Official Series Description


Lab Data Summary

Aggregate lab data for the CROFTON soil series. This aggregation is based on all pedons with a current taxon name of CROFTON, 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 CROFTON 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
102C80P012079NE119002Crofton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0763893,-97.7963867
102C81P011480NE107004Crofton7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6819458,-97.7761078
102C40A2296S1955NE051002Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3172226,-96.9386139
102C40A2370S1956SD099001CROFTON6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6602783,-96.6316681
102C40A2371S1956SD099013Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6666679,-96.5116653
102C40A2246S1959NE051003Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.3927765,-96.9569473
102C00P1256S2000NE173001Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2368889,-96.6283035
102C11N0005S2010SD099202Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6643111,-96.4928194
n/a04N0868S2004NE179002Crofton6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CROFTON 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 CROFTON 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 CROFTON 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 CROFTON 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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Click the image to view it full size.

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 CROFTON 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 CROFTON series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CROFTON 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 CROFTON, 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. NE-2012-02-08-14 | Butler County - February 1982

    Typical pattern of soils in the Ponca-Sharpsburg association and relationship of the soils to topography and parent material (Soil Survey of Butler County, Nebraska; February 1982).

  2. NE-2012-02-10-01 | Cedar County - October 1985

    Typical pattern of soils in the Nora-Crofton-Moody association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

  3. NE-2012-02-10-02 | Cedar County - October 1985

    Typical pattern of soils in the Moody-Nora association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

  4. NE-2012-02-10-03 | Cedar County - October 1985

    Typical pattern of soils in the Crofton-Alcester association and the relationship of the soils to topography and parent material (Soil Survey of Cedar County, Nebraska; October 1985).

  5. NE-2012-02-10-14 | Colfax County - January 1982

    Typical pattern of soils and parent material in the Nora-Crofton-Moody association (Soil Survey of Colfax County, Nebraska; January 1982).

  6. NE-2012-02-10-15 | Colfax County - January 1982

    Typical pattern of soils and parent material in the Moody-Alcester association (Soil Survey of Colfax County, Nebraska; January 1982).

  7. NE-2012-02-13-49 | Knox County - June 1997

    Typical pattern of soils and parent material in the Crofton-Nora-Alcester association (Soil Survey of Knox County, Nebraska; June 1997).

  8. NE-2012-02-13-50 | Knox County - June 1997

    Typical pattern of soils and parent material in the Brunswick-Paka-Simeon association (Soil Survey of Knox County, Nebraska; June 1997).

  9. NE-2012-02-13-61 | Nance County - July 1960

    General soil areas of Nance County from a "bird's-eye view" (Soil Survey of Nance County, Nebraska; July 1960).

  10. NE-2012-02-13-62 | Nance County - July 1960

    Principal soils of Nance County (Soil Survey of Nance County, Nebraska; July 1960).

  11. NE-2012-02-13-63 | Nance County - July 1960

    A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

  12. NE-2012-02-13-69 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Nora-Crofton-Moody association (Soil Survey of Platte County, Nebraska; September 1988).

  13. NE-2012-02-14-12 | Washington County - September 1964

    Soil pattern of the Sharpsburg-Marshall association (Soil Survey of Washington County, Nebraska; September 1964).

  14. NE-2012-02-14-13 | Washington County - September 1964

    Soil pattern of the Monona-Crofton association (Soil Survey of Washington County, Nebraska; September 1964).

  15. NE-2012-02-14-14 | Washington County - September 1964

    Soil pattern of the Luton-Volin and Albaton-Haynie associations (Soil Survey of Washington County, Nebraska; September 1964).

  16. SD-2010-11-01-11 | Minnehaha County - 2004

    Typical pattern of soils and parent material in the Moody-Nora association (Soil Survey of Minnehaha County, South Dakota; 2004).

  17. SD-2012-03-14-06 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Eltree-Yankton-Alcester association (Soil Survey of Bon Homme County, SD; 1983).

  18. SD-2012-03-15-69 | Lake County - December 1973

    Relationship of soils to topography and the underlying materials in the Moody-Nora association (Soil Survey of Lake County, SD; 1973).

Map Units

Map units containing CROFTON 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
Crofton silt loam, 9 to 14 percent slopes, eroded401D237964091082r9zvia11919731:15840
Crofton silt loam, 5 to 9 percent slopes, eroded401C29074091062r9ztia11919731:15840
Crofton silt loam, 12 to 20 percent slopes, eroded401E23524091092r9zwia11919731:15840
Crofton silt loam, 9 to 14 percent slopes, eroded401D29844112262r9zvia16719871:15840
Crofton silt loam, 5 to 9 percent slopes, eroded401C28064112252r9ztia16719871:15840
Crofton silt loam, 2 to 6 percent slopes, eroded401B22924112242r9zlia16719871:15840
Crofton silt loam, 12 to 20 percent slopes, eroded401E21754112272r9zwia16719871:15840
Nora-Crofton complex, 6 to 12 percent slopes, erodedP26C22749432713gj8hmn13320021:12000
Nora-Crofton complex, 12 to 18 percent slopes, erodedP26D2281432714gj8jmn13320021:12000
Crofton-Nora complex, 6 to 11 percent slopes, eroded6694301824269442sn2sne00319751:20000
Crofton-Nora complex, 17 to 30 percent slopes66971220727422842rb05ne00319751:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67891005927422872rb06ne00319751:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded669332394269432sx9kne00319751:20000
Crofton silt loam, coarse, 8 to 17 percent slopes, eroded6674258525556402qyb7ne00319751:20000
Thurman-Crofton complex, 11 to 30 percent slopes67332421427004gbbbne00319751:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668110234269412r9znne00319751:20000
Crofton silt loam, 30 to 60 percent slopes66866994269422r9zqne00319751:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668755422159712r9zsne00319751:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686013625556312pwr9ne00319751:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded67759222161312ts6hne00319751:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded6694263064270262sn2sne01119661:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67892232427422882rb06ne01119661:20000
Crofton-Nora complex, 17 to 30 percent slopes66971917827422852rb05ne01119661:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681137894270302r9znne01119661:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778274622166512ts6gne01119661:20000
Nora-Crofton complex, 11 to 17 percent slopes677617644270572sn2qne01119661:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686064225556322pwr9ne01119661:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded677419322166542sn2rne01119661:20000
Crofton silt loam, 30 to 60 percent slopes66861534270492r9zqne01119661:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded67752722166392ts6hne01119661:20000
Crofton silt loam, 11 to 17 percent slopes, eroded66733055357619d043ne01519761:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded6789622175012rb06ne01519761:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860253525051012pwr9ne02119781:20000
Crofton silt loam, 6 to 11 percent slopes, eroded66873114278162r9zsne02119781:20000
Pohocco, eroded-Crofton complex, 11 to 17 percent slopes8127785116913151trykne02319791:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860498225556462pwr9ne02319791:20000
Pohocco, eroded-Crofton complex, 6 to 11 percent slopes8130286716913141tryjne02319791:20000
Crofton silt loam, 30 to 60 percent slopes6686101116912762r9zqne02319791:20000
Pohocco, eroded-Crofton complex, 17 to 30 percent slopes812899316913161trylne02319791:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668168116912752r9znne02319791:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668749816912732r9zsne02319791:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded6694486904270952sn2sne02719821:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67892980627422912rb06ne02719821:20000
Crofton silt loam, 17 to 30 percent slopes, eroded66811775427126592r9znne02719821:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded6693172384270942sx9kne02719821:20000
Crofton-Alcester silt loams, 20 to 60 percent slopes67875968427092gbf5ne02719821:20000
Crofton silt loam, 30 to 60 percent slopes668612704270912r9zqne02719821:20000
Crofton-Gavins silt loams, 30 to 60 percent slopes6788936427093gbf6ne02719821:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778455934279082ts6gne03719801:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded6774155094279092sn2rne03719801:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668720394278802r9zsne03719801:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668118914278822r9znne03719801:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860181625556332pwr9ne03719801:20000
Crofton silt loam, 2 to 6 percent slopes, eroded668515814278792r9zlne03719801:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67898522169672rb06ne03719801:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded66932722169482sx9kne03719801:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded67751422169662ts6hne03719801:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668734634277642r9zsne03919731:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860268325051002pwr9ne03919731:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681159927126612r9znne03919731:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded677870122169892ts6gne03919731:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded678943422169902rb06ne03919731:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded67747022169982sn2rne03919731:20000
Crofton silt loam, 8 to 17 percent slopes, eroded68602004925051022pwr9ne04319721:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681110234267282r9znne04319721:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668734024267242r9zsne04319721:20000
Crofton silt loam, 2 to 6 percent slopes, eroded66854774267232r9zlne04319721:20000
Crofton silt loam, 30 to 60 percent slopes66866122170352r9zqne04319721:20000
Crofton silt loam, 8 to 17 percent slopes, eroded68602897925050992pwr9ne05119751:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681180404266692r9znne05119751:20000
Crofton silt loam, 6 to 11 percent slopes, eroded6687106574266662r9zsne05119751:20000
Crofton silt loam, 30 to 60 percent slopes668638754266702r9zqne05119751:20000
Crofton silt loam, 2 to 6 percent slopes, eroded668512434266652r9zlne05119751:20000
Crofton-Alcester silt loams, 20 to 60 percent slopes678736322170622df14ne05119751:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded678934722170632rb06ne05119751:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded669319322170562sx9kne05119751:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded669410922170572sn2sne05119751:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778129522170852ts6gne05319751:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686069825051032pwr9ne05319751:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668151622170822r9znne05319751:20000
Crofton silt loam, 30 to 60 percent slopes66865094268812r9zqne05319751:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded677416622170842sn2rne05319751:20000
Crofton silt loam, 6 to 11 percent slopes, eroded6687822170832r9zsne05319751:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded66946987327422802sn2sne10719891:20000
Crofton silt loam, 17 to 30 percent slopes, eroded66812656727126652r9znne10719891:20000
Crofton silt loam, coarse, 8 to 17 percent slopes, eroded66742284525556412qyb7ne10719891:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded66931396411442302sx9kne10719891:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67891259611442322rb06ne10719891:20000
Crofton-Thurman complex, 17 to 30 percent slopes66714785114423517dntne10719891:20000
Crofton-Thurman complex, 6 to 11 percent slopes, eroded66724413114423317dnrne10719891:20000
Crofton silt loam, 2 to 6 percent slopes, eroded6685313125173252r9zlne10719891:20000
Crofton silt loam, 6 to 11 percent slopes, eroded6687240411442262r9zsne10719891:20000
Crofton silt loam, 30 to 60 percent slopes6686125611442292r9zqne10719891:20000
Crofton-Thurman complex, 11 to 17 percent slopes, eroded66701056114423417dnsne10719891:20000
Crofton silt loam, 11 to 17 percent slopes, eroded6673808114422717dnkne10719891:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778750694274282ts6gne11919811:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded6789128234273982rb06ne11919811:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded677582184274272ts6hne11919811:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668124044273962r9znne11919811:20000
Crofton silt loam, 6 to 11 percent slopes, eroded66877844273952r9zsne11919811:20000
Crofton silt loam, 2 to 6 percent slopes, eroded66854344273942r9zlne11919811:20000
Crofton silt loam, 30 to 60 percent slopes66862674273972r9zqne11919811:20000
Crofton silt loam, 17 to 30 percent slopes, eroded66811429522290142r9znne12519581:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded6774413527422702sn2rne12519581:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860300925556382pwr9ne12519581:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded6694112322290042sn2sne12519581:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded677892122289862ts6gne12519581:20000
Crofton-Nora complex, 17 to 30 percent slopes669758527422862rb05ne12519581:20000
Crofton silt loam, 30 to 60 percent slopes66864224274832r9zqne12519581:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded678933522290032rb06ne12519581:20000
Nora-Crofton complex, 11 to 17 percent slopes67762894274962sn2qne12519581:20000
Crofton silt loam, 6 to 11 percent slopes, eroded66872324274612r9zsne12519581:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded66942510427422812sn2sne13919701:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded6693625927422572sx9kne13919701:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded6789265127422992rb06ne13919701:20000
Crofton silt loam, coarse, 8 to 17 percent slopes, eroded6674215825556422qyb7ne13919701:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668172027126682r9znne13919701:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded677830222171552ts6gne13919701:20000
Crofton silt loam, 2 to 6 percent slopes, eroded66852554275572r9zlne13919701:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686010525556362pwr9ne13919701:20000
Crofton silt loam, 6 to 11 percent slopes, eroded66876222171472r9zsne13919701:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded67756222171542ts6hne13919701:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778939994276672ts6gne14119841:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded6774294564276682sn2rne14119841:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded669348844276282sx9kne14119841:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681321427126702r9znne14119841:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686081425556372pwr9ne14119841:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded67894022171982rb06ne14119841:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded6778463234268492ts6gne16719801:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded6789445514268262rb06ne16719801:20000
Crofton silt loam, 17 to 30 percent slopes, eroded6681623227126712r9znne16719801:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded677551004268482ts6hne16719801:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668735234268222r9zsne16719801:20000
Crofton silt loam, coarse, 8 to 17 percent slopes, eroded6674145325556432qyb7ne16719801:20000
Crofton silt loam, 2 to 6 percent slopes, eroded668510014268212r9zlne16719801:20000
Crofton silt loam, 8 to 17 percent slopes, eroded686094725050972pwr9ne16719801:20000
Crofton silt loam, 30 to 60 percent slopes66862754268252r9zqne16719801:20000
Crofton silt loam, 8 to 17 percent slopes, eroded68601011625051042pwr9ne17319661:20000
Crofton silt loam, 6 to 11 percent slopes, eroded668756324277022r9zsne17319661:20000
Crofton silt loam, 17 to 30 percent slopes, eroded668115384277042r9znne17319661:20000
Crofton silt loam, 2 to 6 percent slopes, eroded668592422172692r9zlne17319661:20000
Nora-Crofton complex, 11 to 17 percent slopes, eroded677414603954952sn2rne17720001:12000
Crofton silt loam, 17 to 30 percent slopes, eroded66815083955332r9znne17720001:12000
Crofton silt loam, 8 to 17 percent slopes, eroded686027925051052pwr9ne17720001:12000
Crofton silt loam, 30 to 60 percent slopes6686422173152r9zqne17720001:12000
Crofton silt loam, 6 to 11 percent slopes, eroded6687106934267812r9zsne17919701:20000
Crofton silt loam, 2 to 6 percent slopes, eroded668525264267802r9zlne17919701:20000
Crofton silt loam, 8 to 17 percent slopes, eroded6860100625050982pwr9ne17919701:20000
Crofton silt loam, coarse, 8 to 17 percent slopes, eroded667457525556442qyb7ne17919701:20000
Crofton-Nora complex, 2 to 6 percent slopes, eroded669354322173272sx9kne17919701:20000
Crofton-Nora complex, 6 to 11 percent slopes, eroded669448527422822sn2sne17919701:20000
Crofton-Nora complex, 11 to 17 percent slopes, eroded678934022173322rb06ne17919701:20000
Nora-Crofton complex, 6 to 11 percent slopes, eroded677820422173442ts6gne17919701:20000
Nora-Crofton complex, 2 to 6 percent slopes, eroded67754722173432ts6hne17919701:20000
Eltree-Crofton silt loams, 9 to 15 percent slopesEcD999418263g17csd00919811:20000
Nora-Crofton complex, 6 to 9 percent slopesNcC5634165092sn2tsd07919671:20000
Crofton-Nora complex, 11 to 17 percent slopes, erodedCpD288904166302rb06sd08319711:20000
Nora-Crofton complex, 6 to 9 percent slopesNcC698054460672sn2tsd09919951:24000
Crofton-Nora complex, 9 to 15 percent slopesCrD10099446014gz3ksd09919951:24000
Crofton-Shindler complex, 9 to 15 percent slopesCsD3463446016gz3msd09919951:24000
Crofton-Nora complex, 15 to 25 percent slopesCrE370446015gz3lsd09919951:24000
Nora-Crofton complex, 6 to 9 percent slopesNcC10324183482sn2tsd10119851:20000
Crofton-Nora complex, 6 to 11 percent slopes, erodedCnD2370534536862sn2ssd12719741:20000
Crofton silt loam, 12 to 20 percent slopes, erodedCbE2111064536832r9zwsd12719741:20000
Crofton silt loam, 17 to 30 percent slopes, erodedCbF23694536842r9znsd12719741:20000
Crofton-Nora complex, 2 to 6 percent slopes, erodedCnB14654536852sx9ksd12719741:20000
Nora-Crofton silt loams, 20 to 50 percent slopesNeF601453712h73wsd12719741:20000
Crofton-Boyd association, 15 to 40 percent slopesCoE1721418069g113sd13519771:20000
Crofton-Nora silt loams, 9 to 25 percent slopesCmE1269418068g112sd13519771:20000

Map of Series Extent

Approximate geographic distribution of the CROFTON 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 .