Official Series Description


Lab Data Summary

Aggregate lab data for the LYMAN soil series. This aggregation is based on all pedons with a current taxon name of LYMAN, 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 LYMAN were used in the calculation. Source: KSSL snapshot (updated 2020-03-13). 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
1432013NH6050672013NH605067Lyman1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.0773889,-71.767325
1432014NH6050082014NH605008Lyman1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1014389,-71.7918278
1432014NH6050092014NH605009Lyman1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1015833,-71.7915944
1432014NH6050102014NH605010Lyman1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1040667,-71.7971444
14384P078684VT023002Lyman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.271389,-72.7513885
14308N0130S07ME025001.MonsonLyman6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.0208333,-70.2021667
14340A3950S1976VT015008LYMAN4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5880547,-72.4358368
14340A3953S1976VT015011Lyman2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5483322,-72.6272202
14378P0343S1978VT025004Lyman7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.0102768,-72.5947189
14378P0346S1978VT025007Lyman7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1597214,-72.6388855
1431979MA003004S1979MA003004Lyman3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.508375,-73.0420111
1431979MA003005S1979MA003005Lyman4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.6173833,-72.9602139
14305N0483S2004VT007004Lyman5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3422203,-72.9089432
144B04N0377ME-03-11-019-02Lyman5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.9403889,-69.1105

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the LYMAN 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 LYMAN series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot (updated 2024-10-24), parsed OSD records (updated 2024-10-23) and snapshot of SC database (updated 2024-10-23).

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Select annual climate data summaries for the LYMAN series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

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Geomorphic description summaries for the LYMAN 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 (updated 2024-10-23).

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Competing Series

Soil series competing with LYMAN share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2024-10-23) and snapshot of the SC database (updated 2024-10-23).

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Select annual climate data summaries for the LYMAN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data (updated 2024-10-23).

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Geomorphic description summaries for the LYMAN 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 (updated 2024-10-23).

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Soil series sharing subgroup-level classification with LYMAN, 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 (updated 2024-10-23).

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. MA-2010-09-07-01 | Hampden and Hampshire Counties, Western Part - 1995

    Pattern of soils and parent material in the Lyman-Tunbridge-Peru general soil map (Soil Survey of Hampden and Hampshire Counties, Western Part, Massachusetts; 1995).

  2. MA-2010-09-07-07 | Hampden and Hampshire Counties, Western Part - 1995

    Pattern of soils and parent material in the Peru-Marlow general soil map unit (Soil Survey of Hampden and Hampshire Counties, Western Part, Massachusetts; 1995).

  3. MA-2012-02-01-05 | Berkshire County - February 1988

    Typical pattern of soils and parent material in the Tunbridge-Lyman-Peru general soil map unit (Soil Survey of Berkshire County, Massachusetts; February 1988).

  4. MA-2012-02-02-12 | Hampden and Hampshire Counties, Western Part - December 1995

    Pattern of soils and parent material in the Lyman-Tunbridge-Peru general soil map unit (Soil Survey of Hampden and Hampshire Counties, Western Part, Massachusetts; December 1995).

  5. ME-2010-09-03-01 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Dixfield-Colonel-Marlow general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  6. ME-2010-09-03-03 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Tunbridge-Lyman-Abram general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  7. ME-2010-09-03-07 | Franklin County Area and Part of Somerset County - 2003

    Typical pattern of the soils and underlying material in the Swanville-Boothbay-Nicholville general soil map unit (Soil Survey of Franklin County Area and Part of Somerset County, Maine; 2003).

  8. ME-2012-02-03-01 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Peru-Tunbridge-Marlow map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  9. ME-2012-02-03-02 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Buxton-Scantic-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  10. ME-2012-02-03-03 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Boothbay-Swanville-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  11. ME-2012-02-03-04 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Peru-Swanville-Lyman map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  12. ME-2012-02-03-05 | Knox and Lincoln Counties - January 1987

    The typical pattern of the soils on the landscape and the underlying material and bedrock in the Lyman-Peru-Scantic map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  13. ME-2012-02-03-06 | Knox and Lincoln Counties - January 1987

    The typical pattern of areas of Rock outcrop and the soils on the landscape and the underlying material and bedrock in the Rock outcrop-Lyman-Tunbridge map unit (Soil Survey of Knox and Lincoln Counties, Maine; January 1987).

  14. ME-2012-02-03-07 | Oxford County Area - March 1995

    Typical pattern of the soils and underlying material in the Hermon-Monadnock-Skerry general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

  15. ME-2012-02-03-11 | Oxford County Area - March 1995

    Typical pattern of the soils and underlying material in the Lyman-Tunbridge-Monadnock general soil map unit (Soil Survey of Oxford County Area, Maine; March 1995).

  16. ME-2012-02-03-14 | York County - June 1982

    Typical pattern of soils and underlying material in the Hermon-Lyman association (Soil Survey of York County, Maine; June 1982).

  17. ME-2012-02-03-15 | York County - June 1982

    Typical pattern of soils and underlying material in the Lyman-Rock outcrop-Sebago association (Soil Survey of York County, Maine; June 1982).

  18. ME-2012-02-03-17 | York County - June 1982

    Typical pattern of soils and underlying material in the Lyman-Rock outcrop-Scantic association (Soil Survey of York County, Maine; June 1982).

  19. ME-2012-02-03-19 | York County - June 1982

    Typical pattern of soils and underlying material in the Sulfihemists-Udipsamments association (Soil Survey of York County, Maine; June 1982).

  20. ME-2012-02-03-21 | York County - June 1982

    Typical pattern of soils and underlying material in the Marlow-Brayton-Peru association (Soil Survey of York County, Maine; June 1982).

  21. NH-2012-02-14-06 | Cheshire County - June 1989

    Typical landscape pattern of soils and underlying material in the Berkshire-Tunbridge-Lyman general soil map unit (Soil Survey of Cheshire County, New Hampshire; June 1989).

  22. NH-2012-02-14-11 | Grafton County Area - 1999

    Typical pattern of soils and underlying material in the Marlow-Peru unit (Soil Survey of Grafton County Area, New Hampshire; 1999).

  23. NH-2012-02-14-12 | Grafton County Area - 1999

    Typical pattern of soils and underlying material in the Tunbridge-Lyman unit (Soil Survey of Grafton County Area, New Hampshire; 1999).

  24. NH-2012-02-14-17 | Hillsborough County, Western Part - October 1985

    Typical landscape pattern of soils and parent material in the Marlow-Peru association (Soil Survey of Hillsborough County, New Hampshire, Western Part; October 1985).

  25. NH-2012-02-14-28 | Sullivan County - December 1983

    Typical pattern of soils and underlying material in the Monadnock-Marlow-Lyman unit (Soil Survey of Sullivan County, New Hampshire; December 1983).

  26. NH-2012-02-14-29 | Sullivan County - December 1983

    Typical pattern of soils and underlying material in the Monadnock-Marlow-Hermon unit (Soil Survey of Sullivan County, New Hampshire; December 1983).

  27. NY-2010-09-28-03 | Clinton County - 2006

    The Becket-Tunbridge general soil map unit is associated with the hillsides of bedrock-controlled landscapes in the Adirondack Mountains (Soil Survey of Clinton County, New York; 2006).

  28. NY-2010-09-28-27 | Saratoga County - 2004

    Typical relationship of soils and underlying material in the Berkshire-Becket-Tunbridge general soil map unit, which is generally at an elevation above 1,000 feet (Soil Survey of Saratoga County, New York; 2004).

  29. NY-2012-02-15-51 | Warren County - January 1989

    Typical relationship of soils and underlying deposits in the Hermon-Marlow general soil map unit, which is generally at an elevation above 1,500 feet (Soil Survey of Warren County, New York; January 1989).

  30. VT-2012-03-22-03 | Chittenden County - January 1974

    Relationship of soils in associations 13 and 14 (Soil Survey of Chittenden County, VT; 1974).

  31. VT-2012-03-22-04 | Lamoille County - October 1981

    Typical pattern of soils and underlying material in the Lyman-Tunbridge association (Soil Survey of Lamoille County, VT; 1981).

  32. VT-2012-03-22-05 | Lamoille County - October 1981

    Typical pattern of soils and underlying material in the Berkshire-Marlow-Peru association (Soil Survey of Lamoille County, VT; 1981).

  33. VT-2012-03-22-11 | Windham County - February 1987

    Typical landscape pattern of several soils and underlying material in Windham County (Soil Survey of Windham County, VT; 1987).

  34. VT-2012-03-22-14 | Windham County - February 1987

    Typical landscape pattern of soils and underlying material in the Tunbridge-Marlow-Lyman general soil map unit (Soil Survey of Windham County, VT; 1987).

Map Units

Map units containing LYMAN 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
Lyman-Tunbridge association, 15 to 60 percent slopes, extremely stony904E979622766112ty75ma00319841:25000
Tunbridge-Lyman association, 3 to 15 percent slopes, extremely stony909C507322766542trrmma00319841:25000
Tunbridge-Lyman complex, 25 to 60 percent slopes, very rocky138F430625682372tv94ma01120121:12000
Tunbridge-Lyman complex, 15 to 25 percent slopes, very rocky138D361425682362tv92ma01120121:12000
Tunbridge-Lyman complex, 8 to 15 percent slopes, very rocky138C336525682352tv91ma01120121:12000
Westminster, Lyman and Rock outcrop soils, 25 to 90 percent slopes137F243824943432pq39ma01120121:12000
Lyman-Rock outcrop-Tunbridge complex, 3 to 15 percent slopes126C8402791452ty4tma01120121:12000
Tunbridge-Lyman complex, 0 to 8 percent slopes, very rocky138B78725682342tv8zma01120121:12000
Tunbridge-Lyman association, 15 to 60 percent slopes, extremely stony909E347302776612trrxma60819891:25000
Lyman-Tunbridge association, 3 to 15 percent slopes, extremely stony904C319602776592trryma60819891:25000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rocky122B7292775332trplma60819891:25000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rocky122C6527919072trpnma60819891:25000
Tunbridge-Lyman association, 15 to 60 percent slopes, extremely stony909E11619038512trrxma60919801:15840
Tunbridge-Lyman-Berkshire association, 3 to 15 percent slopes, extremely stony924C181342787152w9q4ma61419931:25000
Lyman-Tunbridge-Berkshire association, 15 to 45 percent slopes, very rocky913E111022787102w9q5ma61419931:25000
Lyman-Tunbridge complex, 0 to 8 percent slopes, rockyHrB150763157002x1cxme00519691:24000
Lyman-Abram complex, 8 to 15 percent slopes, very rockyHsC135583157042x1d1me00519691:24000
Lyman-Tunbridge complex, 8 to 15 percent slopes, rockyHrC116463157012x1cyme00519691:24000
Lyman-Abram complex, 0 to 8 percent slopes, very rockyHsB53673157032x1d0me00519691:24000
Lyman loam, 8 to 15 percent slopes, very rockyLzC47963157102tsvhme00519691:24000
Lyman-Abram complex, 15 to 35 percent slopes, very rockyHsE47943157052x1d2me00519691:24000
Lyman-Tunbridge-Skerry complex, 0 to 15 percent slopes, very stonyLXC24943157982xk05me00519691:24000
Lyman loam, 15 to 35 percent slopes, very rockyLzE14303157112tsvjme00519691:24000
Lyman loam, 3 to 8 percent slopes, rockyLyB14253157072trq7me00519691:24000
Lyman loam, 3 to 8 percent slopes, very rockyLzB12393157092tsvgme00519691:24000
Lyman-Tunbridge complex, 15 to 35 percent slopes, rockyHrD12093157022x1czme00519691:24000
Lyman loam, 8 to 15 percent slopes, rockyLyC11013157082trq9me00519691:24000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTyC10203158272trpnme00519691:24000
Lyman-Tunbridge-Becket complex, 15 to 35 percent slopes, very stonyLUD9063157932xk03me00519691:24000
Lyman-Tunbridge-Monadnock complex, 15 to 35 percent slopes, very stonyLWD8403157962wlpfme00519691:24000
Rock outcrop-Lyman complex, 0 to 80 percent slopes, very stonyRo5673157302x1fbme00519691:24000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTyB5153158262trplme00519691:24000
Lyman-Tunbridge complex, 8 to 15 percent slopes, very stonyLtC4193157912trq1me00519691:24000
Abram-Rock outcrop-Lyman complex, 15 to 60 percent slopesACE4053157522tsv6me00519691:24000
Lyman-Tunbridge-Monadnock complex, 0 to 15 percent slopes, very stonyLWC3533157952wlpdme00519691:24000
Lyman-Tunbridge complex, 15 to 35 percent slopes, very stonyLtD3223157922trq2me00519691:24000
Tunbridge-Lyman complex, 15 to 35 percent slopes, rockyTyD2303158282trppme00519691:24000
Abram-Rock outcrop-Lyman complex, 3 to 15 percent slopesACC1703157622tsv3me00519691:24000
Lyman-Tunbridge complex, 0 to 8 percent slopes, very stonyLtB1453157902trq0me00519691:24000
Lyman-Tunbridge-Monadnock complex, 35 to 60 percent slopes, very stonyLWE1063157972wlphme00519691:24000
Lyman-Tunbridge-Becket complex, 35 to 60 percent slopes, very stonyLUE293157942xk04me00519691:24000
Lyman-Tunbridge complex, 8 to 15 percent slopes, rockyHrC713992844662x1cyme01119741:20000
Lyman-Tunbridge complex, 0 to 8 percent slopes, rockyHrB208512844652x1cxme01119741:20000
Lyman-Abram-Rock outcrop complex, 8 to 15 percent slopesHtC113462844692x1d5me01119741:20000
Lyman-Tunbridge complex, 15 to 35 percent slopes, rockyHrD61532844672x1czme01119741:20000
Lyman loam, 8 to 15 percent slopes, rockyLyC38622844732trqbme01119741:20000
Lyman loam, 15 to 25 percent slopes, rockyLyD33882844742trqcme01119741:20000
Lyman-Abram-Rock outcrop complex, 15 to 35 percent slopesHtD18382844702x1d3me01119741:20000
Lyman-Abram-Rock outcrop complex, 0 to 8 percent slopesHtB17092844682x1d4me01119741:20000
Lyman-Rock outcrop complex, 8 to 15 percent slopesLzC10682844752trqkme01119741:20000
Lyman loam, 3 to 8 percent slopes, rockyLyB5732844722trq8me01119741:20000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTrC276052845942trq4me02719791:20000
Lyman-Rock outcrop complex, 8 to 15 percent slopesLrC272782845492trqjme02719791:20000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTrB148492845932trq3me02719791:20000
Lyman-Rock outcrop complex, 15 to 80 percent slopesLrE139182845502trqpme02719791:20000
Tunbridge-Lyman complex, 15 to 25 percent slopes, rockyTrD63342845952trq5me02719791:20000
Lyman-Rock outcrop complex, 3 to 8 percent slopesLrB48612845482trqhme02719791:20000
Rock outcrop-Lyman complex, 15 to 80 percent slopesRmE9412845822trqvme02719791:20000
Rock outcrop-Lyman complex, 3 to 15 percent slopesRmC4842845812trqtme02719791:20000
Lyman-Rock outcrop complex, 8 to 15 percent slopesLyC374532846402trqjme03119781:20000
Lyman-Rock outcrop complex, 3 to 8 percent slopesLyB194932846392trqhme03119781:20000
Lyman-Rock outcrop complex, 15 to 80 percent slopesLyE156412846412trqpme03119781:20000
Lyman loam, 3 to 8 percent slopes, rockyLnB140622846362trq7me03119781:20000
Lyman loam, 8 to 15 percent slopes, rockyLnC97502846372trq9me03119781:20000
Rock outcrop-Lyman complex, 15 to 80 percent slopesRoE24612846562trqvme03119781:20000
Lyman loam, 15 to 25 percent slopes, rockyLnD22782846382trqdme03119781:20000
Rock outcrop-Lyman complex, 3 to 15 percent slopesRoC12542846552trqtme03119781:20000
Lyman-Rock outcrop-Tunbridge complex, 8 to 15 percent slopesLrC995262847072ty4xme60119831:20000
Lyman-Rock outcrop-Tunbridge complex, 0 to 8 percent slopesLrB292602847062ty4vme60119831:20000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTrB206012847392trq3me60119831:20000
Lyman-Rock outcrop-Tunbridge complex, 15 to 45 percent slopesLrE196182847082ty4yme60119831:20000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTrC186332847402trq4me60119831:20000
Lyman-Brayton variant-Rock outcrop complex, 0 to 8 percent slopesLmB165682847052tsvnme60119831:20000
Rock outcrop-Lyman complex, 3 to 15 percent slopesRmC68402847322trqtme60119831:20000
Rock outcrop-Lyman complex, 15 to 80 percent slopesRmE25122847332trqvme60119831:20000
Tunbridge-Lyman complex, 15 to 25 percent slopes, rockyTrD20172847412trq5me60119831:20000
Lyman loam, 8 to 15 percent slopes, rockyLyC50732847732trqbme60219671:20000
Lyman loam, 15 to 45 percent slopes, very rockyLzE30912847752trqgme60219671:20000
Lyman loam, 3 to 8 percent slopes, rockyLyB22162847722trq8me60219671:20000
Rock outcrop-Thorndike-Lyman association, 15 to 45 percent slopes, very stonyRtE15202847912w3zvme60219671:20000
Lyman loam, 0 to 15 percent slopes, very rockyLzC12372847742trqfme60219671:20000
Rock outcrop-Thorndike-Lyman association, 0 to 15 percent slopes, very stonyRtC10042847902w3ztme60219671:20000
Lyman-Tunbridge complex, 8 to 15 percent slopes, rockyHrC388192848412x1cyme60619661:15840
Lyman-Abram complex, 8 to 15 percent slopes, very rockyHsC359362848442x1d1me60619661:15840
Lyman-Abram complex, 15 to 35 percent slopes, very rockyHsD110292848452x1d2me60619661:15840
Lyman-Tunbridge complex, 0 to 8 percent slopes, rockyHrB96602848402x1cxme60619661:15840
Lyman-Tunbridge complex, 15 to 35 percent slopes, rockyHrD69672848422x1czme60619661:15840
Lyman-Abram complex, 0 to 8 percent slopes, very rockyHsB47832848432x1d0me60619661:15840
Lyman-Tunbridge-Abram complex, 15 to 35 percent slopes, rockyLNE345832850152tsv5me61019921:20000
Lyman-Tunbridge-Abram complex, 3 to 15 percent slopes, rockyLNC221462850142tsv2me61019921:20000
Lyman-Tunbridge-Rock outcrop complex, 3 to 15 percent slopesLyC23812850192trptme61019921:20000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTuB17642850702trplme61019921:20000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTuC16722850712trpnme61019921:20000
Rock outcrop-Abram-Lyman complex, 15 to 60 percent slopesRYE9572850512tsvcme61019921:20000
Lyman-Rock outcrop-Tunbridge complex, 15 to 45 percent slopesLmE7072850182ty4wme61019921:20000
Lyman-Tunbridge complex, 0 to 15 percent slopes, very stonyLuC320872851172ty4zme61119881:20000
Lyman-Tunbridge-Schoodic complex, 8 to 15 percent slopes, very stonyLWC281682851122tsw4me61119881:20000
Schoodic-Rock outcrop-Lyman complex, 15 to 60 percent slopesSGE129592851392tsvyme61119881:20000
Lyman-Schoodic-Rock outcrop complex, 15 to 35 percent slopes, very stonyLTE120092851112tsvxme61119881:20000
Naskeag-Schoodic-Lyman complex, 0 to 8 percent slopes, rockyNBB104982851322tsw5me61119881:20000
Lyman-Schoodic complex, 15 to 35 percent slopes, rockyLsE82172851162tsvwme61119881:20000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTuB75622851512trq3me61119881:20000
Lyman-Brayton-Schoodic complex, 3 to 15 percent slopes , rockyLHC43652851102tsw3me61119881:20000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTuC37922851522trq4me61119881:20000
Tunbridge-Lyman-Marlow complex, 3 to 15 percent slopes, rockyTWC23982851492tsw6me61119881:20000
Lyman-Brayton complex, 3 to 15 percent slopes, very stonyLgB11962851152tsw2me61119881:20000
Brayton-Colonel-Lyman complex, 0 to 8 percent slopes, rockyBYB8357744552szrtme61220161:24000
Lyman-Tunbridge complex, 3 to 15 percent slopes, rockyLTC589814831201ls9lme61220161:24000
Lyman-Tunbridge complex, 15 to 30 percent slopes, rockyLTD2412744563szs5me61220161:24000
Tunbridge-Lyman complex, 3 to 8 percent slopesTlB2149741176sw7xme61220161:24000
Lyman-Abram-Tunbridge complex, 8 to 30 percent slopes, very rockyLXD1422744561szs3me61220161:24000
Tunbridge-Peru-Lyman association, 15 to 30 percent slopes, very stonyTPD1205746040t19tme61220161:24000
Tunbridge-Lyman complex, 30 to 60 percent slopes, extremely stonyTLE629744564szs6me61220161:24000
Tunbridge-Lyman complex, 8 to 15 percent slopes, very stonyTlC544741614swq1me61220161:24000
Tunbridge-Lyman-Urban land association, 0 to 8 percent slopesTuB45714830391ls6zme61220161:24000
Lyman-Abram-Knob Lock complex, 30 to 80 percent slopes, very rockyLKE421744562szs4me61220161:24000
Lyman-Abram complex, 3 to 8 percent slopes, rockyLyB265740664svqdme61220161:24000
Lyman-Abram complex, 8 to 15 percent slopes, rockyLyC240740665svqfme61220161:24000
Lyman-Tunbridge-Monadnock complex, 15 to 35 percent slopes, very stonyLWD567212857842wlpfme61319871:20000
Lyman-Tunbridge-Monadnock complex, 35 to 60 percent slopes, very stonyLWE412682857852wlphme61319871:20000
Lyman-Tunbridge-Monadnock complex, 0 to 15 percent slopes, very stonyLWC184732857832wlpdme61319871:20000
Lyman-Tunbridge-Becket complex, 15 to 35 percent slopes, very stonyLUD135732857812xk03me61319871:20000
Abram-Rock outcrop-Lyman complex, 15 to 60 percent slopesACE119272857262tsv6me61319871:20000
Lyman-Tunbridge-Skerry complex, 0 to 15 percent slopes, very stonyLXC93062857862xk05me61319871:20000
Lyman-Tunbridge-Becket complex, 35 to 60 percent slopes, very stonyLUE42062857822xk04me61319871:20000
Lyman-Tunbridge complex, 8 to 15 percent slopes, very stonyLtC24632857892trq1me61319871:20000
Lyman-Tunbridge complex, 15 to 35 percent slopes, very stonyLtD19922857902trq2me61319871:20000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTyC19712858392trpnme61319871:20000
Abram-Rock outcrop-Lyman complex, 3 to 15 percent slopesACC9272857252tsv3me61319871:20000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTyB8812858382trplme61319871:20000
Tunbridge-Lyman complex, 15 to 35 percent slopes, rockyTyD7502858402trppme61319871:20000
Lyman-Tunbridge complex, 0 to 8 percent slopes, very stonyLtB5572857882trq0me61319871:20000
Peru-Colonel-Lyman association, 3 to 15 percent slopes, very stonyDYC287292853232w9p0me61519941:24000
Colonel-Brayton-Lyman complex, undulating, very stonyCQB87712853129kwmme61519941:24000
Marlow-Lyman-Peru association, 15 to 35 percent slopes, very stonyMND55442853402w9p1me61519941:24000
Lyman-Tunbridge complex, moderately steep, very stonyLTD43062853369kxdme61519941:24000
Lyman-Abram complex, moderately steep, very stonyLAD35152853349kxbme61519941:24000
Berkshire-Lyman association, strongly sloping, very stonyBFC34722853029kw9me61519941:24000
Lyman-Abram complex, very steep, very stonyLAE15222853359kxcme61519941:24000
Berkshire-Lyman association, moderately steep, very stonyBFD12982853039kwbme61519941:24000
Marlow-Lyman-Berkshire association, steep, very stonyMLE9302853399kxhme61519941:24000
Lyman-Tunbridge complex, steep, very stonyLTE6412853379kxfme61519941:24000
Lyman-Tunbridge-Abram complex, 3 to 15 percent slopes, rockyLYC382112855882tsw9me61720041:24000
Naskeag-Tunbridge-Lyman complex, 0 to 8 percent slopes, rockyNCB272752856082tsvrme61720041:24000
Tunbridge-Lamoine-Lyman complex, 3 to 15 percent slopes, very stonyTLC142712856262tswdme61720041:24000
Lyman-Abram-Tunbridge complex, 15 to 60 percent slopes, rockyLUE855314076992tsw0me61720041:24000
Tunbridge-Lyman-Abram complex, 3 to 15 percent slopes, very stonyTyC12372856302tswfme61720041:24000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rockyTuC9752856292trq4me61720041:24000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rockyTuB8732856282trq3me61720041:24000
Abram-Lyman complex, 15 to 35 percent slopes, rockyAbE2412855272tsvzme61720041:24000
Lyman-Tunbridge complex, 3 to 25 percent slopes, very stonyLTC134081909306222sjme62220071:24000
Lyman-Tunbridge complex, 20 to 60 percent slopes, very stonyLTF56221909307222skme62220071:24000
Abram-Lyman complex, 4 to 25 percent slopes, very stonyALC45691909303222sfme62220071:24000
Lyman-Tunbridge-Schoodic complex, 0 to 15 percent slopes, very stonyLYC15511909291222s1me62220071:24000
Lyman-Tunbridge-Abram complex, 3 to 15 percent slopes, very stonyLUC14351909087222kgme62220071:24000
Lyman-Schoodic-Rock outcrop complex, 15 to 45 percent slopes, very stonyLSE8611909292222s2me62220071:24000
Naskeag-Schoodic-Lyman complex, 0 to 8 percent slopes, very stonyNSB5911909293222s3me62220071:24000
Schoodic-Rock outcrop-Lyman complex, 15 to 65 percent slopesSLF4681909302222sdme62220071:24000
Naskeag-Tunbridge-Lyman complex, 0 to 8 percent slopes, very stonyNTB4491909088222khme62220071:24000
Tunbridge-Lyman-Rock outcrop complex, 15 to 25 percent slopes61D397072797062trpknh00519851:20000
Lyman-Tunbridge-Rock outcrop complex, 25 to 60 percent slopes161E277022796112trprnh00519851:20000
Tunbridge-Lyman-Rock outcrop complex, 8 to 15 percent slopes61C191042797052trpjnh00519851:20000
Tunbridge-Lyman-Rock outcrop complex, 0 to 8 percent slopes61B5412797042tv97nh00519851:20000
Tunbridge-Lyman-Rock outcrop complex, 25 to 60 percent slopes61E636792811472trphnh00919861:24000
Tunbridge-Lyman-Rock outcrop complex, 15 to 25 percent slopes61D390842811462trpknh00919861:24000
Tunbridge-Lyman complex, 15 to 25 percent slopes, rocky90D165602812192trpmnh00919861:24000
Tunbridge-Lyman-Rock outcrop complex, 8 to 15 percent slopes61C146972811452trpjnh00919861:24000
Tunbridge-Lyman complex, 8 to 15 percent slopes, rocky90C104582812182trpnnh00919861:24000
Marlow-Lyman-Rock outcrop complex, steep720E89242811799fl9nh00919861:24000
Becket-Lyman-Rock outcrop complex, 35 to 60 percent slopes710E80952811662x9q1nh00919861:24000
Becket-Lyman-Rock outcrop complex, 15 to 35 percent slopes710D72152811652x9q0nh00919861:24000
Tunbridge-Lyman complex, 3 to 8 percent slopes, rocky90B31072812172trplnh00919861:24000
Marlow-Lyman-Rock outcrop complex, hilly720D30662811789fl8nh00919861:24000
Rock outcrop-Lyman complex, steep726E29792811859flhnh00919861:24000
Tunbridge-Lyman-Rock outcrop complex, 0 to 8 percent slopes61B14312811442tv97nh00919861:24000
Skerry-Lyman-Rock outcrop complex, 0 to 15 percent slopes730B8042811912xk0gnh00919861:24000
Rock outcrop-Lyman complex, hilly726D7552811849flgnh00919861:24000
Monadnock-Lyman-Rock outcrop complex, 8 to 15 percent slopesMwC249342798012wlnynh01919811:20000
Monadnock-Lyman-Rock outcrop complex, 15 to 25 percent slopesMwD230172798022wlnznh01919811:20000
Lyman-Monadnock-Rock outcrop complex, 25 to 50 percent slopes, very stonyLsE216082797762wlplnh01919811:20000
Monadnock-Lyman stony fine sandy loams, 8 to 15 percent slopesMvC94872797989d4rnh01919811:20000
Monadnock-Lyman stony fine sandy loams, 15 to 25 percent slopesMvD42612797999d4snh01919811:20000
Monadnock-Lyman stony fine sandy loams, 3 to 8 percent slopesMvB24332797979d4qnh01919811:20000
Monadnock-Lyman-Rock outcrop complex, 0 to 8 percent slopesMwB22152798002wlnxnh01919811:20000
Lyman-Tunbridge-Rock outcrop complex, 15 to 35 percent slopes161D246542791702trpsnh60219831:20000
Lyman-Tunbridge-Rock outcrop complex, 3 to 15 percent slopes161C119002791692trptnh60219831:20000
Tunbridge-Lyman-Monadnock complex, stony, 8 to 15 perce nt slopes160C93582791679chdnh60219831:20000
Tunbridge-Lyman-Monadnock complex, stony, 15 to 25 perc ent slopes160D70532791689chfnh60219831:20000
Tunbridge-Lyman-Monadnock complex, stony, 3 to 8 percen t slopes160B16122791669chcnh60219831:20000
Lyman-Berkshire-Rock outcrop complex, 25 to 60 percent slopes, very stony71E2277316008102wlpknh6031:24000
Lyman-Berkshire complex, 15 to 25 percent slopes, very rocky170D614716008042wlp2nh6031:24000
Lyman-Berkshire complex, 25 to 35 percent slopes, very rocky170E513616008062wlp3nh6031:24000
Lyman-Berkshire complex, 8 to15 percent slopes, very rocky170C489316008022wlp1nh6031:24000
Lyman-Berkshire association, 15 to 35 percent slopes, very rocky780E463616008142wlp9nh6031:24000
Lyman-Berkshire association, 35 to 60 percent slopes, very rocky780F429016008162wlpbnh6031:24000
Lyman-Rock outcrop-Berkshire association, very steep745F423216033561qtf5nh6031:24000
Lyman-Berkshire-Rock outcrop complex, 8 to 25 percent slopes, very stony71D395416008082wlpjnh6031:24000
Rock outcrop-Lyman association, very steep726F240916008931qqvqnh6031:24000
Lyman-Berkshire complex, 0 to 8 percent slopes, very rocky170B86316008002wlp0nh6031:24000
Lyman-Berkshire association, 0 to 15 percent slopes, very rocky780C67516008122wlp8nh6031:24000
Lyman-Rock outcrop-Berkshire association, steep745E26916033501qtdznh6031:24000
Rock outcrop-Lyman association, steep726E6816008911qqvnnh6031:24000
Tunbridge-Lyman-Marlow association, 15 to 35 percent slopes, very stony919D260002806672xk28nh60720001:24000
Tunbridge-Lyman-Rock outcrop complex, 25 to 60 percent slopes61E255382805402trphnh60720001:24000
Tunbridge-Plaisted-Lyman complex, 8 to 15 percent slopes560C134142804829dvtnh60720001:24000
Tunbridge-Plaisted-Lyman complex, 15 to 25 percent slopes560D126062804839dvvnh60720001:24000
Tunbridge-Berkshire-Lyman complex, 8 to 15 percent slopes670C109172805559dy5nh60720001:24000
Tunbridge-Plaisted-Lyman complex, 25 to 35 percent slopes560E106022804849dvwnh60720001:24000
Tunbridge-Berkshire-Lyman complex, 15 to 25 percent slopes670D103042805569dy6nh60720001:24000
Tunbridge-Lyman-Marlow association, 35 to 60 percent slopes, very stony919E92412806682xk29nh60720001:24000
Tunbridge-Lyman-Marlow association, 0 to 15 percent slopes, very stony919B92212806662xk27nh60720001:24000
Tunbridge-Lyman-Rock outcrop complex, steep860E79342806519f18nh60720001:24000
Lyman-Tunbridge-Rock outcrop complex, steep820E79262806339f0pnh60720001:24000
Tunbridge-Lyman-Rock outcrop complex, 15 to 25 percent slopes61D69032805392trpknh60720001:24000
Lyman-Tunbridge-Rock outcrop complex, moderately steep820D47082806329f0nnh60720001:24000
Tunbridge-Plaisted-Lyman complex, 8 to 15 percent slopes, very stony561C43962804869dvynh60720001:24000
Tunbridge-Plaisted-Lyman complex, 3 to 8 percent slopes560B38572804819dvsnh60720001:24000
Tunbridge-Lyman-Rock outcrop complex, 8 to 15 percent slopes61C34822805382trpjnh60720001:24000
Lyman-Tunbridge-Rock outcrop complex, gently sloping820B15902806319f0mnh60720001:24000
Tunbridge-Plaisted-Lyman complex, 3 to 8 percent slopes, very stony561B11442804859dvxnh60720001:24000
Tunbridge-Lyman-Rock outcrop complex, 0 to 8 percent slopes61B8012805372tv97nh60720001:24000
Rock outcrop-Lyman complex, very steep726F7762805739dyrnh60720001:24000
Lyman-Tunbridge-Skerry complex, 0 to 15 percent slopes, very stony972B1062807652xk05nh60720001:24000
Lyman-Tunbridge-Monadnock complex, 15 to 35 percent slopes, very stony971D802807632wlpfnh60720001:24000
Rock outcrop-Lyman complex, strongly sloping726C302805729dyqnh60720001:24000
Lyman-Tunbridge-Monadnock complex, 35 to 60 percent slopes, very stony971E182807642wlphnh60720001:24000
Tunbridge-Lyman-Becket complex, 15 to 25 percent slopes, very stony380D570002801912xk0nnh60920071:24000
Tunbridge-Lyman-Becket complex, 8 to 15 percent slopes, very stony380C556492801902xk0mnh60920071:24000
Tunbridge-Lyman-Becket complex, 25 to 60 percent slopes, very stony380E233632801922xk0pnh60920071:24000
Lyman-Tunbridge-Rock outcrop complex, 35 to 60 percent slopes161E129812801402trpvnh60920071:24000
Tunbridge-Lyman-Becket complex, 0 to 8 percent slopes, very stony380B118422801892xk0lnh60920071:24000
Lyman-Tunbridge-Rock outcrop complex, 15 to 35 percent slopes161D84792801392trpsnh60920071:24000
Tunbridge-Lyman-Rock outcrop complex, 8 to 15 percent slopes161C54282801382trpjnh60920071:24000
Adams-Lyman complex, 8 to 15 percent slopes, rocky190C14742801502x1csnh60920071:24000
Adams-Lyman complex, 15 to 35 percent slopes, very rocky190D8412801512wqnwnh60920071:24000
Rock outcrop-Lyman complex, 3 to 80 percent slopes, very stony571E78927801492q45ynh60920071:24000
Tunbridge-Lyman complex, 15 to 35 percent slopes, very rocky, very bouldery831D57592900802wrc0ny01919951:24000
Tunbridge-Lyman complex, 15 to 35 percent slopes, very rocky, very boulderyTnE46742902432wrc7ny01919951:24000
Tunbridge-Lyman complex, 3 to 15 percent slopes, very rocky , very boulderyTnC33502902422wrc2ny01919951:24000
Lyman-Knob Lock complex, 35 to 60 percent slopes, very rocky, very bouldery861F26422900822xj29ny01919951:24000
Lyman-Tunbridge-Rock outcrop complex, 35 to 70 percent slopes, very boulderyLtF23672901832wrc6ny01919951:24000
Tunbridge-Lyman complex, 3 to 15 percent slopes, very rocky, very bouldery831C15952900792wrbyny01919951:24000
Tunbridge-Lyman complex, 35 to 60 percent slopes, very rocky, very bouldery831F13712900812wrbzny01919951:24000
Tunbridge-Lyman complex, 15 to 35 percent slopes, very rocky, very bouldery831D609743197672wrc0ny03120071:24000
Lyman-Knob Lock complex, 35 to 60 percent slopes, very rocky, very bouldery851F4666714602172xj29ny03120071:24000
Tunbridge-Lyman complex, 35 to 60 percent slopes, very rocky, very bouldery831F280953197682wrbzny03120071:24000
Tunbridge-Lyman complex, 15 to 35 percent slopes, very rocky, very boulderyTuD217083192982wrc7ny03120071:24000
Lyman-Knob Lock complex, 35 to 60 percent slopes, very rocky, very boulderyLyF1186210330352xj2lny03120071:24000
Tunbridge-Lyman complex, 35 to 70 percent slopes, very rocky, very boulderyTuF1027814074552wrc4ny03120071:24000
Tunbridge-Lyman complex, 3 to 15 percent slopes, very rocky , very boulderyTuC53063192972wrc2ny03120071:24000

Map of Series Extent

Approximate geographic distribution of the LYMAN 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 (updated 2024-10-30).