Official Series Description


Lab Data Summary

Aggregate lab data for the BERKS soil series. This aggregation is based on all pedons with a current taxon name of BERKS, 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 BERKS 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
114ACL77311977IN021031Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3904917,-86.9629833
114BJN78101978IN071010Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8389278,-86.0386583
120BDU76021976IN037003Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5075556,-86.7127611
120BDU76091976IN037009Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2710278,-86.7734306
120BPK81021981IN125002Berks1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3139083,-87.0731972
120B95P0231S1990IN119017Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1722641,-86.7333221
120CMR76151976IN109015Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3614278,-86.4482944
120CLW78171978IN093017Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9776278,-86.3837194
120CJN80021980IN071002Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0041889,-86.3050167
120CBR81021981IN013002Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1736111,-86.2584306
120CWS80172015IN175001Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5499806,-85.8913639
12486KY-069-00586KY-069-005Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3769951,-83.4659958
12490KY-135-00590KY-135-005Berks1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4519958,-83.455719
12586P069286WV005006Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0149994,-81.8758316
12586P068586WV047002Berks7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3958321,-81.6319427
126JF-0201984OH081020Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3916056,-80.8118417
12798P015297WV093006Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1869444,-79.6252778
128VPI0136V1992-VA005-136Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7016111,-80.1294444
14759PA0770021959PA077002Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5008333,-75.7136111
14759PA0770071959PA077007Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5625,-75.7144444
14762PA0570171962PA057017Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9908333,-78.0852778
14762PA0570181962PA057018Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0052778,-78.0608333
14764PA0270151964PA027015Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0066667,-77.6919444
14764PA0270161964PA027016Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0255556,-77.6727778
14765PA0550051965PA055005Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9636111,-77.7375
14788PA0550611988PA055061Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2361111,-77.6836111
14757PA025003S1957PA025003Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8547222,-75.5936111
14757PA025005S1957PA025005Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8547222,-75.5491667
14759PA077001S1959PA077001Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5,-75.6827778
14759PA077006S1959PA077006Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5616667,-75.7141667
14740A4032S1960WV003008Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.389473,-77.9758148
14705N0347S2004PA061003Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6649437,-77.9046402
147WVU0058S99WV031012Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9969444,-78.9311111
147WVU0059S99WV031013Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1958333,-78.9397222
147WVU0060S99WV031015Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1730556,-78.8775
147WVU0061S99WV071014Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6716667,-79.1669444
147VPI0146V1992-VA005-146Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7308333,-80.2483333
147VPI0152V1992-VA017-152Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0897222,-79.9397222
147VPI0159V1992-VA017-159Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1751667,-79.9168056
147VPI0160V1992-VA017-160Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.187725,-79.9146444
147VPI0173V1992-VA091-173Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3309167,-79.7458056
147VPI0174V1992-VA091-174Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3355833,-79.7465
147VPI0156V1992-WV075-156Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1646944,-79.9170833
147VPI0157V1992-WV075-157Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1663333,-79.9156944
147VPI0161V1992-WV075-161Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1932222,-79.8986944
n/aAS-0061962OH005006Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAS-0081962-OH005-008Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aAS-0091962-OH005-009Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0071965OH031007Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0081965OH031008Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0251969OH031025Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWN-0571975-OH169-057Berks4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a86IL1910061986IL191006Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a86IL1910071986IL191007Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a86IL1910081986IL191008Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a86IL1910111986IL191011Berks2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P066883KY195005Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P066983KY195006Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P067283KY195009Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a90P027789PA055011Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a90P027889PA055012Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a90P028389PA055017Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a90P028489PA055018Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P014797WV093001Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P014897WV093002Berks6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P015497WV093008Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4347S1963TN129002Berks3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4348S1963TN129003Berks5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BERKS, 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. IN-2012-01-19-29 | Jackson County - October 1990

    Typical pattern of soils and parent material in the Berks-Gilpin-Wellston association (Soil Survey of Jackson County, Indiana; 1990).

  2. KY-2010-09-03-20 | Lewis County - 2004

    Typical pattern of soils and parent material in the Skidmore-Shelocta-Haymond general soil map unit.

  3. KY-2010-09-03-21 | Lewis County - 2004

    Typical pattern of soils and parent material in the Covedale-Trappist general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  4. KY-2010-09-03-22 | Lewis County - 2004

    Typical pattern of soils and parent material in the Blairton-Berks-Brownsville general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  5. KY-2010-09-03-23 | Lewis County - 2004

    Typical pattern of soils and parent material in the Berks-Brownsville-Blairton general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  6. KY-2010-09-03-24 | Lewis County - 2004

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

  7. KY-2010-09-03-30 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Grigsby-Nolin-Elk-Morehead general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  8. KY-2010-09-03-32 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Carpenter-Bledsoe-Berks general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  9. KY-2010-09-03-45 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Rigley-Bledsoe-Alticrest-Berks general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  10. KY-2012-01-27-24 | Carter County - April 1983

    Pattern of soils, topography, and underlying material in the Berks-Cranston-Latham map unit (Soil Survey of Carter County, Kentucky; April 1983).

  11. KY-2012-01-27-74 | Fleming County - October 1993

    Typical pattern of soils and parent material in the Muse-Blairton-Brownsville soil map unit (Soil Survey of Fleming County, Kentucky; October 1993).

  12. KY-2012-02-01-25 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Cranston-Berks association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  13. KY-2012-02-01-26 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Berks-Cranston-Latham association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  14. KY-2012-02-01-29 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Rigley-Brookside-Steinsburg association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  15. KY-2012-02-01-30 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Rigley-Cranston-Steinsburg association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  16. KY-2012-02-01-32 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Muse-Trappist-Latham association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  17. KY-2012-02-01-36 | Montgomery County - January 1986

    The pattern of soils and relationship to topography and underlying material in the Shelocta-Berks-Bledsoe general soil map unit (Soil Survey of Montgomery County, Kentucky; January 1986).

  18. KY-2012-02-01-37 | Pike County - June 1990

    Along the Levisa and Russell Forks of the Big Sandy River, the soils in the valleys are in the Nelse-Shelbiana-Udorthents general soil map unit and those on the mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit (Soil Survey of Pike County, Kentucky; June 1990).

  19. KY-2012-02-01-39 | Pike County - June 1990

    Along Elkhorn Creek and Pine Mountain, the upper faulted mountains are in the Kimper-Sharondale-Berks-Shelocta general soil map unit, the lower mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit, and the valley is in the Yeager-Grigsby-Potomac-Hayter map unit (Soil Survey of Pike County, Kentucky; June 1990).

  20. KY-2012-02-01-41 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Carpenter-Bledsoe-Berks general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  21. 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).

  22. 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).

  23. OH-2010-09-29-11 | Columbiana County -

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

  24. OH-2010-09-29-20 | Fairfield County - 2005

    Typical pattern of soils and parent material in the Shelocta-Berks-Gilpin association (Soil Survey of Fairfield County, Ohio; 2005).

  25. OH-2012-02-16-39 | Scioto County - January 1989

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

  26. 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).

  27. 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).

  28. 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).

  29. 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).

  30. PA-2012-03-12-10 | Bedford County - 1998

    Typical pattern of soils and underlying material in the Buchanan-Dystrochrepts-Meckesville general soil map unit (Soil Survey of Bedford County, PA; 1998).

  31. 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).

  32. 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).

  33. 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).

  34. 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).

  35. 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).

  36. 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).

  37. PA-2012-03-13-19 | Cumberland and Perry Counties - April 1986

    Typical pattern of soils and underlying material in the Hazleton-Laidig-Buchanan association (Soil Survey of Cumberland and Perry Counties, PA; 1986).

  38. 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).

  39. 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).

  40. 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).

  41. 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).

  42. PA-2012-03-13-58 | Lycoming County - November 1986

    Typical pattern of soils and underlying material in the Watson-Allenwood-Alvira association (Soil Survey of Lycoming County, PA; 1986).

  43. 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).

  44. 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).

  45. 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).

  46. 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).

  47. PA-2012-03-14-11 | Snyder County - April 1985

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

  48. 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).

  49. 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).

  50. 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).

  51. VA-2010-11-05-07 | Buchanan County -

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia).

  52. VA-2010-11-05-14 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from "Geology of the Virginia Portion of the Clintwood and Jenkings East Quadrangles" (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  53. VA-2010-11-05-15 | Dickenson 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 Dickenson County, Virginia; 2009).

  54. VA-2010-11-05-16 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  55. VA-2010-11-05-26 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  56. VA-2010-11-05-27 | Lee County - 2006

    Typical pattern of soils in areas of Powell Mountain, Wallen Ridge, and Poor Valley Ridge. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  57. VA-2010-11-05-30 | Russell County - 2007

    Diagram of a sequence of landform positions in areas underlain with limestone, shale, and sandstone in Russell County. 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 Russell County, Virginia; 2007).

  58. VA-2010-11-05-31 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. 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 Russell County, Virginia; 2007).

  59. VA-2010-11-05-32 | Russell County - 2007

    Diagram of a sequence of landform positions along the Clinch River in areas underlain with limestone and shale in Russell County. 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 Russell County, Virginia; 2007).

  60. 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).

  61. VA-2012-05-10-04 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  62. VA-2012-05-11-01 | Dickenson 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 Dickenson County, Virginia; 2009).

  63. VA-2012-05-11-02 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  64. VA-2012-05-11-04 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from “Geology of the Virginia Portion of the Clintwood and Jenkins East Quadrangles” (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  65. VA-2012-05-11-07 | Lee County - 2006

    Typical pattern of soils in the Appalachian Plateau portion of Lee County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  66. VA-2012-05-11-08 | Lee County - 2006

    Typical pattern of soils in areas of Powell Mountain, Wallen Ridge, and Poor Valley Ridge. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to parent material and landform position (Soil Survey of Lee County, Virginia; 2006).

  67. VA-2012-05-11-11 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. 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 Russell County, Virginia; 2007).

  68. VA-2012-05-11-12 | Russell County - 2007

    Diagram of a sequence of landform positions along the Clinch River in areas underlain with limestone and shale in Russell County. 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 Russell County, Virginia; 2007).

  69. VA-2012-05-11-13 | Russell County - 2007

    Diagram of a sequence of landform positions in areas underlain with limestone, shale, and sandstone in Russell County. 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 Russell County, Virginia; 2007).

  70. 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).

  71. WV-2010-11-08-13 | McDowell County - 2004

    Typical relationship of the soils and underlying parent material in the Pineville-Berks general soil map unit (Soil Survey of McDowell County, West Virginia; 2004).

  72. 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).

  73. WV-2012-03-23-10 | Wyoming County - September 1988

    Typical relationship of the soils and the underlying parent material in the Berks-Pineville general soil map unit (Soil Survey of Wyoming County, WV; 1988).

Map Units

Map units containing BERKS 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
Wellston-Berks complex, 12 to 60 percent slopes, eroded986F28623211713739gil05919661:20000
Wellston-Berks complex, 18 to 35 percent slopes986F7695713970ryy9il06920031:12000
Muskingum and Berks soils, 35 to 70 percent slopes955G2313713958ryxxil06920031:12000
Muskingum and Berks soils, 18 to 35 percent slopes955F2209713957ryxwil06920031:12000
Wellston-Berks complex, 35 to 70 percent slopes986G1284713971ryybil06920031:12000
Wellston-Berks complex, 10 to 18 percent slopes986D162713967ryy6il06920031:12000
Muskingum and Berks soils, 10 to 18 percent slopes955D104713955ryxtil06920031:12000
Wellston-Berks complex, 18 to 35 percent slopes986F20829114565717g4pil08720051:12000
Wellston-Berks complex, 10 to 18 percent slopes, eroded986D210294114565517g4mil08720051:12000
Berks, Muskingum, and Weikert soils, 35 to 70 percent slopes793G375714021141j20hil08720051:12000
Berks, Muskingum, and Weikert soils, 18 to 35 percent slopes793F125114021131j20gil08720051:12000
Wellston-Berks complex, 10 to 18 percent slopes, severely eroded986D3628114565617g4nil08720051:12000
Wellston-Berks complex, 10 to 18 percent slopes986D46416039341qv0til08720051:12000
Muskingum and Berks soils, 18 to 35 percent slopes955F29416057901qwypil08720051:12000
Muskingum and Berks soils, 35 to 70 percent slopes955G216087681r01ril08720051:12000
Wellston-Berks complex, 18 to 35 percent slopes986F832808066w3vnil12720041:12000
Muskingum and Berks soils, 18 to 35 percent slopes955F188808053w3v7il12720041:12000
Wellston-Berks complex, 35 to 70 percent slopes986G160808067w3vpil12720041:12000
Muskingum and Berks soils, 35 to 70 percent slopes955G71808054w3v8il12720041:12000
Muskingum and Berks soils, 10 to 18 percent slopes, eroded955D230808052w3v6il12720041:12000
Wellston-Berks complex, 10 to 18 percent slopes986D21808063w3vkil12720041:12000
Muskingum and Berks soils, 10 to 18 percent slopes955D20808051w3v5il12720041:12000
Wellston-Berks complex, 10 to 18 percent slopes, eroded986D210808064w3vlil12720041:12000
Wellston-Berks complex, 18 to 35 percent slopes986F14620606799ncf5il15120031:12000
Muskingum and Berks soils, 18 to 35 percent slopes955F7267606800ncf6il15120031:12000
Wellston-Berks complex, 10 to 18 percent slopes986D5559608491nf5ril15120031:12000
Muskingum and Berks soils, 10 to 18 percent slopes955D1288639880pgv9il15120031:12000
Muskingum and Berks soils, 35 to 70 percent slopes955G1189606801ncf7il15120031:12000
Wellston-Berks complex, 35 to 70 percent slopes986G632636700pcjqil15120031:12000
Wellston-Berks complex, 10 to 18 percent slopes, eroded986D273637431pd99il15120031:12000
Muskingum and Berks soils, 10 to 18 percent slopes, eroded955D232639881pgvbil15120031:12000
Wellston-Berks complex, 15 to 30 percent slopes986F93101789086057il16519741:15840
Berks-Wellston complex, 30 to 60 percent slopes986G30441789096058il16519741:15840
Berks loam, 18 to 35 percent slopes784F76115439261ntl2il19320061:12000
Berks, Muskingum, and Weikert soils, 18 to 35 percent slopes793F279014780431lm0til19920071:12000
Wellston-Berks complex, 18 to 35 percent slopes986F74414782021lm5yil19920071:12000
Berks, Muskingum, and Weikert soils, 35 to 70 percent slopes793G49214780441lm0vil19920071:12000
Wellston-Berks complex, 10 to 18 percent slopes, eroded986D218717117371vg6bil19920071:12000
Wellston-Berks complex, 10 to 18 percent slopes, severely eroded986D32417131121vhmpil19920071:12000
Berks-Trevlac-Wellston complex, 20 to 70 percent slopesBgF97293535583kz9win01319851:15840
Wellston-Berks-Trevlac complex, 6 to 20 percent slopesWaD19210535611kzbsin01319851:15840
Berks channery silt loam, 25 to 75 percent slopesBeG12716122641r3pjin01319851:15840
Berks-Gilpin complex, 30 to 70 percent slopesBdF11531595915c23in02119801:15840
Gilpin-Berks complex, 25 to 50 percent slopesGbF25861629415gk5in02719691:20000
Gilpin-Berks complex, 20 to 50 percent slopesGoF21154535628kzcbin03719781:15840
Gilpin-Berks complex 30 to 60 percent slopesGfF65721615455f34in05519841:15840
Berks-Ebal complex, 15 to 60 percent slopesBcF65501615215f2cin05519841:15840
Berks-Rock outcrop complex, 45 to 70 percent slopesBfG9971615225f2din05519841:15840
Berks channery silt loam, 35 to 80 percent slopesBfG215651631965gtdin10919791:15840
Gilpin-Berks loams, 25 to 50 percent slopesGoF11621619075fgtin12519831:15840
Berks channery silt loam, 25 to 60 percent slopesBkF1791638545hhmin15719901:15840
Gilpin-Berks loams, 18 to 50 percent slopesGnF10177535485kz6qin17519841:15840
Gilpin-Berks-Ebal complex, 18 to 50 percent slopesGpF3544535486kz6rin17519841:15840
Brownsville-Berks channery silt loams, 30 to 70 percent slopes, extremely stonyBxF493917275281vzmqky01120061:12000
Berks channery silt loam, 20 to 50 percent slopesBsF145917275271vzmpky01120061:12000
Berks channery silt loam, 6 to 20 percent slopesBsD42717275261vzmnky01120061:12000
Berks-Cranston association, steepBCF16610550234lgkhky04319801:20000
Brownsville-Berks complex, very rocky, 20 to 55 percent slopes, erodedBwF211499552700lk41ky06919891:20000
Berks-Brownsville complex, 30 to 60 percent slopes, erodedBkF22084552695lk3wky06919891:20000
Berks-Brownsville complex, 30 to 55 percent slopes, very rocky, erodedBnF266973550277lglwky13519981:20000
Berks-Brownsville-Shelocta complex, 30 to 65 percent slopes, erodedBoF251455550278lglxky13519981:20000
Brownsville-Berks complex, 30 to 60 percent slopes, erodedBvF224537550283lgm2ky13519981:20000
Shelocta-Berks complex, 20 to 60 percent slopesSlF5140550543lgwgky17319831:20000
Berks-Rock outcrop-Marrowbone complex, 60 to 120 percent slopesBrG4432550027lgbtky19519861:24000
Berks-Caneyville complex, 50 to 120 percent slopes, very rockyBcG1627550026lgbsky19519861:24000
Berks-Cranston channery silt loams, 30 to 60 percent slopesBcF32140550386lgqdky60519751:20000
Carpenter-Bledsoe-Berks complex, 20 to 70 percent slopes, stonyCkF181105577542w8hyky61620041:24000
Berks-Caneyville complex, 50 to 120 percent slopes, very rockyBcG273550722lh27ky62619971:24000
Carpenter-Bledsoe-Berks complex, 20 to 70 percent slopes, stonyCkF326785508232w8hyky63419891:20000
Bledsoe-Berks-Rock outcrop complex, 20 to 70 percent slopesBsF9064550822lh5gky63419891:20000
Berks-Cranston complex, 40 to 60 percent slopes, very stonyBcF1147550927lh8vky64119941:24000
Berks silt loam, 40 to 70 percent slopesBeF4458314787501lmrmky64519711:20000
Berks channery silt loam, 8 to 15 percent slopesBcC427624010452sgcgmd00120091:12000
Berks channery silt loam, 3 to 8 percent slopesBcB288924010442sgb5md00120091:12000
Berks flaggy silt loam, 25 to 45 percent slopesBdE220618681312sftvmd00120091:12000
Berks flaggy silt loam, 15 to 25 percent slopesBdD149724010392llgwmd00120091:12000
Berks channery silt loam, 15 to 25 percent slopesBcD147224010462sgb7md00120091:12000
Berks flaggy silt loam, 8 to 15 percent slopesBdC48324010382llgvmd00120091:12000
Berks flaggy silt loam, 3 to 8 percent slopesBdB37624010372llgtmd00120091:12000
Berks-Urban land complex, 8 to 15 percent slopesBeC20924010112llfzmd00120091:12000
Berks-Urban land complex, 0 to 8 percent slopesBeB16924010102llfymd00120091:12000
Berks channery silt loam, 0 to 3 percent slopesBcA14124010432sgcmmd00120091:12000
Berks channery silt loam, 3 to 8 percent slopesBeB27795341492sgb5md04319981:12000
Weikert-Berks channery silt loams, 15 to 25 percent slopesWkD16105347412v4w1md04319981:12000
Weikert-Berks channery silt loams, 8 to 15 percent slopesWkC15965347402v4w0md04319981:12000
Berks channery silt loam, 8 to 15 percent slopesBeC11595341522sgcgmd04319981:12000
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
Berks channery loam, 6 to 12 percent slopes, erodedBegC2843548578ldv2nj01919701:24000
Berks channery loam, 12 to 18 percent slopes, erodedBegD2587548579ldv3nj01919701:24000
Berks channery loam, 2 to 6 percent slopesBegB278548577ldv1nj01919701:24000
Berks channery silt loam, 3 to 8 percent slopesBekB1442189605721n04nj04120071:12000
Berks channery silt loam, 25 to 45 percent slopesBekE1289189636621nb3nj04120071:12000
Berks channery silt loam, 0 to 3 percent slopesBekA171189605621n03nj04120071:12000
Urban land-Berks complex, 3 to 8 percent slopesUSBEKB11819078162217gnj04120071:12000
Urban land-Berks complex, 0 to 3 percent slopesUSBEKA1019078152217fnj04120071:12000
Shelocta-Berks association, very steepShF329771701205q0roh00119871:15840
Shelocta-Berks association, steepShE56291701195q0qoh00119871:15840
Berks silt loam, 15 to 25 percent slopesBkD46211700735pz7oh00119871:15840
Berks-Rock outcrop complex, 30 to 60 percent slopesBsG19522881329ntloh00519761:15840
Berks channery silt loam, 12 to 18 percent slopesBrD3852881319ntkoh00519761:15840
Berks-Westmoreland silt loams, 40 to 70 percent slopesBkF6240537339l14joh00919811:15840
Elba-Brookside-Berks complex, 40 to 70 percent slopesEbF4480537355l151oh00919811:15840
Berks-Westmoreland silt loams, 25 to 40 percent slopesBkE760537338l14hoh00919811:15840
Berks-Westmoreland silt loams, 15 to 25 percent slopesBkD320537337l14goh00919811:15840
Westmoreland-Berks complex, 40 to 70 percent slopesWnF1817104901vdx3oh01319781:15840
Berks channery silt loam, 25 to 35 percent slopesBkE115415379662s5hmoh01919811:15840
Berks shaly silt loam, 15 to 25 percent slopesBkD8166537965l1sqoh01919811:15840
Berks channery silt loam, 8 to 15 percent slopesBkC63055379642s5hloh01919811:15840
Berks channery silt loam, 3 to 8 percent slopesBkB27115379632s5hjoh01919811:15840
Berks channery silt loam, 35 to 70 percent slopesBkF10025379672s5hnoh01919811:15840
Berks channery silt loam, 6 to 15 percent slopesBsC55716700131t1sdoh01919811:15840
Berks channery silt loam, 15 to 25 percent slopesBsD55116700142s5hhoh01919811:15840
Berks channery silt loam, 25 to 40 percent slopesBsE49416700151t1sgoh01919811:15840
Berks channery silt loam, 2 to 6 percent slopesBsB22116706771t2gtoh01919811:15840
Berks channery silt loam, 25 to 35 percent slopesBkE191532987382s5hmoh02920051:12000
Berks channery silt loam, 15 to 25 percent slopesBkD135362987372s5hhoh02920051:12000
Berks channery silt loam, 8 to 15 percent slopesBkC130622987362s5hloh02920051:12000
Westmoreland-Berks complex, 40 to 70 percent slopesWkF6858298848b0z8oh02920051:12000
Westmoreland-Berks complex, 25 to 40 percent slopesWkE3530298847b0z7oh02920051:12000
Berks channery silt loam, 3 to 8 percent slopesBkB31992987352s5hjoh02920051:12000
Upshur-Berks complex, 25 to 40 percent slopes, erodedUkE2735298834b0ytoh02920051:12000
Upshur-Berks complex, 15 to 25 percent slopes, erodedUkD2602298833b0ysoh02920051:12000
Berks-Urban land complex, 6 to 15 percent slopesBmC532631456p62koh02920051:12000
Upshur-Berks complex, 6 to 15 percent slopes, erodedUkC2478298832b0yroh02920051:12000
Berks-Urban land complex, 15 to 25 percent slopesBmD335631455p62joh02920051:12000
Berks-Urban land complex, 2 to 6 percent slopesBmB103300246b2fcoh02920051:12000
Shelocta-Berks complex, 25 to 40 percent slopesSeE79621723062wdq7oh04519981:12000
Berks channery silt loam, 35 to 70 percent slopesBkF6241722262s5hnoh04519981:12000
Berks-Upshur association, very steepBcF8690536791l0kvoh05319881:15840
Westmoreland-Berks complex, 40 to 70 percent slopesWnF11696536966l0rhoh05919981:15840
Berks channery silt loam, 35 to 70 percent slopesBeF106665368702s5hnoh05919981:15840
Berks channery silt loam, 25 to 35 percent slopesBeE61045368692s5hmoh05919981:15840
Elba-Berks complex, 40 to 70 percent slopesEkF1208536895l0p6oh05919981:15840
Berks channery silt loam, 15 to 25 percent slopesBeD8775368682s5hhoh05919981:15840
Berks channery silt loam, 8 to 15 percent slopesBeC3295368672s5hloh05919981:15840
Berks channery silt loam, 25 to 35 percent slopesBkE48285367142s5hmoh06719931:15840
Berks-Guernsey complex, 25 to 40 percent slopesBnE4824536718l0hhoh06719931:15840
Berks channery silt loam, 35 to 70 percent slopesBkF44335367152s5hnoh06719931:15840
Berks-Guernsey complex, 15 to 25 percent slopesBnD1123536717l0hgoh06719931:15840
Berks channery silt loam, 15 to 25 percent slopesBkD6085367132s5hhoh06719931:15840
Berks-Aaron complex, 6 to 15 percent slopesBmC495536716l0hfoh06719931:15840
Berks channery silt loam, 6 to 15 percent slopesBkC359536712l0h9oh06719931:15840
Berks-Guernsey complex, 8 to 15 percent slopesBnC3916954961tx9foh06719931:15840
Berks channery silt loam, 8 to 15 percent slopesBeC416954892s5hloh06719931:15840
Berks-Muskingum-Neotoma channery silt loams, 35 to 50 percent slopesBhG32314203611jp03oh07119731:15840
Shelocta-Berks association, very steepSeF30814206791jpbcoh07119731:15840
Berks-Muskingum channery silt loams, 35 to 50 percent slopesBgG30014203581jp00oh07119731:15840
Berks-Muskingum-Neotoma channery silt loams, 18 to 35 percent slopesBhF27814203601jp02oh07119731:15840
Berks-Muskingum-Neotoma channery silt loams, 6 to 18 percent slopesBhD27014203591jp01oh07119731:15840
Berks-Muskingum channery silt loams, 18 to 35 percent slopesBgF19214203571jnzzoh07119731:15840
Shelocta-Berks association, steepSeE1514206781jpbboh07119731:15840
Berks channery silt loam, 12 to 20 percent slopesBfD214205541jp6boh07119731:15840
Shelocta-Berks complex, 25 to 40 percent slopesSbE3063513980962wdq7oh07319861:15840
Westmoreland-Berks complex, 40 to 70 percent slopesWpF122713981101hxvboh07319861:15840
Berks-Westmoreland silt loams, 40 to 70 percent slopesBkF55713982301hxz6oh07319861:15840
Westmoreland-Berks complex, 25 to 40 percent slopesWpE54813981091hxv9oh07319861:15840
Berks-Tarhollow complex, 6 to 15 percent slopesBnC17813981821hxxnoh07319861:15840
Berks-Westmoreland silt loams, 25 to 40 percent slopesBkE12713982291hxz5oh07319861:15840
Berks-Westmoreland silt loams, 15 to 25 percent slopesBkD2213982281hxz4oh07319861:15840
Berks channery silt loam, 35 to 70 percent slopesBrF1213981942s5hnoh07319861:15840
Berks channery silt loam, 12 to 20 percent slopesBrD113981831hxxpoh07319861:15840
Berks silt loam, 25 to 35 percent slopes, very stonyBkE49342868669mhroh07519891:15840
Berks silt loam, 35 to 70 percent slopes, very stonyBkF48012868679mhsoh07519891:15840
Berks silt loam, 15 to 25 percent slopes, very stonyBkD17242868659mhqoh07519891:15840
Berks silt loam, 25 to 70 percent slopesBeF6316769951t91moh07519891:15840
Westmoreland-Berks complex, 40 to 70 percent slopesWtF14647536132kzwloh08119871:15840
Berks-Guernsey complex, 15 to 25 percent slopesBmD9440536056kzt4oh08119871:15840
Berks-Guernsey complex, 8 to 15 percent slopesBmC4400536055kzt3oh08119871:15840
Berks-Guernsey complex, 25 to 40 percent slopesBmE3816536057kzt5oh08119871:15840
Westmoreland-Berks complex, 25 to 40 percent slopesWtE3809536131kzwkoh08119871:15840
Berks shaly silt loam, 15 to 25 percent slopesBkD1234536054kzt2oh08119871:15840
Berks channery silt loam, 8 to 15 percent slopesBkC11155360532s5hloh08119871:15840
Berks channery silt loam, 3 to 8 percent slopesBkB3385360522s5hjoh08119871:15840
Berks channery silt loam, 6 to 15 percent slopesBeC2616529731sh1qoh08119871:15840
Berks-Aaron complex, 6 to 15 percent slopesBlC516529231sh03oh08119871:15840
Upshur-Berks complex, 6 to 15 percent slopes, erodedUkC2416529831sh21oh08119871:15840
Berks channery silt loam, 15 to 25 percent slopesBeD316529742s5hhoh08119871:15840
Berks channery silt loam, 2 to 6 percent slopesBeB116529721sh1poh08119871:15840
Berks-Rock outcrop complex, 30 to 60 percent slopesBeG115930541qgpvoh08319831:15840
Berks-Upshur association, very steepBcF11914550791kv41oh08719891:15840
Berks channery silt loam, 2 to 6 percent slopesBgB4451709975qy1oh08919861:15840
Berks channery silt loam, 15 to 25 percent slopesBgD3701709982s5hhoh08919861:15840
Berks-Westmoreland complex, 40 to 70 percent slopesBhF315407621nq90oh08919861:15840
Berks silt loam, 25 to 50 percent slopesBeF7081710945r15oh09119771:15840
Berks silt loam, 18 to 25 percent slopesBeE2251710935r14oh09119771:15840
Berks silt loam, 25 to 70 percent slopesBrF11402883089p08oh10319741:15840
Berks-Westmoreland silt loams, 40 to 70 percent slopesBkF515274121n8dcoh10519911:15840
Berks-Westmoreland complex, 35 to 70 percent slopesBeF1328537422l176oh11519921:15840
Berks-Westmoreland complex, 40 to 70 percent slopesBfF89715411281nqntoh11519921:15840
Berks channery silt loam, 35 to 70 percent slopesBdF5955374212s5hnoh11519921:15840
Berks-Westmoreland complex, 40 to 70 percent slopesBkF21175537858l1p8oh11919891:15840
Berks channery silt loam, 25 to 35 percent slopesBeE75015378572s5hmoh11919891:15840
Berks channery silt loam, 15 to 25 percent slopes, erodedBeD21585537856l1p6oh11919891:15840
Westmoreland-Berks complex, 40 to 70 percent slopesWrF29814256331jvh5oh11919891:15840
Berks channery silt loam, 3 to 8 percent slopesBeB1615378552s5hjoh11919891:15840
Berks channery silt loam, 15 to 25 percent slopesBeD11114256202s5hhoh11919891:15840
Berks channery silt loam, 2 to 6 percent slopesBgB614256421jvhgoh11919891:15840
Berks channery silt loam, 35 to 70 percent slopesBkF141935369802s5hnoh12119861:15840
Berks channery silt loam, 25 to 35 percent slopesBkE23505369792s5hmoh12119861:15840
Berks channery silt loam, 40 to 70 percent slopesBcF200014817961lqxwoh12119861:15840
Berks shaly silt loam, 15 to 25 percent slopesBkD1700536978l0rwoh12119861:15840
Berks shaly silt loam, 8 to 15 percent slopesBkC300536977l0rvoh12119861:15840
Berks channery silt loam, 15 to 25 percent slopesBcD16514817942s5hhoh12119861:15840
Berks channery silt loam, 25 to 40 percent slopesBcE15014817951lqxvoh12119861:15840
Berks channery silt loam, 8 to 15 percent slopesBcC314817932s5hloh12119861:15840
Berks-Westmoreland complex, 40 to 70 percent slopesBcF14515416581nr6xoh12719841:15840
Berks channery silt loam, 25 to 35 percent slopesBbE5715416572s5hmoh12719841:15840
Berks channery silt loam, 12 to 18 percent slopesBrD9321707245qn7oh13919711:15840
Berks channery silt loam, 2 to 6 percent slopesBrB4061707225qn5oh13919711:15840
Berks channery silt loam, 6 to 12 percent slopesBrC3251707235qn6oh13919711:15840
Berks-Rock outcrop complex, steepBsF2311707255qn8oh13919711:15840
Berks-Tarhollow complex, 6 to 15 percent slopesBgC37271708415qs0oh14119971:15840
Berks channery silt loam, 12 to 20 percent slopesBeD3761708395qryoh14119971:15840
Berks channery silt loam, 20 to 35 percent slopesBeE1871708405qrzoh14119971:15840
Berks channery silt loam, 8 to 15 percent slopesBeC89135372212s5hloh14519841:15840
Berks silt loam, 12 to 18 percent slopesBeD2615954721qk6voh15119671:15840
Berks channery silt loam, 35 to 70 percent slopesBlF415954852s5hnoh15119671:15840
Berks silt loam, 18 to 25 percent slopesBeE315954731qk6woh15119671:15840
Westmoreland-Berks complex, 25 to 40 percent slopesWyE115955231qk8hoh15119671:15840
Berks channery silt loam, 25 to 35 percent slopesBkE115955042s5hmoh15119671:15840
Berks channery silt loam, 25 to 70 percent slopesBeF476825294wpsdoh15319691:20000
Berks channery silt loam, 25 to 35 percent slopesBkE214105362782s5hmoh15719811:15840
Berks channery silt loam, 35 to 70 percent slopesBkF130755362792s5hnoh15719811:15840
Berks shaly silt loam, 15 to 25 percent slopesBkD3400536277l018oh15719811:15840
Berks shaly silt loam, 8 to 15 percent slopesBkC1730536276l017oh15719811:15840
Berks channery silt loam, 25 to 40 percent slopesBfE129215893701qbw0oh15719811:15840
Berks silt loam, 3 to 8 percent slopesBeB560536275l016oh15719811:15840
Berks channery silt loam, 40 to 70 percent slopesBfF41515893711qbw1oh15719811:15840
Berks channery silt loam, 8 to 15 percent slopesBfC8115893692s5hloh15719811:15840
Berks channery silt loam, 6 to 15 percent slopesBrC1915893831qbwfoh15719811:15840
Berks channery silt loam, 15 to 25 percent slopesBfD1915893822s5hhoh15719811:15840
Berks-Tarhollow complex, 6 to 15 percent slopesBgC3482536355l03soh16319981:15840
Shelocta-Berks complex, 25 to 40 percent slopesSfE50214818492wdq7oh16319981:15840
Berks silt loam, 25 to 70 percent slopesBrF80132871629mt9oh16919811:15840
Berks silt loam, 18 to 25 percent slopesBrE10702871619mt8oh16919811:15840
Berks silt loam, 12 to 18 percent slopesBrD4862871609mt7oh16919811:15840
Berks-Rock outcrop complex, 30 to 60 percent slopesBvG122169342ddx0oh16919811:15840
Berks channery silt loam, 8 to 15 percent slopesBkC194825417662sgcgpa00919891:24000
Berks channery silt loam, 15 to 25 percent slopesBkD186455417672sgb7pa00919891:24000
Berks channery silt loam, 25 to 35 percent slopesBkE142995417682sgbbpa00919891:24000
Bedington-Berks complex, 25 to 35 percent slopes, very stonyBdE11877541764l5r8pa00919891:24000
Berks channery silt loam, 3 to 8 percent slopesBkB65115417652sgb5pa00919891:24000
Bedington-Berks complex, 15 to 25 percent slopes, very stonyBdD6246541763l5r7pa00919891:24000
Bedington-Berks complex, 15 to 25 percent slopesBcD4253541761l5r5pa00919891:24000
Bedington-Berks complex, 8 to 15 percent slopes, very stonyBdC3548541762l5r6pa00919891:24000
Bedington-Berks complex, 8 to 15 percent slopesBcC3223541760l5r4pa00919891:24000

Map of Series Extent

Approximate geographic distribution of the BERKS 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 .