ProminentmottlesRaised shorelineSoil horizonSoil morphologySoil permeabilitySoil pr<strong>of</strong>ileSoil reactionspots <strong>of</strong> colour in soilhorizons, caused by impededdrainage, whose contrastwith the basic horizon colouris high.wave-cut side slopes <strong>of</strong>glacial till or hummockyridges <strong>of</strong> mainly stratifieds<strong>and</strong>s <strong>and</strong> gravels, depositedat the shore <strong>of</strong> an ancientglacial lake.a distinct layer <strong>of</strong> soil,approximately parallel to theground surface. Usually twoto six horizons occur withinone metre <strong>of</strong> the groundsurface .the constitution <strong>of</strong> the soil,including the texture,structure, consistence, colour<strong>and</strong> other physical, chemical,<strong>and</strong> biological properties <strong>of</strong>the various soil horizons thatmake up the soil pr<strong>of</strong>ile.the ease with which gases orliquids penetrate or passthrough the soil . <strong>The</strong> soilpermeability classes used todescribe the soils in thisreport are based on thosedescribed in the publication"CanSIS Manual fordescribing soils in the field"(12).a vertical section <strong>of</strong> the soilthrough all its horizons, <strong>and</strong>extending in to the parentmaterialthe degree <strong>of</strong> acidity oralkalinity <strong>of</strong> a soil, usuallyexpressed as a pH value.Descriptive terms commonlyassociated with certainranges in pH are : extremelyacid, 45 or less ; verystrongly acid, 4.6-5 .0 ;strongly acid, 5.1-5 .5 ;mediumacid, 5 .6-6 .0, slightlyacid, 6.1-6.5; neutral, 6.6-73,slightly alkaline, 7.4-7.8,moderately alkaline, 7 .9-8 .4;<strong>and</strong> strongly alkaline, 8.5 ormore . <strong>The</strong>se descriptions arecontained in the publication"CanSIS Manual fordescribing soils" (12) .Soil structureSoil textureFigure 12.the combination orarrangement <strong>of</strong> primary soilparticles into secondaryparticles, units or peds .the relative proportions <strong>of</strong>the various particle sizefractions in a soil, asdescribed by the soil textureclasses shown in Figure 12.<strong>The</strong> s<strong>and</strong> portion <strong>of</strong> thetriangle may be furthersubdivided into coarse s<strong>and</strong>,s<strong>and</strong>, fine s<strong>and</strong> <strong>and</strong> very fines<strong>and</strong>, based on theproportions <strong>of</strong> various s<strong>and</strong>sizes within the s<strong>and</strong>fraction. . Likewise, loamys<strong>and</strong> may be divided intoloamy coarse s<strong>and</strong>, loamys<strong>and</strong>, loamy fine s<strong>and</strong> <strong>and</strong>loamy very fine s<strong>and</strong> . Whenthe gravel percentage isbetween 20 <strong>and</strong> 50 percent,the textural class is modifiedby "gravelly", e.g. gravellys<strong>and</strong>y loam . When thegravel percentage is greaterthan 50 percent, the texturalclass name is modified by"very gravelly", e .g . verygravelly s<strong>and</strong>y loam.Soil Texture Classes
Soil typeSolumSpillwayStereoscopeSurficialgeology .the primary soil unit in thisreport for which alldescriptive <strong>and</strong> interpretiveinformation applies .the upper horizons <strong>of</strong> a soilin which the parent materialhas been modified <strong>and</strong> inwhich most plant roots arecontained . It usually consists<strong>of</strong> A <strong>and</strong> B horizons .an ab<strong>and</strong>oned channelformed by flowing glacialmeltwater.an optical instrument used toobtain a three-dimensionalimage <strong>of</strong> the l<strong>and</strong> surfacefrom aerial photographs .that branch <strong>of</strong> geologydealing with surfacel<strong>and</strong>forms <strong>and</strong> theunconsolidated materials thatcomprise them.Tolerable soil lossVeneerVery fine texturedthe rate at which soil can beremoved before theagricultural productivity <strong>of</strong>the l<strong>and</strong> is adverselyaffected .a layer <strong>of</strong> unconsolidatedmaterial up to one metrethick deposited on thesurface <strong>of</strong> some othercontrasting deposit.a term applied to soilmaterials which fall withinthe very fine textural group .<strong>The</strong> very fine textural groupis a group <strong>of</strong> soil textureswhich contain more than40% clay. Common soiltextures associated with thisgroup include silty clay <strong>and</strong>clay (see Figure 11).* Most definitions for this glossary were based on the following sources :<strong><strong>Agri</strong>culture</strong> <strong>Canada</strong>, Research Branch. Revised 1976. Glossary <strong>of</strong> Terms in Soil Science. Publication1459, 44 pp .Soil Conservation Society <strong>of</strong> America . 1970. Resource Conservation Glossary. 52 pp .