Official Series Description


Lab Data Summary

Aggregate lab data for the WEIKERT soil series. This aggregation is based on all pedons with a current taxon name of WEIKERT, 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 WEIKERT 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
108A99P0012S1998IN171001Weikert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2783318,-87.2866669
111DMY80181980IN107018Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9933028,-86.9870306
111DWN84211984IN171021Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3074833,-87.2641361
120A95P020093IL087054EWeikert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4853457,-88.7356061
120CWS81012015IN175002Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5653417,-85.9024583
12458PA0650041958PA065004Weikert5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1116667,-79.1255556
12458PA0650141958PA065014Weikert5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0677778,-79.11
12510KY-125-00410KY125FSC004Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.980999,-84.2699738
12665PA0030011965PA003001Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6663889,-80.0891667
12665PA0030041965PA003004Weikert4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5,-79.8777778
128VPI0145V1992-VA005-145Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7052778,-80.1502778
14788PA0090111988PA009011Weikert4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8083333,-78.4161111
14788PA0090161988PA009016Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8411111,-78.3902778
14788PA0550671988PA055067Weikert4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2219444,-77.7033333
14788PA0990311988PA099031Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6241667,-76.9744444
14740A4038S1960WV003007Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4500008,-77.9333344
14793P0795S1993PA055039Weikert7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9222221,-77.753334
14793P0796S1993PA055040Weikert6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9225006,-77.7555542
14705N0348S2004PA061004WEIKERT6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6649704,-77.9043579
147VPI0142V1992-VA005-142Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7869444,-80.1788889
147VPI0144V1992-VA005-144Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9202778,-80.0144444
147VPI0151V1992-VA017-151Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0955,-79.9212778
147VPI0172V1992-VA091-172Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3187778,-79.7346389
147VPI0149V1992-WV075-149Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1167222,-79.9421389
147VPI0150V1992-WV075-150Weikert2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.10875,-79.9295833
n/aAS-0101962-OH005-010Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAT-W011962-OH009-W01Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAT-W021962-OH009-W02Weikert3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WEIKERT 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 WEIKERT 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 WEIKERT 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 WEIKERT 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 WEIKERT 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 WEIKERT 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 WEIKERT 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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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 WEIKERT, 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. KY-2012-01-30-04 | Grayson County - December 1972

    Relationship of soils to topography and underlying material in the Zanesville-Gilpin-Wellston-Weikert association (Soil Survey of Grayson County, Kentucky; December 1972).

  2. KY-2012-01-30-05 | Grayson County - December 1972

    Relationship of soils to topography and underlying material in the Caneyville-Weikert-Zanesville association (Soil Survey of Grayson County, Kentucky; December 1972).

  3. KY-2012-02-01-09 | Madison County - March 1973

    Relationship of soils to topography and underlying material in the Colyer-Weikert-Captina association (Soil Survey of Madison County, Kentucky; March 1973).

  4. MD-2010-09-07-12 | Washington County - 2003

    Relationship of soils to topography and underlying material in the Weikert-Berks-Clearbrook general soil map unit (Soil Survey of Washington County, Maryland; 2003).

  5. MD-2012-02-03-27 | Washington County - 2003

    Relationship of soils to topography and underlying material in the Weikert-Berks-Clearbrook general soil map unit (Soil Survey of Washington County, Maryland; 2003).

  6. PA-2010-09-30-05 | Clinton County - 2007

    Typical pattern of soils and parent material that are dominant along the footslopes of the Allegheny Front (Soil Survey of Clinton County, Pennsylvania; 2007).

  7. PA-2010-09-30-06 | Clinton County - 2007

    Typical pattern of soils and parent material throughout the Susquehanna Lowland Section (Soil Survey of Clinton County, Pennsylvania; 2007).

  8. PA-2010-09-30-10 | Franklin County -

    Relationship of soils to topography and underlying material in the Berks-Weikert general soil map unit (Soil Survey of Franklin County, Pennsylvania).

  9. PA-2010-09-30-15 | Fulton County - 2004

    Relationship of soils to topography and the underlying material in the Hazleton-Sideling-Dekalb general soil map unit (Soil Survey of Fulton County, Pennsylvania; 2004).

  10. PA-2012-03-12-02 | Allegheny County - August 1981

    Relationship of soils to geology and physiography in soil association 5 (Soil Survey of Allegheny County, PA; 1981).

  11. 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).

  12. 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).

  13. PA-2012-03-12-08 | Beaver and Lawrence Counties - April 1982

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

  14. 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).

  15. PA-2012-03-12-12 | Bedford County - 1998

    Typical pattern of soils and parent material in the Berks-Weikert-Blairton general soil map unit (Soil Survey of Bedford County, PA; 1998).

  16. PA-2012-03-12-15 | Berks County - September 1970

    Cross section of the northern part of Berks County showing soils of associations 1, 2, and 3 (Soil Survey of berks County, PA; 1970).

  17. PA-2012-03-12-18 | Blair County - October 1981

    Typical pattern of soils and underlying material in the Berks-Brinkerton-Weikert association (Soil Survey of Blair County, PA; 1981).

  18. 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).

  19. 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).

  20. PA-2012-03-13-17 | Cumberland and Perry Counties - April 1986

    Typical pattern of soils and underlying material in the Berks-Weikert-Bedington association (Soil Survey of Cumberland and Perry Counties, PA; 1986).

  21. 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).

  22. PA-2012-03-13-24 | Fayette County - March 1973

    Parent material, position, and pattern of soils in the Guernsey-Westmoreland-Clarksburg soil association (Soil Survey of Fayette County, PA; 1973).

  23. 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).

  24. PA-2012-03-13-30 | Franklin County - August 1975

    Relationship of underlying material and topography in association 5 (Soil Survey of Franklin County, PA; 1975).

  25. PA-2012-03-13-33 | Fulton County - 2004

    Diagram showing pattern of soils and their parent material on a mountain slope and in an adjacent valley in eastern Fulton County (Soil Survey of Fulton County, PA; 2004).

  26. PA-2012-03-13-34 | Greene and Washington Counties - September 1983

    Typical pattern of soils and underlying material in the Dormont-Culleoka association (Soil Survey of Greene and Washington Counties, PA; 1983).

  27. 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).

  28. 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).

  29. PA-2012-03-13-40 | Juniata and Mifflin Counties - April 1981

    Typical pattern of soils and underlying material of the Berks-Weikert association (Soil Survey of Juniata and Mifflin Counties, PA; 1981).

  30. PA-2012-03-13-53 | Lebanon County - August 1981

    Pattern of soils in the Bedington-Berks-Holly general soil map unit (Soil Survey of Lebanon County, PA; 1981).

  31. PA-2012-03-13-57 | Lycoming County - November 1986

    Typical pattern of soils and underlying material in the Weikert-Berks-Hartleton association (Soil Survey of Lycoming County, PA; 1986).

  32. PA-2012-03-13-75 | Montour County - April 1985

    Typical pattern of soils and underlying material in the Weikert-Berks-Hartleton association (Soil Survey of Montour County, PA; 1985).

  33. PA-2012-03-14-04 | Northampton County - July 1974

    Typical pattern of soils and underlying material in association 4 (Soil Survey of Northampton County, PA; 1974).

  34. PA-2012-03-14-05 | Northumberland County - March 1985

    Typical pattern of soils and underlying material in the Weikert-Berks-Hartleton association (Soil Survey of Northumberland County, PA; 1985).

  35. PA-2012-03-14-10 | Snyder County - April 1985

    Typical pattern of soils and underlying material in the Weikert-Hartleton association (Soil Survey of Snyder County, PA; 1985).

  36. PA-2012-03-14-14 | Somerset County - December 1983

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

  37. PA-2012-03-14-22 | Union County - March 1985

    Typical pattern of soils and underlying material in the Weikert-Berks-Hartleton association (Soil Survey of Union County, PA; 1985).

  38. VA-2012-05-11-17 | Washington County Area and the City of Bristol - 2006

    Schematic cross section of the major geologic strata and dominant soils in Washington County (A-A´). Route of cross section is shown in figure 9 (Soil Survey of Washington County Area and the City of Bristol, Virginia; 2006).

  39. VA-2012-05-11-18 | Washington County Area and the City of Bristol - 2006

    Schematic cross section of the major geologic strata and dominant soils in Washington County (A´-A´´). Route of cross section is shown in figure 9 (Soil Survey of Washington County Area and the City of Bristol, Virginia; 2006).

Map Units

Map units containing WEIKERT 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
Berks, Muskingum, and Weikert soils, 35 to 70 percent slopes793G375714021141j20hil08720051:12000
Berks, Muskingum, and Weikert soils, 18 to 35 percent slopes793F125114021131j20gil08720051:12000
Berks, Muskingum, and Weikert soils, 18 to 35 percent slopes793F279014780431lm0til19920071:12000
Berks, Muskingum, and Weikert soils, 35 to 70 percent slopes793G49214780441lm0vil19920071:12000
Weikert-rock outcrop complex, 35 to 80 percent slopesWfG9661630815gppin10719841:15840
Weikert channery silt loam, 40 to 80 percent slopesWcG12281632605gwgin10919791:15840
Weikert silt loam, 25 to 70 percent slopesWeG22861598635cbwin13319791:15840
Weikert Variant fine sandy loam, 35 to 80 percent slopes, very boulderyWpG8541631845gt0in17119871:15840
Weikert-Culleoka complex, 6 to 12 percent slopesWcC745415924871qg3kky00120061:12000
Weikert-Culleoka complex, 12 to 20 percent slopesWcD678015924881qg3lky00120061:12000
Culleoka-Weikert complex, 2 to 6 percent slopesCwB150215924861qg3jky00120061:12000
Urban land-Weikert-Culleoka complex, 2 to 20 percent slopesUw146614133791jfqwky00120061:12000
Frondorf-Weikert complex, 20 to 40 percent slopesFwF33108549057lfbjky04719771:20000
Frondorf-Weikert complex, 12 to 20 percent slopesFwD17697549056lfbhky04719771:20000
Weikert-Ramsey-Gilpin stony complex, 20 to 30 percent slopesWgE20385549693lg01ky08519671:20000
Weikert-Ramsey-Gilpin stony complex, 30 to 50 percent slopesWgF17290549695lg03ky08519671:20000
Weikert channery silt loam, 12 to 30 percent slopesWcE12080549691lfzzky08519671:20000
Weikert-Ramsey-Gilpin stony complex, 20 to 30 percent slopes, severely erodedWgE35020549694lg02ky08519671:20000
Weikert channery silt loam, 12 to 30 percent slopes, severely erodedWcE33870549692lg00ky08519671:20000
Gilpin-Weikert complex, 25 to 60 percent slopesGwF133715330741ng90ky11120051:12000
Weikert channery silt loam, 40 to 80 percent slopesWeG722413979271hxnfky15119681:20000
Rockcastle-Weikert complex, 20 to 50 percent slopesRlF13965549996lg9tky17919671:15840
Frondorf-Weikert complex, 20 to 45 percent slopesFwF16020551160lhjcky21919841:20000
Frondorf-Weikert complex, 12 to 20 percent slopesFwD8320551159lhjbky21919841:20000
Weikert channery silt loam, 40 to 80 percent slopesWcF16524552307ljqcky62819731:20000
Frondorf-Weikert-Wellston complex, 12 to 20 percent slopesFwD690549461lfrkky62919791:20000
Frondorf-Weikert-Wellston complex, 6 to 12 percent slopesFwC380549460lfrjky62919791:20000
Frondorf-Weikert-Wellston complex, 20 to 50 percent slopesFwF170549462lfrlky62919791:20000
Weikert and Ramsey stony soils, 20 to 50 percent slopesWrE169624530222nbkrky64619661:15840
Weikert and Ramsey stony soils, 12 to 20 percent slopesWrD57724530212nbkqky64619661:15840
Frondorf-Weikert complex, 20 to 50 percent slopesFwF55424528652nbdpky70919951:20000
Weikert channery silt loam, 25 to 45 percent slopesWeE2740024012582w6mymd00120091:12000
Weikert channery silt loam, 15 to 25 percent slopesWeD1510324012572v4vsmd00120091:12000
Weikert channery silt loam, 8 to 15 percent slopesWeC628824012562v4w5md00120091:12000
Weikert channery silt loam, 25 to 45 percent slopes, very flaggyWfE606624012622wkdfmd00120091:12000
Weikert-Rock outcrop complex, 45 to 65 percent slopesWgF315424012692llq9md00120091:12000
Weikert very flaggy silt loam, 45 to 65 percent slopesWfF221224012632llq3md00120091:12000
Weikert channery silt loam, 45 to 65 percent slopesWeF188624012592llpzmd00120091:12000
Weikert very flaggy silt loam, 15 to 25 percent slopesWfD164524012612llq1md00120091:12000
Weikert channery silt loam, 3 to 8 percent slopesWeB149724012552v4vrmd00120091:12000
Weikert-Rock outcrop complex, 25 to 45 percent slopesWgE89924012682llq8md00120091:12000
Weikert very flaggy silt loam, 8 to 15 percent slopesWfC44524012602llq0md00120091:12000
Weikert-Urban land complex, 15 to 25 percent slopesWkD15924010562llhfmd00120091:12000
Weikert-Rock outcrop complex, 15 to 25 percent slopesWgD15224012672llq7md00120091:12000
Weikert very channery silt loam, 25 to 65 percent slopesWeF65875347312wkdkmd04319981:12000
Weikert very channery silt loam, 15 to 25 percent slopesWeD32205347302v4vymd04319981:12000
Weikert very channery silt loam, 8 to 15 percent slopesWeC31775347292v4vxmd04319981:12000
Weikert-Berks channery silt loams, 15 to 25 percent slopesWkD16105347412v4w1md04319981:12000
Weikert-Berks channery silt loams, 8 to 15 percent slopesWkC15965347402v4w0md04319981:12000
Weikert very channery silt loam, 3 to 8 percent slopesWeB12485347282v4vwmd04319981:12000
Weikert-Berks channery silt loams, 3 to 8 percent slopesWkB11495347392v4vzmd04319981:12000
Berks-Weikert channery silt loams, 8 to 15 percent slopesBfC5345341572sgdbmd04319981:12000
Berks-Weikert channery silt loams, 3 to 8 percent slopesBfB3885341562sgd9md04319981:12000
Berks-Weikert-Urban land complex, 8 to 25 percent slopesBkD2375341662y18gmd04319981:12000
Berks-Weikert-Urban land complex, 0 to 8 percent slopesBkB565341612y18hmd04319981:12000
Shelocta-Cruze-Weikert association, steepSgE7714205621jp6loh07119731:15840
Weikert shaly silt loam, 35 to 70 percent slopesWkF3791711755r3soh09119771:15840
Weikert channery fine sandy loam, 1 to 6 percent slopesWeB3442878219nhkoh09319721:15840
Gilpin-Weikert complex, 25 to 70 percent slopesGsF1016508871sdwfoh09919661:15840
Shelocta-Cruze-Weikert association, steepSgE82816890171tpkfoh13119841:15840
Shelocta-Cruze-Weikert association, steepShE339701709605qwvoh14119971:15840
Weikert channery silt loam, 25 to 50 percent slopes, moderately erodedWeF211582881029nsmoh15119671:15840
Weikert channery silt loam, 18 to 25 percent slopes, moderately erodedWeE24822881019nsloh15119671:15840
Weikert channery silt loam, 12 to 18 percent slopesWeD2112881009nskoh15119671:15840
Weikert channery silt loam, 6 to 12 percent slopesWeC1372880999nsjoh15119671:15840
Gilpin, Weikert, Culleoka channery silt loams and 25 to 80 percent slopesGSF470745416872wds4pa00319731:15840
Culleoka-Weikert shaly silt loams, 15 to 25 percent slopesCwD2581541672l5n9pa00319731:15840
Culleoka-Weikert shaly silt loams, 8 to 15 percent slopesCwC1307541671l5n8pa00319731:15840
Weikert-Rock outcrop complex, 25 to 80 percent slopesWEF10625417342wdrzpa00319731:15840
Culleoka-Weikert shaly silt loams, 3 to 8 percent slopesCwB757541670l5n7pa00319731:15840
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF11188524224872wds3pa00520121:24000
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGwD3870924224902wds2pa00520121:24000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC734824224892wds1pa00520121:24000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB673724224882wds0pa00520121:24000
Weikert channery silt loam, 3 to 8 percent slopesWeB274616782472wdrxpa00520121:24000
Weikert channery silt loam, 8 to 15 percent slopesWeC142716782482wdrypa00520121:24000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGsF5073129002762wds3pa00719781:15840
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGsD1306529002752wds2pa00719781:15840
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGsC630929002742wds1pa00719781:15840
Weikert-Rock outcrop complex, 25 to 80 percent slopesWeF496429003212wdrzpa00719781:15840
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGsB210029002732wds0pa00719781:15840
Weikert channery silt loam, 35 to 65 percent slopesWkF249645418622v4wbpa00919891:24000
Weikert channery silt loam, 25 to 35 percent slopesWkE13942541861l5vdpa00919891:24000
Weikert channery silt loam, 8 to 15 percent slopesWkC84845418592v4w5pa00919891:24000
Weikert channery silt loam, 15 to 25 percent slopesWkD78485418602v4vspa00919891:24000
Weikert very flaggy silt loam, 25 to 60 percent slopesWlF1852541863l5vgpa00919891:24000
Berks-Weikert complex, 8 to 15 percent slopesBkC576255429782sgbjpa01119971:24000
Berks-Weikert complex, 3 to 8 percent slopesBkB291395429772sgbhpa01119971:24000
Weikert-Berks complex, 15 to 25 percent slopesWeD161535430962v4w3pa01119971:24000
Berks-Weikert complex, 25 to 60 percent slopesBkF150995429802sgcrpa01119971:24000
Berks-Weikert complex, 15 to 25 percent slopesBkD113515429792wkdrpa01119971:24000
Weikert-Berks complex, 3 to 8 percent slopesWeB51345430952v4w4pa01119971:24000
Berks-Weikert complex, 0 to 3 percent slopesBkA7055429762sgbfpa01119971:24000
Berks-Weikert channery silt loams, 25 to 70 percent slopesBmF183135423262sgctpa01319781:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD31165424192v4vspa01319781:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC20095424182v4w5pa01319781:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB12475424172v4vrpa01319781:20000
Berks-Weikert channery silt loams, 15 to 25 percent slopesBmD11715423252sgbppa01319781:20000
Berks-Weikert channery silt loams, 8 to 15 percent slopesBmC9575423242sgbnpa01319781:20000
Edom-Weikert complex, 8 to 15 percent slopesEmC736542346l6c1pa01319781:20000
Edom-Weikert complex, 15 to 25 percent slopesEmD667542347l6c2pa01319781:20000
Edom-Weikert complex, 3 to 8 percent slopesEmB284542345l6c0pa01319781:20000
Culleoka-Weikert channery silt loams, 8 to 15 percent slopesCyC1663543622l7p6pa01719971:24000
Culleoka-Weikert channery silt loams, 3 to 8 percent slopesCyB1208543621l7p5pa01719971:24000
Weikert-Culleoka complex, 15 to 25 percent slopesWfD706543761l7tppa01719971:24000
Weikert channery silt loam, 8 to 15 percent slopesWeC64543759l7tmpa01719971:24000
Weikert channery silt loam, 0 to 8 percent slopesWeB25543758l7tlpa01719971:24000
Weikert channery silt loam, 15 to 25 percent slopesWeD14543760l7tnpa01719971:24000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGoF122345381852wds3pa01919841:15840
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGoD113575381842wds2pa01919841:15840
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGoC70405381832wds1pa01919841:15840
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGoB59715381822wds0pa01919841:15840
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGWF8543541910l5wzpa02119781:20000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC3584541917l5x6pa02119781:20000
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGwD3471541918l5x7pa02119781:20000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB2671541916l5x5pa02119781:20000
Berks-Weikert channery silt loam, 8 to 15 percent slopesBwC808830986502y0qmpa02519601:20000
Berks-Weikert channery silt loam, 3 to 8 percent slopesBwB644530986492y0qlpa02519601:20000
Berks-Weikert channery silt loam, 15 to 25 percent slopesBwD610230986512y0qnpa02519601:20000
Weikert-Berks channery silt loam, 25 to 35 percent slopesWbE447230986532y0qqpa02519601:20000
Weikert-Berks channery silt loam, 35 to 100 percent slopes, very rockyWbF258630986542y0qrpa02519601:20000
Berks-Weikert channery silt loam, 0 to 3 percent slopesBwA64030986482y0qkpa02519601:20000
Berks-Weikert channery silt loam, 15 to 25 percent slopes, rockyBxD16630986522y0qppa02519601:20000
Berks and Weikert soils, 25 to 70 percent slopesBMF282775382432xtjnpa02719751:20000
Weikert shaly silt loam, 5 to 15 percent slopesWeC2556538356l26bpa02719751:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD17365383572v4vspa02719751:20000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF102405634962wds3pa03120121:24000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC49635297602wds1pa03120121:24000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB19035297592wds0pa03120121:24000
Berks-Weikert complex, 25 to 60 percent slopesBeE9916543893l7yypa03520021:24000
Berks-Weikert complex, 15 to 25 percent slopesBeD5736543891l7ywpa03520021:24000
Weikert channery silt loam, 35 to 80 percent slopes, moderately erodedWcF2154235395702w6n9pa03719651:20000
Weikert channery silt loam, 20 to 35 percent slopes, moderately erodedWcD2149375395692w6ncpa03719651:20000
Weikert channery silt loam, 12 to 20 percent slopes, moderately erodedWcC287205395682wkc4pa03719651:20000
Weikert channery silt loam, 3 to 12 percent slopes, moderately erodedWcB284425395672wkc3pa03719651:20000
Weikert very stony silt loam, 35 to 80 percent slopesWeF2301539572l3gkpa03719651:20000
Litz and Weikert shaly silt loams, 20 to 35 percent slopes, severely erodedLrD3727539525l3f1pa03719651:20000
Litz and Weikert shaly silt loams, 35 to 50 percent slopes, moderately erodedLrE2595539526l3f2pa03719651:20000
Weikert very stony silt loam, 12 to 35 percent slopesWeD294539571l3gjpa03719651:20000
Litz and Weikert shaly silt loams, 12 to 20 percent slopes, severely erodedLrC3290539524l3f0pa03719651:20000
Weikert very channery silt loam, 8 to 15 percent slopesWeC80676937982v4vxpa04119801:15840
Weikert very channery silt loam, 15 to 25 percent slopesWeD71636937992v4vypa04119801:15840
Weikert and Klinesville very shaly silt loams, 25 to 75 percent slopesWkF5512693800r8ynpa04119801:15840
Weikert very channery silt loam, 3 to 8 percent slopesWeB22496937972v4vwpa04119801:15840
Weikert shaly silt loam, 25 to 40 percent slopes, moderately erodedWeE24221540777l4qfpa04319671:15840
Weikert shaly silt loam, 15 to 25 percent slopes, moderately erodedWeD2616540776l4qdpa04319671:15840
Weikert shaly silt loam, 5 to 15 percent slopes, moderately erodedWeC2598540775l4qcpa04319671:15840
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF1415015910872wds3pa05120051:24000
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGwD81115910862wds2pa05120051:24000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC32015910852wds1pa05120051:24000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB26115910842wds0pa05120051:24000
Weikert channery silt loam, 3 to 8 percent slopesWeB130845452312v4vrpa05519991:24000
Weikert channery silt loam, 8 to 15 percent slopesWeC122815452322v4w5pa05519991:24000
Weikert very channery silt loam, 25 to 65 percent slopesWkF97775452302wkdkpa05519991:24000
Weikert channery silt loam, 15 to 25 percent slopesWeD84905452332v4vspa05519991:24000
Weikert very channery silt loam, 8 to 15 percent slopesWkC75945452262v4vxpa05519991:24000
Weikert very channery silt loam, 15 to 25 percent slopesWkD61095452282v4vypa05519991:24000
Weikert very channery silt loam, 3 to 8 percent slopesWkB31255452242v4vwpa05519991:24000
Klinesville and Weikert soils, 25 to 60 percent slopesKWF42177544886l8zzpa05719991:24000
Weikert channery silt loam, 8 to 15 percent slopesWeC93855449472v4w5pa05719991:24000
Weikert channery silt loam, 15 to 25 percent slopesWeD66205449482v4vspa05719991:24000
Weikert channery silt loam, 3 to 8 percent slopesWeB13775449462v4vrpa05719991:24000
Berks-Weikert association, steepBMF645735419542sgbspa06119741:20000
Berks-Weikert channery silt loams, 15 to 25 percent slopesBlD209275419632sgbppa06119741:20000
Edom-Weikert complex, 15 to 25 percent slopesEgD10868541987l5zgpa06119741:20000
Edom-Weikert complex, 8 to 15 percent slopesEgC8816541986l5zfpa06119741:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD88005420472v4vspa06119741:20000
Edom-Weikert complex, 25 to 60 percent slopesEgF5287541988l5zhpa06119741:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC32425420462v4w5pa06119741:20000
Edom-Weikert complex, 3 to 8 percent slopesEgB2386541985l5zdpa06119741:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB8115420452v4vrpa06119741:20000
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGwD2809417209292wds2pa06320121:24000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF1837317209312wds3pa06320121:24000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC1225617209282wds1pa06320121:24000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB267817209272wds0pa06320121:24000
Gilpin-Weikert channery silt loams, 25 to 100 percent slopes, very stonyGxF190517208861vrqgpa06320121:24000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF716823989722wds3pa06520121:12000
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGwD394823989712wds2pa06520121:12000
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGwB195523989692wds0pa06520121:12000
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGwC182023989702wds1pa06520121:12000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGsF495129004282wds3pa07319781:15840
Weikert-Rock outcrop complex, 25 to 80 percent slopesWeF251529004732wdrzpa07319781:15840
Gilpin-Weikert channery silt loams, 15 to 25 percent slopesGsD77829004272wds2pa07319781:15840
Gilpin-Weikert channery silt loams, 8 to 15 percent slopesGsC14129004262wds1pa07319781:15840
Gilpin-Weikert channery silt loams, 3 to 8 percent slopesGsB6329004252wds0pa07319781:15840
Weikert channery silt loam, 15 to 25 percent slopesWeD359428712972v4vspa07519761:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB295528712662v4vrpa07519761:20000
Weikert shaly silt loam, 25 to 50 percent slopesWeE2408541346l59spa07519761:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC212828712802v4w5pa07519761:20000
Berks-Weikert complex, 3 to 8 percent slopes1BkB4475413512sgbhpa07519761:20000
Berks-Weikert complex, 8 to 15 percent slopes1BkC725413502sgbjpa07519761:20000
Weikert-Berks complex, 3 to 8 percent slopes1WeB65413522v4w4pa07519761:20000
Berks-Weikert complex, 25 to 60 percent slopes1BkF35413542sgcrpa07519761:20000
Weikert-Berks complex, 15 to 25 percent slopes1WeD15413532v4w3pa07519761:20000
Berks-Weikert complex, 3 to 8 percent slopesBkB201125431122sgbhpa07719971:24000
Berks-Weikert complex, 8 to 15 percent slopesBkC188215431132sgbjpa07719971:24000
Berks-Weikert complex, 25 to 60 percent slopesBkF143965431152sgcrpa07719971:24000
Berks-Weikert complex, 15 to 25 percent slopesBkD115705431142wkdrpa07719971:24000
Weikert-Berks complex, 15 to 25 percent slopesWeD16975432152v4w3pa07719971:24000
Berks-Weikert complex, 0 to 3 percent slopesBkA13395431112sgbfpa07719971:24000
Weikert-Berks complex, 3 to 8 percent slopesWeB2645432142v4w4pa07719971:24000
Weikert and Klinesville channery silt loams, 8 to 15 percent slopesWeC6772964939yj9pa07919741:20000
Weikert and Klinesville channery silt loams, 3 to 8 percent slopesWeB5202964929yj8pa07919741:20000
Weikert and Klinesville channery silt loams, 15 to 25 percent slopesWeD4452964949yjbpa07919741:20000
Weikert and Klinesville shaly silt loams, 25 to 80 percent slopesWkE53747539138l30kpa08119811:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD32035391372v4vspa08119811:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC17305391362v4w5pa08119811:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB6585391352v4vrpa08119811:20000
Weikert and Klinesville soils, steepWKE60212963679yd7pa08919751:20000
Weikert-Hartleton channery silt loams, 3 to 8 percent slopesWhB28162963739ydfpa08919751:20000
Weikert-Hartleton channery silt loams, 8 to 15 percent slopesWhC27982963749ydgpa08919751:20000
Weikert-Hartleton channery silt loams, 15 to 25 percent slopesWhD10502963759ydhpa08919751:20000
Weikert channery silt loam, 15 to 25 percent slopes, erodedWeD38362963729yddpa08919751:20000
Weikert channery silt loam, 8 to 15 percent slopes, erodedWeC36252963719ydcpa08919751:20000
Weikert channery silt loam, 3 to 8 percent slopes, erodedWeB35552963709ydbpa08919751:20000
Weikert and Klinesville shaly silt loams, steepWkE11935539035l2x7pa09319801:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD33965390342v4vspa09319801:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC29255390332v4w5pa09319801:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB12185390322v4vrpa09319801:20000
Berks-Weikert complex, 3 to 8 percent slopesBkB165265432402sgbhpa09520071:12000
Berks-Weikert complex, 8 to 15 percent slopesBkC120815432412sgbjpa09520071:12000
Berks-Weikert complex, 25 to 60 percent slopesBkF58565432432sgcrpa09520071:12000
Berks-Weikert complex, 15 to 25 percent slopesBkD47845432422wkdrpa09520071:12000
Berks-Weikert complex, 0 to 3 percent slopesBkA23445432392sgbfpa09520071:12000
Weikert-Berks complex, 8 to 15 percent slopesWkC172819489862z1p7pa09520071:12000
Weikert-Berks complex, 15 to 25 percent slopesWkD152419489872v4w3pa09520071:12000
Weikert-Berks complex, 3 to 8 percent slopesWkB100619489852v4w4pa09520071:12000
Weikert and Klinesville shaly silt loams, steepWkE33662539683l3l4pa09719801:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD84205396822v4vspa09719801:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC77045396812v4w5pa09719801:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB43335396802v4vrpa09719801:20000
Weikert and Klinesville very shaly silt loams, 25 to 75 percent slopesWkF29890694025r95xpa09919801:15840
Weikert very channery silt loam, 15 to 25 percent slopesWeD85116940242v4vypa09919801:15840
Weikert very channery silt loam, 8 to 15 percent slopesWeC41796940232v4vxpa09919801:15840
Weikert very channery silt loam, 3 to 8 percent slopesWeB18806940222v4vwpa09919801:15840
Weikert and Klinesville shaly silt loams, steepWKF31290539759l3nlpa10719771:20000
Weikert and Klinesville shaly silt loams, steepWkE23521540860l4t3pa10919801:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD166805408592v4vspa10919801:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC139305408582v4w5pa10919801:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB61315408572v4vrpa10919801:20000
Berks-Weikert association, steepBMF355408692sgbspa10919801:20000
Berks and Weikert soils, 25 to 70 percent slopesBkF23290542064l61ypa11119771:20000
Berks-Weikert channery silt loams, 15 to 25 percent slopesBkD66935420632sgbppa11119771:20000
Berks-Weikert channery silt loams, 8 to 15 percent slopesBkC41665420622sgbnpa11119771:20000
Berks-Weikert channery silt loams, 3 to 8 percent slopesBkB28405420612sgblpa11119771:20000
Weikert and Klinesville shaly silt loams, steepWkE8480540958l4x8pa11919801:20000
Weikert channery silt loam, 15 to 25 percent slopesWeD20675409572v4vspa11919801:20000
Weikert channery silt loam, 8 to 15 percent slopesWeC20535409562v4w5pa11919801:20000
Weikert channery silt loam, 3 to 8 percent slopesWeB13355409552v4vrpa11919801:20000
Gilpin-Weikert channery silt loams, 25 to 70 percent slopesGwF110525446112wds3pa12920031:24000

Map of Series Extent

Approximate geographic distribution of the WEIKERT 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 .