Official Series Description


Lab Data Summary

Aggregate lab data for the COLBY soil series. This aggregation is based on all pedons with a current taxon name of COLBY, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to COLBY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
67A40A3432S1950WY015002Colby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0283318,-104.2477798
67A40A3433S1950WY015003Colby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0125008,-104.2186127
67B40A3856S1960CO099001Colby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1580544,-102.3949966
67B40A3857S1960CO099002Colby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0888901,-102.230278
67B40A3858S1960CO099005Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7677765,-102.7019424
67B40A3859S1960CO099006Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7918278,-102.6524889
6940A3854S1958CO099002Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0258331,-102.7038879
6940A3855S1958CO099003Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0125008,-102.6844406
7282P017481NE029001Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4952774,-101.4716644
7289P014088NE029001Colby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4130554,-101.6269455
7240A1779S1957KS075001COLBY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0369453,-101.8708344
7240A1780S1957KS075002COLBY6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0730553,-101.9897232
7201P0087S2001KS071001Colby7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5535545,-101.7940521
7210N1325S2010KS075003Colby8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0201944,-101.7611389

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COLBY soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the COLBY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the COLBY series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the COLBY series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with COLBY share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the COLBY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the COLBY series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with COLBY, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CO-2011-05-27-14 | Prowers County - 1966

    Main soils and underlying materials in soil association 1 (Soil Survey of Prowers County, Colorado; 1966).

  2. CO-2011-05-27-15 | Prowers County - 1966

    Main soils and underlying materials in soil association 2 (Soil Survey of Prowers County, Colorado; 1966).

  3. CO-2011-05-27-19 | Prowers County - 1966

    Cross sections showing relationships of the soils to the landscape and to the underlying geologic formations in Prowers County. The upper cross section shows relationships in the western part of the county, and the lower shows those in the eastern part of the county (Soil Survey of Prowers County, Colorado; 1966).

  4. KS-2012-01-20-19 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Colby-Razor association (Soil Survey of Cheyenne County, Kansas; 1989).

  5. KS-2012-01-20-20 | Cheyenne County - June 1989

    Typical pattern of soils and parent material in the Colby-Ulysses-Keith association (Soil Survey of Cheyenne County, Kansas; 1989).

  6. KS-2012-01-23-02 | Finney County - November 1965

    Typical cross section of the valley of the Arkansas River (Soil Survey of Finney County, Kansas; 1965).

  7. KS-2012-01-23-12 | Grant County - December 1969

    Relationships of soils in association 1. Included is a small part of association 3 (Soil Survey of Grant County, Kansas; 1969).

  8. KS-2012-01-23-13 | Grant County - December 1969

    Relationships of soils in association 2 (Soil Survey of Grant County, Kansas; 1969).

  9. KS-2012-01-23-14 | Grant County - December 1969

    Relationships of soils in association 3 (Soil Survey of Grant County, Kansas; 1969).

  10. KS-2012-01-23-15 | Grant County - December 1969

    Relationships of soils in association 4 (Soil Survey of Grant County, Kansas; 1969).

  11. KS-2012-01-23-16 | Grant County - December 1969

    Relationships of soils in association 5 (Soil Survey of Grant County, Kansas; 1969).

  12. KS-2012-01-23-23 | Greeley County - December 1961

    Approximate geologic cross section (north and south) through central Greeley County (Soil Survey of Greeley County, Kansas; 1961).

  13. KS-2012-01-23-24 | Greeley County - December 1961

    Cross section of the valley of White Woman Creek in Greeley County (Soil Survey of Greeley County, Kansas; 1961).

  14. KS-2012-01-23-25 | Hamilton County - November 1961

    Geologic profile extending in a north-south direction through the central part of Hamilton County (Soil Survey of Hamilton County, Kansas; 1961).

  15. KS-2012-01-23-32 | Haskell County - October 1968

    Landscape showing soils of the Richfield-Spearville-Ulysses association in the southeastern part of the county (Soil Survey of Haskell County, Kansas; 1968).

  16. KS-2012-01-23-33 | Haskell County - October 1968

    Typical topographic relation of three soil associations: Otero-Colby-Likes association in the southwestern corner; Richfield-Ulysses association to the north; and Satanta-Manter association to the east (Soil Survey of Haskell County, Kansas; 1968).

  17. KS-2012-01-23-43 | Kearny County - November 1963

    Cross section of the county showing the relationship of some of the soils of the uplands to the parent material and topography (Soil Survey of Kearny County, Kansas; 1963).

  18. KS-2012-01-23-44 | Kearny County - November 1963

    An approximate geologic profile of Kearny County, extending in a north-south direction across the county near Hartland (Soil Survey of Kearny County, Kansas; 1963).

  19. KS-2012-01-24-20 | Morton County - December 1963

    Geologic cross section of the western part of the county. (Based on plate 6 of "Geology and Ground-Water Resources of Morton Co., Kans." (6).) (Soil Survey of Morton County, Kansas; 1963.)

  20. KS-2012-01-25-33 | Scott County - December 1965

    Typical cross section of part of the valley of Ladder (Beaver) Creek (Soil Survey of Scott County, Kansas; 1965).

  21. KS-2012-01-25-34 | Scott County - December 1965

    An approximate geologic profile extending in an east-west direction across Scott County near Shallow Water (Soil Survey of Scott County, Kansas; 1965).

  22. KS-2012-01-26-01 | Sheridan County - March 1984

    Typical pattern of soils in the Keith-Ulysses-Kuma association (Soil Survey of Sheridan County, Kansas; 1984).

  23. KS-2012-01-26-02 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Colby-Keith association (Soil Survey of Sheridan County, Kansas; 1984).

  24. KS-2012-01-26-03 | Sheridan County - March 1984

    Typical pattern of soils in the Ulysses-Pendend-Colby association (Soil Survey of Sheridan County, Kansas; 1984).

  25. KS-2012-01-26-06 | Sherman County - March 1973

    Typical pattern of major soils in soil association 2 (Soil Survey of Sherman County, Kansas; 1973).

  26. KS-2012-01-26-08 | Sherman County - March 1973

    Major range sites in Sherman County (Soil Survey of Sherman County, Kansas; 1973).

  27. KS-2012-01-26-09 | Sherman County - March 1973

    A cross section of Sherman County soils extending through the center of the county (Soil Survey of Sherman County, Kansas; 1973).

  28. KS-2012-01-26-11 | Stanton County - December 1961

    Diagram of the Manter-Dalhart-Ulysses soil association in the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  29. KS-2012-01-26-12 | Stanton County - December 1961

    Pattern of soils of the upland in northeastern Stanton County and cross section of part of the valley of Bear Creek (Soil Survey of Stanton County, Kansas; 1961).

  30. KS-2012-01-26-24 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Ulysses-Colby association (Soil Survey of Wallace County, Kansas; 1986).

  31. KS-2012-01-26-25 | Wallace County - March 1986

    Typical pattern of soils and underlying material in the Colby-Kim-Midway association (Soil Survey of Wallace County, Kansas; 1986).

  32. KS-2012-01-26-30 | Wichita County - November 1965

    Cross section of association 2 along White Woman Creek (Soil Survey of Wichita County, Kansas; 1965).

  33. KS-2012-01-26-31 | Wichita County - November 1965

    Relationship of soils to the landscape and to the common parent materials of Wichita County (Soil Survey of Wichita County, Kansas; 1965).

  34. NE-2012-02-10-09 | Chase County - November 1982

    Typical landscape pattern of the soils and underlying material in the Colby association (Soil Survey of Chase County, Nebraska; November 1982).

  35. NE-2012-02-10-25 | Dundy County - February 1963

    Typical area in the Anselmo-Keith soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  36. NE-2012-02-10-26 | Dundy County - February 1963

    Typical area in the Colby soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  37. NE-2012-02-10-27 | Dundy County - February 1963

    Colby soil association merging with the Bridgeport-Havre soil association (Soil Survey of Dundy County, Nebraska; February 1963).

  38. NE-2012-02-10-29 | Dundy County - February 1963

    The Bridgeport-Havre soil association, on the right, merges with the Sandy alluvial land-Las association (Soil Survey of Dundy County, Nebraska; February 1963).

  39. NE-2012-02-13-19 | Hall County - January 1962

    Topography, soils, and parent materials, in the southeastern part of Hall County (Soil Survey of Hall County, Nebraska; January 1962).

  40. NE-2012-02-13-24 | Hayes County - August 1982

    The relationship of soils to topography and parent material in the Colby-Ulysses association (Soil Survey of Hayes County, Nebraska; August 1982).

  41. NE-2012-02-13-26 | Hayes County - August 1982

    The relationship of soils to topography and parent material in the Bridget-McCook-Gibbon association (Soil Survey of Hayes County, Nebraska; August 1982).

  42. NE-2012-02-13-74 | Red Willow County - April 1967

    Typical pattern of soils in the Holdrege-Keith association (Soil Survey of Red Willow County, Nebraska; April 1967).

  43. NE-2012-02-13-75 | Red Willow County - April 1967

    Typical pattern of soils in the Hord, terrace-McCook-Bridgeport association (Soil Survey of Red Willow County, Nebraska; April 1967).

  44. SD-2012-03-15-29 | Fall River County - April 1982

    Pattern of soils in the Norka association (Soil Survey of Fall River County, SD; 1982).

  45. SD-2012-03-15-55 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Weta-Cactusflat and Blackpipe-Wortman associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

  46. SD-2012-03-15-91 | Shannon County - April 1971

    Representative pattern of soils in association 1 (Soil Survey of Shannon County, SD; 1971).

  47. SD-2012-03-15-92 | Shannon County - April 1971

    Representative pattern of soils in association 2 (Soil Survey of Shannon County, SD; 1971).

  48. SD-2012-03-15-93 | Shannon County - April 1971

    Representative pattern of soils in association 4 (Soil Survey of Shannon County, SD; 1971).

Map Units

Map units containing COLBY as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Adena-Colby association, gently slopingAcC604319403734vgco00119681:20000
Adena-Colby association, moderately slopingAcD322399403834vhco00119681:20000
Colby loam, 6 to 15 percent slopesCgE14064940492w5d6co00119681:20000
Adena-Colby silt loams, 1 to 5 percent slopesAdC307319410534xnco00519711:20000
Fondis-Colby silt loams, 3 to 5 percent slopesFoC91739413434ylco00519711:20000
Adena-Colby silt loams, 5 to 9 percent slopesAdD47269410634xpco00519711:20000
Colby silt loam, 1 to 5 percent slopesCoC37269412734ycco00519711:20000
Colby silt loam, 6 to 15 percent slopesCoE2641941282w5d4co00519711:20000
Adena-Colby fine sandy loams, 1 to 5 percent slopesAcC18159410334xlco00519711:20000
Colby and Adena soils, 1 to 9 percent slopes, erodedCyD218159412934yfco00519711:20000
Adena-Colby fine sandy loams, 5 to 9 percent slopesAcD11349410434xmco00519711:20000
Colby silt loam, 1 to 3 percent slopesCoB4445941833505co00919661:20000
Colby silt loam, 0 to 3 percent slopesCbB389129920742v1qyco00919661:20000
Colby silt loam, terrace, 0 to 2 percent slopesCtA1833941853507co00919661:20000
Colby silt loam, terrace, 0 to 2 percent slopesCtB155730790472t52tco00919661:20000
Colby silt loam, 3 to 9 percent slopesCoD812941843506co00919661:20000
Colby silt loam, 0 to 1 percent slopesCoA669941823504co00919661:20000
Colby silt loam, 3 to 9 percent slopesCoC56330404812v1r2co00919661:20000
Colby silt loam, 0 to 3 percent slopesCyB183629922002v1qyco01119651:15840
Satanta-Colby complex, 3 to 5 percent slopes393992794328354vco01719851:24000
Colby silt loam, 1 to 4 percent slopes, eroded6622900943512t52xco01719851:24000
Colby-Satanta complex, 5 to 12 percent slopes101263594297353vco01719851:24000
Colby silt loam, 3 to 9 percent slopes65645529923992v1r2co01719851:24000
Colby silt loam, 1 to 4 percent slopes, eroded855233078956355lco01719851:24000
Colby silt loam, 4 to 12 percent slopes9319394352355mco01719851:24000
Colby silt loam, 0 to 3 percent slopes572409929922012v1qyco06119771:24000
Colby silt loam, 1 to 3 percent slopes10166382942837357rco06119771:24000
Colby silt loam, 3 to 9 percent slopes11570394419357sco06119771:24000
Colby silt loam, 3 to 9 percent slopes58367929922032v1r2co06119771:24000
Norka-Colby silt loams, 5 to 15 percent slopes56588629684937s5co06319961:24000
Norka-Colby silt loams, 3 to 5 percent slopes5555000968502w5ddco06319961:24000
Colby silt loam, 3 to 5 percent slopes1630644283770137qvco06319961:24000
Colby silt loam, 6 to 15 percent slopes173008428376942w5d4co06319961:24000
Norka-Colby-Weld silt loams, 3 to 5 percent slopes5725273968592w5dvco06319961:24000
Norka-Colby silt loams, 0 to 3 percent slopes54194669685237s8co06319961:24000
Colby silt loam, 0 to 3 percent slopes1001414029922072v1qyco06319961:24000
Colby silt loam, 1 to 3 percent slopes155672283769337qdco06319961:24000
Colby silty clay loam, dry, 1 to 3 percent slopes1935689680537qrco06319961:24000
Colby-Aridic Ustorthents complex, 9 to 25 percent slopes, gullied2015869681237qzco06319961:24000
Satanta-Colby complex, 3 to 5 percent slopes77759687537t0co06319961:24000
Colby-Weld silt loams, 1 to 5 percent slopes122495691052032t52zco07320011:24000
Colby silt loam, 3 to 9 percent slopes121224661052022v1r2co07320011:24000
Colby silt loam, 0 to 3 percent slopes12043781052012v1qyco07320011:24000
Wagonwheel-Colby-Stoneham association, 5 to 12 percent slopes111792594473359jco07519741:24000
Colby loam, 6 to 20 percent slopes193809944982w5d8co07519741:24000
Colby-Adena loams, 3 to 5 percent slopesCnC118511104153pwsco08719651:24000
Colby-Adena loams, 5 to 9 percent slopesCnD109841104163pwtco08719651:24000
Colby-Adena loams, 1 to 3 percent slopesCnB47251104143pwrco08719651:24000
Colby loam 5 to 9 percent slopesCbD44031104083pwkco08719651:24000
Colby loam, 3 to 5 percent slopesCbC32321104073pwjco08719651:24000
Colby loam, 9 to 30 percent slopes, erodedCbE213411104102w5dbco08719651:24000
Colby loam, 1 to 3 percent slopesCbB11731104063pwhco08719651:24000
Colby sandy loam, 3 to 5 percent slopesCdC5981104123pwpco08719651:24000
Colby loam, 6 to 15 percent slopesCgE45029330552w5d6co08719651:24000
Colby sandy loam, 1 to 3 percent slopesCdB2521104113pwnco08719651:24000
Colby sandy loam, 5 to 9 percent slopesCdD2291104133pwqco08719651:24000
Colby silt loam, 0 to 3 percent slopesCbB4900929922062v1qyco09919631:15840
Colby silt loam, 0 to 3 percent slopesCmAB38064294283635n5co09919631:15840
Colby silt loam, 3 to 5 percent slopesCbC996030790552v1r0co09919631:15840
Colby fine sandy loam, 0 to 3 percent slopesCyB431130790522v1qzco09919631:15840
Colby fine sandy loam, 0 to 3 percent slopesCfAB32579479935n1co09919631:15840
Colby silt loam, terrace, 0 to 2 percent slopesCtB248530790532t52tco09919631:15840
Colby silt loam, 3 to 5 percent slopesCmC21459480535n7co09919631:15840
Colby fine sandy loam, 3 to 5 percent slopesCyC120030790832v1r1co09919631:15840
Colby silt loam, sand substratum, 0 to 1 percent slopesCsA5249480735n9co09919631:15840
Colby silt loam, 0 to 1 percent slopesCmA472283769935n4co09919631:15840
Colby fine sandy loam, terrace, 0 to 2 percent slopesCyA35930790542t52vco09919631:15840
Colby silt loam, clay substratum, 0 to 1 percent slopesCoA3049480635n8co09919631:15840
Colby fine sandy loam, 3 to 5 percent slopesCfC2239480135n3co09919631:15840
Colby fine sandy loam, 0 to 1 percent slopesCfA1679479835n0co09919631:15840
Colby silt loam, 1 to 3 percent slopesCmB519480435n6co09919631:15840
Colby fine sandy loam, 1 to 3 percent slopesCfB319480035n2co09919631:15840
Colby-Ulysses silt loams, 3 to 5 percent slopesCuC10329493135s9co11519691:15840
Colby-Ulysses silt loams, 5 to 9 percent slopesCuD2389493235sbco11519691:15840
Colby-Norka loams, 5 to 9 percent slopes171138269497635trco12119821:24000
Norka-Colby loams, 3 to 5 percent slopes4773038950092w5dcco12119821:24000
Colby loam, 6 to 15 percent slopes8636379949752w5d6co12119821:24000
Norka-Colby very fine sandy loams, 3 to 9 percent slopes4650079500835vsco12119821:24000
Colby-Ustic Torriorthents complex, 9 to 30 percent slopes1845659497735tsco12119821:24000
Wagonwheel-Colby-Stoneham complex, 5 to 12 percent slopes828819505035x4co12119821:24000
Colby silt loam, 6 to 15 percent slopes1186713950532w5d4co12519761:24000
Colby silt loam, 3 to 6 percent slopes1041715950522v9ftco12519761:24000
Colby-Torriorthents complex, gullied, 15 to 25 percent slopes12373789505435x8co12519761:24000
Wiley-Colby complex, 1 to 3 percent slopes8226492952663643co61819761:24000
Colby-Adena loams, 3 to 9 percent slopes182149995195361tco61819761:24000
Colby loam, 1 to 3 percent slopes151855795192361qco61819761:24000
Colby loam, 0 to 1 percent slopes14798095191361pco61819761:24000
Wiley-Colby complex, 3 to 5 percent slopes837529952673644co61819761:24000
Colby loam, 3 to 5 percent slopes16689895193361rco61819761:24000
Colby loam, 5 to 9 percent slopes17371095194361sco61819761:24000
Wiley-Colby complex, 0 to 1 percent slopes81767952653642co61819761:24000
Wiley and Colby soils, 5 to 18 percent slopesWcE374895351366vco62419631:20000
Wiley and Colby soils, 3 to 5 percent slopesWcC195895350366tco62419631:20000
Colby silty clay loam, 1 to 3 percent slopesCoB4230497562jprdco64319751:20000
Colby silty clay loam, 3 to 5 percent slopesCoC2191497563jprfco64319751:20000
Weld-Colby complex, 0 to 3 percent slopesWoB2144497617jpt5co64319751:20000
Colby silty clay loam, 5 to 9 percent slopesCoD991497564jprgco64319751:20000
Colby-Gaynor associationCt985497566jprjco64319751:20000
Colby silty clay loam, wet, 0 to 3 percent slopesCsB601497565jprhco64319751:20000
Weld-Colby complex, 3 to 5 percent slopesWoC574497618jpt6co64319751:20000
Colby silty clay loam, wet, 0 to 3 percent slopesCsB223210306jprhco64419801:24000
Colby silt loam, 6 to 15 percent slopes158012251511495612w5d4ks02319871:24000
Colby silt loam, 3 to 6 percent slopes15794980511495602v9ftks02319871:24000
Colby silt loam, 20 to 50 percent slopes15822440611495632v9g2ks02319871:24000
Colby silt loam, 10 to 25 percent slopes1581118711495622v9g1ks02319871:24000
Colby silt loam, 10 to 25 percent slopes1581593711505692v9g1ks03919851:24000
Colby silt loam, 6 to 15 percent slopes158098711505702w5d4ks03919851:24000
Colby silt loam, 6 to 15 percent slopes158078111506632w5d4ks06319741:24000
Colby loam, 5 to 12 percent slopes1572376813806532w5d9ks06719651:24000
Colby silt loam, 3 to 6 percent slopes157913213806542v9ftks06719651:24000
Colby silt loam, 1 to 3 percent slopes15781544611518282v9fsks07119591:24000
Colby silt loam, 6 to 15 percent slopes1580758311518302w5d4ks07119591:24000
Colby silt loam, 3 to 6 percent slopes1579747211518292v9ftks07119591:24000
Colby silt loam, 1 to 3 percent slopes157814101311522132v9fsks07519591:24000
Colby silt loam, 6 to 15 percent slopes15803300511522152w5d4ks07519591:24000
Colby silt loam, 3 to 6 percent slopes15793076411522142v9ftks07519591:24000
Colby silt loam, 0 to 1 percent slopes15777213115221217nz4ks07519591:24000
Colby loam, 5 to 12 percent slopes1572123113806152w5d9ks08119651:24000
Colby silt loam, 1 to 3 percent slopes15781647611522582v9fsks09319611:24000
Colby silt loam, 6 to 15 percent slopes1580904411522602w5d4ks09319611:24000
Colby silt loam, 3 to 6 percent slopes1579898911522592v9ftks09319611:24000
Colby silt loam, 6 to 15 percent slopes158050411520142w5d4ks10119661:24000
Colby silt loam, 6 to 15 percent slopes15807382311505112w5d4ks10919621:24000
Colby silt loam, 3 to 6 percent slopes1579182711505102v9ftks10919621:24000
Colby silt loam, 10 to 25 percent slopes15811580437729752v9g1ks15319791:24000
Colby silt loam, 6 to 15 percent slopes1580282277729792w5d4ks15319791:24000
Colby silt loam, 20 to 50 percent slopes158242307729762v9g2ks15319791:24000
Colby silt loam, 3 to 6 percent slopes15796137729782v9ftks15319791:24000
Colby silt loam, 6 to 15 percent slopes15801298711519742w5d4ks17119631:24000
Colby loam, 5 to 12 percent slopes1572626313826232w5d9ks17519631:24000
Colby loam, 3 to 5 percent slopes1571176613826221hdqqks17519631:24000
Colby silt loam, 6 to 15 percent slopes15805106411499912w5d4ks17919821:24000
Colby silt loam, 6 to 15 percent slopes15806032211496142w5d4ks18119671:24000
Colby silt loam, 3 to 6 percent slopes1579227911496132v9ftks18119671:24000
Colby silt loam, 1 to 3 percent slopes157814911496122v9fsks18119671:24000
Colby silt loam, 1 to 3 percent slopes1578733613825552v9fsks18719591:24000
Colby silt loam, 6 to 15 percent slopes1580283913825572w5d4ks18719591:24000
Colby silt loam, 3 to 6 percent slopes1579182213825562v9ftks18719591:24000
Colby loam, 5 to 12 percent slopes157223713825542w5d9ks18719591:24000
Colby silt loam, 6 to 15 percent slopes15803894411504562w5d4ks19319781:24000
Colby silt loam, 3 to 6 percent slopes15795127111501902v9ftks19919841:24000
Colby silt loam, 6 to 15 percent slopes15803832711501912w5d4ks19919841:24000
Colby silt loam, 6 to 15 percent slopes15801110711519382w5d4ks20319631:24000
Colby silt loam, 1 to 3 percent slopes15789411519362v9fsks20319631:24000
Colby silt loam, 3 to 6 percent slopes15791011519372v9ftks20319631:24000
Colby association, hillyCY11936345901cly3mt60719701:24000
Colby silty clay loam, 4 to 8 percent slopesCp10777345907cly9mt60719701:24000
Colby-Midway complex, 8 to 15 percent slopesCW9400345899cly1mt60719701:24000
Colby silt loam, 4 to 8 percent slopesCm8708345904cly6mt60719701:24000
Colby silty clay loam, 8 to 15 percent slopesCr7007345908clybmt60719701:24000
Colby-Keiser silty clay loams, 4 to 8 percent slopesCv6209345911clyfmt60719701:24000
Colby-Clapper silt loams, rollingCU6008345898cly0mt60719701:24000
Colby association, rollingCX3918345900cly2mt60719701:24000
Keiser-Colby complex, gently undulatingKf3419346022cm20mt60719701:24000
Colby silt loam, 8 to 15 percent slopesCn2956345905cly7mt60719701:24000
Colby silty clay loam, 1 to 4 percent slopesCo700345906cly8mt60719701:24000
Colby-Beauvais silt loams, undulatingCs177345909clycmt60719701:24000
Colby silt loam, 4 to 8 percent slopesCg8130347047cn42mt61119711:24000
Colby silt loam, 8 to 15 percent slopesCh2249347048cn43mt61119711:24000
Colby silt loam, 2 to 4 percent slopesCf1622347046cn41mt61119711:24000
Keith-Colby silt loams, 9 to 12 percent slopesKhD34613527472tvtcsd00720041:20000
Lakoa-Colby, cool silt loams, 9 to 50 percent slopesP192F459126688772rvddsd01919701:24000
Colby-Norka silt loams, 6 to 15 percent slopesCnD42863550982tvtqsd04719801:24000
Colby-Norka silt loams, cool, 6 to 15 percent slopesP080D2229273312430wn1sd04719801:24000
Colby-Norka silt loams, 6 to 15 percent slopesCmC497725808862tvtqsd60620111:24000
Colby silt loam, 9 to 40 percent slopesClF27222580885cygmsd60620111:24000
Thirtynine-Colby, cool silt loams, 6 to 9 percent slopesU365C4825829192pf5ssd60620111:24000
Colby-Norka silt loams, cool, 6 to 15 percent slopesP080D29276813430wn1sd60720111:24000
Keith-Colby silt loams, 12 to 25 percent slopesKhE782029255312tvtdsd61019651:20000
Keith-Colby silt loams, 9 to 12 percent slopesKhD779829254942tvtcsd61019651:20000
Norka-Colby silt loams, 6 to 15 percent slopesNpD25752582644cy3bsd61120111:24000
Colby silt loam, 6 to 15 percent slopesCoD18042581010cy27sd61120111:24000
Thirtynine-Colby, cool silt loams, 9 to 15 percent slopesU365D9925828772pf5rsd61120111:24000
Thirtynine-Colby, cool silt loams, 6 to 9 percent slopesU365C1125828782pf5ssd61120111:24000
Thirtynine-Colby, cool silt loams, 6 to 9 percent slopesU365C65624853252pf5ssd61220111:20000
Thirtynine-Colby, cool silt loams, 9 to 15 percent slopesU365D45824853242pf5rsd61220111:20000
Keith-Colby silt loams, 9 to 12 percent slopesKhD4056725827082tvtcsd61320111:24000
Keith-Colby silt loams, 12 to 25 percent slopesKhE2699025827092tvtdsd61320111:24000
Thirtynine-Colby, cool silt loams, 9 to 15 percent slopesU365D161825828342pf5rsd61320111:24000
Ulysses-Colby complex, sand substratum, 3 to 9 percent slopesUcC10962582743cv4tsd61320111:24000
Thirtynine-Colby, cool silt loams, 6 to 9 percent slopesU365C14725828352pf5ssd61320111:24000
Lakoa-Colby, cool silt loams, 9 to 50 percent slopesP192F92427681762rvddwy01119781:24000
Norka and Colby loams, 0 to 6 percent slopesNrB64331047253hz7wy61519651:20000
Colby loam, 3 to 10 percent slopesCoC48261046763hxnwy61519651:20000
Colby-Tassel complex, 2 to 8 percent slopesCtC38901046783hxqwy61519651:20000
Colby loam, 10 to 20 percent slopesCoD12291046773hxpwy61519651:20000

Map of Series Extent

Approximate geographic distribution of the COLBY soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .