RURAL MUNICIPALITY OF

WILLOW CREEK, NUMBER 458

MAY 1,1987 (Revised March 1, 1989)

1. INTRODUCTION

This report and map have been prepared as an interim document to enable the'Sask- atchewan Institute of Pedology to make available pertinent soil data and interpretive soil information for this municipality. A final report and maps, which will include this and other data, are being produced and published. The final report and accompanying maps will not, however, be available for three to five years.

The information presented within this report is designed for the interpretation of various soil and landscape properties that may benefit planning and land management within the municipality. Due to the preliminq nature of this report, the final soil map and interpretive data may be slightly altered before the final publication is printed.

Saskatchewan Soi1 Survey. Page i 2. TABLE OF CONTENTS

1. INTRODUCTION ...... i .. 2. TABLE OF CONTENTS ...... 11 3. HOW TO USE THIS MAP AND REFORT ...... 1 4. EXPLANATION OF THE MAP SYMBOL ...... 3 4.1 Slope Classes ...... 3 4.2 Surface Forms ...... 3 4.3 Surface Texture ...... 5 5. SOIL INTERPRETATION SYMBOLS ...... 8 5.1 Salinity ...... 8 5.2 Irrigation Suitability ...... 11 5.3 Agncultural Capability ...... 15

5.4 Stones ...... 19 5.5 Wetiands and Drainage ...... 19 5.6 Sand and Grave1 ...... 22

5.7 Surface pH ...... 24

5.8 Wind Erosion ...... 25 . 5.9 Water Erosion ...... 27

5.10 Past Wind and Water Erosion ...... 29 6. AREA FACTS ...... 3 1 7. SOLMAP UNIT DESCRIPTIONS ...... 33

8. SOIL INTERPRETATIONS ...... 49 9. FURTHER INFORMATION ...... 54 3. HOW TO USE THIS MAP AND REPORT

THESOIL MAP - The soil map, contained in the back cover of this report, shows al1 soil areas delineated - during the mapping of the municipality. The soils, and some of their properties, are represented on the map by a.series of symbols that identify the kinds and distribution of the component soils within each delineation. This symbol sequence is illustrated below.

Soil Association: Delineation No.: (186) LcSb (La Corne-Shellbrook) Soil Map Unit No.: (2) Slope Class: 3-4 (2- 10% slopes) Surface Texture: fl -VI (fine sandy loam to very fine sandy loam) (hummocky-dissected)

- The soil association and map unit (e.g,, LcSb2) indicate the types of soils present within ’ the delineation. A description of these soils is presented in Section 7 entitied, “Soil Map Unit - Descriptions”. An explanation of the symbols for surface form, slope class and surface texture is presented in Section 4 entitled, “Explanation of The Map Symbol”.

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Saskatchewan Soil Survey. Page 1 - How to Use This Map and Report, Cont.

OTHERINTERPRETATIONS

The final report will include a series of interpretive maps that will provide information on such aspects of soils as salinity, irrigation suitability, agricultural capabiiity, stoniness, wetlands and drainage, surface pH, wind and water erosion, and Sand and grave1 occurrences. This information is also provided in this report, but in a tabular rather than rnap form. This information can be obtained by determinhg the delineation number from the soi1 map and refening to Section 8 for a listing of the symbols. Then, by refemng to the appropriate subsection in Section 5 entitled, “Soil Interpretation Symbols”, an explanation of the symbols can be obtained.

EXAMPLE

If one wanted to know the agricultural capability classification for area 186 (used in example on previous page), turn to Section 8 and look up the number 186 listed in the left-hand column under the heading, “Delineation Number”, then read across to the symbols listed in the column headed, “Agricultural Capability”. There, the symbols 3(5)TW2(4)MT5( 1)W occur. Then, tum to Subsection 5.3, entitled, “Agricultural Capability ”, for an explanation of these symbols. From this explanation, it can be ascertained that 50% of the area has been rated Class 3 and has moderately severe limitations due to topography and wetness, 40% of the area has been rated Class 2 because of moderate moisture and topographic limitations, and 10%of the area has been ratedclass 5 because of excess wetness.

Saskatchewan Soil Survey. Page 2 4. EXPLANATION OF THE MAP SYMBOL

4.1 SLOPECLASSES

Class Description

1 Nearly level- slopes of 0.5% or less.

2 Very gently sloping - slopes up to 2% but dominantly 0.5 t02%

3 Gently sloping - slopes up to 5% but dominantly 2 to 5%

4 Moderately sloping - slopes up to 10% but dominantly 5 to 10%

5 Strongly sloping - slopes up to 15% but dominantly 10 to 15%

6 Steeply sloping - slopes up to 30% but dominantly 15 to 30%

7 Very steeply sloping - slopes dominantly greater than 30%

Note: A one-percent slope is a change in elevation of one metre in a horizontal distance of 100 metres

4.2 SURFACEFORMS

Mineral Surface Forms Erosional Modifiers

MaP MaP Symbol Name Symbol Name

~ H Hummocky C Channelled 1 Inclined D Dissected L Level G Gullied M Rolling R Ridged T Terraced U Undulating

~ ~~~~

Saskatchewan Soi1 Survey. Page 3 Surface Forms, Cont.

Hummock y Landscapes with a complex pattern of generally short, steep slopes extending from prominent knolls to somewhat rounded depressions or kettles are termed hummocky. They are called hummocky dissected where shallow gullies join one low area or kettle to the next. Occasionally, areas have a complex of ridged and hummocky features. They are called hummocky-ridged.

Inclined Landscapes in which the generai slope is in one direction, only, are called inclined. Where shallow gullies occur along the slope, the areas are called inclined dissected; where a series of parallel or subparallel, deep gullies or ravines occur, they are called inclined gullied. Along flood plains of rivers and streams where the inclined surface is broken by abandoned river channels they are called inciined channelled.

Level Landscapes that are flat or have very gently sloping surfaces are said to be level. Along floodplains of rivers and streams where the level surface is broken by abandoned river channels they are calied level channelled.

Ridged Landscapes that have a linear pattern, usually of short and straight parallel ridges but sometimes a single, sinuous ridge or a series of intersecting ridges are termed ridged.

Rolling Landscapes that are characterized by a regular sequence of moderate slopes extending from rounded, sometimes confined, concave depressions to broad, rounded convexities produc- ing a waveiike pattern of moderate relief are termed rolling.

Terraced Areas, usually dong a Valley, that have a steep, short scarp slope and a horizontal or gently inclined surface above it are called terraced.

Undulating Landscapes that are characterized by a sequence of gentle slopes extending from smooth rises to gentle hollows, that impart a wavelike pattern to the land surface are called undulating. Where shallow gullies extend from one low area to the next in these landscapes they are called undulating dissected and where the undulating surface is broken by abandoned river channels they are called unduiating channelled. Where a series of parallel or subparallel, deep gullies or ravines occur, they are called undulating gullied.

Saskatchewan Soi1 Survey. Page 4 Surface Forms, Cont.

Organic Surface Forms

MaP Symbol Name

H Horizontal R Ribbed

Horizontal ûrganic landscapes with flat peat surfaces that are not broken by marked elevations and depressions. On a microtopographic scale the surface may be very hummocky with local topography of up to 0.6 m (2 ft.). Where very low ridges occur on these leve€landscapes, they are called horizontal-ribbed.

Ribbed Organic landscapes with generally flat peat surfaces that have a pattern of very low parallel or reticulate ridges. They are generally associated with Sedge Peats.

4.3 SURFACETEXTURE

SOILTEXTURE

A mineral soil is a mixture of various-sized mineral particles, decaying organic matter, air and water. The mineral particles, exclusive of Stones and gravel, may be grouped into three particle-size fractions; sands (the largest or coarsest), silts, and clays (the smallest or finest). The relative proportions of these particle-size fractions in a soil determine its texture. Thus, sand, when dominant, yields a sandy- or coarse-textured soil, whereas a fine-textured soil is made up largely of silt and Clay. The terms ‘light’ and ‘heavy’, often used to refer to sandy- and clayey- textured soils, respectively, are actually a measure of the power required to till the soil and were originally related to the number of horses required to pull the plough -light or sandy land was described as one-horse land, and heavy land as four-horse land. These terms have nothing to do with the actual weight of soil, as a given volume of dry Sand actually weighs slightly more than that of Clay.

Saskatchewan Soi1 Survey. Page 5 Surface Texture, Cont.

Textural class names such as sandy loam, Clay loam, heavy Clay and the like are given to soils based upon the relative proportions of sand, silt and Clay. Three broad, yet fundamental, textural groups are recognized: sands, loams and clays.

SANDS - The Sand group includes soils in which the sand particles make up at least 70% of the material by weight. Two main classes are recognized: Sand and loamy sand.

CLAYS - The Clay group contains at least 35% Clay, and in most cases more than 40%. Class names are: sandy Clay, silty Clay, Clay and heavy Clay. Soils of this group are often called ‘gumbo’.

LOAMS - The loam group is intermediate in texture between the coarse- textured sands and the fine-textured clays, and usually contains a significant proportion of each particle-size fraction. Class names include: sandy loam, silt loam, silty Clay loam, sandy Clay loam, Clay loam and loam.

TEXTURALTRIANGLE

100

90 ---*--- The textural triangle shows the per- 80 \ centage of sand, silt and Clay in each 70 I I ’\1 * 60

O5 50 cz 3 40 K w n 30

20

10

O O 10 x) 30 40 50 60 70 80 90 100 PERCENT SAND

Saskatchewan Soi1 Survey. Page 6 Surface Texture, Cont.

Map Symbol Soil Texture CIass

Coarse -Textured

GS Gravelly Sand S Sand FS Fine Sand GLS Gravelly loamy Sand LS Loamy Sand

Moderately Coarse-Textured

GSL Gravelly sandy loam SL Sandy loam FL Fine sandy loam VL Very fine sandy loam GL Gravelly loam

Me dium-Textured

SCL Sandy Clay loam FCL Fine sandy Clay loam VCL Very fme sandy Clay loam L Loam

Moderately Fine-Textured

SIL Silt loam CL Clay loam SIÇL Silty Clay loam

Fine-Textur ed

C Clay SIC Silty Clay HC Heavy Clay

Saskatchewan Soil Survey. Page 7 5. SOIL INTERPRETATION SYMBOLS 5.1 SALINJTY

A saline soil is a soil with sufficient amounts of water soluble salts to inhibit the uptake of moisture by plants. This inhibition of water uptake results in moisture stress andreduced plant growth. The most common soluble salts in Saskatchewan soils are magnesium and sodium sulfates. Calcium sulfates also occur but are not as easily dissolved and are less harmful. Calcium, magnesium and sodium chlorides may also be present. The presence of saline soils can often be recognized by bare spots in the crop or as uneven stands of grain or forage. Very strongly saline soils usually develop a white surface crut dunng dry weather. Where less Salt is present, the soil is grayish in color when dry and the subsoil often has streaks or specks of Salt at a depth of 5 to 25 cm (2 to 10 in.) or deeper. In some cases, it may not be possible to see the sait and a soil anaiysis must be carried out.

MANAGEMENTOF SALINE SOILS

Saline soils should be managed in such a way as to either prevent further spread or intensification of the problem, or, where possible, to reclaim land which has already become salinized. Since most of the salinity is the result of groundwater movement, the key to control lies in the effective management of groundwater flow and water table levels. One method of achieving this objective is to use precipitation where it falls preventing it from entering the groundwater system. Extending the cropping rotation in saline areas will cycle more precipita- tion through crops rather than ailowing it to reach the water table. This practice is most effective in areas of recharge where water that reaches the water table is very often responsible for soil salinization on lower slopes. Saline soils should be cropped continuously or seeded to long-term forage crops. High moisture use crops will intercept incoming groundwater and may lower the water table. Crop production on saline soils may also be improved by using farmyard manure or green manure, growing Salt-tolerant crops and improving surface or subsoil drainage. Fertilizer may help if soils are weakiy or moderately saline. The choice of crops which can be grown on saline soils should be based on a soil test. It must be recognized, however, that, even though a crop is considered to be tolerant to a specific degree of salinity, some yield reduction can be expected. On some soils, the use of subsurface drainage installations may be effective in lowering the water table and reducing soil salinity. These drainage installations are most effective in relatively permeable materials affected by shallow water tables. Subsurface drainage may be costly and potentiai sites need to be studied and water tables monitored for a period of time to determine the feasibility of this drainage method to produce the desired results. Drainage of water ponded in sloughs may be beneficial in controlling soil salinity. In some areas, the source of water entering the shallow groundwater flow systems is the water ponded in these sloughs. Drainage of any type, however, requires an approved permit. In Saskatchewan, anyone installing drainage works may be held responsible for any subsequent damage caused by the drained water.

Saskatchewan Soi1 Survey. Page 8 Salinity, Cont.

Further information on soil salinity and drainage can be found in the publications: Understanding Sait-Affected Soiis and Subsurface Drainage for Saiiniîy Control, available frorn Saskatchewan Agriculture.

SALINXTY SYMBOL

e.g. 1WA

1 - Soil salinity extent class W - Soil salinity degree class A - Landscape position

EXTENTAND DEGREEOF SALINESOILS

- The salinity symbol indicates the extent and degree of the Salt-affected soils and is based on field observation alone. The extent of soil salinity was estimated as a percentage of the area of the map delineation in which soi1 salinity occurred. Estimates of the degree of soil salinity - were based on the observed effect of the salinity on crop growth.

Soil ' SaIinity Extent Class Limits

~- Extent Class % Of Area Affected

O

O- 3

3 - 10

10 - 20

20 - 40

40 - 70

> 70

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Saskatchewan Soil Survey. Page 9 Salinity, Cont.

Soil Salinity Degree Classes

Electrical Conductivity Salinity of 0-60 cm depth Degree (mS/cm) Effect on Crop Growth

Nonsaline O- 2 There are no visible effects of salts on the growth of crops

Weak cw) 2- 4 Yields of very sensitive crops may be restricted

Moderate (M) 4- 8 Yields of many crops are restricted

Strong (S) 8- 16 Only tolerant crops yield satisfactorily

Very Strong (V) 16+ Only a few very tolerant crops yield satisfactorily

LANDSCAPEPOSITION

P Saline soils occur on the edges of depressions, sloughs or runways. Al1 soils in the bottoms of the depressions are leached and nonsaline. These areas generally occur on relatively level or very gentle regional slopes.

A Saline soils occur throughout the bottoms of depressions and sloughs. Salinity may extend out from the slough or depression but is generaily the strongest in the most low- lying areas of the landscape.

D Saline soils extend throughout the bottoms of dissections and small runways in the landscape. It is very simïlar to class A, however, it is restricted to soil areas which have dissections and/or runways.

S Saline soils occur on the sides of hills and slopes well above any slough or depression. The occurrence of salinity is controlled by stratigraphic differences in the surficial materials.

1 Saline soil materials generally occur on knolls and upper slopes. In these areas, salts occur below the A horizon due toinsufficient infiltration of precipitation to leach the salts out of the root zone. In some areas, erosion has removed sufficient topsoil to expose saline soil or to cause saline soils to be nearer the surface. Salts in these areas are usually of weak degree and are at or slightly higher than the degree of natural salts occurring in the parent material. Saskatchewan Soil Survey. Page 10 5.2 IRRIGATION SUITABILITY

INTRODUCTION

The irrigation suitability rating is baseci on measured or interpreted soil and landscape characteristics described on the map and in the various sections of this report. The suitability rating uses limiting factors to predict the potential landscape-water-crop interaction. It also considers the potential long-term consequences of irrigation such that the soil will remain permanently productive while being irrigated. It does not consider water availability and quality, climate, or economics. Within any one map delineation there may be smaller soil areas which have higher or lower irrigation suitability than that indicated by the map symbol. Any decision regarding irrigation should only be made after a field-specific examination is made.

IRRIGATION SYMBOL

e.g. ILCmvt,

2C - Irrigation class m - Soil limitations v, t, - Landscape limitations

The combination of soil and landscape categories, based upon the most limiting features present, determines the irrigation class and suitability rating.

- Soil Landscape Category Category Description

.- A nonlimiting B slightly limiting C moderately limiting y D severely-limiting

Thus, the example above indicates that the area in question has slight limitations due to soil factors and moderate limitations due to landscape factors. An explanation of the suitability classes and soil and landscape limitations is presented on the following pages.

Saskatchewan Soil Survey. Page Il - Irrigation Suitability, Cont.

- IRRIGATIONSUIIABILITY CLASSES

Class Rating Degree of Limitation Description

1A Excellent No soil or landscape These soils are medium textured, well limitations drained and hold adequate available moisture. Topography is level to nearly level. Gravity irrigation methods may be feasible.

2A Good Slight soil andor Slight soil andor landscape limitations 2B landscape limitations may limit the range of crops that can be 1B grown, require higher development inputs and require greater management skills. Sprinkler irrigation is usually the only feasible method of water application.

3A Fair Moderate soil andor Moderate soil andor landscape limita- 3B landscape limitations tions reduce the range of crops that may be 3c grown and increase development and im- 1c provement costs. Management may in- 2c clude special conservation techniques to minimize soil erosion, limit Salt move- ment, limit water table build-up or flooding of depressional areas. Sprinkler irrigation is usually the only feasible method of water application.

4A Poor Severe soil and/or Severe soil anaor landscape limitations 4B landscape limitations generally result in a soil that is unsuitable 4c for sustained irrigation. Some lands may 4D have limited potential when special 1D crops, irrigation systems, and soil and 2D water conservation techniques are used. 3D

Saskatchewan Soi1 Survey. Page 12 - Irrigation Suitability, Cont.

- LANDSCAPELIMITATIONS

~~

Symbol Description

t Slope - refers to the presence of simple slopes (t,) in undulating landscapes, or complex slopes (5) in hummocky or inclined landscapes. Complex slopes are often more limiting than simple slopes. Topography may affect the type of irrigation system, design and management required.

P Stones - refers to the amount of stonepresent on the surface and in the soil. Stones may reduce the available water-holding capacity of the soil, increase development costs and restrict the types of crops that may be grown.

Inundation - refers to the frequency of flooding. The inunda- tion hazard is used mainly in areas adjacent to rivers.

Impact on Nontarget Areas - refers to the hazard resulting from the impact -of applied irrigation water on an adjacent nonirrigated area. The hazards may include such effects as higher water tables, wetter soils, development or build-up of saline areas, or flooding and sedimentation caused by runoff.

V Horizontal Variabiiity - refers to the horizontal variations caused by texture, soil structure, and landscape pattern that may result in the surface ponding of imgated soils.

Saskatchewan Soi1 Survey. Page 13 Irrigation SuitabiIity, Cont.

SOILLIMITATIONS

Symbol Description

d Structure - soil structurai properties that restrict root and water penetration. Commonly used with soils that have a dense B horizon and an A horizon that is subject to crusting.

k Hydraulic Conductivity - the rate at which water moves through a saturated soil. Used mainly on soil areas that swell upon wetting, restricting water movement through the soil.

m Available Water-Holding Capacity - the amount of water held by a soil that can be absorbed by plants. Coarse-textured soils with a low water-holding capacity are considered to be relatively inefficient for irrigation, as compared to medium-textured soil. Soils with this limitation also have relatively high hydraulic con- ductivities and intake rates.

Geological Uniformity - the uniformity of the soil texture with depth. The greater the textural difference between the surface and subsoil, the greater the potential for the development of perched water tables and lateral water movement.

Intake Rate - the rate of movement of water into the soil. It is closely associated with hydraulic conductivity which controls the rate at which watermoves through the soil, and thus affects the rate at which water is able to enter the soil. Usually used on fine- textured soils that have relatively low intake rates requiring relatively light water application rates.

W Drainage - the rate of removal of water from a soil in relation to supply. Indicates areas of mainly poorly drained soiis.

S Salinity - the presence of soluble salts that may affect the growth of crops. The potential exists for lower yields, or for lateral Salt movemen t into adjacent areas.

Saskatchewan Soi1 Survey. Page 14 5.3 AGRICULTURALCAPABIL~Y

AGRICULTURALCAPABILITY SYMBOL

The agricultural capability symbol is composed of: fist, a number that indicates the capability class, followed by a bracketed number that indicates the percentage of the area composed of soils with the indicated capability class, and, lastly, a letter (or letters) that indicate(s) the soil, landscape or climatic limitations that determine the degree of limitation (capability class).

EX AMPLE

Class 3 soil 3 (6)M5(4)TE~~ Limitationdueto adverse topography (T) 6/10 or 60% ,, and erosion damage (E) Limitation due to insufficient 4/10 or 40% of the delineation moisture-holding capacity (M) Class 5 soil

3(6)M5(4)TE means that 60% of the area was placed in class 3 due to a limitation in moisture-holding capacity and 40% of the area in Class 5 because of limitations due to topography and erosion damage.

Saskatchewan Soi1 Survey. Page 15 - Agricultural Capability, Cont.

- CAPABILITYCLASS (DEGRES OF LIMITATION)

The mineral soils of Saskatchewan are grouped into seven capability classes. Soils rated Classes 1to 3 are considered suitable for sustained production of cornmon cultivated field crops, those rated Class 4 are considered marginal for sustained production of cornmon cultivated field crops, those rated Class 5 are considered capable only of permanent Pasture and hay production, those rated Class 6 are considered suitable only for use as native Pasture, and those rated Class 7 are considered unsuitable for either the production of field crops or for use as native Pasture.

CLASS 1 Soils in this class have no signifiant limitations in use for crops.

CLASS 2 Soils in this class have moderate limitations that restrict the range of crops or require moderate conservation practices.

CLASS 3 Soilsin this class have moderately severe limitations that restrict the range of crops or require special conservation practices.

CLASS 4 Soils in this class have severe limitations that restrict the range of crops or require special conservation practices, or both.

CLASS 5 Soils in this class have very severe limitations that restrict their use to the production of native or tame species of perennial forage crops. hnprovement practices are feasible.

CLASS 6 Soils in this class are capable of producing native forage crops only. Improvement practices are not feasible.

CLASS 7 Soils in this class have no capability for arable agriculture or permanent Pasture.

CLASS O Unimproved or virgin organic soils are not included in classes 1 to 7, and are designated by the letter ‘Oy.

Saskatchewan Soi1 Survey. Page 16 - Agricultural Capab ility , Cont.

- CAPABILITYSUBCLASS (KIND OF LIMITHION)

The capability subclass represents a grouping of soils that have the same kind of limitations for crop production. If more than one limiting condition is recognized in a particular area, the subclasses are listed in order of their importance.

Climatic Limitations - Limitations due to climatic deficiencies.

Cm Depicts a moisture deficiency due to insufficient precipitation.

cs Depicts a heat deficiency expressed in tenns of length of growing season and frost-free period.

Soil Limitations - Limitations due to soil deficiencies are caused by adverse physical, chemical and morphological properties of the soil.

D Depicts adverse soil structure in the upper layers (A and B horizons) that affects the condition of the seedbed, prevents or restricts rmt growth and penetration, or adversely affects moisture penneability and percolation.

F Depicts adverse fertility characteristics of soils having naturally low inherent fertility due to lack of available numents, high acidity or alkalinity, high calcium carbonate content or inadequate cation exchange capacity.

M Depicts an insufficient soil water-holding capacity, due to the combined effects of the texturai characteristics of the top 1 m (3 to 4 ft.) and by the organic matter content of the surface horizon.

N Depicts excessive soil salinity.and applies to soils with either high alkalinity or a sufficient content of soluble salts to adversely affect crop growth or the range of crops which can be grown.

S Depicts a variety of adverse soil characteristics. It is used in a collective sense in place of subclasses M, D, F and N, where more than two of them are present, or where two of these occur in addition to some other limitation.

Saskatchewan Soil Survey. Page 17 - Agricultural Capability, Cont.

LandscaDe L imitations - Limitations due to adverse characteristics of the soil landscape.

T Depicts a limitation in agricultural use of the soil as the result of unfavorable topography. It includes hazards to cultivation and cropping imposed by increas- ing degree of slope as well as by the irregularity of field pattern and lack of soil uniformity .

W Depicts a limitation due toexcess water caused by either poor soil drainage, a high groundwater table or to seepage and local runoff. It does not include limitations that are the result of flooding.

P Depicts a limitation caused by excess Stones and it applies to soils that are sufficiently stony that the difficulty of tillage, seeding and harvesting are significantly increased.

E Depicts a limitation caused by actual damage from wind andor water erosion.

1 Depicts a limitation due to inundation and applies to soils subjected to flooding by lakes or streams, but does not include local ponding in undrained depressions.

R Depicts a limitation due to shallowness to bedrock and applies to soils where the rooting zone is restricted.

X Soils having a moderate limitation due to the accumulative effect of two or more adverse characteristics of the soil and the landscape which singly are not serious enough to affect the class rating.

Saskatchewan Soi1 Survey. Page 18 5.4 STONES

Symbol Description

so Nomton y.

s1 Slightly stony - Stones seldom hinder cultivation. Light clearing is occasionally required.

s2 Moderately stony - Stones are.a moderate hindrance to cultivation. Annual clearing is usually required.

s3 Very stony - Stones cause a serious hindrance to cultivation. Sufficient Stones to require clearing on an annual basis.

s4 Excessively stony - Stones prohibit cultivation or make clearing a major task. Cultivation is usually severely hindered, even after regular, heavy clearing.

U Unclassified.

5.5 WETLANDSAND DRAINAGE

Wetlands, commonly referred to as sloughs, ponds or marshes, develop in depres- sional areas that receive surface runoff f?om the surrounding landscape, but lack external drainage. They are frequentiy flooded in the spring and may contain water throughout the year. Although most are considered agricultural wastelands, they are often critical wildlife habitats.

Four types of wetlands, based on the duration of flooding and the proportion of the area pennanently occupied by open water and the occurance of organic materials are recog- nized: organic wetlands, wet meadows, marshes, and open water wetlands.

Surface drainage, or runoff, refers to the loss of water from an area by flow over the land surface. The water either ends up in local undrained depressions or, following a network of local channels, creeks and streams, is carried out of the area. Surface drainage is controlled principally by two factors: (1) the texture and structural characteristics of the soil, and (2) the direction, steepness and frequency of slopes, often-referred to as the topography.

Saskatchewan Soi1 Survey. Page 19 Wetlands and Drainage, Cont.

Symbol Extent of Wetlands

Reeional Runoff

Al O - 5% A2 5 -15% A3 15- 40%

Local Runoff and Accumulation

B1 O - 5% B2 5 -15% B3 15- 40%

Major Accumulation

c1 O - 5% c2 5 -15% c3 15- 40% c4 40- 70%

DW Organic Wetlands DX We t Meadows DY Marshes DZ Open Water Wetlands - Wetlands and Drainage, Cont.

- SURFACEDRAINAGE CLASSES

A Areas of Regional Surface Water Runoff - These are landscapes where most, if not all, of the water that is shed locally is carried out of the area to major creeks, rivers or lakes. They are usually characterized by the presence of gullies.

B Areas of Local Runoff and Accumulation of Surface Water - These are landscapes where water that is shed from upper slopes collects in local depressions that are too small to be shown on the map. They are usually recognized by chaotic, hummocky landscapes with numerous, enclosed depressions or sloughs.

C Areas of Major Accumulation of Surface Water - These are typically low-lying flat or depressional landscapes that receive surface runoff from surrounding areas resulting in temporary periods of wetness due to occasional flooding.

D Wetland Areas - These are areas that receive sufficient water from runoff and other sources to be considered a wetland. They are primarily nonagricultural lands made up of wet, poorly drained soils, or organic soils. These areas are described in greater detail in the following section.

WETLANDTYPE

DW Organic Wetlands - These areas are dominated by shallow organic soils. Wet poorly drained soils occur near the margins and al1 soils remain saturated for most of the year.

DX Wet Meadows - These areas consist mainly of wet, poorly drained soils. Flooding - occurs mainly in the spring but can last until midsumer. These are often hayland areas but may be partially cultivated during periods of drought.

- DY Marshes - These areas consist of wet, poorly drained soils near the edges with shallow open water in the centre. Flooding usually persists until late sumer and occasionally throughout the year. Haying may take place around the slough margins but these areas are rarely cultivated.

DZ Open Water Wetlands - These areas are dominated by shallow open water with wet, poorly drained soils around the outer fringes. They are permanently flooded.

~ ~~ ~ ~

Saskatchewan Soi1 Survey. Page 21 5.6 SANDAND GRAVEL

The Sand and gravel symbol shows the location of near surface sources of sandy and gravelly materials. The materiais can range from mixtures of Sand and silt to coarse gravelly Sand. These materiais may be used for concrete, sub-base for roads, traffic gravel or pervious borrow for fil1 purposes. This symbol does not suggest whether any of these areas contain sands and gravels of sufficient volume or quaiity to enable commercial development.

The term sandrefers to materials with greater than 50% Sand and with less than 15% Clay. Grave1 refers to materials having a significant component of particles greater than 2 mm in diameter.

Symbol Description

SGO No sandy or gravelly materials recognized.

s1 Very limited areas of sandy materials (1-15% of landscape).

G1 Very limited areas of gravelly materials (1-15% of landscape).

SG1 Very limited areas of sandy and gravelly materials (1-15% of landscape). s2 Limited areas of sandy materiais (15-40% of landscape).

G2 Limited areas of gravelly materials (15-40% of landscape).

SG2 Limited areas of sandy and gravelly materials (15-40% of land- sc ape) . s3 Extensive areas of sandy materials (40-70% of landscape).

G3 Extensive areas of gravelly materials (40-70% of landscape).

SG3 Extensive areas of sandy and gravelly materials (40-70% of landscape). s4 Very extensive areas of sandy materials (greater than 70% of landscape). G4 Very extensive areas of gravelly materials (greater than 70% of landscape). SG4 Very extensive areas of sandy and gravelly materials (greater than 70% of landscape). U Unclassified.

Saskatchewan Soi1 Survey. Page 22 Sand and Gravel, Cont.

CHARACTERISTICSOF SAND AND GRAVELPITS

The following table lists the legal location and provides information on various charac- teristics of Sand and grave1pits in this municipality. The data was compiled by the Saskatchewan Research Council based on detailed field investigations by the Saskatchewan Department of Highways and Transportation.

Characteristics of Sand and Gravel Pits in the Willow Creek Rural Municipality, No. 458

Tesied Legal Location Thickness Texture (%) 114 Sec Twp Rg Mer (m) Gravel” Sand Fines Comments

NO TEST INFORMATION AVAILABLE

~~

* “Gravel” refers to material greater than 5 mm diameter (Industrial Classification).

“Sand” refers to matenal greater than 0.071 mm and less than 5 mm diameter.

“Fines” refers to materiai less than 0.071 mm in diameter.

Saskatchewan Soi1 Survey. Page 23 5.7 SURFACE PH Surface pH Classes

The pH scale, which ranges from O to ~~ ~~~~ ~ 14 is used to indicate the relative acidity or Percent alkalinity of a solution. The pH of a soil is Symbol Surface pH Class related to the concentration of hydrogen ions in the soii solution. A soil with a pH value of x1 X5A3B2 7.0 is said to be neutral, while one with a value less than 7.0 is said to be acidic, and one with A0 A5B5 a value greater than 7.0 is said to be alkaline. Al A7B2C’ A2 A5B2C3 The pH values indicated in the table in Section 8.0 are for the surface layer of soil A3 A3B4C3 which ranges in thickness from 10 to 20 cm. A4 A3B3C3D‘ The soil pH was measured in 0.01M CaC1,. A BO B7A2C’ soil with a pH between 6.5 and 7.5 provides the best environment for crop growth. Yields B1 B4C4A2 of sweet clover and alfalfa are reduced below B2 B7C3 a pH of 6.0. A pH of 5.0 or less may reduce B3 BSC5 the yields of wheat, barley and canola. B4 B6C3D’ c1 C5B4D’ pH Class pH Range c2 C7B3 c3 C7B2D’ X less than 5.0 c4 C9D’ A 5.0 to 5.5 c5 C7B‘D2 B 5.6 to 6.5 D1 D5C5 C 6.6 to 7.5 D2 D7C3 D3 D9C1 D greater than 7.5

EXAMPLE

Symbol > B1 = B4C4A2

B4 - 40% of surface area has a pH in the “B” range (5.6 - 6.5) C4 - 40% of surface area has a pH in the “C” range (6.6 - 7.5) A’ - 20% of surface area has a pH in the “A” range (5.0 - 5.5)

Saskatchewan Soi1 Survey. Page 24 5.8 WINDEROSION

WINDEROSION POTENTIAL In Saskatchewan, there was relatively little wind erosion while Our soils were under natural vegetation, but, since the early 19Oo’s, erosion has had profound effects resulting in excessive losses of topsoil from agricultural land. In the past, there was little concern about soil losses due to wind erosion because of Our inability to monitor the importance and extent of these losses. Presentiy, we are able to study and understand the physical, chemical and biological properties which control wind erosion and thereby we can classify and predict a soils wind erosion potential. The wind erosion potential of the soils in this municipality is based on the dominant surface texture, topography, ridge roughness and climatic conditions within an area. These features are used to predict a soil’s susceptibility to winderosion. The actual amount of past wind erosion that has occurred is not considered in this report. As well, the influence of management practices is not part of the initial evaluation even though this parameter has a pronounced effect on the potential erodibility of soils. Surface Texture The relative proportions of Sand, silt and Clay present influence a soil’s ability to absorb andretain moisture and, consequently, to form aggregatesresistant to wind erosion. Coarse-textured soils have a “single grain” structure lacking sufficient -amounts of silt and Clay to bind individuai Sand particles together. Consequently, these soils are readily broken down and eroded by wind. Fine-textured soils have a high water-holding capacity and strong surface attraction. This results in a good soil structure with a high degree of resistance to wind erosion. However, under certain conditions, fine-textured soils wili aggregate into Sand-sized particles, and in this condition are quite susceptible to erosion by wind. Medium-textured soils contain sufficient amounts of silt and Clay to bind Sand grains, forming a good soil structure resistant to granulation and, consequently, wind erosion.

Topography The influence of topography, which includes such features as the differences in relief or height between one place and another, the direction, steepness and frequency of slopes, and the comparative roughness of the land’s surface al1 have a pronounced effect on the potential erodibility of soils. In general, the greater the slope of the land (Section 4.1), the greater the potentiai for wind erosion to occur.

Climate The clirnatic information used to calculate potential wind erosion is based on the average wind velocity and the precipitation-evaporation index for a particular location. This information was compiled from officiai weather records of specific Saskatchewan locations. Soil-Ridge Roughness The soil-ridge roughness factor refers to the roughness of the soil surface in the form of ridges which result mainly from the operation of tillage and planting equipment. The fields are classified as smooth, semi-ridged, or ridged.

Saskatchewan Soi1 Survey. Page 25 Wind Erosion, Cont.

Class Susceptibility Description

1 Very LQW Soils in this class have a very low susceptibility to wind erosion. Good soil management and average growing conditions will produce a crop with suf- ficient trash cover to protect these soils against wind erosion.

2 LOW Soils in this class have alow susceptibility to wind erosion. Good soil management and average growing conditions may produce a crop with suf- ficient trash cover to protect these soils against wind erosion.

3 Moderate Soils in this class have a moderate susceptibility to wind erosion. Average growing conditions may not supply adequate trash cover to protect these soils against wind erosion. Enhanced soil man- agement practices are necessary to control wind erosion.

4 High Soils in this class have a high susceptibility to wind erosion. Average growing conditions will not provide sufficient trash cover to protect these soils against wind erosion. Conversion of coarse- textured soils to Pasture or forage crops will pre- vent severe degradation of the soil.

5 Very High Soils in this class have a very high susceptibility to winderosion. These soils should not be used for annual cropping, but rather for Pasture and forage crops which will protect the surface from severe degradation.

6 Extremely High Soils in this class have an extremely high suscep- tibility to winderosion. These soils must be left in permanent Pasture and are not capable of main- taining arable agriculture.

U Unclassified Unclassified areas (Wetlands).

Saskatchewan Soi1 Survey. Page 26 5.9 WATEREROSION

POTENTIALWATER EROSION OF SOILS

The potential water erosion classes are obtained from calculations using the Universal Soil Loss Equation. This equation takes into account soil texture, soil organic matter content, dope length and gradient, soil infiltration rates, soil surface structure and the rainfall erosivity.

The distribution of soil particle sizes (soil texture) influences the soil’s potential for erosion. The silt-size particles are most easily transported by water followed by Clay and sand- sized particles. Thus, soils high in silt are more easily eroded.

Soilorganic matter acts like a“glue”, binding soil particles together so that a greater force is required to break away individual particles that can be transported by water. Soils of higher organic matter contents will, therefore, be less erodible than those with lower contents.

Slope length and gradient are very important to a soil’s potential to erode. These factors control the amount and speed of water movement over the soil surface. Long, steep slopes are much more erodible than short, gentle slopes.

The rate of infdtration of water affects the amount of water that will run over the surface of the soil. Runoff occurs once the rate of water accumulation exceeds the rate of infiltration. Fine-textured soils such as clays have much lower rates of infiltration than coarser-textured soils. The rate of infiltration is also influenced by the origin of the materials. Soils of similar textures but different origins may have different rates of infiltration.

Soil surface structure influences the speed of water movement and, therefore, the erosive force the water exerts on the soil. A rough soil surface causes much slower water movement and therefore there is less erosive force.

Rainfall erosivity refers to the intensity and amount of rainfall an area receives. An area that receives gentle, short showers will experience less erosion than one subjected to prolonged downpours with all other conditions being equal.

Potential water erosion classes assigned to soil map units assume the soil to be under conventional summerfallow. Thus, the class assigned represents the maximum potential for erosion. If dissections or gullies were observed in the field, this was noted by a “D”or a “G” next to the class number since there may be higher potential erosion rates associated with these - features.

When using this information, it should be remembered that the class assigned to an area - is an estimation of potential erosion for the entire area and that actual rates for individual soils within that area may vary significantly from the assigned class.

- Saskatchewan Soil Survey. Page 27 Water Erosion, Cont.

Class Suscept i bili ty Description

1 Very Low Little or no susceptibility to water erosion.

2 LOW Slight susceptibility to water erosion.

3 Moderate Moderate susceptibility to water erosion. Conventional farming practices will result in a steady loss of soil due to water erosion. Conservation practices should be instituted to prevent degradation of these soils.

4 High High susceptibility to water erosion. Rapid loss of soil will occur unless conservation practices are instituted. Al1 gullies in these areas should be grassed.

5 Very Hïgh Very high susceptibility to water erosion. These soils should not be broken due to their water erosion hazard. If broken, perennial crops or permanent forage should replace annual crops.

U Unclassified Unciassified areas (Wetlands).

D or G If an area was observed to be gullied (G) or Modifiers dissected (dissections being shallow gullies that can be crossed with farm implements) (D), these symbols were added to the erosion class symbol to indicate that higher rates of erosion may occur on the steeper slopes dong the edges of the dissection or gully if they are left unprotected.

Saskatchewan Soi1 Survey. Page 28 5.10 PASTWIND AND WATEREROSION

An erosion rating has been assigned to each soil area. This rating reflects the surveyor’s best estimate of the extent and degree of erosion that has occurred in an area since cultivation. Areas that have never been cultivated usually have enough vegetative cover to protect the soil surface from erosion and, therefore, remain relatively unaffected. Some uncultivated areas, however, do have clear evidence of recent erosion.

The rating system contains six classes with the degree of past wind and water erosion ranging from unaffected (WO) to very severe (W5). These classes, with the exception of WO (unaffected), are assigned modifiers (G, K, B) which identify the type of erosion that has occurred. Wetlands, nonsoil areas and some uncultivated area were not classified and are designated with a ‘U’.

Class Description

U Unclassi fied

wo Unaffected. No evidence of past wind or water erosion. w1 Weak. Soils are slightly eroded.

W K The knolls have slightly thinner A horizons and are lighter in color than midslopes. There is no noticeable thickening of the surface horizon on mid- to lower slopes.

W B Wind has removed part of the soil surface resulting in thinner A horizons. There is very little mixing of the A and B horizons and little sign of soil accumulation on mid- and lower slopes.

W1G A few very shallow dissections are present indicating very slight evidence of water erosion.

w2 Moderate. Soils are moderately eroded.

W2K Erodedknolls make up 5- 15% of the area. Theknolls are much lighter in color than midslopes. There is a noticable thickening of the surface horizon on lower slopes due to accumulation of upper slope material.

W2B Wind has removed part of the A horizon resulting in moderately thin A horizons. There is slight mixing of A and B horizons during tillage and some evidence of soil accumulation near fencelines and wind- breaks.

W2G Shallow dissections are present. The dissections may easily be crossed by farm implements and have little effect on cultivation. There is evidence of ri11 erosion (small channels a few centimeters deep, occurring after substantial rains or snowmelt). Saskatchewan Soi1 Survey. Page 29 Past Wind and Water Erosion, Cont.

~~ Class Description

w3 Strong. Soils are strongly eroded.

W3K Eroded knolls make up 1540% of the area. The knolls are much lighter in color than midslopes. A large portion of the A horizon has been removed and redistributed to lower slopes. On knolls, subsoil has been incorporated into the cultivated horizon.

W3B Wind has removed a significant amount of the A horizon. Regular tillage results in a thorough mixing of the B horizon with the remaining A horizon. Accumulation of wind-blown material occurs dong fencelines and windbreaks.

W3G Distinct dissections are present. The dissections may be crossed by farm hnplements with some difficulty, and have a moderate effect on cultivation. These dissections should be seeded to grass to prevent further damage from erosion. w4 Severe. Soils are severely eroded.

W4K Eroded knolls make up 40-70% of the area. The eroded knolls are white in color, with light colors extending well ont0 the midslope position. Erosion has destroyed the soil profile on upper slopes.

W4B Wind has removed most of the A horizon and frequently part of the B horizon. Occasional blowout areas are present, creating a very ' unstable surface.

W4G Occasional shallow gullies are present. The gullies cannot be crossed by farm implements, and therefore, cannot be cultivated for annual cropping. Reclamation for improved Pasture is difficult unless erosion can be controlled.

~ w5 Very Severe. Soils are very severely eroded.

W5K Eroded knolls make up greater than 70% of the area. The knolls and midslopes are white in color. Erosion has destroyed the soil profile on upper and midslope positions.

W5B Wind has removed most of the soil profile. Blowout holes are numerous and easily carved into the subsoil or parent material. Areas between blowouts are deeply buried by eroded soil material. At best, this land should be utilized for native or improved Pasture.

W5G Deep gullies occur frequently. Soil profiles have been destroyed except in small areas between gullies. The gullies are deep enough to prevent cultivation. These areas should be permanently grassed.

Saskatchewan Soil Survey. Page 30 6. AREAFACTS

RURAL MUNICIPALITY OF WILLOW CREEK

NUMBER 458

Hectares Acres TOTAL,AREA ...... 85243 210639 SOIL CAF'ABEI" FOR AGRICULTURE Class 1 ...... 21648 53494 Class 2 ...... 16208 4005 1 Class 3 ...... 19647 48550 Class 4 ...... 963 1 23800 Class 5 ...... 13017 32167 Class 6 ...... 3666 9060 Class 7 ...... 380 940 Class O ...... 1033 2552 IRRIGATION SUITABILITY Excellent ...... O O Good ...... 16855 4 1650 Fair...... 33016 8 1584 Poor ...... 35363 87384 SALINITY Very Strong ...... O O Strong ...... 45 111 Moderate ...... 602 1488 Weak ...... 5 63 1392 None ...... 84032 207646 SAND AND GRAVEL Sandy ...... 13369 33037 Sandy and Gravelly ...... O O Grave11y ...... 96 238 STONES Non .Slightly Stony ...... 85235 210619 Moderately Stony ...... O O Very Stony ...... O O Excessive ...... O O SURFACE pH (Soil Acidity) x ( < 5.5) ...... O O A (5.5 - 6.0) ...... 9407 23246 B (6.1 - 6.7) ...... 37 186 91889 C (6.8 - 7.5) ...... 33070 81718 D ( > 7.5) ...... 5570 13763

Saskatchewan Soil Survey. Page 31 Area Facts, Cont.

RURAL MUNICIPALITY OF WILLOW CREEK

NUMBER 458

Hectares Acres TEXTURES Sands ...... 14055 3473 1 Sandy Loams ...... 23202 57333 Loams ...... 26414 65272 Clay Loams ...... 19621 48484 Clays ...... 1554 3842 WIND EROSION POTENTIAL Very Low ...... 42293 104507 Low ...... 26039 64343 Moderate ...... i ...... 10453 25830 High ...... 4784 11822 Very High ...... 652 1611 Exîremely High ...... O O WATER EROSION POTENTIAL Very Low ...... 27433 67787 Low ...... 49558 122533 Moderate ...... 4524 11180 High ...... 1261 3116 Very High ...... O O WETLANDS AND POORLY DRAINED SOLS Open water and lakes ...... 472 1168 Wet, poorly drained soils ...... 2795 6908

Saskatchewan Soi1 Survey. Page 32 7. SOIL MAP UNIT DESCRIPTIONS LEGEND

MAP SYMBOL SOILS

Ar borfiel d Gray Solonetzic soils formed in clayey lacustrine materials; Clay loam to Clay surface textures. Ar4 Mainly weak solonetzic Arborfield soils, with strong solonetzic Arborfield soils on lower slopes, and poorly drained soils in depressions.

Alluvium Weakly developed and poorly drained soils formed in recent deposits of streams and rivers; variable surface textures. Av5 Mainly poorly drained Alluvium soils occumng over most of the landscape. Blaine Lake Black soils formed in silty lacustrine materials; silt loam to silty clayloam surface textures. B b4 Mainly orthic Blaine Lake soils, with calcareous Blaine Lake soils on upper slopes and knolls. Bb5 Mainly orthic Blaine Lake soils, with poorly drained soils in depressions. Bb12 Mainly gleyed orthic Blaine Lake soils, with orthic Blaine Lake soils on upper slopes. Blaine Lake Black soils formed in shallow, silty lacustrine materials underlain by (Clay substrate) clayey lacustrine materials; silty Clay loam surface textures. BblOC Mainly a mixture of gleyed orthic and gleyed leached Blaine Lake soils, with poorly drained soils in depressions. Blaine Lake Black soils formed in shallow, silty lacustrine materials underlain by (grave1 gravelly fluvial materials; silt loam surface textures. substrate) Bb3G Mainly orthic Blaine Lake soils, with leached Blaine Lake soils on lower slopes and in depressions. Blaine Lake- A mixture of Black (Blaine Lake) and Thick Black (Hoey) soils Hoey formed in silty lacustrine materials; silt loam to loam surface textures. BbHhl Mainly orthic Blaine Lake soils, with orthic Hoey soils on lower slopes and in depressions.

Saskatchewan Soi1 Survey. Page 33 Soil Map Unit Descriptions, Cont.

BbHh5 Mainly orthic Blaine Lake soils, with a mixture of leached Blaine Lake and Hoey soils on mid- to lower slopes, orthic Hoey soils on some lower slopes, and poorly drained soils in depressions. Blaine Lake- A mixture of Black (Blaine Lake) and Dark Gray (Kamsack) soils Kamsack formed in silty lacustrine materials; loam to silty Clay loam surface tex- tures. BbKal Mainly orthic Blaine Lake soils, with orthic Kamsack soils on lower slopes. Blaine Lake- A mixture of Black soils formed in silty lacustrine materials (Blaine Melfort Lake) and Black and Thick Black soils formed in clayey lacustrine ma- terials (Melfort); loam to siIt loam (Bb) and silty Clay loam to silty Clay (Mr) surface textures. BbMr2 Mainly orthic Blaine Lake soils, with a mixture of orthic and thick orthic Melfort soils on lower slopes, and poorly drained soils in depressions. BbMr3 Mainly orthic Blaine Lake soils, with orthic Melfort soils on mid- to lower slopes, and leached Melfort soils in depressions. Breden bury Thick Black soils formed in loamy lacustrine rnaterials; loam to fine and very fine sandy loam surface textures. Bu3 Mainly orthic Bredenbury soils, with leached Bredenbury soils on lower slopes and in depressions. Bredenbury- A mixture of Thick Black soils formed in loamy lacustrine materials Blaine Lake (Bredenbury) and Black soils formed in silty lacustrine materials (Blaine Lake); loam (Bu, Bb) to silt loam (Bb) surface textures. BuBb2 Mainly orthic Bredenbury soils, with gleyed orîhic Bredenbury soils on lower slopes, orthic Blaine Lake soils on upper slopes and knolls, and poorly drained soils in depressions. Bredenbury- A mixture of Thick Black (Bredenbury) andBlack (Hamlin) soils Hamlin forrned in loamy lacustrine materials; loam to fine sandy loarn surface textures. BuHm2 Mainly calcareous Bredenbury soils on mid- and lower slopes, with carbon- ated Bredenbury soils on some lower slopes, orthic Hamlin soils on upper slopes and knolls, and poorly drained soils in depressions. Cut Knife' Black soils formed in shallow, silty lacustrine materials underlain by glacial till; silty Clay loam surface textures. Cfl Mainly orthic Cut Knife soils occurring over most of the landscape.

1. Formerly Blaine Lake (tiil substrate)

Saskatchewan Soil Survey. Page 34 Soil Map Unit Descriptions, Cont.

Carrot River Gleyed Dark Gray soils formed in sandy fluvial materials; sandy loam to fine sandy loam surface textures. Cr6 Mainly gleyed orthic Carrot River soils, with carbonated Carrot River soils on mid- to lower slopes, and peaty poorly drained soils in depressions. Cr8 Mainly carbonated Carrot River soils, with gleyed orthic Canot River soils on some upper slopes and knolls, and peaty poorly drained soils in depres- sions. Carrot River- A mixture of Gleyed Dark Gray (Carrot River) and weakly developed Pine Gray (Pine) soils formed in sandy fluvial materials; fine sandy loam (Cr) to loamy sand (Cr, Pn) and sand (Pn) surface textures. CrPn2 Mainly gleyed orthic Carrot River soils, with carbonated Carrot River soils on lower slopes, weakly developed Pine soils on some upper slopes and knolls, and poorly drained soils in depressions. Carrot River- A mixture of Gleyed Dark Gray (Carrot River) and Gray (Sylvania) Sylvania soils formed in sandy fluvial materials; loamy Sand to fine sandy loam surface textures. CrSyl Mainly carbonated Carrot River soils, with gleyed dark gray wooded Sylva- nia soils on upper slopes and knolls, and poorly drained soils in depressions. CrSy2 Mainly gleyed orthic Canot River soils, with dark gray wooded Sylvania soils on upper slopes and knolls, and poorly drained soils in depressions. Eldersley Gray soils formed in clayey lacustrine materials; Clay loam to Clay surface textures, Ed3 Mainly dark gray wooded Eldersley soils occurring over most of the land- scape. Eldersley- A mixture of Gray (Eldersley) and Dark Gray (Tisdale) soils formed in Tisdale clayey lacustrine materials; Clay loam, Clay and silty Clay surface tex- tures. EdTil Mainly dark gray wooded Eldersley soils, with orthic Tisdale soils on lower slopes and îhrough depressions. EdTi2 Mainly gleyed dark gray wooded Eldersley soils, with a mixture of orthic and gleyed orthic Tisdale soils on lower slopes, and poorly drained soils in depressions. EdTi4 Mainly a mixture of dark gray wooded and gleyed dark gray wooded Eldersley soils, with gleyed orthic Tisdale soils on lower slopes and through depressions. Gronlid Gleyed Dark Gray soils formed in loarny lacustrine materials; fine sandy loam to very fine sandy loam surface textures. Go2 Mainly carbonated Gronlid soils, with poorly drained soils in depressions. Saskatchewan Soil Survey. Page 35 Soil Map Unit Descriptions, Cont.

Mainly gleyed orthic Gronlid soils, with poorly drained soils in depressions. Go6 Mainly gleyed orthic Gronlid soils, with carbonated Gronlid soils on lower slopes, and poorly drained soils in depressions. Go8 Mainly carbonated Gronlid soils, with gleyed orthic Gronlid soils on upper slopes and knolls, and poorly drained soils in depressions. Gronlid- A mixture of Gleyed Dark Gray (Gronlid) and Gray (La Corne) soils La Corne formed in loamy lacustrine materials; fine sandy loam and very fine sandy loam to loam surface textures. GoLc2 Mainly gleyed orthic Gronlid soils, with dark gray wooded La Corne soils on upper slopes and knolis, and poorly drained soils in depressions. GoLclO Mainly carbonated Gronlid soils, with dark gray wooded La Corne soils on upper slopes and knolis, and poorly drained soils in depressions. Gronlid- A mixture of Gleyed Dark Gray (Gronlid) and Dark Gray (Shellbrook) Shellbrook soils formed in loamy lacustrine materials; sandy loam (Go) to fine sandy loam (Go, Sb) and very fine sandy loam (Sb) surface textures. GoSblO Mainly carbonated Gronlid soils, with gleyed orthic Gronlid soils on midslopes, orthic Shellbrook soils on upper slopes and knolls, and poorly drained soils in depressions. Hoey Thick Black soils formed in silty lacustrine materials; laam to silt loam surface textures. Hhl Mainly orthic Hoey soils occurring over most of the landscape. Hh6 Mainly orthic Hoey soils, with leached poorly drained soils in depressions. HWY Thick Black soils formed in shallow, silty lacustrine materiah underlain (Clay substrate) by clayey lacustrine materials; silty Clay loam to loam surface textures. HhlC Mainly orthic Hoey soils occurring over most of the landscape. Hoey- A mixture of Thick Black (Hoey) and Black (Blaine Lake) soils formed Blaine Lake in silty lacustrine materials; loam, silt loam, Clay loam and silty Clay loam surface textures. HhBbl Mainly orthic Hoey soils, with orthic Blaine Lake soils on upper slopes and knolls. HhBb2 Mainly orthic Hoey soils, with a mixture of orthic and leached Blaine Lake soils on upper slopes, and poorly drained soils in depressions. HhBb6 Mainly orthic Hoey soils, with orthic Blaine Lake soils on upper slopes and knolls, and leached poorly drained soils in depressions.

Saskatchewan Soil Survey. Page 36 Soil Map Unit Descriptions, Cont.

HhBb7 Mainly orthic Hoey soils, with a mixture of calcareous Blaine Lake and Hoey soils on upper slopes and knolls, orthic Blaine Lake soirs on some mid- to upper slopes, and poorly drained soils in depressions. HhBb8 Mainly a mixture of orthic Hoey soils on midslopes and gleyed orthic Hoey soils on lower slopes, with a mixture of orthic Blaine Lake soils on upper slopes and gleyed orthic Blaine Lake soils on some midslopes, and poorly drained soils in depressions. Hoey-Kamsack A mixture of Thick Black (Hoey) and Dark Gray (Kamsack) soils formed in silty lacustrine materials; silt loam to silty Clay loam surface textures. HhKal Mainly orthic Hoey soils, with orthic Kamsack soils on lower slopes and through depressions. Hoey-Melfort A mixture of Thick Black soils formed in silty lacustrine materials (Hoey) and Black and Thick Black soils formed in clayey lacustrine materials (Melfort); silt loam (Hh) to silty Clay loam (Hh, Mr) surface textures. HhMr3 Mainly orthic Hoey soils, with a mixture of leached Hoey soils on some upper slopes and 1eachedMelfortsoils in depressions, and a mixture of orthic and thick orthic Melfort soils on lower slopes. HhMrS Mainly orthic Hoey soils, with a mixture of orthic and thick orthic Melfort soils on lower slopes, and poorly drained soils in depressions. HhMr6 Mainly orthic Hoey soils, with leached Hoey soils on some mid- to upper slopes, leached Melfort soils on lower slopes, and poorly drained soils in depressions. Hillwash Weakly developed soils formed in various deposits associated with steep and eroding Valley sides; variable surface textures. Hw Mainly shallow, eroded and weakly developed Hillwash soils on steep, gullied valiey side slopes. Hillwash- A mixture of weakly developed soils formed in various deposits Alluvium associated with steep and eroding Valley sides (Hillwash) and variable- textured alluvial materials occurring on stream flood plains (Allu- vium); variable surface textures. HwAvl Mainly shallow, eroded and weakly developed Hillwash soils on steep, gullied Valley side slopes, and poorly drained Alluvium soils on stream flood plains. Kamsack Dark Gray soils formed in silty lacustrine materials; loam to silt loam surface textures. Ka1 Mainly orthic Kamsack soils occurring over most of the landscape. Ka3 Mainly orthic Kamsack soils, with calcareous Kamsack soils on upper slopes and knolls. Saskatchewan Soil Survey. Page 37 Soil Map Unit Descriptions, Cont.

Ka5 Mainly a mixture of orthic Kamsack soils on mid- to upper slopes and knolls and gleyed orthic Kamsack soils on mid- to lower slopes, with poorly drained soils in depressions. Ka6 Mainly a mixture of orthic Kamsack soils on mid- to upper slopes and knolls and gleyed orthic Kamsack soils on mid- to lower slopes and in depressions. Ka7 Mainly orthic Kamsack soils, with carbonated Kamsack soils on lower slopes, and poorly drained soils in depressions. Ka8 Mainly orthic Kamsack soils, with poorly drained soils in depressions. - Kail Mainly a mixture of calcareous Kamsack soils on upper slopes and knolls and carbonated Kamsack soils on mid- and lower slopes, with poorly drainedsoils in depressions. Ka12 Mainly carbonated Kamsack soils, with poorly drained soils in depressions. Ka13 Mainly gleyed orthic Kamsack soils, with carbonated Kamsack soils on - lower slopes, and poorly drained soils in depressions. Kamsack- A mixture of Dark Gray (Kamsack) and Black (Blaine Lake) soils - Blaine Lake formed in silty lacustrine materials; silt loam to silty Clay loam surface textures. - KaBb2 Mainly orthic Kamsack soils, with orthic Blaine Lake soils on upper slopes, and poorly drained soils in depressions. KaBbS Mainly a mixture of orthic and gleyed orthic Kamsack soils, with a mixture - of orthic and gleyed orthic Blaine Lake soils on lower slopes, and poorly drained soils in depressions. - KaBb6 Mainly orthic Kamsack soils, with orthic Blaine Lake soils on upper slopes, and leached poorly drained soils in depressions. Kamsack- A mixture of Dark Gray (Kamsack) and Gray (Porcupine Plain) soils Porcupine Plain formed in silty lacustrine materials; silt loam to silty Clay loam surface textures. KaPpl Mainly orthic Kamsack soils, with dark gray wooded Porcupine Plain soils on upper slopes and knolls. KaPp2 Mainly gleyed orthic Kamsack soils, with gleyed dark gray wooded Porcu- pine Plain soils on upper slopes and knolls, and poorly drained soils in depressions. KaPp4 Mainly gleyed orthic Kamsack soils, with dark gray wooded Porcupine Plain soils on upper slopes and knolls.

Saskatchewan Soil Survey. Page 38 Soil Map Unit Descriptions, Cont.

Kamsack- Dark Gray soils formed in a mixture of silty (Kamsack) and loamy Shellbrook (Shellbrook) lacustrine materials; silt loam (Ka) to loam (Ka, Sb) and very fine sandy loam (Sb) surface textures. KaSbl Mainly orthic Kamsack soils, with orthic Shellbrook soils on upper slopes and knolls. KaSb2 Mainly orthic Kamsack soils, with carbonated Kamsack soils on lower slopes, orthic Shellbrook soils on upper slopes and knolis, and poorly drained soils in depressions. KaSbS Mainly orthic Kamsack soils, with orthic Shellbrook soils on upper slopes and knolls, and poorly drained soils in depressions. Kamsack- Dark Gray soils formed in a mixture of silty (Kamsack) and clayey Tisdale (Tisdale) lacustrine materials; silt loam (Ka) to silty Clay loam (Ti) surface textures. KaTil Mainly a mixture of orthic and gleyed orthic Kamsack soils, with a mixture of orthic and gleyed orthic Tisdale soils on mid- to lower slopes and through depressions.

KaTi2 Mainly a mixture of orthic and calcareous Kamsack soils on mid- to upper slopes and knolls, with orthic Tisdale soils on mid- to lower slopes, and poorly drained soils in depressions. KaTi4 Mainly a mixture of gleyed orthic and carbonated Kamsack soils, with a mixture of gleyed orthic Tisdale soils on midslopes and carbonated Tisdale soils on lower slopes and through depressions. La Corne Gray soils formed in loamy lacustrine materials; very fine sandy loam to loam surface textures.

Lc8 Mainly dark gray wooded La Corne soils, with gleyed dark gray wooded La Corne soils on lower slopes, and poorly drained soils in depressions. - La Corne- A mixture of Gray (La Corne) and Dark Gray (Shellbrook) soils formed Shellbrook in loamy lacustrine materials; sandy loam to loam and sandy Clay loam surface textures. - LcSb2 Mainly dark gray wooded La Corne soils, with orthic Shellbrook soils on mid- to lower slopes, and poorly drained soils in depressions. LcSb3 Mainly dark gray wooded La Corne soils, with orthic Shellbrook soils on mid- to lower slopes, carbonated Gronlid soils on some lower slopes, and poorly drained soils in depressions. LcSb4 Mainly a mixture of dark gray wooded La Corne soils on midslopes and gray wooded La Corne soils on upper slopes and knolls, with orthic Shellbrook soils on lower slopes and through depressions.

Saskatchewan Soil Survey. Page 39 Soil Map Unit Descriptions, Cont.

Moss Peat Organic soils formed in a mixture of materials derived mainly from mosses and forest vegetation. MPlM Mainly mesic Moss Peat soils less than 1 m (3 to 4 ft.) thick occurring over most of the landscape. Moss Peat- Organic soils formed in a mixture of materials derived from mosses and Sedge Peat forest vegetation (Moss Peat) and sedges, meadow grasses and shrubs (Sedge Peat). MPSEM Mainly mesic Moss Peat soils 1to 2 m (3 to 6 ft.) thick on upper slopes, with mesic Sedge Peat soils 1 to 2 m (3 to 6 ft.) thick on extensive lowlands and through depressions. Melfort Black and Thick Black soils formed in clayey lacustrine materials; Clay loam to Clay surface textures. Mrl Mainly orthic Melfort soils occurring over most of the landscape. Mr2 Mainly orthic Melfort soils, with thick orthic Melfort soils on lower slopes, and poorly drained soils in depressions. Mr3 Mainly orthic Melfort soils, with thick orthic Melfort soils on lower slopes, and a mixture of saline and gleyed Melfort soils on some lower slopes and in depressions. Mr5 Mainly orthic Melfort soils, with poorly drained soils in depressions. Mr6 Mainly thick orthic Melfort soils, with orthic Melfort soils on upper slopes. Mr8 Mainly orthic Melfort soils, with thick orthic Melfort soils on mid- to lower slopes, and gleyed orthic Melfort soils on some lower slopes and in depres- sions. Mr9 Mainly orthic Melfort soils, with thick orthic Melfort soils on mid- to lower slopes, and leached Melfort soils on lower slopes and in depressions. Mrll Mainly a mixture of orthic and gleyed orthic Melfort soils, with poorly drained soils in depressions. Mr13 Mainly orthic Melfort soils, with amixture of solonetzic, saline andfer gleyed Melfort soils on lower slopes and through depressions. Mr15 Mainly a mixture of saline and carbonated Melfort soils, with poorly drained soils in depressions.

Saskatchewan Soil Survey. Page 40 Soil Map Unit Descriptions, Cont.

Melfort- A mixture of Black and Thick Black soils formed in clayey lacustrine Blaine Lake materials (Melfort) and Black soils formed in silty lacustrine materials (Blaine Lake); Clay loam to silty Clay loam (Mr, Bb) and loam to silt loam (Bb) surface textures. MrBbl Mainly a mixture of orthic Melforî soils on midslopes and gleyed orthic Melfort soils on lower slopes, with a mixture of orthic and gleyed orthic Blaine Lake soils on upper slopes and knolls. MrBb3 Mainly leached Melfort soils, with orthic Melfort soils on some lower slopes, and a mixture of orthic and leached Blaine Lake soils on upper slopes and knolls. MrB b4 Mainly a mixture of orthic Melfort soils on mid- to lower slopes and leached Melfort soils in depressions, with a mixture of orthic and leached Blaine Lake soils on upper slopes. MrB b5 Mainly a mixture of orthic and thick orthic Melfort soils, with orthic Blaine Lake soils on upper slopes and knolls, and poorly drained soils in depres- sions. MrBb7 Mainly a mixture of orthic and thick orthic Melfort soils, with a mixture of gleyed orthic and leached Melfort soils on lower slopes, and orthic Blaine Lake soils on upper slopes. Melfort -Hoey A mixture of Black and Thick Black soils formed in clayey lacustrine materials (Melfort) and Thick Black soils formed in silty lacustrine materials (Hoey); Clay loam (Mr) to silt loam and loam (Hh) surface textures. MrHhl Mainly orthic Melfort soils, with gleyed orthic Melfort soils on lower slopes and through depressions, and orthic Hoey soils on upper slopes and knolls. MrHh2 Mainly a mixture of orthic and thick orthic Melfort soils, with leached Melfort soils on lower slopes, orthic Hoey soils on upper slopes and knolls, and poorly drained soils in depressions. Melfort-Tisdale A mixture of Black and Thick Black (Melfort) and Dark Gray (Tisdale) soils formed in clayey lacustrine materials; Clay loam, silty Clay loam, Clay and silty Clay surface textures. MrTil Mainly a mixture of orthic and gleyed orthic Melfort soils, with a mixture of orthic and gleyed orthic Tisdale soils on mid- to lower slopes and in depres- sions. MrTiS Mainly gleyed orthic Melfort soils, with gleyed orthic Tisdale soils on upper slopes, and poorly drained soils in depressions.

Saskatchewan Soil Survey. Page 41 Soi1 Map Unit Descriptions, Cont.

Melfort-Tisdale A mixture of Black and Thick Black (Melfort) and Dark Gray (Tisdale) (till substrate) soils formed in shallow, clayey lacustrine materials underlain by glacial till; silty Clay loam, silty Clay and Clay surface textures. MrTiST Mainly gleyed orthic Melfort soils, with gleyed orthic Tisdale soils on upper slopes, and poorly drained soils in depressions. Meadow Poorly Drained soils formed in variable-textured alluvial materials; variable surface textures. Mwl Mainly poorly drained Meadow soils occurring over most of the landscape. Mw3 Mainly a mixture of poorly drained and saline poorly drained Meadow soils occurring over most of the landscape. Mw4 Mainly peaty, saline poorly drainedMeadow soils occurring over most of the landscape. Mw5 Mainly poorly drained Meadow soils, with a mixture of weakly developed poorly drained Meadow soils in higher landscape positions and peaty poorly drained Meadow soils in lower landscape positions.

Mw6 Mainly a mixture of poorly drained Meadow soils in mid- and upper slope positions and peaty poorly drained Meadow soils in lower landscape posi- tions. Northern Light- A mixture of Gray (Northern Light) and Dark Gray (Tiger Hills) soils Tiger Hillsl formed in shallow, silty lacustrine materials underlain by glacial till; loam to silt loam surface textures. NrTgl Mainly a mixture of gray wooded Northern Light soils on upper slopes and knolls and dark gray wooded Northern Light soils on midslopes, with orthic Tiger Hills soils on lower slopes and through depressions. Nisbet Dark Gray soils formed in sandy fluvial materials; loamy sand to sandy loam surface textures. Nt 1 Mainly orthic Nisbet soils occurring over most of the landscape. Nt7 Mainly orthic Nisbet soils, with eroded Nisbet soils on knolls. Nisbet- A mixture of Dark Gray (Nisbet) and Gleyed Dark Gray (Carrot River) Carrot River soils formed in sandy fluvial materials; loamy sand (Nt) to sandy loam and very fine sandy loam (Nt, Cr) surface textures. NtCrl Mainly orthic Nisbet soils, with gleyed orthic Carrot River soils on mid- to lower slopes and through depressions.

1. Formerly Porcupine Plain-Kamsack (till substrate)

Saskatchewan Soi1 Survey. Page 42 Soil Map Unit Descriptions, Cont.

Nisbet- A mixture of Dark Gray soils formed in sandy fluvial materials (Nisbet) Gronlid and Gleyed Dark Gray soils formed in loamy lacustrine materials (Gronlid); loamy Sand (Nt) to sandy loam (Go) surface textures. NtGo4 Mainly orthic Nisbet soils, with carbonated Gronlid soils on lower slopes and through depressions. Nisbet -Pine A mixture of Dark Gray soils (Nisbet) and weakly developed Gray soils, some of which have been dnd worked (Pine), formed in sandy fluvial materials; sandy loam (Nt) to sand (Pn)surface textures. NtPnl Mainly orthic Nisbet soils, with weakly developed Pine soils on upper slopes and knolls. Nisbet- Dark Gray soils formed in a mixture of sandy fluvial materials (Nisbet) Shellbrook and loamy lacustrine materials (Shellbrook); sandy loam to loamy Sand (Nt) and fine sandy loam to very fine sandy loam (Sb) surface textures. NtSbl Mainly orthic Nisbet soils, with orthic Shellbrook soils on lower slopes and through depressions. NtSbS Mainly orthic Nisbet soils, with orthic Shellbrook soils on lower slopes,and poorly drained soils in depressions. Nisbet- A mixture of Dark Gray (Nisbet) and Gray (Sylvania) soils formed in Sylvania sandy fluvial materials; sandy loam to loamy sand surface textures. NtSy2 Mainly orthic Nisbet soils, with dark gray wooded Sylvania soils on upper slopes and knolls, and poorly drained soils in depressions. Pathlow A mixture of Gray and Dark Gray soils formed in a mixture of glacial till, eroded glacial till and shallow, silty lacustrine materials underlain by eroded glacial till; loam to silt loam surface textures. Pa2 Mainly a mixture of gray wooded and dark gray wooded Pathlow soils on mid- and upper slopes, with orthic Pathlow soils on lower slopes. Pine Weakly developed Gray soils formed in sandy fluvial materials, some of which have been dndworked; sand to loamy Sand surface textures. Pnl Mainly leached Pine soils occurring over most of the landscape. Pn2 Mainly a mixture of weakly developed Pine soils on mid- to upper slopes and knolls and leached Pine soils on lower slopes and in depressions. Pn3 Mainly weakiy developed Pine soils occumng over most of the landscape.

Saskatchewan Soil Survey. Page 43 Soil Map Unit Descriptions, Cont.

Pine- A mixture of weakly developed Gray (Pine) and Gleyed Dark Gray Carrot River (Carrot River) soils formed in sandy fluvial materials, some of which have been wind worked (Pine); Sand to loamy Sand (Pn) and sandy loam to very fine sandy loam (Cr) surface textures. PnCr2 Mainly weakiy developed Pine soils, with gleyed orthic Carrot River soils on mid- to lower slopes and through depressions. PnCr3 Mainly weakly developed Pine soils, with a mixture.of gleyed orthic and carbonated Carrot River soils on mid- to lower slopes, and poorly drained soils in depressions. PnCr4 Mainly amixture of weakly developedpine soils on knolls, leachedPine soils on Ad- to upper slopes and gleyed 1eachedPinesoils on mid- to lower slopes, with a mixture of gleyed orthic and carbonated Canot River soils on some lower slopes, and poorly drained soils in depressions. Pine-Nisbet A mixtureof weakly developed Gray (Pine) and Dark Gray (Nisbet) soils formed in sandy fluvial materials, some of which have been wind worked (Pine); Sand (Pn) to loamy Sand (Pn, Nt) and sandy loam to very fine sandy loam (Nt) surface textures. PnNt 1 Mainly weakly developed Pine soils on upper slopes and knolls, with orthic Nisbet soils on lower slopes and through depressions. Porcupine Plain Gray soils formed in silty lacustrine materials; loam to silt loam surface textures.

PPl Mainly dark gray wooded Porcupine Plain soils occurring over most of the landscape. Porcupine Plain- Gray soils formed in a mixture of silty (Porcupine Plain) and clayey Eldersley (Eldersley) lacustrine materials; silt loam (Pp) to Clay (Ed) surface textures. PpEd2 Mainly a mixture of dark gray wooded and gleyed dark gray wooded Porcupine Plain soils on upper slopes and knolls, with a mixture of dark gray wooded and gleyed dark gray wooded Eldersley soils on mid- to lower slopes, and poorly drained soils in depressions. Porcupine Plain- A mixture of Gray (Porcupine Plain) and Dark Gray (Kamsack) soils Kamsack formedin silty lacustrine materials; loam, silt loam and Clay loam surface textures. PpKa2 Mainly dark gray wooded Porcupine Plain soils, with calcareous Kamsack soils on upper slopes and knolls, and poorly drained soils in depressions. Porcupine Plain- Gray soils formed in a mixture of silty (Porcupine Plain) and loamy La Corne (La Corne) lacustrine materials; silt loam (Pp) to fine sandy loam (Lc) surface textures. PpLc3 Mainly gleyed dark gray wooded Porcupine Plain soils, with dark gray wooded La Corne soils on upper slopes and knolls. Saskatchewan Soil Survey. Page 44 ~ ~~

- Soil Map Unit Descriptions, Cont.

- Runway Weakly developed and poorly drained soils formed in various deposits associated with shallow drainage channels and gullies; variable surface textures. Rw Mainly a mixture of poorly drained Runway soils on Channel bottoms and eroded or weakly developed Runway soils on Channel side slopes. Sedge Peat Organic soils formed in a mixture of materials derived from sedges, meadow grasses and shrubs. SPlM Mainly mesic Sedge Peat soils less than 1 m (3 to 4 ft.) thick occurring over most of the landscape. SP2M Mainly mesic Sedge Peat soils 1 to 2 m (3 to 6 ft.) thick occurring over most of the landscape. Sedge Peat- A mixture of Organic soils formed in a mixture of materials derived Arbow from sedges, meadow grasses and shrubs (Sedge Peat) and Poorly Drained soils formed in variable-textured alluvial materials (Arbow); variable (Aw) surface textures. SPAwl Mainly mesic Sedge Peat soils 1 to 2 m (3 to 6 ft.) thick adjacent to Stream channels, with peaty poorly drained Arbow soils on mid- and upper slopes. Shellbrook Dark Gray soils formed in loamy lacustrine materials; sandy loam to very fine sandy loam surface textures. Sbl Mainly orthic Shellbrook soils occurring over most of the landscape. Sb2 Mainly orthic Shellbrook soils, with poorly drained soils in depressions. Sb5 Mainly orthic Shellbrook soils, with calcareous Shellbrook soils on upper slopes and knolls. Shell brook- A mixture of Dark Gray (Shellbrook) and Gleyed Dark Gray (Gronlid) Gronlid soils formed in loamy lacustrine materials; sandy loam to very fine sandy loam surface textures. SbGo2 Mainly orthic Shellbrook soils, with carbonated Gronlid soils on lower slopes, and poorly drained soils in depressions. SbGo4 Mainly orthic Shellbrook soils, with carbonated Gronlid soils on lower slopes and through depressions. Shell brook- Dark Gray soils formed in a mixture of loamy (Shellbrook) and silty Kamsack (Kamsack) lacustrine materials; fine sandy loam to sandy loam (Sb) and loam to silt loam (Ka) surface textures. SbKal Mainly orthic Shellbrook soils, with orthic Kamsack soils on lower slopes and through depressions.

Saskatchewan Soil Survey. Page 45 Soil Map Unit Descriptions, Cont.

SbKa2 Mainly orthic Shellbrook soils, with calcareous Shellbrook soils on knolls, carbonated Kamsack soils on lower slopes, and poorly drained soils in depressions. SbKa3 Mainly orthic Shellbrook soils, with carbonated Kamsack soils on some lower slopes, carbonated Gronlid soils on mid- to lower slopes, and poorly drained soils in depressions. Shellbrook- A mixture of Dark Gray (Shellbrook) and Gray (La Corne) soils La Corne formed in loamy lacustrine materials; sandy loam, fine sandy loam, very fine sandy loam and loam surface textures. SbLcl Mainly orthic Shellbrook soils, with dark gray wooded La Corne soils on upper slopes and knolls. SbLc2 Mainly orthic Shellbrook soils, with dark gray wooded La Corne soils on upper slopes and knolls, carbonated Gronlid soils on some lower slopes, and poorly drained soils in depressions. Sylvania Gray soils formed in sandy fluvial materials; loamy Sand and sandy loam surface textures.

SY2 Mainly a mixture of dark gray wooded Sylvania soils on mid- and lower slopes and in depressions and gray wooded Sylvania soils on upper slopes and knolls.

SY3 Mainly dark gray wooded Sylvania soils occurring over most of the land- scape.

SY7 Mainly dark gray wooded Sylvania soils, with poorly drained soils in depressions.

SY8 Mainly a mixture of gleyed dark gray wooded and gleyed gray wooded Sylvania soils, with poorly drained soils in depressions. Sylvania- A mixture of Gray soils formed in sandy fluvial materials (Sylvania) Gronlid and Gleyed Dark Gray soils formed in loamy lacustrine materials (Gronlid); loamy Sand (Sy) to sandy loam (Go) surface textures. SyGo4 Mainly dark gray wooded Sylvania soils, with carbonated Gronlid soils on lower slopes and through depressions. Sylvania-Nisbet A mixture of Gray (Sylvania) and Dark Gray (Nisbet) soils formed in sandy fluvial materials; fine sandy loam to loamy Sand surface textures. SyNt 1 Mainly a mixture of dark gray wooded Sylvania soils on midslopes and gray wooded Sylvania soils on upper slopes and knolls, with orthic Nisbet soils on lower slopes and through depressions.

Saskatchewan Soil Survey. Page 46 Soil Map Unit Descriptions, Cont.

- Sylvania-Pine A mixture of Gray (Sylvania) and weakly developed Gray (Pine) soils formedin sandy fluvial materials, some of which have been wind worked

- (Pine); loamy sand (Pn, Sy) to very fine sandy loam (Sy) surface textures. Sypnl Mainly dark gray wooded Sylvania soils, wiîh weakiy developed Pine soils on upper slopes and knolls. - Tiger Hillsl Dark Gray soils formed in shallow, silty lacustrine materials underlain by glacial till; loam to silt loam and silty Clay loam surface textures. Mainly a mixture of orthic Tiger Hills soils on mid- to upper slopes and knolls and gleyed orthic Tiger Hills soils on mid- to lower slopes, with poorly drained soils in depressions. Mainly a mixture of orthic Tiger Hills soils on mid- to upper slopes and knolls and gleyed orthic Tiger Hills soils on mid- to lower slopes and in depressions. Tiger Hills- A mixture of Dark Gray (Tiger Hills) and Gray (Northern Light) - Northern Light2 soils formed in shallow, silty lacustrine materials underlain by glacial till; loam to silt loam surface textures. TgNrl Mainly orthic Tiger Hills soils, with dark gray wooded Northern Light soils on upper siopes and knolls. TgNrS Mainly orthic Tiger Hills soils, with dark gray wooded Northern Light soils on upper slopes, and poorly drained soils in depressions. Tisdale Dark Gray soils formed in clayey lacustrine materials; Clay loam to Clay surface textures. Ti4 Mainly a mixture of calcareous and weakly developed Tisdale soils, with orthic Tisdale soils on lower slopes and through depressions. Till Mainly a mixture of orthic Tisdale soils on upper slopes and knolls and gleyed orthic Tisdaie soils on lower slopes, with poorly drained soils in depressions. Tisdale- A mixture of Dark Gray (Tisdale) and Gray (Eldersley) soils formed in Eldersley clayey lacustrine materials; Clay loam and Clay surface textures. TiEd2 Mainly a mixture of orthic and gleyed orthic Tisdale soils, with gleyed dark gray wooded Eldersley soils on lower slopes, and poorly drained soils in depressions. Tisdale- A mixture of Dark Gray (Tisdale) and Gray (Eldersley) soils formed in Eldersley shallow, clayey lacustrine materials underlain by glacial till; silty Clay (till substrate) loam to silty Clay surface textures. TiEd3T Mainly a mixture of orthic and gleyed orthic Tisdale soils, with gleyed dark gray wooded Eldersley soils on lower slopes and through depressions. - 1. Formerly Kamsack (tiil substrate) 2. Formerly Kamsack-Porcupine Plain (tiil substrate)

Saskatchewan Soil Survey. Page 47 - Tisdale-Melfort A mixture of Dark Gray (Tisdale) and Black and Thick Black (Melfort) soils formed in clayey lacustrine materials; Clay loam, silty Clay loam, - Clay and silty clay surface textures. TiMrl Mainly a mixture of orthic and gleyed orthic Tisdale soils, with a mixture of orthic and gleyed orthic Melfort soils on mid- to lower slopes and through depressions. TiMr5 Mainly a mixture of orthic and gleyed orthic Tisdale soils, with a mixture of orthic and gleyed orthic Melfort soils on lower slopes, and poorly drained soils in depressions. Wetland Poorly drained soils and shallow open water associated with wet, depressional areas; variable surface textures. Wzl Wet meadows. Mainly poorly drained soils, with shallow open water in centrai areas. WZ2 Marshes. A mixture of poorly drained soils and shallow open water. WZ3 Open water wetiands. Mainly shailow open water, with some poorly drained soils in marginal areas.

Saskatchewan Soi1 Survey. Page 48 8. SOIL INTERPRETATIONS

AREA MAPUNIT PUT "SA !?: EROS ACRES ----____ _-----_-____-______- - ______-_ - - -

1 AR4 2-1 UD m SICL-SIC 4Ckv A0 so A3 SG O 1 2D W1K 344.9 2 TIED3T 2-3 m m SICL-SIC 2Bqvtl BO s1 A2 SGO 1 1D W2G 49.3 3 PA2 3 HR 1WP L-SIL 2Bdvt2 BO SI 81 G1 1 2 W2K 290.9 4 TIMR5 2-3 u) lWA CL-C 3cqv BO so A3 SGO 1 1D W1K 454.2 5m 2-6 IHD rn U 4Dct2 D1 s1 A3 SGO 1 4D U 258.9 6 TIMRS 2-3 M lWPA CL-C 3cqv BO so A3 SGO 1 1D W1K 1514.8 7 TIED2 2 U m CL-C zcdqv BO SO 83 SGO 1 1 wo 933.3 8 NRTGl 3-2 H 2t-m L-SIL 3cst2 BO s1 B2 SG O 1 2 W1K 317.1 9 EDTI4 2-3 M 1WP CL-C 2Bdat.l BO SO A2 SGO 1 2D W1K 340.9 10 FW 3-6 UI O U 4Dct2 82 so A3 SGO 1 4 U 6.9 11 HWAVl 3-6 HIC O SICL-SIC 4Dct2 c3 s1 A3 SGO 1 4 W5G 201.2 12 TIMR5 2 U 1WA CL-SIC 3cqv B2 so 83 SG O 1 1 wo 724.5 13 PA2 3 HR 1WP L 2Bdvt2 BO s1 B1 G1 1 2 W2K 97.4 14 KAPP2 2-3 U m CL zcdqv 82 50 83 SGO 1 1 W1K 831.2 15 BBlOC 2-3 U 3SA SICL 4Dsv 82 50 83 SGO 1 1 wo 370.5 16 MRHHl 2-3 u) 2MA SICL-SIL 3Bsvtl BO so A2 SGO 1 10 W1K 1392.2 17 MR3 2 U 3SA CL-C 4Bsv 82 SO 82 SGO 1 1 wo 561. O 18 'K6 2-3 H m SIL-L 2Bsvt2 82 s1 82 SG O 1 1 W2K 297.7 19 MRTI5 2 u) m CL-SICL 2Casv BO SO A3 SG O 1 1D W1K 3063.3 20 FW 3-4 HD O U 4Dct2 DI SO A3 SGO 1 30 W2G 13.0 21 TIMRl 3 ID O SIC-C 3Bqt2 82 50 Al SGO 1 2D W2G 33.7 22 TIMR5 2-3 U O SIC 3cqv A4 50 83 SGO 1 1 wo 161.0 23 FW 3-4 HD O U 4Dct2 D1 SO A3 SG O 1 3D WZG 65.2 24 TIMR5 2-3 U O SIC 3cqv A4 so B3 SGO 1 1 wo 472.4 25 E65 3-4 HD O U 4Dct2 D1 so A3 SGO 1 3D W2G 5.5 26 BB12 2 U 1WP SICL-CL 2Bqv B2 50 82 SG O 1 1 wo 931. O 27 KAT11 2-3 u) 1WP SIL-SICL IBvtl B2 sa Al SGO 1 1D W1K 2282.5 28 MRBB7 2 U 2MA SICL-CL 3Bsv 82 SO 82 SGO 1 1 wo 3558.3 29 HHBB8 2-3 U 2MP SIL-SICL 3csv 82 SO 83 SGO 1 1 wo 890.8 30 GP U G4 U U 7.4 31 PA2 3-5 HRD 1WP L-SIL 2Ddt2 BO s1 81 G1 1 3D W2K 187.7 32 MRll 2-3 U 2t.m SICL-SIC 3Dsv BO SO B3 SGO 1 1 wo 1752.3 33 cF1 3 HR 1WP SICL 2-2 B2 s1 82 SG O 1 2 WI K 210.5 . 34 WZ2 1 L 2MA U 4cui BO so DY SGO U U 534.0 35 MRTIS 2 U 3MA C-CL 4csv BO SO 83 SG O 1 1 wo 713.3 36 WZ3 1 L 1WP U 4cwi BO so DZ SG O U U 74.9 37 KAPPl 3 H 1WP L 2Bdvt2 B2 so 82 SGO 1 2 W2K 10.5 38 KAPPl 3 H 1WP L 2Bdvt2 82 50 B2 SGO 1 2 W2K 311.8 39 TG5 3-2 H 1Mp SIL-SICL 2cst2v B2 s1 B3 * SGO 1 2 W2K 1145.8 40 MRTIST 3-2 u) m CL-SIC 2cC7q-J BO SO A3 SGO 1 2D W2K 1322.2 41 MRTIl 2 M m SIC-CL 3BQv BO SO A2 SGO 1 1D W1K 504. O 42 MRHHZ 2 U 1WP SICL-L 2cqv BO so 83 SGO 1 1 wo 2112.9 43 m5 2 U 3MA SICL 4Cwi D1 SO DX SG O 1 1 wo 272.9 44 FR2 2 U 1WP SICL-CL 2cqv BO so B3 SG O 1 1 wo 1511.5 45 MR13 2 U 1Mp SICL-SIL 2Bqsv BO SO 82 SGO 1 1 wo 302.1 46 MRBB4 3-4 HD 1WP SICL-CL 2cqt2 BO SO Al SGO 1 20 W1K 138.8 47 m 2-3 M 2WP U 4Dct2 D1 so A3 SGO 1 3D W3G 255.9 48 HHMRS 3-2 U 1Mp SIL-SICL 2csv B2 so B3 SGO 1 2 W1K 1410.3 49 MRBB3 3-2 U 1WP SICL-L 28qvtl BO SO B2 SGO 1 2 W1K 211.5 50 MRBB3 3-2 U 1WP SICL-L 2BqvtI BO su B2 SGO 1 2 WIK 941.6 51 WZ3 1 L 1WP U 4cui B2 SO DZ SG O U U 84.6 52 HHMR6 2 U 1Mp L-CL 2csv 82 SO 83 SG O 1 1 wo 1442.4 53 wz1 1 L m U 4cwi BO so DX SGO U U 75.7 54 wz2 1 L 1Mp U 4cwi B2 SO DY SGO U U 142.6 55 wz1 1 L 1MA U 4cwi 82 50 DX SGO U U 97.3 56 TGMü 3-2 U 1WP L-SIL 2cdv B2 SO B3 SGO 1 2 W1K 1752.5 57 BBMR2 2-3 U 1WP SIL-SICL 1cv 82 so 83 SGO 1 1 wo 1114.5 58 FW 3-4 ID 2WP U 4Dct2 D1 50 A3 SGO 1 3D U 718.8 59 BBMR3 3 HD 1WP SIL-SICL 1Bvt2 82 SO A2 SGO 1 2D W2G 1450.9 60 Tw 3-4 ID 1WP U 4Dct2 D1 50 A3 SG O 1 3D W4G 228.0 61 BBMR3 3 HD IWP SIL-SICL 1Bvt2 B2 so A2 SGO 1 2D W2G 663.9 62 KABB2 3 H 1WP L-SIL lcv B2 SO B3 SGO 1 2 W1K 1436.1 63 HHMR3 2-3 U 1WP SIL-SICL lBvtl 82 SO 82 SGO 1 1 wo 2169.3 64 FSi 4-3 ID 2WP U 4Dct2 D1 50 A3 SG O 1 3D W3G 524.3 65 HHMR3 2 u> lMP SIL-SICL 2BsV B2 so A2 SGO 1 1D W1K 1245.2 66 HHBB2 3-4 w 2Mp L-SIL 3cst2v 82 SO A3 SGO 1 2D W2G 558.3 67 WZ2 1 L 2-m U 4cwi 82 so DY SG O U U 162.3 68 BBHHS 2 U 3MA L-SICL 4Dsv B2 S3 83 SGO 1 1 wo 793.0 69 BB3G 3-4 HD 1WP SIL 2cqt2 82 SO Al G3 1 20 W2G 273.6 70 8 U G4 U U 13.3 71 MP5B4 3-4 HD 1WP SICL-CL 2cqt2 BO 50 Al SGO 1 2D W1K 241.3 72 MR9 2 UD 1W SICL-CL 2% BO so Al SGO 1 1D WIK 2378.9 73 wz2 1 L 2MP U 4Cwi D1 so DY SGO U U 218.4 74 MRl5 2 U 5MA SICL 4Dsv D1 SO B3 SGO 1 1 wo .111.3 75 TGNRl 3 L-SIL 2Bdvt2 BO 50 Al SGO 1 2D W2G 545.8 Saskatchewan Soi1 Survey. Page 49 Soil Interpretations, Cont.

AREA MAPUNIT SMPE LAND SAL- SURFACE IRRIG- CLASS FORM INITY TEXTURE ATION ____ ------

76 M6 2 U m C 4cwi D1 4 (7)w5 (3)w so DX SGO 1 1 wo 203.7 77 MR8 2 U 1WP CL 2Bqv BO l(9) 3(1 )W SO 82 SGO 1 1 wo 555.5 78 MR3 2 U -Mp CL 4Bsv BO 1 (8)3(1)N5(1) W so 82 SGO 1 1 wo 325.6 79 wz2 1 L 1WP U 4cwi BO 5 (6)W6 (4) W SO DY SGO U U 75.8 80 MRBB7 3 UD 1WP SICL-CL ZBqVtl BO 119) 3(1) W SO A2 SGO 1 2D W1K 1715.0 81 MR9 2 U 1WP SICL-CL 2Aq BO 1(10) so B1 SGO 1 1 wo 2550.3 82 WZ1 1 L lM!? U 4cwi BO 5 (6)W4 (4) W so DX SGO U U 139.2 83 wz1 1 L 1Mp U 4cwi BO 5(6)W4(4)W so DX SGO U U 22.1 84 m1 1 L lM!? U 4cwi BO 5 (6)W4 (4) W so DX SGO U U 32.1 85 HHBBl 3 UD 1WP L-SIL lBtlv B2 1(5)2 (4)M3(1)W so A2 SGO 1 2D W1K 1568.9 86 MR1 3-2 rn 1WP SICL-CL 2Bqtl BO 1(10) so Al SGO 1 2D W1K 227.4 81 Ew 3 ID 1WP U 4Dct2 D1 4(7)Wl'5(3)WE SO A3 SGO 1 3D W4 G 56.4 88 MR1 3-2 UD 1WP SICL-CL 2Bqtl BO l(10) so Al SGO 1 2D W1K 139.5 89 MRBBl 2-3 UD 1WP SICL-SIL 2Bqvtl BO 1(5)2 (4)M5(1)W SO A2 SGO 1 1D W1K 1315.5 90 MRBBl 3 In> 1WP CL-SICL PBqVtl BO 1(9)3(l)W so A2 SGO 1 2D W1K 717. 8 91 BBMR3 3 HD 1WP SICL-CL 2Bqvt2 B2 2(9)T5(1)W so A2 SGO 1 2D W1K 2.2 92 Fsi 3-4 UD 1WP U 4Dct2 D1 3 (6)W4 (3)W5 (1)W SO A3 SGO 1 3D W2G 5.5 93 Ew 3-2 ID m U 4Dct2 c3 5 (6)W3 (4) ïW SO A3 SGO 1 30 W2G 17.1 94 Ew 3-2 ID 2Me U 4Dct2 c3 5 (6)W3 (4)TW so A3 SGO 1 3D W2G 123.7 95 Fsi 3 HC 1WP U 4Dct2 c3 5(8)WE7(2)W so A3 SGO 1 3 W4G 56.3 96 MRBB5 3-4 HD 1WP SICL-CL 2cqt2v B2 2(5)T3(3)T4 (2)W so A3 SGO 1 2D W2G 1004.3 97 BBHHl 3 HD 1WP SICL 2Bqt2 B2 2(10)TE so Al SGO 1 2D W2G 848.3 98 Ew 4-5 IG 2WP U 4Dct2 D1 6 (5)WE4 (4) "3 (1)T SO A3 SGO 1 4G W4G 356.3 99 Fsi 4-3 ID 2WP U 4Dct2 D1 3 (6)T5 (4)WE so A3 SG O 1 3D W4G 378.8 100 HHBB6 3-4 HD 1WP SICL 2Dqv 82 3(5)TW2 (4)TE5(1)W SO A3 SGO 1 20 W2G 982.5 101 MRBBl 3 UD 1WP SICL 2-1 82 1(9)3(1)W so A2 SG O 1 20 W1K 551.8 102 MR!5 4-3 H 1WP SIC-SICL 3DW 83 3 (6)ïW2 (3)T5 (1 W so B3 SG O 1 2 W2K 15.5 103 HHBBl 3-4 H 1WP L-SICL 1Ct2 82 2 (5)T3 (4) T4 (1) W so B2 SGO 1 2 W2K 160.6 104 Fsi 4-3 ID 2WP U 4Dct2 D1 6(10)WE so A3 SG O 1 3D U 180.2 105 BBHHl 3-4 HD 1WP SIL-L 1Dv B2 2 (6)TE3(4) TW so A2 SG O 1 2D W2G 502.8 106 Fsi 2 UD rn U 4Dct2 D1 3(5)WE6(5)W SO A3 SGO 1 3D U 143.9 101 BBHHl 3-4 HD 1WP SIL-L 1Dv 82 2 (6)TE3(4)TW SO A2 SGO 1 2D W2G 768.2 108 HHBB8 3-4 H 1WP L-SIL lCt2V 82 2 (5)MT3(3)T5 (2)W SO 83 SGO 1 2 W2K 479.1 109 BBHHl 3-2 U 1WP SIL-L lBtlv 82 2(5)M1 (4)3(l)W so 82 SGO 1 2 W1K 1169.0 110 .Ew 3-4 ID 1wD U 4Dct2 D1 3(7)TE6(3)WE so A3 SGO 1 3D W3G. 105.5 111 HH6 3-2 UD 1WP SIL-SICL 1cv 82 l(8) 3(1)W5 (1)W so A3 SGO 1 2D W1K 863.4 112 Ew 3-4 ID 2WP U 4Dct2 D1 3 (7)TE6 (3)WE so A3 SGO 1 3D W3G 143.6 113 HHlC 3 UD 1WP SICL-L 2-1 82 1(9)3(1)W so A2 SGO 1 2D W1K 1174.8 114 WZ1 1 L lMA U 4cwi BO 5 (7)w4 (3)w so DX SGO U U 11.6 115 Ew1 1-2 U m L-CL 4Cwl D1 3 (6)NW4 (1) W so DX SGO 1 1 wo 120.8 116 MR6 2 U 1WP SICL 2Bqv BO 1(9) 3(1)W so 82 SGO 1 1 wo 743.4 111 HHBBl 2-3 U 1WP SIL-SICL lBvtl B2 1 (6)2 (3)M4 (1)W SO B2 SGO 1 1 wo 691.1 118 HHKAl 3-2 UD 1WP SIL-SICL 1Bvtl B2 l(10) so Al SGO 1 2D W1K 479.2 119 Ew 3-4 ID 2WP U . 4Dct2 D1 3(6)TI6(4)W so A3 SGO 1 3D W3G 169.7 120 m3 1 L 1WP U 4cwi B2 7 (8)W6(2) W so DZ SG O U U 19.7 121 HHKAl 3-4 UD 1WP SIL-SICL lBvtl B2 1(6)4(4)TE SO Al SG O 1 2D W2G 147.8 122 HH1 3 HD 1WP SIL-SICL 1Bvt2 82 2 (9)TE3(1)W SO A2 SG O 1 2D W2G 194.9 123 KH1 3 HD 1WP SIL-SICL lBvt2 82 2 (9)TE3(1)W SO A2 SGO 1 2D W2G 199.2 124 Iw 3-4 ID 1MA U 4Dct2 D1 3 (7)T6(3) WE so A3 SGO 1 3D W4G 81.6 125 HEiKAl 3-4 m 1WP SIL-SICL lBvtl 82 1 (6)2 (4 )TE so Al SGO 1 2D W2G 48.8 126 KA1 3-4 H 1WP L-SIL 1Ct2 82 2 (6)T3(3)T5 (1)W so B2 SGO 1 2 W2K 1114.8 127 AV5 2-3 uc PIP CL-SICL 4Dwsv Dl 5(6)WE4(4)NW SO c4 SGO 1 1 W4G 868.6 128 sB2 4-3 H 1WP FL-VCL lCt2v c3 3 (8) Mr5 (2 W so 83 SGO 2 3 W2K 1296.2 129 KABB6 3-4 H SIL-L 2cst2v c3 2 (4 )MT3 (4) T5 (2)W so B3 SGO 1 2 W2K 1355.5 130 HHBB8 2-3 U 2Me L-CL 3csv c3 1(6)2(2)M5(2)W so B3 SGO 1 1 wo 437.1 131 Mi4 3-2 H ZMA VL-L 4cwi Di 4 (8)W5 (2)W SO DX SG O 1 1 wo 539.6 132 KA8 4 H 1WP L-SIL lCt2V c3 3(8)TF,5(2)W SO B3 SGO 1 2 W3K 479.0 133 Mil 2 U lMA L-CL 4cwi D1 4 (10)W so DX SGO 1 1 wo 366.6 134 LCSB2 3-4 H 1WP VL 2Cdt2v c3 3(6)Mr2 (2)E5(2)W so B3 SGO 2 2 W2K 1155.7 135 KA3 4-5 H 1WP SIL 1Ct2 c3 3 (6)TE4(3) T5 (1)W so B2 SGO -1 2 W3K 329.0 136 KASBl 3-4 H 1WP L-VL 1Ct2 B2 2 (5)ME3(4) T5 (1)W SO B2 SGO 1 2 W3K 872.2 131 HHl 3-4 H 1WP SIL-SICL 1Ct2 SO B2 SGO 1 2 W3K 1147.2 138 AV5 2-3 uc 2MP SICL-SIC 4DW SO c4 SGO 1 1 W4G 857.3 139 BBHHl 2-3 UD 1WP SIL-L lBtlV so A2 SG O 1 1D W1K 988.5 140 Ew 4-3 ID 2WP U 4DctZ SO A3 SGO 1 30 U 178.7 141 HHBBl 3-4 H 1WP L-SICL 1Ct2 so B2 SGO 1 2 W2K 74.0 142 HHBBl 3 HD 1WP SIL 1cv so A3 SGO 1 2D W2G 380.1 143 Tw 3 ID 1WP U 4Dct2 so A3 SGO 1 3D W2G 12.4 144 884 4-3 HD 1WP SIL-SICL 1Dv so A2 SGO 1 3D W2G 30.9 145 BB5 3-2 U 1WP L-SICL 1cv SO B3 SGO 1 2 W1 K 158.6 146 BBKAl 3-2 U 1WP L lBtlV SO 82 SG O 1 2 W1K .161.3 147 SBK1 3-4 m 1WP VL-L 1Ct2 so A2 SGO 1 2D W2K 547.9 148 WZ3 1 L IWP U 4cwi SO DZ SGO u U 109.7 149 KASB5 3-4 H lMP L-VL 2cst2v SO B3 SGO 1 2 W2K 1163.0 150 Bu3 3-4 H 1WP VL-L 1Ct2 SO B1 SGO 1 2 W2K 152.3 151 BUBB2 3-4 H 1WP VL-L lCtZV SO B3 SGO 1 2 W2K 454.2 152 NTSY2' 3-4 H 1WP Ls 3hV 50 B3 s4 2 2 W3B 430.2 153 BUHM2 3 H lM!? VL-L 2csv SO 83 SGO 1 2 W1K 154.6 154 WZ2 1 L 1WP U 4cwi so DY SGO U U 66.4 155 Nï7 3 H O Ls-s îmv so B2 s4 4 2 W4B 51.6

Saskatchewan~- ..~_ Soil Survey. Page 50 Soil Interpretations, Cont.

IRRIG- PH ATION __

156 KASB5 3 H 1WP L-VL 1CV c3 SO B3 SGO 1 2 W1B 379.6 157 NTSB5 3-2 H 1WP LS-VL 3Qnvt2 c3 SO B3 s3 2 2 W2B 371.6 158 SBKA3 3 H 1Mp SL-L 2msv c5 so B3 SGO 1 2 W2K 110.4 159 f.w6 2 u 1MA FL 4cwi D1 SO DX SGO 2 1 wo 362.9 160 CRPNZ 3-2 H 1WP LS-s 3Dmv c3 SO B3 s4 4 1 W3B 129.1 161 NTSY2 3 H 1WP Is 3Dmv B2 SO B3 54 2 2 W4 B 747.4 162 SB1 3-2 UI 1WP VL lBtlv c3 SO B2 SGO 2 2 W2K 200.6 163 WZ2 1 L 1WP u 4cwi c3 SO DY SGO U u 248.6 164 SB2 4-3 H 1WP VL 1CtZV c3 so 83 SGO 2 2 W2K 982.8 165 WZ1 1 L m U 4cwi 82 so DX SG O U U 126.5 166 SBGOP 2-3 u IWP VL 1CV c3 SO 83 SGO 2 1 wo 75.6 167 NTCRl 3 H 1WP LS-VL 3Qnv c3 so B2 s4 2 2 W2B 449.7 168 SBGO2 2-3 u 1WP VL ICV c3 so B3 SG O 2 1 wo 163.6 169 LCSB4 4-3 H 1WP VL 2Cdt2 c3 SO B2 SG O 2 2 W3K 175.1 170 m2 1 L 1WP U 4cwi c3 so DY SG O U U 110.5 171 SB2 3 H 1Mp L-VL 2Dsv c3 SO B3 SG O 1 2 W2K 383.1 172 SBLC2 3-4 H 1WP L-VL 1ct2v c3 so B3 SG O 1 2 W2K 363.6 173 SïW1 3-4 HD 1WP FL-LS 2Qnvt2 BO SO A2 s4 2 2D W2B 698.1 174 SYPN1 3 HR O L.5 3ht2 Al so Bl s4 2 1 W3B 165.4 175 SPiM 2 H m 4cwi D1 SO DW SG O 1 U wo 203.2 176 SYGO4 4 H IWP Ls-SL 3Qnt2 84 so B1 s3 4 1 W3K 297.8 177 SBLCl 4 H 1WP FL-VL 1Ct2 c3 so Bl SG O 2 3 W2K 131.6 178 GOSBlO 3 H 2WP FL-VL ZDsv c3 SO 03 SG O 2 2 W2K 1153.6 179 LC8 3 H IWP FL 2Ddv c3 so 83 SG O 2 2 W2K 329.1 180 KASB2 3 H 2WP L-VL 2csv B2 so B3 SGO 1 2 W2K 1225.3 181 w3 2-3 U 4MA FL 4cwi D1 so DX SGO 2 1 wo 862.7 182 LCSB2 4-5 H 2WP L-FL 2Cdt2v c3 SO 83 SGO 2 3 W3K 1100.9 183 SY3 4 H 1WP FL 2Cdmt2 82 so B2 s4 2 2 W3K 308.7 184 LCSB2 4-3 H 1WP FL 2Cdt2v c3 SO B3 SG O 2 3 W2K 445.2 185 SY7 4-3 HR 1WP SL-FL 2Qnt2v B2 so B3 s4 2 2 W4K 855.3 186 ES82 3-4 HD 1WP FL-VL 2Ddv c3 SO A3 SGO 2 2D W2G 1502.9 187 SB5 4-5 HD 1WP FL-VL 1Ct2 c3 so Al SGO 2 3D W2G 240.8 188 SBG04 4-5 IH 1WP VCL 2Dw c3 so A2 SGO 1 3 W3K 158.8 189 KA11 3-2 U 1WP SIL lBtl 82 so B1 SG O 1 2 W1K 101.0 190 KAT12 3-4 H 1WP L-c 1cvt2 82 SO B1 SGO 1 2 W2K 302.5 191 SBKAl 3-4 HD 1WP FL-L 1Ct2 c3 SO A2 SGO 1 2D W2G 526.9 192 KAil 3 H 1WP L-SIL 1Bt2 c3 so B1 SGO 1 2 W1K 848.0 193 KABB2 2-3 u 1WP L-SIL 1CV 82 SO 83 SGO 1 1 W1 K 1310.1 194 KABB2 2-3 u 1WP L-SIL 1cv 82 so 03 SGO 1 1 W1K 741.6 195 KAT14 3 H 1WP SIL-CL 1BVt2 82 so B1 SGO 1 2 WlK 324.6 196 fw 3-4 HD 1WP u 4Dct2 D1 ÇO A3 SGO 1 3D W4G 105.2 197 KAT14 3 H 1WP SIL-CL 1Bvt2 82 SO B1 SG O 1 2 W1K 200.7 198 PP1 3 H 1WP s IL-CL 2Bdvt2 BO SO B1 SGO 1 2 W1K 135.6 199 HWAvl 5-2 HG 3Mp CL-C 4Dct2 D1 so A3 SGO 1 3G W4G 332.9 200 PPKIU 3 H 1WP L-SIL 2Bdvt2 BO so 82 SGO 1 2 W2K 460.0 201 SBKAl 3-4 HD 1WP FL-L 1Ct2 c3 so A2 SGO 1 2D W2G 46.4 202 SBKA2 3 H 1WP FL-SIL 1DV c3 so B3 SG O 1 2 W2K 803.7 203 Mû 2-3 u 2MP FL 3Dsv c3 so B3 SGO 2 2 W1K 149.4 204 Mi3 2-3 U 4t.m FL 4cwi D1 SO DX SGO 2 1 W2K 217. O 205 LCSB3 4-3 H 1WP FL ZDdv c3 so B3 SG O 2 3 W3K 604.8 206 Mi3 3-2 u 4MA FL 4cwi D1 so DX SG O 2 1 W2K 76.9 207 K8 3-2 u m FL-VCL 3csv c3 SO 83 SGO 1 2 W2K 462.9 208 MLClO 3 HD 2WA FL-VL 2Dsv c3 so A3 SG O 2 2D W2G 238.2 209 LCSBZ 3 H 1WP SL 2Ddmv c3 so 83 SGO 2 2 W2K 7808.2 210 TI4 4 HD 1WP C 3Cqt2 B2 so Al SG O 1 2D W2K 68.3 211 Hw 5-4 HD O u 4Dct2 B2 SO Al SG O 1 4D W4G 151.6 212 Hw 5-4 HD O u 4Dct2 B2 so Al SG O 1 4D W4G 102.7 213 LCSBZ 3 H 1WP SL PD&v c3 so B3 SG O 2 2 W2K 211.2 214 LCSB2 3 H 1WP SL PD&v c3 SO B3 SGO 2 2 W2K 48.4 215 Tw 3-4 ID 1WP u 4Dct2 D1 so A3 SG O 1 3D U 40.6 216 KA6 2-3 UD 1WP L-SIL lBtl B2 SO Al SG O 1 1D W1K 1168.3 217 KA13 3 HD 2WP SIL ZDsv B2 so A3 SGO 1 2D W2K 259.0 218 PPLC3 2-3 u 1WP SIL-FL ZBdtlv BO SO 82 SGO 1 2 WlK 689.8 219 KABB5 2-3 u 2MP SIL-SICL 3csv B2 so R3 SGO 1 1 WIK 948.5 220 KA6 3-2 H 1WP L-SIL 1Ct2 82 ÇO B1 SGO 1 2 W1K 919.8 221 Hw 5-4 HD O u 4Dct2 B2 SO Al SGO 1 4D U 37.2 222 Hw 5-4 HD O U 4Dct2 B2 ÇO Al SGO 1 4D U 11.8 223 Hw 5-4 HD O u 4Dct2 B2 ÇO Al SGO 1 4D U 5.3 224 WPl 3 H 1WP SIL 2BdVt2 82 SO B1 SGO 1 2 W1K 712.0 225 Ri? 3-4 HD O u 4Dct2 D1 SO A3 SGO 1 3D W2G 113.1 226 WPl 3 H 1WP SIL 2Bdvt2 82 SO B1 SGO 1 2 W1K 516.6 227 F54 3-4 HD O u 4Dct2 D1 so A3 SGO 1 3D W2G 56.0 228 TI11 2-3 U O CL 3cqv 82 SO B3 SGO 1 1 W1K 30.8 229 SP2M 2 H O 4cwi D1 so DW SGO 1 U U 141.3 230 TI11 2-3 U O SICL-SIC 3cqv B2 SO B3 SGO 1 1 W1K 523.9 231 fw 3-4 HD O u 4Dct2 D1 so A3 SGO 1 3D W2G 42.3 232 KA5 3 H m CL 3Dsv B2 ÇO B3 SGO 1 2 W1K 485.9 233 TI11 3-2 U O SIC-SICL 3cqv 82 50 83 SGO 1 2 wo 223.7 234 Hw 5-4 HD O u 4Dct2 B2 ÇO Al SGO 1 4D U 73.2 235 AV5 2-3 HC 2WP VL-SICL ~DWV D1 so c4 SGO 1 2 W4G 1124.0 Saskatchewan Soil Survev. Page 51 Soi1 Interpretations, Cont.

AREA MAPUNIT SLOPE LAND SAL- SURFACE IRRIG- PH CWS FORM INITY TEXTURE ATION ---- ___--__ _---

236 HW 5-4 HD O U 4Dct2 82 50 Al SGO 1 4D W4G 266.3 237 HW 5-4 HD O U 4Dct2 B2 so Al SGO 1 4D U 107.0 238 GOLCZ 3-2 H 1WP SL-L 2mv 82 SO 83 SG O 1 2 W2K 1961.8 239 SY8 3 H O SL ZD&v 82 so 83 s4 2 2 W2K 180.7 240 KA6 3-2 U 1WP SICL 2Eqtl B2 SO B1 SGO 1 2 W1K 764. O 241 PPEDZ 3 H 1WP SIL-C 2cdv BO so 83 SGO 1 2 W1K 2106.1 242 GOSBlO 3 HD 2WP VL 2Dsv c3 50 A3 SGO 2 2D W2K 568.1 243 KAPP4 3 U 1WP SIL ZBdvtl B2 SO 81 SGO 1 2 W1K 959.8 244 EDTIl 2-3 U 1WP C 3Wl BO so B1 SGO 1 1 wo 25.8 245 Kvi 2-5 HD O U 4DCt2 c3 so A3 SGO 1 3D U 251.7 246 ED3 4-5 HD 1WP C 3Cqt2 BO so Al SGO 1 3D W3G 135.1 247 WP4 3 U IWP SIL 2Bdvtl B2 SO B1 SGO 1 2 W1K 124.5 248 EDTIl 2-3 U 1WP C 3Bqtl BO so El SG O 1 1 wo 556.5 249 EDTIl 3-4 m O CL 2Cdqt2 BO so A2 SG O 1 2D W2G 148.0 250 EDTI2 2-3 UD 1WP SIC-CL 3cqv 80 so A3 SGO 1 2D W1K 166.5 251 EDTIl 3-4 ID O CL 2Cdqt2 BO so A2 SGO 1 2D W2G 40.6 252 EDTIl 3-4 ID O CL 2Cdqt2 BO SO A2 SGO 1 2D W2G 188.2 253 Iw 2-5 HD O U . 4Dct2 c3 SO A3 SG O 1 3D U 135.2 254 EDTIl 3-4 m O CL 2Cdqt2 BO so A2 SGO 1 2D W2G 96.9 255 Iw 2-5 HD O U 4Dct2 c3 so A3 SGO 1 3D U 18.9 256 EDTIl 3-4 ID O n 2Cdqt2 BO so A2 SGO 1 2D W2G 7.1 257 KAPPZ 3 HD 1WP SIL-SICL 2cdv B2 so A3 SG O 1 2D WlK 2637.1 258 Fw 3 HD O U 4Dct2 B2 so A3 SG O 1 3D W2G 40.8 259 Fw 3 HD O U 4Dct2 B2 so A3 SGO 1 3D W2G 5.4 260 KA5 3-2 U 1WP SIL 10, B2 so B3 SG O 1 2 WlK 1198.6 261 KA1 3 ID O L 1Bt2 82 so Al SGO 1 2D W1K 262.0 262 Iw 2-4 HD O U 4Dct2 D1 so A3 SGO 2 3D U 253.2 263 KA1 3 ID O L 18t2 B2 SO Al SGO 1 2D W1K 207.9 264 Iw 3 HD O U 4Dct2 B2 SO A3 SGO 1 3D W2G 2.3 265 MPSP2M 2 H O 4cwi D1 so DW SGO 1 U U 74.1 266 Go8 3 H 1WP VL-L 1cv c3 SO B3 SG O 1 2 W1K 306.9 267 CRSYZ 3 H 1WP LS-FL 3Dmv c3 so B3 s4 2 1 W3K 153.5 268 Go6 3-2 U 1WP FL-VL 1DV c3 SO 83 SG O 2 2 W1K 1260.5 269 CRSY2 3 H 1WP LS-FL 3Dmv c3 so 83 s4 2 1 W3K 55.2 270 PN3 3-4 H O s-LS 4Qnt2 Al so B1 54 4 1 W3K 42.8 271 CR6 3 H 1WP SL-LS zmv c3 SO 83 s4 2 2 W2K 598.7 272 PN3 3-4 H O s-LS 4Qnt2 Al so B1 s4 4 1 W3K 223.4 273 cR6 3 H 1WP SL-Ls 2Dmv c3 so 83 54 2 2 WZK 730.6 274 Iw 2-3 HD O U 4Dct2 c3 SO A3 SGO 2 3D U 55.1 275 cR6 3 H 1WP SL-LS 2Dmv c3 SO B3 s4 2 2 W2K 149.4 216 PNCR2 3 H O LS-SL 3Dmv A2 SO B2 s4 4 1 W3K 111.3 277 PNCW 3 H O LS-SL 3Dmv A2 SO B2 s4 4 1 W3K 11.1 278 SY3 3 H O LS-SL 35nvt2 Al SO 61 s4 2 1 W3K 114.9 279 Iw 3 HD O U 4Dct2 c3 SO A3 SGO 4 30 U 265.1 280 PN3 3-4 H O Ls 3Qnt2 Al SO B1 s4 4 2 W3K 191.2 281 WY1 3 H 1WP SL-Ls 2mv c3 SO B3 s4 2 2 W3K 604.7 282 SB1 3 H O n 1Bt2 c3 so B1 SGO 2 2 W2K 4i.2 283 WY1 3 H 1WP SL-LS zmv c3 SO 83 s4 2 2 W3K 4.9 284 Iw 3 HD O U 4Dct 2 c3 50 A3 SGO 4 3D U 21.4 285 CRSYl 3 H 1WP SL-Ls 2mv c3 so 83 s4 2 2 W3K 4.5 286 IW 3 w O U 4DctZ c3 so A3 SGO 4 3D U 23.4 287 Kvi 3 HD O U 4Dct2 c3 so A3 SGO 4 3D U 52.4 288 cR8 3 H 1WP Ls-SL 3hnv c5 so B3 s4 2 1 W2K 10.1 289 SBLC1 3 H 1WP SL-VL 25nvt2 c3 so B1 SGO 2 2 W2K 36.1 290 cR8 3 H 1WP LS-SL 3hnv c5 so B3 s4 2 1 W2K 578.1 291 . P"T1 3 HD O S-LS 45nvt2 Al so Al s4 4 1D W3B 1513.8 292 GO6 3-2 U 1WP FL-VL 1Dv c3 so B3 SGO 2 2 W1K 3311.2 293 GO5 2 U 1WP FL-VL 1DV c3 SO B3 SG O 2 2 W1K 401.4 294 KA13 3-2 U 1WP L-SIL 1cv c3 SO 83 SG O 1 2 WlK 137.4 295 Fw 2-4 HD O U 4Dct2 D1 so A3 SG O 2 3D W3G 206.8 296 KA13 3-2 U 1WP L-SIL 1CV c3 50 83 SGO 1 2 W1K 817.2 297 GOLC2 3 H 1WP SL-FL 2Dmv c3 SO 83 SG O 2 2 W2K 1113.0 298 SB1 3-4 ID O FL 1Ct2 c3 SO Al SGO 2 2D W2G 338.2 299 SB1 3-4 ID O FL lCt2 c3 50 Al SG O 2 2D W2G 378.6 300 GoLCZ 3 H 1WP SL-FL 2Dmv c3 so 83 SGO 2 2 W2K 6924.5 301 KA12 2-3 U 2WP L 2Dsv 82 so B3 SGO 1 1 W1K 1671.4 302 Mi1 2-3 UD 2WP CL-SIC 4cwi D1 SO DX SG O 1 1D W2G 195.9 303 KAPP2 3 HD 1WP SIL-SICL 2cdv B2 SO A3 SG O 1 2D W2K 1400.8 304 GOSB10 3 H 1WP SL-VL 2mv c3 so B3 SGO 2 2 W2K 1092.1 305 Go2 2-3 H 1WP SL-VL 2mv c3 SO 83 SGO 2 1 W2G 634.9 306 S31 3-4 HD O SL-VL 2Qnt2 c3 SO Al SGO 2 2D W3G 366.4 307 SBLCl 2-3 UD O FL lBtl c3 S3 Al SGO 2 2D W2G 531.4 308 SEGO4 3 H 1WP n 1Bt2 c3 so 81 SGO 2 2 W2B 310.9 309 mN1 2-3 U O LS-S 3Bmvtl Al so B1 s4 4 1 W2B 238.0 310 NTCRl 2 U O LS-SL 3Env c3 SO B1 s4 2 1 W1 B 713.9 311 PN1 3-2 U O S 4ûntl Al so B1 54 4 1 W2B 171.3 312 Kvi 3 UD O U 4Dct2 D1 SO SGO 4 3D W2G 84.9 313 SBLCl 3-4 UD O VL lBtl c3 so 2 SGO 2 2D W2G 420.7 314 NTCRl 2 U O LS-SL 3Env c3 SO B1 s4 2 1 W1B 1902. O 315 SPAWl 2 H O SL 4cwi c3 SO DW SG O 2 U U 508.3 Saskatchewan Soi1 Survey. Page 52 Soil Interpretations, Cont.

AREA MWUNIT SLOPE LAND SAL- SURFACE IRRIG- -- CLksS----- FOFS.1-______INITY TEXTURE ATION

316 PNNTl 3 U O S-LS 4Bmvtl Al 5(6)MF4(4)ME so B1 s4 4 1 W3B 957.3 317 SP2M 2 H O 4CnI D1 0(5)4(5)W SO DW SG O 1 U U 54.2 318 PWl 3-2 U O s-LS 4hvtl Al 5(6)MF4(4)ME so B1 s4 4 1 W3B 1.4 319 PNNTl 3-2 U O S-LS 4mnVtl Al 5(6)MF4(4)Mr SO B1 s4 4 1 W3B 137.4 320 NTPNl 3-2 U O LS-s îmvtl Al 4(6)M5(4)MF so B1 s4 4 2 W2B 1051.4 321 cR8 2 U O SL zmv C5 3(9)tW5(1)W SO 83 s4 2 1 wo 422.8 322 NTCFU 2 U IWP LS-SL 3mv C3 4(6)M3(4)M so 81 s4 2 1 W1B 1014.6 323 cR8 2 U 2WP SL zmsv C5 3(9)tW5(1)W so 83 s4 2 1 wo 87.0 324 WZ3 1 L 1WP U 4cni C5 1(7)W6(3)W SO DZ SGO U U 20.4 325 WZ3 1 L 1WP U 4cwi C5 7(7)W6(3)W SO DZ SGO U U 32.3 326 SEGO4 2-3 U 1WP FL lBtl C3 3(10)M so B1 SGO 2 2 W1K 217.0 327 CR8 2 U 2WP SL 2msv C5 3(9)MW5(1)W SO 83 54 2 1 wo 125.6 328 NTSB1 2-3 U O SL-FL 2mvt1 C3 3110)M so 81 s3 2 1 W1B 122.5 329 PN1 3 H O s 4mt2 Al 5(10)MF SO 81 54 4 1 W2B 122.4 330 NTCRl 2 U O LS-SL 3mv C3 4 (6)M3(4)M so El 54 2 1 W1B 1161.8 331 PN1 3 U O s 4Eïntl Al 5(10)MF so B1 s4 4 1 W2B 127.3 332 NTSB1 2-3 U O SL-FL 2mvt1 C3 3(10)M so B1 53 2 1 W1B 207.4 333 Iw 2-3 UD 1WP U 4Dct2 D1 7(7)W6(3)W SO A3 SGO 1 3D U 508.3 334 NTSB1 2-3 U O SL-FL 2Bmvtl C3 3(10)M SO B1 53 2 1 W1B 130.6 335 NTSBl 2-3 U O SL-FL 2Bmvtl C3 3(10)M SO B1 s3 2 1 W1B 105.1 336 Mïl 2 U O Ls-SL 3mv C3 4(6)M3(4)M so B1 s4 2 1 W1B 202.6 331 SP2M 2 H O 4Cwi D1 0(9)4(1)W SO DW SG O 1 U U 215.6 338 PN3 3 U O s 4mtl Al S(10)MF so B1 s4 4 1 W2B 108.8 339 NT1 2 U O LS-SL 3mv C3 4(6)M3(4)M SO B1 s4 2 1 W1B 224.8 340 PNW 3 H O s-LS 4mv A2 5(8)MF4(2)WE so 82 s4 4 1 W3B 226.0 341 NTSBl 3-2 U O LS-SL 3mvtl C3 4(6)M3(4)M so B1 53 2 2 W1K 420.9 342 GO2 2-3 m 2MP FL 3Dsv C5 3(9)Md5(1)W so A3 SGO 2 10 W2G 1182.0 343 W6 2 U 2WP FL 4cwi D1 4(10)W SO DX SGO 2 1 wo 235.2 344 cR8 2-3 U 1WP SL 2Dmv C5 3(8)Mw5(2)W SO B3 s4 2 1 W1B 452.9 345 NE04 3 H 1WP LS-SL 3mv C3 3(4)M4(4)M5(2)W SO B3 53 2 2 W1B 486.1 346 SY2 3 H O Ls 3Bmt2 Al 5(10)MF SO B1 s4 2 1 W3B 288.6 347 W6 2-3 U 2MA VL 4cwi D1 4 (7)W5 (3)W SO DX SG O 2 1 wo 119.4 348 PNCR3 3-2 U 1WP LS-VL 3mv A2 5(6)Md3(4)MW so B3 s4 4 1 W2B 281.5 349 PNCEW 3-2 U 1WP Ls-VL 3mv A2 5(6)Md3(4)MW SO B3 s4 4 1 W2B 18.1 350 WZ3 1 L 1WP U 4cwi A2 7(10)W so DZ SGO U U 68.0 351 PNCR3 2-3 U 1WP Ls 3mv A2 5(6)tW4(4)MW SO B3 s4 4 1 W1B 46.9 352 PNCR3 2-3 U 1WP Ls 3mv A2 5(6)MA4 (4)MV so 83 54 4 1 WlB 47.3 353 PNCR3 2-3 U 1WP Ls 3mv A2 5(6)WA4 (4)MW so 83 54 4 1 W1B 518.3 354 SPAWl 2 H O SL 4Cwi C3 0(8)6(2)W . so DW SGO 2 U u 2193.1 355 CRPN2 2 U O Ls 3Rnv C3 5(6)Md4(4)ME SO B3 s4 2 1 W3B 689.2 356 SY3 2 U O Ls 3- Ai 5(10)MF so El 54 2 1 W2B 598.1 357 SYPNl 2-3 U O Ls 3mt1 Al 5(10)MF so El 54 2 1 W2B 363.3 358 SYPN1 3-4 U O VL-LS 2cCknv Ai 3(6)ME5(4)MF so B1 54 2 2 W2B 411.5 359 SY3 2-3 U O Ls-VL 3mv Al 5(6)MF3(4)M SO B1 54 2 1 W2B 173.4 360 PNNTl 3-2 U O LS-VL 3mv Al 5(6)MF3(4)ME SO B1 s4 4 1 W3B 565.1 361 PN1 4 H O Ls mt2 Al 5(10)MF so B1 s4 4 2 W3B 1340.7 362 Sï3 3-2 U O VL 2Bdmtl Al 3(10)M so Bl s4 2 2 W2B 329.9 363 PN2 3-2 U O S 4Bmtl Al 6(10)MF so B1 s4 4 1 W2B 257.8 364 SYPNl 2-3 U O Ls 3mt1 Al 5(10)MF SO B1 s4 2 1 W3B 675.5 365 PN2 3-4 H O Ls 3mt2 Ai 5(10)MF so B1 s4 4 1 W3B 224.7 366 FSi 4-5 VD O U 4Dct2 D1 3(5)TE4 (4)TE5(1)W SO A2 SGO 3 4D U 117.7 361 PN2 3-4 H O Ls 3mt2 Al 5(10)MF sa 81 s4 4 1 W3B 132.3 368 MPlM 2 H O 4-1 Al O(10) SO DW SG O 1 U U 106.9 369 PN2 5-4 H O s 4Qnt2 Al 6(10)MF so B1 54 5 1 U 1611.3 370 PN2 2-3 U O S-LS 4mv Al 6(6)MF5(4)MW SO 82 s4 4 1 U 4259.7 371 PNCR4 2-3 U 1WP LS-VL 3mv A2 5(8)tW3(2)M SO 83 s4 4 1 W2B 6909.O 372 cR8 2-3 U 1MA VL-Lç 2msv C5 3(5)M4(3)MW5(2)W so 83 54 2 1 WIB 812.6 373 CRPN2 2 U lMP VL-Lç 3mv C3 3(6)M5(4)tW SO B3 54 2 1 W1B 571.8 314 W1 2 U lMPA VL 4Cwl D1 4 (5)W6 (5)W so DX SGO 2 1 wo 168.5

Saskatchewan Soil Survey. Page 53 9. FURTHER INFORMATION

For more information about the data contained in this report or for more information about the Saskatchewan Soil Survey contact:

Saskatchewan Soil Survey #210 John Mitchell Building University of Saskatchewan SASKATOON, Saskatchewan s7N owo

Telephone: (306) 975-4060

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