Official Series Description


Lab Data Summary

Aggregate lab data for the WHARTON soil series. This aggregation is based on all pedons with a current taxon name of WHARTON, 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 WHARTON 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
12461PA0630571961PA063057Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8541667,-79.0172222
12486KY-069-00686KY-069-006Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4100533,-83.5082169
12461PA063053S1961PA063053Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8955556,-79.0188889
124AT-W07S1962OH009W07Wharton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3593803,-82.2662753
12676PA1290501976PA129050Wharton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3866667,-79.5136111
12772PA1290191972PA129019Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1675,-79.2794444
12773PA0330161973PA033016Wharton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2075,-78.4119444
12772PA12902072PA129020Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1666667,-79.2758333
12773PA03301773PA033017Wharton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1958333,-78.4052778
12788PA02101588PA021015Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5119444,-78.7733333
n/a81KY-109-00681KY-109-006Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4008S1955WV077007Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4009S1955WV077010Wharton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WHARTON 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 WHARTON 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 WHARTON 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 WHARTON 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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Competing Series

Soil series competing with WHARTON 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 WHARTON 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 WHARTON 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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Soil series sharing subgroup-level classification with WHARTON, 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. NY-2012-02-15-44 | Seneca Nation of Indians - August 1984

    Typical relationship of soils to parent material in the Allegheny River Valley (Soil Survey of Seneca Nation of Indians, New York; August 1984).

  2. OH-2010-09-29-24 | Vinton County - 2004

    Typical pattern of soils and parent material in the Shelocta-Brownsville-Germano general soil map unit (Soil Survey of Vinton County, Ohio; 2004).

  3. OH-2010-09-29-25 | Vinton County - 2004

    Typical pattern of soils and parent material in the Omulga-Philo general soil map unit (Soil Survey of Vinton County, Ohio; 2004).

  4. OH-2012-02-16-40 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Latham-Wharton-Shelocta association (Soil Survey of Scioto County, Ohio; January 1989).

  5. PA-2012-03-12-03 | Allegheny County - August 1981

    The pattern of soils and underlying material in the Gilpin--Wharton-Upshur soil association (Soil Survey of Allegheny County, PA; 1981).

  6. PA-2012-03-12-06 | Beaver and Lawrence Counties - April 1982

    Pattern of soils and parent material in Gilpin-Wharton-Weikert association (Soil Survey of Beaver and Lawrence Counties, PA; 1982).

  7. PA-2012-03-12-07 | Beaver and Lawrence Counties - April 1982

    Pattern of soils and parent material in Gilpin-Upshur-Weikert association (Soil Survey of Beaver and Lawrence Counties, PA; 1982).

  8. PA-2012-03-12-09 | Beaver and Lawrence Counties - April 1982

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

  9. PA-2012-03-12-20 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Hublersburg-Murrill-Opequon association (Soil Survey of Blair County, PA; 1981).

  10. PA-2012-03-13-01 | Cambria County - September 1985

    Typical pattern of soils and parent material in the Cookport-Hazleton-Laidig association (Soil Survey of Cambria County, PA; 1985).

  11. PA-2012-03-13-02 | Cambria County - September 1985

    Typical pattern of soils and parent material in the Gilpin-Ernest-Wharton association (Soil Survey of Cambria County, PA; 1985).

  12. PA-2012-03-13-03 | Cambria County - September 1985

    Typical pattern of soils and parent material in the Brinkerton-Wharton-Cavode association (Soil Survey of Cambria County, PA; 1985).

  13. PA-2012-03-13-08 | Centre County - August 1981

    Typical pattern of soils and underlying material in association 2 (Soil Survey of Centre County, PA; 1981).

  14. PA-2012-03-13-09 | Centre County - August 1981

    Typical pattern of soils and underlying material in association 3 (Soil Survey of Centre County, PA; 1981).

  15. PA-2012-03-13-12 | Clearfield County - August 1988

    Typical pattern of soils and underlying material in the Rayne-Gilpin-Ernest association (Soil Survey of Clearfield County, PA; 1988).

  16. PA-2012-03-13-23 | Fayette County - March 1973

    Parent material, position, and pattern of soils in the Gilpin-Wharton-Ernest soil association (Soil Survey of Fayette County, PA; 1973).

  17. PA-2012-03-13-25 | Fayette County - March 1973

    Parent material, position, and pattern of soils in the Monongahela-Philo-Atkins soil association (Soil Survey of Fayette County, PA; 1973).

  18. PA-2012-03-13-35 | Indiana County - January 1968

    Parent material, position, and pattern of soils in the Gilpin-Wharton-Cavode association (Soil Survey of Indiana County, PA; 1968).

  19. PA-2012-03-13-36 | Indiana County - January 1968

    Parent material, position, and pattern of soils in the Gilpin-Wharton-Upshur association (Soil Survey of Indiana County, PA; 1968).

  20. PA-2012-03-13-38 | Indiana County - January 1968

    Parent material, position, and pattern of soils in the Monongahela-Allegheny-Pope-Philo association (Soil Survey of Indiana County, PA; 1968).

  21. PA-2012-03-14-12 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Rayne-Gilpin-Wharton-Cavode soils (Soil Survey of Somerset County, PA; 1983).

  22. PA-2012-03-14-16 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Ernest-Rayne-Gilpin soils (Soil Survey of Somerset County, PA; 1983).

  23. PA-2012-03-14-29 | Venango County - December 1975

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

  24. PA-2012-03-14-30 | Warren and Forest Counties - October 1985

    Typical landscape and underlying material of the Hazleton-Cookport-Cavode map unit (Soil Survey of Warren and Forest Counties, PA; 1985).

  25. VA-2010-11-05-06 | Buchanan County -

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia).

  26. VA-2012-05-10-03 | Buchanan County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia; 2009).

  27. WV-2012-03-23-02 | Boone County - June 1994

    Typical pattern of soils and parent material in the Berks-Shelocta general soil map unit (Soil Survey of Boone County, WV; 1994).

  28. WV-2012-03-23-03 | Boone County - June 1994

    Typical pattern of soils and parent material in the Kaymine-Cedarcreek-Dekalb general soil map unit (Soil Survey of Boone County, WV; 1994).

Map Units

Map units containing WHARTON 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
Shelocta-Wharton complex, 20 to 55 percent slopesSrF1573552739lk59ky06919891:20000
Wharton channery silt loam, 8 to 15 percent slopes, very stonyWtC127724012762llqjmd00120091:12000
Wharton channery silt loam, 3 to 8 percent slopesWrB69324012712llqcmd00120091:12000
Wharton channery silt loam, 3 to 8 percent slopes, very stonyWtB68624012752llqhmd00120091:12000
Wharton channery silt loam, 8 to 15 percent slopesWrC59224012722llqdmd00120091:12000
Wharton channery silt loam, 15 to 25 percent slopes, very stonyWtD25824012772llqkmd00120091:12000
Wharton channery silt loam, 0 to 3 percent slopesWrA18324012702llqbmd00120091:12000
Wharton-Urban land complex, 0 to 8 percent slopesWuB17824010592llhjmd00120091:12000
Wharton channery silt loam, 0 to 3 percent slopes, very stonyWtA14324012742llqgmd00120091:12000
Wharton channery silt loam, 15 to 25 percent slopesWrD12924012732llqfmd00120091:12000
Wharton silt loam, 3 to 8 percent slopesWhB222005329472vxhrmd02319701:20000
Wharton silt loam, 8 to 15 percent slopesWhC211105329482sfv6md02319701:20000
Wharton silt loam, 15 to 25 percent slopesWhD1652893392vxhqny60519811:24000
Wharton silt loam, 8 to 15 percent slopesWhC192893382sfv6ny60519811:24000
Latham-Wharton silt loams, 15 to 25 percent slopesLdD87189587921mtdoh00119871:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C211024504462n7wnoh05319881:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D23624504472n7wpoh05319881:15840
Latham-Wharton silt loams, 15 to 25 percent slopes, erodedLhW1D23438424510392n8hsoh07919811:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C22064424510372n8hqoh07919811:15840
Wharton silt loam, 15 to 25 percent slopesWhD111105359992t5mnoh07919811:15840
Wharton silt loam, 8 to 15 percent slopesWhC42995359982t5mmoh07919811:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D2259424510402n8htoh07919811:15840
Shelocta-Wharton-Latham association, steepSWLZE1167124510532n8j7oh07919811:15840
Wharton-Latham silt loams, 25 to 40 percent slopesWhL1E116024510592n8jfoh07919811:15840
Wharton-Latham silt loams, 15 to 25 percent slopesWhL1D16624510582n8jdoh07919811:15840
Wharton-Latham silt loams, 6 to 15 percent slopesWhL1C13124510572n8jcoh07919811:15840
Shelocta-Wharton-Latham association, steepSWLZE1185024511162n8l8oh08719891:15840
Latham-Wharton silt loams, 15 to 25 percent slopesLhW1D11127424626982nnmwoh13119841:15840
Wharton silt loam, 15 to 25 percent slopesWhD15265377482t5mnoh13119841:15840
Shelocta-Wharton-Latham association, steepSWLZE147624626992nnmxoh13119841:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C22424799902p7mpoh13119841:15840
Wharton silt loam, 8 to 15 percent slopesWhC816890432t5mmoh13119841:15840
Latham-Wharton complex, 15 to 25 percent slopesLgD6211709815qxjoh14119971:15840
Shelocta-Wharton-Latham association, steepSWLZE17063524800482p7pkoh14519841:15840
Wharton silt loam, 15 to 25 percent slopesWfD70335373302t5mnoh14519841:15840
Wharton-Urban land complex, 8 to 20 percent slopesWkD2077537331l148oh14519841:15840
Latham-Wharton silt loams, 15 to 25 percent slopesLhW1D1142324526672nb69oh14519841:15840
Wharton silt loam, 8 to 15 percent slopesWfC1414608192t5mmoh14519841:15840
Wharton-Latham silt loams, 15 to 25 percent slopesWhL1D11996224533792nby8oh16319981:15840
Wharton-Latham silt loams, 25 to 40 percent slopesWhL1E11607924533802nby9oh16319981:15840
Wharton-Latham silt loams, 6 to 15 percent slopesWhL1C11492724533782nby7oh16319981:15840
Rarden-Wharton silt loams, 8 to 15 percent slopes, erodedRrW1C2250624539332ncj4oh16319981:15840
Latham-Wharton silt loams, 15 to 25 percent slopes, erodedLhW1D273024533602nbxnoh16319981:15840
Rarden-Wharton silt loams, 15 to 25 percent slopes, erodedRrW1D29724539342ncj5oh16319981:15840
Wharton silt loam, 8 to 15 percent slopesWhC134125417362t5mmpa00319731:15840
Wharton silt loam, 3 to 8 percent slopesWhB117505417352t185pa00319731:15840
Wharton silt loam, 15 to 25 percent slopesWhD43387806762t5mnpa00319731:15840
Urban land-Wharton complex, gently slopingUWB3335541730l5q5pa00319731:15840
Urban land-Wharton complex, moderately steepUWD2633541731l5q6pa00319731:15840
Gilpin-Wharton complex, 15 to 25 percent slopesGwD80747960t39rpa00319731:15840
Gilpin-Wharton silt loams, 8 to 15 percent slopesGwC47748872t485pa00319731:15840
Wharton silt loam, 3 to 8 percent slopesWhB1293816782502t185pa00520121:24000
Wharton-Gilpin silt loams, 15 to 25 percent slopesWtD996416782541tbc7pa00520121:24000
Wharton-Gilpin silt loams, 8 to 15 percent slopesWtC703716782531tbc6pa00520121:24000
Wharton silt loam, 8 to 15 percent slopesWhC655516782512t5mmpa00520121:24000
Wharton-Gilpin silt loams, 3 to 8 percent slopesWtB271416782521tbc5pa00520121:24000
Wharton-Vandergrift complex, 8 to 15 percent slopesWvC163116782561tbc9pa00520121:24000
Wharton-Vandergrift complex, 3 to 8 percent slopesWvB109316782551tbc8pa00520121:24000
Wharton-Vandergrift complex, 15 to 25 percent slopesWvD55516811221tfbrpa00520121:24000
Wharton silt loam, 8 to 15 percent slopesWhC888729003242t5mmpa00719781:15840
Wharton silt loam, 3 to 8 percent slopesWhB670729003232t185pa00719781:15840
Wharton-Gilpin silt loams, 15 to 25 percent slopesWnD33532900325l6mypa00719781:15840
Urban land-Wharton complex, 0 to 8 percent slopesUwB11922900317l6mppa00719781:15840
Urban land-Wharton complex, 8 to 25 percent slopesUwD4762900318l6mqpa00719781:15840
Wharton silt loam, 0 to 3 percent slopesWhA39829003222t184pa00719781:15840
Wharton channery silt loam, 8 to 15 percent slopes, very stonyWxC2312541869l5vnpa00919891:24000
Wharton channery silt loam, 3 to 8 percent slopes, very stonyWxB1808541868l5vmpa00919891:24000
Wharton variant silt loam, 3 to 8 percent slopesWvB1919542422l6fhpa01319781:20000
Wharton silt loam, 3 to 8 percent slopesWhB8245424202vxhrpa01319781:20000
Wharton silt loam, 8 to 15 percent slopesWhC2205424212sfv6pa01319781:20000
Gilpin-Wharton complex, 15 to 25 percent slopesGpD25999538187l20wpa01919841:15840
Gilpin-Wharton silt loams, 8 to 15 percent slopesGpC25486538186l20vpa01919841:15840
Wharton silt loam, 3 to 8 percent slopesWaB199945382232t185pa01919841:15840
Wharton silt loam, 8 to 15 percent slopesWaC74675382242t5mmpa01919841:15840
Wharton silt loam, 0 to 3 percent slopesWaA7305382222t184pa01919841:15840
Wharton-Gilpin complex, 8 to 15 percent slopesWgC203415419452vxhwpa02119781:20000
Wharton-Gilpin complex, 15 to 25 percent slopesWgD171085419462vxhtpa02119781:20000
Wharton silt loam, 3 to 8 percent slopesWaB160335419432vxhrpa02119781:20000
Wharton silt loam, 8 to 15 percent slopesWaC34535419442sfv6pa02119781:20000
Wharton silt loam, 3 to 8 percent slopesWhB1049427179292vxhrpa02719751:20000
Wharton silt loam, 8 to 15 percent slopesWhC17915383602sfv6pa02719751:20000
Wharton silt loam, 0 to 3 percent slopesWhA3565383582vxhppa02719751:20000
Wharton-Gilpin silt loams, 15 to 25 percent slopesWgD85051885363218w5pa03120121:24000
Wharton silt loam, 3 to 8 percent slopesWhB56775297562t185pa03120121:24000
Wharton silt loam, 8 to 15 percent slopesWhC53925297572t5mmpa03120121:24000
Wharton silt loam, 15 to 25 percent slopesWhD18805297582t5mnpa03120121:24000
Urban land-Wharton complex, 0 to 8 percent slopesUwB683529783ks8spa03120121:24000
Wharton silt loam, 0 to 3 percent slopesWhA5545637932t184pa03120121:24000
Wharton-Gilpin silt loams, 8 to 15 percent slopesWgC2541885362218w4pa03120121:24000
Urban land-Wharton complex, 8 to 25 percent slopesUwD66529785ks8vpa03120121:24000
Wharton silt loam, 3 to 8 percent slopesWhB255305385602vxhrpa03319811:20000
Wharton silt loam, 8 to 15 percent slopesWhC229445385612sfv6pa03319811:20000
Wharton silt loam, 15 to 25 percent slopesWhD43545385622vxhqpa03319811:20000
Wharton-Cookport complex, 0 to 8 percent slopes, very stonyWgB6574544131l86mpa03520021:24000
Wharton silt loam, 0 to 8 percent slopes, very stonyWeB4330544130l86lpa03520021:24000
Wharton silt loam, 3 to 8 percent slopesWbB23105441282vxhrpa03520021:24000
Gilpin-Wharton silt loams, 15 to 25 percent slopesGwD604543976l81mpa03520021:24000
Wharton silt loam, 8 to 15 percent slopesWbC3945441292sfv6pa03520021:24000
Wharton silt loam, 8 to 15 percent slopesWrC1005515910742sfv6pa05120051:24000
Wharton silt loam, 3 to 8 percent slopesWrB998515910732vxhrpa05120051:24000
Wharton silt loam, 15 to 25 percent slopesWrD499715910752vxhqpa05120051:24000
Wharton-Gilpin complex, 15 to 25 percent slopesWgD404015910792vxhtpa05120051:24000
Wharton silt loam, 8 to 25 percent slopes, very stonyWsD286515911471qdqbpa05120051:24000
Wharton-Gilpin complex, 8 to 15 percent slopesWgC205515910782vxhwpa05120051:24000
Wharton silt loam, 0 to 8 percent slopes, very stonyWsB146915911461qdq9pa05120051:24000
Wharton silt loam, 25 to 35 percent slopesWrE65915910762vxhspa05120051:24000
Wharton-Gilpin complex, 3 to 8 percent slopesWgB46415910772vxhvpa05120051:24000
Wharton silt loam, 25 to 35 percent slopes, very stonyWsE27915911481qdqcpa05120051:24000
Wharton silt loam, 0 to 3 percent slopesWrA24815910722vxhppa05120051:24000
Urban land-Wharton complex, 0 to 8 percent slopesUwB14615911191qdpfpa05120051:24000
Urban land-Wharton complex, 8 to 25 percent slopesUwD5815911201qdpgpa05120051:24000
Wharton silt loam, 2 to 10 percent slopesWhB511542048l61fpa06119741:20000
Wharton silt loam, 3 to 8 percent slopesWhB1535317209372t185pa06320121:24000
Wharton silt loam, 8 to 15 percent slopesWhC733417209382t5mmpa06320121:24000
Wharton silt loam, 0 to 3 percent slopesWhA531017209362t184pa06320121:24000
Wharton silt loam, 15 to 25 percent slopesWhD71917209402t5mnpa06320121:24000
Wharton silt loam, 3 to 8 percent slopesWhB160723990162vxhrpa06520121:12000
Wharton silt loam, 0 to 3 percent slopesWhA96523990152vxhppa06520121:12000
Wharton silt loam, 15 to 25 percent slopesWhD70631800532t5mnpa06520121:12000
Wharton silt loam, 8 to 15 percent slopesWhC35223990172sfv6pa06520121:12000
Wharton silt loam, 8 to 15 percent slopesWhC149229004762t5mmpa07319781:15840
Wharton-Gilpin silt loams, 15 to 25 percent slopesWnD14092900477l6mypa07319781:15840
Wharton silt loam, 3 to 8 percent slopesWhB61729004752t185pa07319781:15840
Urban land-Wharton complex, 8 to 25 percent slopesUwD702900470l6mqpa07319781:15840
Urban land-Wharton complex, 0 to 8 percent slopesUwB402900469l6mppa07319781:15840
Wharton silt loam, 0 to 3 percent slopesWhA1329004742t184pa07319781:15840
Wharton silt loam, 3 to 8 percent slopesWaB38825399212vxhrpa08319841:20000
Wharton silt loam, 0 to 8 percent slopes, very stonyWxB33414524221krcbpa08319841:20000
Wharton silt loam, 8 to 15 percent slopesWaC2014524172sfv6pa08319841:20000
Wharton silt loam, 15 to 25 percent slopesWaD614524082vxhqpa08319841:20000
Wharton channery silt loam, 0 to 8 percent slopesWhB29724338352mpltpa10519531:24000
Wharton channery silt loam, 8 to 25 percent slopesWhD18524338332mplrpa10519531:24000
Wharton silt loam, 3 to 8 percent slopesWhB246325421232vxhrpa11119771:20000
Wharton silt loam, 8 to 15 percent slopesWhC117515421242sfv6pa11119771:20000
Wharton very stony silt loam, 3 to 8 percent slopesWvB7112542126l63ypa11119771:20000
Wharton very stony silt loam, 8 to 25 percent slopesWvD5686542127l63zpa11119771:20000
Wharton silt loam, 15 to 25 percent slopesWhD32265421252vxhqpa11119771:20000
Wharton silt loam, 3 to 8 percent slopesWhB80485389482t185pa12119711:20000
Wharton silt loam, 8 to 15 percent slopesWhC31705389492t5mmpa12119711:20000
Wharton silt loam, 8 to 15 percent slopesWrC351965446672t5mmpa12920031:24000
Wharton silt loam, 3 to 8 percent slopesWrB243575446662t185pa12920031:24000
Wharton silt loam, 15 to 25 percent slopesWrD62575446682t5mnpa12920031:24000
Urban land-Wharton complex, 0 to 8 percent slopesUwB2893544596l8pmpa12920031:24000
Urban land-Wharton complex, 8 to 25 percent slopesUwD2313557364lpzhpa12920031:24000
Wharton silt loam, 0 to 8 percent slopes, very stonyWsB2048544603l8pvpa12920031:24000
Wharton silt loam, 8 to 25 percent slopes, very stonyWsD1789544604l8pwpa12920031:24000
Wharton silt loam, 3 to 8 percent slopesWaB289975391982vxhrpa60719861:20000
Wharton silt loam, 8 to 15 percent slopesWaC173025391992sfv6pa60719861:20000
Wharton silt loam, 15 to 25 percent slopesWaD38785392002vxhqpa60719861:20000
Wharton silt loam, 8 to 25 percent slopes, very stonyWxD3208539202l32mpa60719861:20000
Wharton silt loam, 0 to 8 percent slopes, very stonyWxB2980539201l32lpa60719861:20000
Wharton silt loam, 3 to 8 percent slopesWhB80385392712vxhrpa60919791:20000
Wharton silt loam, 8 to 15 percent slopesWhC48675392722sfv6pa60919791:20000
Wharton silt loam, 15 to 25 percent slopesWhD17725392732vxhqpa60919791:20000
Wharton-Blairton complex, 15 to 35 percent slopes55D552834401x085va00520031:24000
Wharton-Blairton complex, 8 to 15 percent slopes55C314834400x084va00520031:24000
Wharton-Blairton complex, 8 to 15 percent slopes61C52414514261kqb6va01720051:24000
Wharton-Blairton complex, 15 to 35 percent slopes61D48614514271kqb7va01720051:24000
Blairton-Wharton complex, 3 to 8 percent slopes8B25514514251kqb5va01720051:24000
Wharton-Gilpin-Berks complex, 15 to 25 percent slopes31D112616708611t2nrva02720061:24000
Wharton-Gilpin-Marrowbone complex, 8 to 15 percent slopes32C71116709421t2rcva02720061:24000
Wharton-Blairton complex, 15 to 35 percent slopes58E49925121132q9jzva09120101:24000
Blairton-Wharton complex, 3 to 8 percent slopes7B31625120262q7v6va09120101:24000
Wharton-Blairton complex, 8 to 15 percent slopes58C29925121142q9k0va09120101:24000
Wharton-Gilpin-Berks complex, 15 to 25 percent slopes59D24916712331t31rva16720061:24000
Wharton-Gilpin-Marrowbone complex, 8 to 15 percent slopes60C2416718911t3qzva16720061:24000
Wharton silt loam, 3 to 8 percent slopesWrB4205132752t185wv00119651:12000
Wharton silt loam, 8 to 15 percent slopesWrC2915132762t5mmwv00119651:12000
Wharton silt loam, 15 to 25 percent slopesWrD755132772t5mnwv00119651:12000
Gilpin-Wharton silt loams, 15 to 35 percent slopesGwE6305514857k8r9wv00519881:24000
Wharton-Clearbrook channery silt loams, 3 to 8 percent slopesWrB97517101991vdlqwv0371:24000
Wharton-Clearbrook channery silt loams, 8 to 15 percent slopesWrC49917102001vdlrwv0371:24000
Gilpin-Wharton complex, 15 to 35 percent slopesGrE3899553351lkt1wv04320051:24000
Gilpin-Wharton complex, 20 to 30 percent slopesGwD2817514629k8hywv60119661:15840
Wharton-Gilpin complex, 10 to 20 percent slopesWgC779514627k8hwwv60119661:15840
Clymer and Wharton soils, 3 to 15 percent slopes, very rubblyCWC5516750071t6zhwv60219651:20000
Wharton silt loam, 3 to 8 percent slopesWhB36716025842t185wv60419701:12000
Wharton silt loam, 8 to 15 percent slopesWhC12117131992t5mmwv60419701:12000
Wharton very stony silt loam, 3 to 15 percent slopesWoC1253556002lnkkwv60819731:20000
Wharton silt loam, 3 to 8 percent slopesWnB9745560002vxhrwv60819731:20000
Wharton silt loam, 8 to 15 percent slopesWnC5425560012sfv6wv60819731:20000
Wharton silt loam, 8 to 15 percent slopesWrC23115158442sfv6wv61019731:20000
Wharton silt loam, 15 to 25 percent slopesWrD4705158452vxhqwv61019731:20000
Wharton silt loam, 8 to 15 percent slopesWhC13155144242sfv6wv61119771:20000
Wharton silt loam, 15 to 25 percent slopesWhD4905144252vxhqwv61119771:20000
Wharton silt loam, 3 to 8 percent slopesWhB4655144232vxhrwv61119771:20000
Wharton stony silt loam, 3 to 15 percent slopesWoC12281515972k9x8wv62819801:20000
Clymer and Wharton rubbly soils, 3 to 15 percent slopesCwB6401515890k9tmwv62819801:20000
Clymer and Wharton rubbly soils, 15 to 35 percent slopesCwD3987515891k9tnwv62819801:20000
Wharton stony silt loam, 15 to 35 percent slopesWoD2227515973k9x9wv62819801:20000
Wharton channery silt loam, 3 to 8 percent slopesWnB1418515971k9x7wv62819801:20000

Map of Series Extent

Approximate geographic distribution of the WHARTON 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 .