Soils of the - Agriculture and Agri-Food Canada
Soils of the - Agriculture and Agri-Food Canada Soils of the - Agriculture and Agri-Food Canada
COGHLAN SOILS (CG) Location and Extent : Coghlan soils occupy a few areas south of Langley and in the vicinities of Hopingto n and the Abbotsford Airport . There are about 310 ha of pure map units and 30 ha of Coghlan-Defehr soi l complex . Topography and Elevation : The topography of Coghlan soils varies from level or slightly depressional t o very gently sloping . Slope gradients are less than 3 percent and elevations range from 30 to 50 m above se a level . Parent Material and Texture : Coghlan soils have developed from coarsetextured glaciofluvial deposits which have small amounts of silty eolian material on or mixed into the surface . Surface textures vary fro m gravelly sandy loam to loam and grade to gravelly sand or sandy gravel below about 20 cm . The surfaces are moderately stony and a cemented layer is present below about 30 cm . Soil Moisture Characteristics : Coghlan soils are imperfectly drained . They are rapidly pervious and hav e slow surface runoff and low water holding capacity . The soils are subject to seepage accumulation from higher , adjacent areas and a fluctuating, perched watertable is present during periods of high precipitation . General Soil Description : Coghlan soils have a dark gray to grayish-brown, friable, loamy, cultivate d surface about 15 cm thick which is underlain by 5 to 15 cm of light gray, leached, sandy material containing a few reddish mottles . This, in turn, is underlain by about 50 cm of yellowish-brown or reddish-brown, hard , strongly cemented, gravelly material which grades to loose, gravelly sand or gravel below about 80 cm . Soi l reaction ranges from very strongly acid in the surface to medium acid in the subsoil . Soil classification is Gleyed Ortstein Humo-Ferric Podzol. Commonly Associated Soils : Defehr, Lehman, Columbia, Abbotsford and Lynden soils are usuall y closely associated with Coghlan soils . None, however, have cemented subsurface layers . Defehr and Lynden soils differ also by being sandy rather than gravelly in subsoil texture . Lehman soils are poorly drained whil e Abbotsford soils have silty surface and subsurface layers and are well drained . Vegetation : Most areas of Coghlan soils are cleared and cultivated or used for urban purposes . Uncleare d areas support a variable forest of western red cedar, western hemlock, red alder, willow, birch, black cottonwoo d and vine maple . Rooting depth is moderately restricted below about 40 cm by cemented soil layers . General Land Use Comments : (1) Coghlan soils are limited for agriculture by low fertility and low wate r holding capacity ; these can be improved by adequate fertilization and irrigation . The fluctuating watertables , particularly present during high rainfall periods, are harmful to perennial crops and some watertable control i s beneficial . (2) Coghlan soils are moderately to poorly suited for urban and related development . High periodic watertables make basement and other excavations difficult to excavate during portions of the year and they ar e likely to contain water for varying periods . The operation of septic tanks is impaired during high watertabl e periods and incomplete filtration by the coarse-textured subsoils may potentially contaminate groundwater . (3 ) Coghlan soils seem moderately suited for forest production . Estimated yearly growth of western red cedar is 7 t o 9 m 3 of wood/ha . 56
COLUMBIA SOILS Location and Extent : Columbia soils occupy substantial areas on the uplands of the Lower Fraser Valley . The largest areas are in the Columbia Valley south of Cultus Lake . in the vicinities of Peardonville and Hopington , - South of Langley and in Glen Valley. There are about 3330 ha of pure map units and 2370 ha of soil complexe s dominated by Columbia soils . The complexes are mostly with Abbotsford . Lehman . Defehr and Peardonville Soils . Topography and Elevation : The topography of Columbia soils is usually level to gently undulating w,tr i _ f slope gradients below 5 percent . Scattered areas are strongly sloping or strongly rolling with slopes to 2 0 -Lori percent and, along terrace scarps, slopes may rise to over 60 percent . The soils mainly he between 30 and 10 0 m above sea level but range to 200 m above sea level in the Columbia Valley . Plate 16 Columbia soil profile (Orthic Humo-Ferric Podzol). These soils have - - developed in gravelly glaclofluvial deposits . Sometimes a thin layer (less than 1 5 , cm thick) of silty eolian material is mixed into the surface Parent Material and Texture : Columbia soils have developed from deep. coarse-textured . stratifie d glaclofluvial deposits, usually with a thin (less than 20 cm thick), silty . eolian veneer mixed into or on the surface . Surface textures range from loam to gravelly loamy sand but sandy loam or gravelly sandy loam are mos t common . Subsurface and subsoil textures are gravel or gravelly sand and contain some sand lenses . Stones and cobbles are common throughout . 5 7 1
- Page 21 and 22: during the growing season (May to S
- Page 23 and 24: Plate 3 Dyke along the Fraser River
- Page 25 and 26: SURFICIAL GEOLOGIC DEPOSITS Several
- Page 27 and 28: ---------------- TABLE 2 The relati
- Page 29 and 30: CHAPTER TWO SOIL CLASSIFICATION AND
- Page 31 and 32: CHAPTER THREE DESCRIPTION OF THE SO
- Page 33 and 34: UPLANDS STREA M Figure 6. A schemat
- Page 35 and 36: Description of the Soils
- Page 37 and 38: n Plate 5 Abbotsford soil profile (
- Page 39 and 40: - _ I Plate 6 Landscape typical of
- Page 41 and 42: General Soil Description : Albion s
- Page 43 and 44: ANNACIS SOILS (AS) Location and Ext
- Page 45 and 46: ARNOLD SOILS . (AR) Location and Ex
- Page 47 and 48: BATES SOILS (BT) Location and Exten
- Page 49 and 50: BEHARREL SOILS . (BL) Location and
- Page 51 and 52: BERRY SOILS (BR) Location and Exten
- Page 53 and 54: BLANEY SOILS . (BE) Location and Ex
- Page 55 and 56: BONSON SOILS (BN) Location and Exte
- Page 57 and 58: ' - -_) - r or - ' _ ti _ L , -~ s,
- Page 59 and 60: BUCKERFIELD SOILS (BK) Location and
- Page 61 and 62: Plate 13 Buntzen soil profiie -. -H
- Page 63 and 64: CALKINS SOILS (CN) Location and Ext
- Page 65 and 66: CAPILANO SOILS . (CP) Location and
- Page 67 and 68: CASCADE SOILS . (CC) Location and E
- Page 69 and 70: CHEHALIS SOILS (CS) Location and Ex
- Page 71: Plate 14 Cloverdale soil pro/0e fHu
- Page 75 and 76: COQUITLAM SOILS . (CO) Location and
- Page 77 and 78: subsurface layers to extremely acid
- Page 79 and 80: DEAS SOILS (DS) Location and Extent
- Page 81 and 82: DELTA SOILS (DT) Location and Exten
- Page 83 and 84: Plate 20 Dennett soil profile (Typi
- Page 85 and 86: DEWDNEY SOILS (DW) Location and Ext
- Page 87 and 88: DURIEU SOILS (DU) Location and Exte
- Page 89 and 90: ELK SOILS (EK) Location and Extent
- Page 91 and 92: EMBREE SOILS : (EM) Location and Ex
- Page 93 and 94: ERROCK SOILS (ER) Location and Exte
- Page 95 and 96: FADDEN SOILS (FD) Location and Exte
- Page 97 and 98: FELLOWS SOILS . (FS) Location and E
- Page 99 and 100: GLEN VALLEY SOIL S Location and Ext
- Page 101 and 102: GOLDEN EARS SOILS . (GE) t . Locati
- Page 103 and 104: GOODY SOILS (GY) Location and Exten
- Page 105 and 106: GRIGG SOILS (GG ) Location and Exte
- Page 107 and 108: GUICHON SOILS (GU) Location and Ext
- Page 109 and 110: HAMMOND SOILS . (HA) Location and E
- Page 111 and 112: HARRISON SOILS . (HR) Location and
- Page 113 and 114: HAZELWOOD SOILS (HD) Location and E
- Page 115 and 116: HERON SOILS (HN ) Location and Exte
- Page 117 and 118: HOLLYBURN SOILS (HB) Location and E
- Page 119 and 120: HOPEDALE SOILS (HP) Location and Ex
- Page 121 and 122: JUDSON SOILS (JN) Location and Exte
COLUMBIA SOILS<br />
Location <strong>and</strong> Extent : Columbia soils occupy substantial areas on <strong>the</strong> upl<strong>and</strong>s <strong>of</strong> <strong>the</strong> Lower Fraser Valley .<br />
The largest areas are in <strong>the</strong> Columbia Valley south <strong>of</strong> Cultus Lake . in <strong>the</strong> vicinities <strong>of</strong> Peardonville <strong>and</strong> Hopington ,<br />
- South <strong>of</strong> Langley <strong>and</strong> in Glen Valley. There are about 3330 ha <strong>of</strong> pure map units <strong>and</strong> 2370 ha <strong>of</strong> soil complexe s<br />
dominated by Columbia soils . The complexes are mostly with Abbotsford . Lehman . Defehr <strong>and</strong> Peardonville<br />
<strong>Soils</strong> .<br />
Topography <strong>and</strong> Elevation :<br />
The topography <strong>of</strong> Columbia soils is usually level to gently undulating w,tr i<br />
_ f slope gradients below 5 percent . Scattered areas are strongly sloping or strongly rolling with slopes to 2 0<br />
-Lori percent <strong>and</strong>, along terrace scarps, slopes may rise to over 60 percent . The soils mainly he between 30 <strong>and</strong> 10 0<br />
m above sea level but range to 200 m above sea level in <strong>the</strong> Columbia Valley .<br />
Plate 16 Columbia soil pr<strong>of</strong>ile (Orthic Humo-Ferric Podzol). These soils have<br />
- - developed in gravelly glacl<strong>of</strong>luvial deposits . Sometimes a thin layer (less than 1 5<br />
,<br />
cm thick) <strong>of</strong> silty eolian material is mixed into <strong>the</strong> surface<br />
Parent Material <strong>and</strong> Texture :<br />
Columbia soils have developed from deep. coarse-textured . stratifie d<br />
glacl<strong>of</strong>luvial deposits, usually with a thin (less than 20 cm thick), silty . eolian veneer mixed into or on <strong>the</strong> surface .<br />
Surface textures range from loam to gravelly loamy s<strong>and</strong> but s<strong>and</strong>y loam or gravelly s<strong>and</strong>y loam are mos t<br />
common . Subsurface <strong>and</strong> subsoil textures are gravel or gravelly s<strong>and</strong> <strong>and</strong> contain some s<strong>and</strong> lenses . Stones<br />
<strong>and</strong> cobbles are common throughout .<br />
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1