Official Series Description


Lab Data Summary

Aggregate lab data for the CANFIELD soil series. This aggregation is based on all pedons with a current taxon name of CANFIELD, 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 CANFIELD 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
13963PA0850061963PA085006Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1005556,-80.0919444
13966PA1210071966PA121007Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4016667,-79.9966667
13966PA1210081966PA121008Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3966667,-79.9780556
14765PA0890091965PA089009Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9688889,-75.1755556
14765PA0890101965PA089010Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9230556,-75.2622222
n/aWN-S011953-OH169-S01Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-0331954-OH007-033Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-0441954-OH007-044Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-0451954-OH007-045Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-0461954-OH007-046Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0031954-OH099-003Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0041954-OH099-004Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-S031954-OH169-S03Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-S081954-OH169-S08Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s141955-OH169-S14Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-S151955-OH169-S15Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-S161955-OH169-S16Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAB-0811956-OH007-081Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-0121956-OH029-012Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-0221957-OH029-022Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0161957-OH099-016Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTR-0131957-OH155-013Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s171957-OH169-S17Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s181957-OH169-S18Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s201957-OH169-S20Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-0521958-OH029-052Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-0671958-OH029-067Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0231958-OH099-023Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-1071959-OH029-107Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCO-1111959-OH029-111Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s261959-OH169-S26Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s271959-OH169-S27Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s281959-OH169-S28Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s291960-OH169-S29Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s301960-OH169-S30Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAS-0011961-OH005-001Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0261961-OH099-026Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s431961-OH169-S43Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aSK-0041962-OH151-004Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aSK-0051962-OH151-005Canfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s411964-OH169-S41Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-s421964-OH169-S42Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMH-0471965-OH099-047Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aST-0051965-OH153-005Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aRC-0061966-OH139-006Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aRC-0071966-OH139-007Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aST-0251966-OH153-025Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aSK-0301968-OH151-030Canfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPG-0031969-OH133-003Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAS-0261972-OH005-026Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTR-0181974-OH155-018Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTR-0211975-OH155-021Canfield4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CANFIELD 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 CANFIELD 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 CANFIELD 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 CANFIELD 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 CANFIELD 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 CANFIELD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the CANFIELD 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.

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

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

Soil series sharing subgroup-level classification with CANFIELD, 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. OH-2010-09-29-10 | Columbiana County -

    Representative pattern of soils and parent materials in the Canfield-Ravenna soils association (Soil Survey of Columbiana County, Ohio).

  2. OH-2012-02-16-17 | Columbiana County - February 1968

    A schematic drawing showing the relationship of soils on the Wisconsin glacial outwash plain (in the valley to the right) and on the Wisconsin till plain (Soil Survey of Columbiana County, Ohio; February 1968).

  3. PA-2012-03-12-04 | Beaver and Lawrence Counties - April 1982

    Pattern of soils and parent material in Ravenna-Canfield-Frenchtown association (Soil Survey of Beaver and Lawrence Counties, PA; 1982).

  4. PA-2012-03-12-05 | Beaver and Lawrence Counties - April 1982

    Pattern of soils and parent material in Canfield-Ravenna-Loudonville association (Soil Survey of Beaver and Lawrence Counties, PA; 1982).

  5. PA-2012-03-13-63 | Mercer County - April 1971

    Relationship of soils and underlying material in association 1 (Soil Survey of Mercer County, PA; 1971).

  6. PA-2012-03-13-64 | Mercer County - April 1971

    Relationship of soils and underlying material in associations 2 and 3 (Soil Survey of Mercer County, PA; 1971).

  7. PA-2012-03-14-25 | Venango County - December 1975

    Pattern of soils and underlying material in Canfield-Ravenna association (Soil Survey of Venango County, PA; 1975).

Map Units

Map units containing CANFIELD 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
Canfield silt loam, 2 to 6 percent slopesCaB210092881362v03toh00519761:15840
Canfield silt loam, 6 to 12 percent slopesCaC14672881372v040oh00519761:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCaC211072881382v043oh00519761:15840
Canfield silt loam, 6 to 12 percent slopesCcC431902987422v040oh02920051:12000
Canfield silt loam, 2 to 6 percent slopesCcB350442987412v03toh02920051:12000
Canfield silt loam, 12 to 20 percent slopesCcD63142987432v04doh02920051:12000
Urban land-Canfield complex, 2 to 6 percent slopesUtB26922988392v03woh02920051:12000
Canfield silt loam, 20 to 35 percent slopesCcE21502987442v04goh02920051:12000
Urban land-Canfield complex, 6 to 12 percent slopesUtC11132988402v042oh02920051:12000
Canfield silt loam, 2 to 6 percent slopesCdB117622875322v03toh05519791:15840
Canfield silt loam, 6 to 12 percent slopesCdC25702875332v040oh05519791:15840
Canfield silt loam, 2 to 6 percent slopesCdB136502868772v03toh07519891:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC249502868792v043oh07519891:15840
Canfield silt loam, 6 to 12 percent slopesCdC12602868782v040oh07519891:15840
Canfield silt loam, 0 to 2 percent slopesCdA216769962v03qoh07519891:15840
Canfield silt loam, 2 to 6 percent slopesCaB26586135592v03toh08319831:15840
Canfield silt loam, 6 to 12 percent slopesCaC6026135602v040oh08319831:15840
Canfield silt loam, 2 to 6 percent slopesCdB240888167282v03toh09919661:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC238478167302v043oh09919661:15840
Canfield-Urban land complex, 2 to 6 percent slopesCeB20118167312v03voh09919661:15840
Canfield silt loam, 6 to 12 percent slopesCdC9158167292v040oh09919661:15840
Urban land-Canfield complex, 2 to 6 percent slopesUdB27616521992v03woh09919661:15840
Canfield silt loam, 12 to 20 percent slopesCdD5016521822v04doh09919661:15840
Urban land-Canfield complex, 6 to 12 percent slopesUdC3116522002v042oh09919661:15840
Canfield silt loam, 20 to 35 percent slopesCdE1316521832v04goh09919661:15840
Canfield silt loam, 2 to 6 percent slopesCdB89972883152v03toh10319741:15840
Canfield-Urban land complex, 6 to 12 percent slopesCeC7962883182v041oh10319741:15840
Canfield silt loam, 0 to 2 percent slopesCdA7142883142v03qoh10319741:15840
Canfield silt loam, 2 to 6 percent slopes, erodedCdB24782883162v03yoh10319741:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC24592883172v043oh10319741:15840
Canfield silt loam, 2 to 6 percent slopesCaB57411703412v03toh11719861:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCaC29831703432v043oh11719861:15840
Canfield silt loam, 6 to 12 percent slopesCaC6051703422v040oh11719861:15840
Canfield silt loam, 2 to 6 percent slopes, erodedCaB21115932472v03yoh11719861:15840
Canfield silt loam, 2 to 6 percent slopesCdB177282884102v03toh13319731:15840
Canfield-Urban land complex, 2 to 6 percent slopesCfB13372884142v03voh13319731:15840
Canfield silt loam, 6 to 12 percent slopesCdC11572884112v040oh13319731:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC27842884122v043oh13319731:15840
Canfield silt loam, 0 to 2 percent slopesCdA3092884092v03qoh13319731:15840
Canfield-Urban land complex, 6 to 12 percent slopesCfC1862884152v041oh13319731:15840
Canfield silt loam, 2 to 6 percent slopesCdB204731707302v03toh13919711:15840
Canfield silt loam, 6 to 12 percent slopesCdC15671707322v040oh13919711:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC29711707332v043oh13919711:15840
Canfield silt loam, 2 to 6 percent slopes, erodedCdB26921707312v03yoh13919711:15840
Canfield silt loam, 2 to 6 percent slopesCdB409592879562v03toh15119671:15840
Canfield silt loam, 6 to 12 percent slopesCdC100482879572v040oh15119671:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC281122879582v043oh15119671:15840
Canfield-Urban land complex, 2 to 6 percent slopesCeB56692879612v03voh15119671:15840
Canfield-Urban land complex, 6 to 12 percent slopesCeC21052879622v041oh15119671:15840
Canfield silt loam, 0 to 2 percent slopesCdA11922879552v03qoh15119671:15840
Canfield silt loam, 12 to 18 percent slopes, erodedCdD211872879602v04coh15119671:15840
Canfield silt loam, 12 to 18 percent slopesCdD4732879592v04boh15119671:15840
Canfield silt loam, moderately deep, 6 to 12 percent slopesCfC1602879642v04koh15119671:15840
Canfield silt loam, moderately deep, 2 to 6 percent slopesCfB1052879632v04joh15119671:15840
Canfield silt loam, 8 to 15 percent slopesCgC5215954572v044oh15119671:15840
Canfield silt loam, 12 to 20 percent slopesCddD3615955052v04doh15119671:15840
Urban land-Canfield complex, 2 to 6 percent slopesUtB2115955212v03woh15119671:15840
Canfield silt loam, 20 to 35 percent slopesCddE915955062v04goh15119671:15840
Canfield silt loam, 2 to 6 percent slopesCdB184788253042v03toh15319691:20000
Canfield-Urban land complex, 2 to 6 percent slopesCfB105968253082v03voh15319691:20000
Canfield-Urban land complex, 6 to 12 percent slopesCfC29048253092v041oh15319691:20000
Canfield silt loam, 6 to 12 percent slopes, erodedCdC211658253062v043oh15319691:20000
Canfield silt loam, 6 to 12 percent slopesCdC8628253052v040oh15319691:20000
Canfield silt loam, 0 to 2 percent slopesCdA8538253032v03qoh15319691:20000
Canfield silt loam, sandstone substratum, 2 to 6 percent slopesCeB2758253072v04loh15319691:20000
Canfield silt loam, 2 to 6 percent slopesCfB124002870022v03toh15519861:15840
Canfield silt loam, 6 to 12 percent slopesCfC23452870032v040oh15519861:15840
Canfield-Urban land complex, 2 to 6 percent slopesCgB10152870042v03voh15519861:15840
Canfield silt loam, 8 to 15 percent slopesCdC1705362892v044oh15719811:15840
Canfield silt loam, 6 to 12 percent slopesCeC10815894062v040oh15719811:15840
Canfield silt loam, 2 to 6 percent slopesCeB7615894052v03toh15719811:15840
Canfield silt loam, 2 to 6 percent slopesCdB555232871682v03toh16919811:15840
Canfield silt loam, 6 to 12 percent slopes, erodedCdC247792871712v043oh16919811:15840
Canfield silt loam, 0 to 2 percent slopesCdA30352871672v03qoh16919811:15840
Canfield-Urban land complex, 2 to 6 percent slopesCfB20942871722v03voh16919811:15840
Canfield silt loam, 2 to 6 percent slopes, erodedCdB217242871692v03yoh16919811:15840
Canfield silt loam, 6 to 12 percent slopesCdC16492871702v040oh16919811:15840
Canfield silt loam, 12 to 18 percent slopes, erodedCdD2622170242v04coh16919811:15840
Canfield silt loam, sandstone substratum, 2 to 6 percent slopesCeB222170502v04loh16919811:15840
Canfield silt loam, 3 to 8 percent slopesCdB329929002392v03zpa00719781:15840
Canfield silt loam, 8 to 15 percent slopesCdC280329002402v044pa00719781:15840
Canfield silt loam, 15 to 25 percent slopesCdD41929002412v04fpa00719781:15840
Canfield silt loam, 3 to 8 percent slopesCfB164519131272v03zpa01919841:15840
Canfield silt loam, 8 to 15 percent slopesCfC54319131282v044pa01919841:15840
Canfield silt loam, 15 to 25 percent slopesCfD6719131292v04fpa01919841:15840
Canfield channery silt loam, 3 to 8 percent slopes, moderately erodedCfB21856539463l3c1pa03719651:20000
Wooster and Canfield very stony loams, 0 to 12 percent slopesWsB629539585l3gzpa03719651:20000
Canfield silt loam, 3 to 8 percent slopesCdB2968929003912v03zpa07319781:15840
Canfield silt loam, 8 to 15 percent slopesCdC1978329003922v044pa07319781:15840
Canfield silt loam, 15 to 25 percent slopesCdD487829003932v04fpa07319781:15840
Urban land-Canfield complex, 0 to 8 percent slopesUcB196429004632v03spa07319781:15840
Urban land-Canfield complex, 8 to 25 percent slopesUcD41229004642v048pa07319781:15840
Canfield silt loam, 3 to 8 percent slopesCdB2349752962182v03zpa08519671:20000
Canfield silt loam, 8 to 15 percent slopesCdC2187842962192v044pa08519671:20000
Canfield silt loam, 15 to 25 percent slopesCdD254772962212v04fpa08519671:20000
Canfield silt loam, 0 to 3 percent slopesCdA25202962172v03rpa08519671:20000
Canfield silt loam, 25 to 35 percent slopesCdE15362962222v04hpa08519671:20000
Canfield silt loam, 8 to 15 percent slopes, severely erodedCdC36782962202v045pa08519671:20000
Canfield-Urban land complex, 2 to 6 percent slopesCeB416122022v03vpa08519671:20000
Canfield gravelly silt loam, 3 to 8 percent slopesCdB116105389032v046pa12119711:20000
Canfield gravelly silt loam, 8 to 15 percent slopesCdC89895389042v047pa12119711:20000
Canfield gravelly silt loam, 8 to 25 percent slopes, extremely stonyCeD70945389062v049pa12119711:20000
Canfield gravelly silt loam, 3 to 8 percent slopes, extremely stonyCeB14585389052v03xpa12119711:20000

Map of Series Extent

Approximate geographic distribution of the CANFIELD 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 .