Detailed Soil Survey of the Mount Revelstoke Summit Area.

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Mount Copeland (6,060 feet ASL) .At Revelstoke mean annual precipitationis 42 .0 inches with about 17 inches occurring as snow and at Mount Copelandthere isa total precipitation of 95 .2 inches with about 83 .4 inches assnow .VegetationThe Summit area represents the upper limit of the continuousforest zone in this area . This timberline zone (Daubenmire, 1943) orforest-tundra ecotone (Weaver and Clements, 1938 ; Marr, 1961) is characterizedby clumps and individuals of coniferous trees, Abies lasiocarpa withoccasional Picea engelmannii and meadows of mixed herbaceous vegetation(dominant species include Luetkea p_ectinata , Carex spp ., Valerianasitchensis , Arnica latifolia , Erigeron peregrinus , Antennaria lanata , andpatches of Cassiope mertensiana ) .The forested areas are dominated byAbies lasiocarpa ,with Rhododendron albiflorum and Vaccinium membranaceumunderstory vegetation .Complete descriptions and a map of plant communities are includedin the report by Landals and Scotter (in prep .) .Plant nomenclature isaccording to Hitchcock and Cronquist (1973) .A table of scientific andcommon plant names is included in the Appendix .History and DevelopmentMount Revelstoke Park was established in 1914 and in 1927 thefirst road was built to the Summit .A commercial tourist lodge wasoperated on the Summit from 1940 to 1963 . In 1967 the road was rebuiltto its present gravel surfaced standards .the area is presently a day-use area only .The lodge has been removed andA system of hiking trails
traverses the area, originating from the two parking lots, which arelocated at the Summit and beside Balsam Lake .These trails connect theSummit area to Millar Lake, Eva Lake, and Jade Lakes . Because of thedead end nature of the road at the scenic Summit and the sedentary natureof most park visitors, use of the area is concentrated into a smallarea surrounding the parking lots where people walk around the smallSummit area to look at the view .
Page 2 and 3: DETAILED SOIL SURVEYOF THEMOUNT REV
Page 4 and 5: PageSOIL PRODUCTIVITY 53BIBLIOGRAPH
Page 6 and 7: LIST OF PLATESPagePLATE 1 . Humo-Fe
Page 8 and 9: INTRODUCTIONIn recent years Parks C
Page 10 and 11: THE STUDY AREAGeographic LocationTh
Page 12 and 13: calcareous rocks in the study area
Page 16 and 17: METHODS OF INVESTIGATIONField Techn
Page 18 and 19: 116 . Pyrophosphate-Extractable Alu
Page 20 and 21: 13FIGURE 2 .DIAGRAM OF A SOIL PROFI
Page 22 and 23: 15Soils of the Summit AreaThe soils
Page 24 and 25: MISCELLANEOUS MAPPING UNITSRBedrock
Page 26 and 27: AhBhf20 cm-Plate l .The Humo-Ferric
Page 28 and 29: 21extremely sloping land surfaces o
Page 30 and 31: Soil Map Unit 3(Orthic and Cumulic
Page 32 and 33: 25These soils have severe limitatio
Page 34 and 35: 27Horizon Depth (cm) Color Texture
Page 36 and 37: 295-a20 cm-5 -bPlate 5 .The hummock
Page 38 and 39: 31stands are made up of Abies lasio
Page 40 and 41: 6-aAeBfR20 cm-6 -bPlate 6 .The Lith
Page 42 and 43: 37INTERPRETATIONSSoil Properties an
Page 44 and 45: 39TABLE 4,GUIDES FOR ASSESSING SOIL
Page 46 and 47: 41TABLE 6 .GUIDES FOR ASSESSING SOI
Page 48 and 49: 43TABLE 8 .GUIDES FOR ASSESSING SOI
Page 50 and 51: 45especially where bedrock is close
Page 52 and 53: TABLE 10 . DEGREE AND NATURE OF SOI
Page 54 and 55: 49The soils of map units 1, 8 and 9
Page 56 and 57: 51compounds thus inhibiting percola
Page 58 and 59: 53PRODUCTIVITYProductivity ratings
Page 60 and 61: S4 XTABLE 11 . DISTRIBUTION OF SOIL
Page 62 and 63: 57BIBLIOGRAPHYAlberta Department of
Page 64 and 65:
59Terzaghi, K . and R .B . Peck . 1
Page 66 and 67:
61ecosystem .While the activities i
Page 68 and 69:
TABLE A. CLASSES OF FRAGILITY FOR P
Page 70 and 71:
TABLE B. CLASSES OF FRAGILITY FOR S
Page 72 and 73:
67than to channel use to a rarer ty
Page 74 and 75:
69approximately 10 cm thickness and
Page 76 and 77:
71ANALYTICAL DATA 1HorizonDepthcmCa
Page 78 and 79:
73several species of common occurre
Page 80 and 81:
75Soil Map Unit 3The imperfectly to
Page 82 and 83:
77Soil Classification :Orthic Regos
Page 84 and 85:
79ANALYTICAL DATA 3BHorizonDepthcmC
Page 86 and 87:
81Elevation : 6,000 ft . ASL (1,830
Page 88 and 89:
82ANALYTICAL DATA 4HorizonDepthcmCa
Page 90 and 91:
Aspect :southeastElevation : 6,200
Page 92 and 93:
Soil Map Unit 6Hummocky microrelief
Page 94 and 95:
ANALYTICAL DATA 6HorizonDepthcmCaC1
Page 96 and 97:
Location : S-7Parent Material :glac
Page 98 and 99:
Soil Map Unit 8These soils have med
Page 100 and 101:
Elevation : 6,250 ft . ASL (1,910 m
Page 102 and 103:
orizonPyrophosphate96ANALYTICAL DAT
Page 104 and 105:
Slope : 5%Aspect :northElevation :
Page 106 and 107:
Soil Map Unit 10Map Unit 10 soils h
Page 108 and 109:
Vegetation : Abies lasiocarpa (shru
Page 110 and 111:
104ANALYTTCAL DATAlOBHorizonDepthcm
Page 112 and 113:
A further separation of sands is ma
Page 114 and 115:
(D1) Rapidly drained - soil moistur
Page 116 and 117:
110TABLE 13 . UNIFIED SOIL CLASSIFI
Page 118 and 119:
GLOSSARYThis is included to define
Page 120 and 121:
illuviation -the process of deposit
Page 122 and 123:
pH - a notation used to designate t
Page 124:
LATIN AND COMMON NAMES OF PLANTS ME
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Detailed Soil Survey of the Mount Revelstoke Summit Area.

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