Official Series Description


Lab Data Summary

Aggregate lab data for the CLYMER soil series. This aggregation is based on all pedons with a current taxon name of CLYMER, 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 CLYMER were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12461PA0630581961PA063058Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8680556,-78.9763889
12402N0242S01PA031060Clymer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3058891,-79.5940857
12461PA063055S1965PA063002Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8694444,-79.0319444
12782PA0810521982PA081052Clymer2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5230556,-77.4827778
12787PA0270831987PA027083Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8516667,-78.2097222
12788PA0330331988PA033033Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1325,-78.5752778
12788PA0330351988PA033035Clymer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1336111,-78.4202778
12788PA0350211988PA035021Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2219444,-77.7525
12788PA0510211988PA051021Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9344444,-79.4341667
12779PA08300879PA083008Clymer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6266667,-78.9416667
12780P035180WV067005Clymer7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1605568,-80.8838882
12780P035280WV067006Clymer7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.163887,-80.8652802
12701P006698PA129121Clymer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.335556,-79.0208359
12701P006798PA129123Clymer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3402786,-79.023613
12707N0394S2002PA065001Clymer6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3254166,-79.0477219
14766PA1070051966PA107005Clymer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8013889,-76.1516667
14766PA1070061966PA107006Clymer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7358333,-76.3088889
n/aCS-0091965-OH031-009Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0101965-OH031-010Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0131965-OH031-013Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCS-0141965-OH031-014Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTU-F011967-OH157-F01Clymer2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTU-F021967-OH157-F02Clymer3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aTU-f031967-OH157-F03Clymer2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0081978-OH079-008Clymer4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

Geomorphic description summaries for the CLYMER 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 hills figure.

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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 CLYMER, 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-2012-02-01-19 | McCreary-Whitley Area - 1970

    General location of the Wellston, Muse, and Clymer soils on broad, gently rolling to rolling uplands in association 4 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  2. KY-2012-02-01-21 | McCreary-Whitley Area - 1970

    General location of the Clymer and Dekalb soils on a gently rolling to rolling plateau in association 6 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  3. KY-2012-02-01-22 | McCreary-Whitley Area - 1970

    General location of Tate, Clymer, and Dekalb soils and of sandstone cliffs that are characteristic of association 7 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  4. KY-2012-02-01-24 | McCreary-Whitley Area - 1970

    The relationship of rock formations and relief to some of the soil associations on the general soil map of the McCreary-Whitley Area (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  5. 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).

  6. 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).

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

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

  8. 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).

  9. 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).

  10. PA-2012-03-13-07 | Centre County - August 1981

    Typical pattern of soils and underlying material in association 1 (Soil Survey of Centre County, PA; 1981).

  11. PA-2012-03-13-13 | Clearfield County - August 1988

    Typical pattern of soils and underlying material in the Cookport-Hazleton-Clymer association (Soil Survey of Clearfield County, PA; 1988).

  12. PA-2012-03-13-14 | Clearfield County - August 1988

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

  13. 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).

  14. PA-2012-03-13-21 | Cumberland and Perry Counties - April 1986

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

  15. PA-2012-03-13-37 | Indiana County - January 1968

    Parent material, position, and pattern of soils in the Dekalb-Clymer-Cookport association (Soil Survey of Indiana County, PA; 1968).

  16. PA-2012-03-13-51 | Lancaster County - May 1985

    Typical pattern of soils and underlying material in the Clymer-Chester unit (Soil Survey of Lancaster County, PA; 1985).

  17. PA-2012-03-13-59 | Lycoming County - November 1986

    Typical pattern of soils and underlying material in the Dekalb-Laidig-Buchanan association (Soil Survey of Lycoming County, PA; 1986).

Map Units

Map units containing CLYMER 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
Clymer loam, 3 to 8 percent slopesCmB20424011012lljwmd00120091:12000
Clymer loam, 8 to 15 percent slopesCmC12624011022lljxmd00120091:12000
Clymer loam, 0 to 3 percent slopesCmA8524011002lljvmd00120091:12000
Clymer channery loam, 0 to 10 percent slopesCrB1740532904kwjgmd02319701:20000
Clymer loam, 8 to 15 percent slopesCmC1000537348l14toh00919811:15840
Steinsburg-Clymer association, steepScE10366536841l0mgoh05319881:15840
Clymer silt loam, 3 to 8 percent slopesCkB307536796l0l0oh05319881:15840
Clymer loam, 15 to 25 percent slopesChD288536795l0kzoh05319881:15840
Clymer silt loam, 8 to 15 percent slopesCkC241536797l0l1oh05319881:15840
Clymer silt loam, 8 to 15 percent slopesCkC12011536014kzrsoh07919811:15840
Clymer loam, 15 to 25 percent slopesChD11551536012kzrqoh07919811:15840
Rigley-Clymer association, steepRmE10609536042kzspoh07919811:15840
Clymer silt loam, 3 to 8 percent slopesCkB736536013kzrroh07919811:15840
Steinsburg-Clymer association, steepSrE47014605151l0sdoh07919811:15840
Steinsburg-Clymer association, steepSfE2456536183kzy7oh08719891:15840
Clymer loam, 15 to 25 percent slopesChD1416890331tpkyoh13119841:15840
Rigley-Clymer association, steepRkE416890401tpl5oh13119841:15840
Clymer silt loam, 8 to 15 percent slopesCkC416890352t32moh13119841:15840
Clymer silt loam, 8 to 15 percent slopesCkC2114608171l134oh14519841:15840
Steinsburg-Clymer association, steepSvE7214818451lqzgoh16319981:15840
Clymer silt loam, 8 to 15 percent slopesCrC2914818431lqzdoh16319981:15840
Clymer silt loam, 12 to 18 percent slopesClD733536465l07boh16719731:15840
Clymer silt loam, 6 to 12 percent slopesClC613536464l079oh16719731:15840
Clymer silt loam, 8 to 15 percent slopesCmC14625416652t32mpa00319731:15840
Clymer silt loam, 15 to 25 percent slopesCmD1458541666l5n3pa00319731:15840
Clymer silt loam, 3 to 8 percent slopesCmB950541664l5n1pa00319731:15840
Clymer loam, 8 to 15 percent slopesCmC408829002502t32kpa00719781:15840
Clymer loam, 3 to 8 percent slopesCmB287231800342t32jpa00719781:15840
Clymer loam, 15 to 25 percent slopesCmD63029002512t32lpa00719781:15840
Hazleton-Clymer association, 8 to 25 percent slopes, extremely stonyHTC19627541799l5sdpa00919891:24000
Hazleton-Clymer association, 25 to 45 percent slopes, extremely stonyHTE13662541800l5sfpa00919891:24000
Clymer very stony loam, 3 to 8 percent slopesCyB3200542339l6btpa01319781:20000
Clymer very stony loam, 8 to 25 percent slopesCyD1822542340l6bvpa01319781:20000
Clymer loam, 3 to 8 percent slopesCvB983542338l6bspa01319781:20000
Clymer loam, 3 to 8 percent slopesCmB30785381632t32jpa01919841:15840
Clymer silt loam, 8 to 15 percent slopesCmC15382282t32mpa01919841:15840
Clymer very stony sandy loam, 0 to 8 percent slopesCvB26080538266l23fpa02719751:20000
Clymer very stony sandy loam, 8 to 25 percent slopesCvD9496538267l23gpa02719751:20000
Clymer sandy loam, 3 to 8 percent slopesClB2761538264l23cpa02719751:20000
Clymer sandy loam, 8 to 15 percent slopesClC646538265l23dpa02719751:20000
Clymer channery loam, 3 to 8 percent slopesClB5460563167lx0ppa03120121:24000
Clymer channery loam, 8 to 15 percent slopesClC2447563168lx0qpa03120121:24000
Clymer loam, 0 to 8 percent slopes, very stonyCnB1905524750km1fpa03120121:24000
Clymer channery loam, 0 to 3 percent slopesClA890529780ks8ppa03120121:24000
Clymer loam, 0 to 8 percent slopesCmB471886499yrgrpa03120121:24000
Clymer loam, 8 to 15 percent slopesCmC65886498yrgqpa03120121:24000
Hazleton-Clymer very stony loams, 0 to 8 percent slopesHdB23016538539l2d7pa03319811:20000
Clymer channery loam, 3 to 8 percent slopesClB13574538512l2ccpa03319811:20000
Hazleton-Clymer channery loams, 3 to 8 percent slopesHcB8911538537l2d5pa03319811:20000
Clymer very stony loam, 0 to 8 percent slopesCmB6808538514l2cfpa03319811:20000
Hazleton-Clymer channery loams, 8 to 15 percent slopesHcC6419538538l2d6pa03319811:20000
Clymer channery loam, 8 to 15 percent slopesClC4171538513l2cdpa03319811:20000
Clymer very stony loam, 8 to 15 percent slopesCmC2606538515l2cgpa03319811:20000
Hazleton-Clymer channery loams, 8 to 25 percent slopes, extremely stonyHmD54904544013l82tpa03520021:24000
Clymer channery loam, 0 to 8 percent slopes, extremely stonyCfB28787543939l80fpa03520021:24000
Clymer-Cookport channery loams, 0 to 8 percent slopes, extremely stonyCgB19114543940l80gpa03520021:24000
Hazleton-Clymer channery loams, 0 to 8 percent slopes, extremely stonyHmB5790544012l82spa03520021:24000
Clymer-Hazleton sandy loams, 0 to 8 percent slopes, extremely stonyChB5538543943l80kpa03520021:24000
Clymer channery loam, 3 to 8 percent slopesCeB2667543937l80cpa03520021:24000
Clymer loam, 3 to 8 percent slopesCdB2259543934l808pa03520021:24000
Hazleton-Clymer channery loams, 3 to 8 percent slopesHlB2127544009l82ppa03520021:24000
Hazleton-Clymer channery loams, 8 to 15 percent slopesHlC1468544010l82qpa03520021:24000
Clymer channery loam, 8 to 15 percent slopesCeC381543938l80dpa03520021:24000
Clymer channery loam, 0 to 3 percent slopesCeA355543936l80bpa03520021:24000
Hazleton-Clymer channery loams, 15 to 25 percent slopesHlD309544011l82rpa03520021:24000
Clymer loam, 8 to 25 percent slopesCdD79543935l809pa03520021:24000
Hazleton-Clymer association, gently slopingHGB71013836131hfrppa03719651:20000
Hazleton-Clymer association, slopingHGC38013836151hfrrpa03719651:20000
Clymer very stony loam, 8 to 25 percent slopesCmD4106693706r8vmpa04119801:15840
Clymer very stony loam, 0 to 8 percent slopesCmB847693705r8vlpa04119801:15840
Hazleton-Clymer complex, 8 to 25 percent slopes, extremely stonyHxD855215911691qdr1pa05120051:24000
Clymer channery loam, 3 to 8 percent slopesCmB390615911051qdnzpa05120051:24000
Hazleton-Clymer complex, 0 to 8 percent slopes, extremely stonyHxB320815911681qdr0pa05120051:24000
Clymer channery loam, 8 to 15 percent slopesCmC239315911061qdp0pa05120051:24000
Clymer channery loam, 15 to 25 percent slopesCmD124815911071qdp1pa05120051:24000
Clymer loam, 8 to 25 percent slopes, very stonyCnD100115911601qdqrpa05120051:24000
Clymer loam, 0 to 8 percent slopes, very stonyCnB28815911591qdqqpa05120051:24000
Hazleton and Clymer soils, 8 to 25 percent slopes, extremely stonyHOD1977544870l8zgpa05719991:24000
Clymer very stony loam, 8 to 15 percent slopesCvC6960541981l5z8pa06119741:20000
Clymer very stony loam, 3 to 8 percent slopesCvB3065541980l5z7pa06119741:20000
Clymer channery loam, 3 to 8 percent slopesClB563541978l5z5pa06119741:20000
Clymer channery loam, 8 to 15 percent slopesClC405541979l5z6pa06119741:20000
Clymer channery loam, 3 to 8 percent slopesClB1162417208531vrpdpa06320121:24000
Hazleton-Clymer complex, 0 to 8 percent slopes, extremely stonyHxB508117208921vrqnpa06320121:24000
Hazleton-Clymer complex, 8 to 25 percent slopes, extremely stonyHxD435517208931vrqppa06320121:24000
Clymer channery loam, 8 to 15 percent slopesClC406017208541vrpfpa06320121:24000
Clymer channery loam, 3 to 8 percent slopesClB148223989422lj97pa06520121:12000
Clymer channery loam, 8 to 15 percent slopesClC120923989432lj98pa06520121:12000
Clymer very stony loam, 8 to 25 percent slopesClD3719542738l6rppa07119821:15840
Clymer very stony loam, 3 to 8 percent slopesClB1916542737l6rnpa07119821:15840
Clymer very stony loam, 25 to 50 percent slopesClF837542739l6rqpa07119821:15840
Clymer loam, 3 to 8 percent slopesCmB21431800352t32jpa07319781:15840
Clymer loam, 8 to 15 percent slopesCmC18329004022t32kpa07319781:15840
Clymer loam, 15 to 25 percent slopesCmD7329004032t32lpa07319781:15840
Clymer channery loam, 3 to 8 percent slopesCmB15443539063l2y4pa08119811:20000
Clymer very stony loam, 0 to 8 percent slopesCnB14493539065l2y6pa08119811:20000
Clymer very stony loam, 8 to 25 percent slopesCnD13930539066l2y7pa08119811:20000
Hazleton-Clymer channery loams, 8 to 25 percent slopes, extremely stonyHmD19401019425136sppa08119811:20000
Clymer channery loam, 8 to 15 percent slopesCmC1688539064l2y5pa08119811:20000
Hazleton-Clymer channery loams, 0 to 8 percent slopes, extremely stonyHmB2991019423136smpa08119811:20000
Hazleton-Clymer channery loams, 3 to 8 percent slopesHlB591019417136sfpa08119811:20000
Hazleton-Clymer channery loams, 8 to 15 percent slopesHlC311019436136t1pa08119811:20000
Clymer loam, 3 to 8 percent slopesClB3322539896l3t0pa08319841:20000
Clymer extremely stony loam, 0 to 8 percent slopesCxB85082962939y9vpa08919751:20000
Clymer extremely stony loam, 8 to 25 percent slopesCxC13012962949y9wpa08919751:20000
Clymer loam, 0 to 3 percent slopesCpA12612962909y9rpa08919751:20000
Clymer loam, 3 to 8 percent slopesCpB10682962919y9spa08919751:20000
Clymer loam, 8 to 15 percent slopesCpC6502962929y9tpa08919751:20000
Hazleton and Clymer extremely stony sandy loams, 0 to 8 percent slopesHuB282538997l2w0pa09319801:20000
Hazleton and Clymer extremely stony sandy loams, 8 to 25 percent slopesHuD234538998l2w1pa09319801:20000
Hazleton and Clymer extremely stony sandy loams, 8 to 25 percent slopesHuD8879539636l3jmpa09719801:20000
Hazleton and Clymer extremely stony sandy loams, 25 to 80 percent slopesHuF6308539637l3jnpa09719801:20000
Hazleton and Clymer extremely stony sandy loams, 0 to 8 percent slopesHuB2094539635l3jlpa09719801:20000
Clymer channery loam, frigid, 0 to 8 percent slopes, extremely stonyCmfB896324401482mx5gpa10519531:24000
Clymer channery loam, frigid, 8 to 15 percent slopes, extremely stonyCmfC565224401472mx5fpa10519531:24000
Clymer channery loam, frigid, 15 to 25 percent slopes, extremely stonyCmfD197924401462mx5dpa10519531:24000
Clymer-Cookport channery loams, 0 to 8 percent slopes, extremely stonyCncB133524325742mn94pa10519531:24000
Clymer, frigid-Elko channery loams, 0 to 8 percent slopes, extremely stonyCneB114629990422x4x0pa10519531:24000
Clymer channery loam, 8 to 15 percent slopes, extremely stonyCmC80324325682mn8ypa10519531:24000
Hazleton-Clymer channery loams, 8 to 25 percent slopes, extremely stonyHmD48224401612mx5wpa10519531:24000
Clymer-Hazleton sandy loams, 0 to 8 percent slopes, extremely stonyCnhB26224325762mn96pa10519531:24000
Clymer channery loam, 0 to 8 percent slopes, extremely stonyCmB18024325672mn8xpa10519531:24000
Hazleton-Clymer channery loams, 0 to 8 percent slopes, extremely stonyHmB11724401602mx5vpa10519531:24000
Clymer channery loam, 15 to 25 percent slopes, extremely stonyCmD5924325692mn8zpa10519531:24000
Hazleton-Clymer association, slopingHGC16764539720l3mbpa10719771:20000
Hazleton-Clymer association, gently slopingHGB16017539719l3m9pa10719771:20000
Hazleton and Clymer extremely stony sandy loams, 25 to 80 percent slopesHuF9533540819l4rspa10919801:20000
Hazleton and Clymer extremely stony sandy loams, 8 to 25 percent slopesHuD9300540818l4rrpa10919801:20000
Hazleton and Clymer extremely stony sandy loams, 0 to 8 percent slopesHuB2277540817l4rqpa10919801:20000
Clymer very stony loam, 3 to 12 percent slopesCsB35562971119z57pa11719731:20000
Clymer channery loam, 3 to 12 percent slopesCmB26402971109z56pa11719731:20000
Hazleton and Clymer extremely stony sandy loams, 25 to 80 percent slopesHuF8565540919l4w0pa11919801:20000
Hazleton and Clymer extremely stony sandy loams, 8 to 25 percent slopesHuD3858540918l4vzpa11919801:20000
Hazleton and Clymer extremely stony sandy loams, 0 to 8 percent slopesHuB3002540917l4vypa11919801:20000
Hazleton-Clymer complex, 8 to 25 percent slopes, extremely stonyHcD6687544571l8ntpa12920031:24000
Hazleton-Clymer complex, 0 to 8 percent slopes, extremely stonyHcB3259544570l8nspa12920031:24000
Clymer channery loam, 8 to 15 percent slopesCeC21814138981jg8mpa60719861:20000
Clymer channery loam, 0 to 8 percent slopes, extremely stonyCfB4214138991jg8npa60719861:20000
Clymer channery loam, 8 to 15 percent slopes, extremely stonyCfC3014148261jh7kpa60719861:20000
Clymer channery loam, 3 to 8 percent slopesCeB2614138971jg8lpa60719861:20000
Clymer fine sandy loam, slopingClC541519198kf8bva03519651:15840
Clymer fine sandy loam, moderately steepClD243519199kf8cva03519651:15840
Clymer channery loam, 3 to 15 percent slopes11B275516510kbgmva04319801:15840
Berks-Clymer complex, 7 to 15 percent slopes1C7310517091kc2cva12119801:15840
Clymer sandy loam, 15 to 35 percent slopes57D306625254432rtjsva6061:24000
Clymer sandy loam, 3 to 15 percent slopes57C116625254422rjx0va6061:24000
Clymer sandy loam, 35 to 60 percent slopes57E85925254442rtjtva6061:24000
Clymer-Dekalb complex, very steepCDF212047512830k6mxwv03919761:20000
Clymer-Dekalb complex, steepCDE23557512829k6mwwv03919761:20000
Clymer-Dekalb complex, moderately steepCDD6449512828k6mvwv03919761:20000
Clymer loam, 10 to 15 percent slopesCaC510512831k6mywv03919761:20000
Clymer loam, 3 to 8 percent slopesCmB2944186422820kwdwv07719551:24000
Clymer loam, 8 to 15 percent slopesCmC456186422920kwfwv07719551:24000
Clymer gravelly loam, 3 to 8 percent slopesCkB194186422620kwbwv07719551:24000
Clymer loam, 0 to 3 percent slopesCmA123186422720kwcwv07719551:24000
Clymer and Wharton soils, 3 to 15 percent slopes, very rubblyCWC5516750071t6zhwv60219651:20000
Clymer and Wharton rubbly soils, 3 to 15 percent slopesCwB6401515890k9tmwv62819801:20000
Clymer and Wharton rubbly soils, 15 to 35 percent slopesCwD3987515891k9tnwv62819801:20000
Clymer stony loam, 3 to 15 percent slopesCsB3123515888k9tkwv62819801:20000
Clymer stony loam, 15 to 35 percent slopesCsD820515889k9tlwv62819801:20000
Clymer-Gilpin complex, 30 to 70 percent slopesCnF240432516578k9xwwv7131:24000
Clymer-Gilpin complex, 15 to 30 percent slopesCnD46022516577k9xvwv7131:24000

Map of Series Extent

Approximate geographic distribution of the CLYMER 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 .