberta Instituteof PedologyUnivers
Page 4 and 5: CHAPTER V - ECOLOGICAL INTEGRATION
Page 6 and 7: TABLES1 . Temperature (°C) ranges
Page 10 and 11: 18. Sampled Eluviated Dystric Bruni
Page 12 and 13: 53. RD3 sample site with the heathe
Page 14 and 15: ABSTRACTMount Revelstoke and Glacie
Page 16 and 17: NFig . 1 . Location and drainage sy
Page 18 and 19: MRNP contains several high elevatio
Page 20 and 21: o'Table 2 . Temperature data (°C)
Page 22 and 23: Table 4. Snow depths for stations i
Page 24 and 25: STRUCTURAL FRAMEWOR KBedrock in the
Page 26 and 27: area (Fulton et al. 1984) which inc
Page 28 and 29: Table 6. Characteristics of Residuu
Page 30 and 31: Table 7. Characteristics of colluvi
Page 32 and 33: Table 8 . Characteristics of morain
Page 34 and 35: Table 9 . Characteristics of Ice Co
Page 36 and 37: Fig . 5 . Textural variation among
Page 38 and 39: ORGANIC COMPONENTThe organic landfo
Page 40 and 41: Soil Reaction : with a pH meter usi
Page 42 and 43: BRUNISOLIC SOIL SBrunisolics occur
Page 44 and 45: Gleysolics are most common on flat
Page 46 and 47: CHAPTER III - VEGETATIO NP .L .Achu
Page 48 and 49: Fig . 6 . Ecoregions of Mount Revel
Page 50 and 51: ALPINE ECOREGIO NThe Alpine Ecoregi
Page 52 and 53: C14 is mature successionally with s
Page 54 and 55: In the western Cascades of Washingt
Page 56 and 57: Table 17 . Stands of the balsam pop
Page 58 and 59:
C47: Tsuga mertensiana-Abies lasioc
Page 60 and 61:
Table 20 . Stands of the Engelmann
Page 62 and 63:
Table 22 . Stands of the western he
Page 64 and 65:
Table 23 . Stands of the western re
Page 66 and 67:
Binkley and Graham (1981) describe
Page 68 and 69:
Table 26. Stands of the Engelmann s
Page 70 and 71:
011 : Picea spp ./Ledum groenlandic
Page 72 and 73:
Table 29 . Stands of the aspen-west
Page 74 and 75:
Vegetation : The tree layer is open
Page 76 and 77:
Table 32 . Stands of the subalpine
Page 78 and 79:
Table 34 . Stands of the subalpine
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Table 36 . Stands of the willow-mou
Page 82 and 83:
Table 38 . Stands of the alder/skun
Page 84 and 85:
Table 40. Stands of the mountain av
Page 86 and 87:
Other Studies : H2 is also describe
Page 88 and 89:
Vegetation : Carex aquatilis (50-80
Page 90 and 91:
Table 45 . Stands of the fleabane-v
Page 92 and 93:
H21 : Carex spp .(sedge )Environmen
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species not climax for the site . S
Page 96 and 97:
calcareous conditions are more comm
Page 98 and 99:
SAMPLING RATIONALEMethods were chos
Page 100 and 101:
third are highly important . The fi
Page 102 and 103:
SMALL MAMMAL ASSOCIATION 1Shrubland
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Avalanche alder shru bSMALL MAMMAL
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Definitive Speciesfreq . dens . fre
Page 108 and 109:
Vegetation Type correlate swillow/h
Page 110 and 111:
Upper Subalpine coniferous closed f
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Vegetation Type correlatessubalpine
Page 114 and 115:
RemarksThe average DI is 4 .1 .In t
Page 116 and 117:
Additional SpeciesHermit Thrush .09
Page 118 and 119:
Brown Creeper .073 Nashville Warble
Page 120 and 121:
CHAPTER V • ECOLOGICAL INTEGRATIO
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EcosectionsEcoregions are conceptua
Page 124 and 125:
ECOLOGICAL (BIOPHYSICAL) LEGEND COR
Page 126 and 127:
Fig . 8 . Landscape schematic of to
Page 128 and 129:
Table 50 . Wildlife features of AB
Page 130 and 131:
Current landform construction is ve
Page 132 and 133:
Table 52. Wildlife features of AK E
Page 134 and 135:
Fig . 10 . Landscape schematic of t
Page 136 and 137:
Table 54 .EcositeWildlife features
Page 138 and 139:
Table 56 . Wildlife features of CE
Page 140 and 141:
Table 58 . Wildlife features of CM
Page 142 and 143:
Fig. 11 . Landscape schematic of to
Page 144 and 145:
Table 60. Wildlife features of CT E
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GF - GRIFFITH ECOSECTIO NThe Griffi
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WILDLIFEGF is the most important to
Page 150 and 151:
Table 63 . Definitive features of t
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GEOMORPHOLOGYHE3 is geomorphically
Page 154 and 155:
Table 67. Definitive features of He
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wash and soil creep . A few tracts
Page 158 and 159:
Table 68 .Wildlife features of HR E
Page 160 and 161:
Table 69 . Definitive features of J
Page 162 and 163:
Table 70 . Wildlife features of JD
Page 164 and 165:
GEOMORPHOLOG YThe predominant genet
Page 166 and 167:
KX - KUSKANAX ECOSECTIONThe Kuskana
Page 168 and 169:
Table 75 . Definitive features of t
Page 170 and 171:
and aprons are a poorly sorted, til
Page 172 and 173:
NC3, and NC4 have the same hemlock
Page 174 and 175:
from Bm and Bf (Brunisolic soils) t
Page 176 and 177:
Table 80 .Wildlife features of NC E
Page 178 and 179:
Table 81 . Definitive features of R
Page 180 and 181:
WILDLIFESMA 13 is assumed to be pre
Page 182 and 183:
Such soils indicate episodic deposi
Page 184 and 185:
WILDLIFEWR1 Wildlife FeaturesUngula
Page 186 and 187:
MISCELLANEOUS LANDSCAPE SCR - COLLU
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unvegetated . A few tracts have spa
Page 190 and 191:
Bamberg, S .A. and J . Major . 1968
Page 192 and 193:
Day, D., C. Zinkan and G. Wickware
Page 194 and 195:
Jurdant, M., D .S . Lacate, S .C. Z
Page 196 and 197:
Ogilvie, R .T . 1976 . The Alpine a
Page 198 and 199:
Sneddon, J .I ., L.M . Lavkulich, a
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Whittaker, R .H . 1967 . Gradient a
Page 202 and 203:
POLYPODIACEAEAdiantum pedatum L . v
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Sambucus racemosa L. var . melanoca
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CORNACEAECornus canadensis L .Cornu
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LABIATAEGaleopsis tetrahit L .Lycop
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Anemone parviflora Michx. G tAquile
Page 212 and 213:
Tellima grandiflora (Pursh) Dougl .
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GRAMI NEA Ex Agroelymus mossii Lepa
Page 216 and 217:
ORCHIDACEA ECorallorhiza maculata R
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Dicranella heteromalla (Hedw .) Sch
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Bryoria pseudofuscescens (Gyeln.) B
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Usnea scabrata Nyl . RXanthoria ele
Page 224 and 225:
Turkey Vulture Cathartes aura (Linn
Page 226 and 227:
Lazuli Bunting Passerina amoena (Sa
Page 228 and 229:
APPENDIX C - CORRELATION OF MAP UNI
Page 230 and 231:
MR & GNP Lardeau Seymour ArmJN2KX1
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Table D1 . Pedon (Alberta 1983 No .
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1 =li slu!
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Table D5. Pedon (Alberta 1981 No .
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44 M W N. M M .VI+MM Mw.N3
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Table D9 . Pedon (Alberta 1983 No .
Page 242 and 243:
Table 11 . Pedon (Alberta 1983 No.
Page 244 and 245:
Page 246 and 247:
Table D15 . Pedon (Alberta 1983 No
Page 248 and 249:
Page 250 and 251:
Table D19. Pedon (Alberta 1983 No.
Page 252 and 253:
Page 254 and 255:
Page 256 and 257:
Page 258 and 259:
Page 260 and 261:
Page 262 and 263:
Page 264 and 265:
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Page 268 and 269:
OPEN FOREST VEGETATION TYPES9: Pice
Page 270 and 271:
COLORPLATE S1-64
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11 . Sampled C)rtbic Ilumo -Eerric
Page 274 and 275:
21 . Western hemlock-wester nred ce
Page 276 and 277:
34. HR5 (lower to mid slope (and AK
Page 278 and 279:
47. Sampled Orthic Dystri cBrunisol
Page 280:
59. Sampled Orthic Glevsol u fthe W
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Ecological Land Classification of Mount Revelstoke and Glacie r ...

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