Official Series Description


Lab Data Summary

Aggregate lab data for the JUDSON soil series. This aggregation is based on all pedons with a current taxon name of JUDSON, 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 JUDSON 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
102C94P009593NE039001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7750015,-96.9166641
102C94P008693NE173002Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.2497215,-96.7986145
102CUMN2734S1978MN133001 (2734)Judson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6555176,-96.3919983
102CUMN2731S1978MN133002 (2731)Judson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5868607,-96.4430618
102CUMN2909S1978MN133012 (2909)Judson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5439873,-96.1831512
104X53-8-1S1985IA105001Judson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1448512,-91.0573942
105X1918S1959IA191002Judson1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.3300446,-91.8343522
105X49-8B-1S1983IA097004Judson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0738763,-90.3948259
10603N099103NE109005Judson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6848907,-96.8510818
10606KS00560206KS005602Judson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5036125,-95.3647232
10695P00631994NE067001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.079464,-96.712532
10694P05501994NE131001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6377792,-96.1611099
10694P05511994NE131002Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7247238,-96.3477783
10695P00641994NE133001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1369629,-96.3891907
10695P00651994NE133002Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0586319,-96.1444626
10694P009793NE023001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2799988,-97.0416641
10694P054894NE109001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8561096,-96.5055542
10694P054994NE109002Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6061096,-96.5922241
10640A1799S1953KS177001JUDSON5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1086121,-95.8802795
10640A1800S1953KS177002JUDSON4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.086113,-95.797226
107A96P0224S1996IA193005Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.5023613,-95.9328613
107B95P032494NE177013Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6127777,-96.2555542
107B12N0011S2011NE153003Judson8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1548889,-96.1562778
107B13N0536S2012IA009002Judson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5778109,-94.881395
107B13N0540S2012IA027003Judson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.9711567,-94.8172417
n/a94P041594KS043001Judson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the JUDSON 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 JUDSON 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 JUDSON 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 JUDSON 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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Click the image to view it full size.

Competing Series

Soil series competing with JUDSON 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 JUDSON 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 JUDSON 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.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with JUDSON, 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. IA-2010-09-02-28 | Polk County - 2000

    Typical pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Polk County, Iowa; 2000).

  2. IA-2010-09-02-30 | Polk County - 2000

    Typical pattern of soils and parent material in the Sharpsburg-Shelby-Lamoni association (Soil Survey of Polk County, Iowa; 2000).

  3. IA-2010-09-03-06 | Woodbury - 2006

    Typical pattern of soils and underlying material in the Galva association (Soil Survey of Woodbury County, Iowa; 2006).

  4. IA-2010-09-03-08 | Woodbury - 2006

    Typical pattern of soils and underlying material in the Monona-Ida-Judson association (Soil Survey of Woodbury County, Iowa; 2006).

  5. IA-2010-09-09-12 | Crawford County - 2007

    Typical pattern of soils and parent material in the Monona association (Soil Survey of Crawford County, Iowa; 2007).

  6. IA-2010-09-09-13 | Crawford County - 2007

    Typical pattern of soils and parent material in the Marshall-Judson association (Soil Survey of Crawford County, Iowa; 2007).

  7. IA-2010-09-09-15 | Crawford County - 2007

    Typical pattern of soils and parent material in the Nodaway association (Soil Survey of Crawford County, Iowa; 2007).

  8. IA-2010-09-09-16 | Crawford County - 2007

    A cross section showing the relationship between soils and parent material in the eastern part of Crawford County (Soil Survey of Crawford County, Iowa; 2007).

  9. IA-2011-05-31-04 | Audubon County - 1984

    Pattern of soils and parent material in the Marshall-Exira association (Soil Survey of Audubon County, Iowa; 1984).

  10. IA-2011-05-31-05 | Audubon County - 1984

    Pattern of soils and parent material in the Marshall-Shelby-Adair association (Soil Survey of Audubon County, Iowa; 1984).

  11. IA-2011-05-31-06 | Audubon County - 1984

    Pattern of soils and parent material in the Sharpsburg-Shelby-Marshall association (Soil Survey of Audubon County, Iowa; 1984).

  12. IA-2011-05-31-07 | Audubon County - 1984

    Pattern of soils and parent material in the Colo-Ackmore-Zook association (Soil Survey of Audubon County, Iowa; 1984).

  13. IA-2011-05-31-48 | Hardin County - 1985

    Pattern of soils and parent material in the Tama-Colo association (Soil Survey of Hardin County, Iowa; 1985).

  14. IA-2011-06-01-18 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Marshall-Exira association (Soil Survey of Montgomery County, Iowa; 1989).

  15. IA-2011-06-01-19 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Sharpsburg-Shelby association (Soil Survey of Montgomery County, Iowa; 1989).

  16. IA-2011-06-01-20 | Montgomery County - 1989

    Typical pattern of soils and parent material in the Gara-Ladoga association (Soil Survey of Montgomery County, Iowa; 1989).

  17. IA-2011-06-01-36 | Polk County - 2000

    Typical pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Polk County, Iowa; 2000).

  18. IA-2011-06-01-37 | Polk County - 2000

    Typical pattern of soils and parent material in the Sharpsburg-Shelby-Lamoni association (Soil Survey of Polk County, Iowa; 2000).

  19. KS-2012-01-20-06 | Brown County - September 1960

    Typical cross section of the strongly sloping loess hills (Soil Survey of Brown County, Kansas; 1960).

  20. KS-2012-01-20-07 | Brown County - September 1960

    Typical cross section of the rolling till-limestone uplands (Soil Survey of Brown County, Kansas; 1960).

  21. MN-2010-09-10-10 | Sherburne County -

    Typical pattern of soils and parent material in the Yutan-Aksarben-Pohocco association (Soil Survey of Sherburne County, Minnesota).

  22. MO-2010-09-08-05 | Holt County - 1997

    Typical pattern of soils and parent material in the Marshall-Contrary association (Soil Survey of Holt County, Missouri; 1997).

  23. MO-2010-09-08-06 | Holt County - 1997

    Typical pattern of soils and parent material in the Marshall-Exira-Shelby association (Soil Survey of Holt County, Missouri; 1997).

  24. MO-2012-02-06-13 | Buchanan County - September 1989

    Pattern of soils and parent material in the Marshall-Contrary association (Soil Survey of Buchanan County, Missouri; September 1989).

  25. NE-2012-02-08-16 | Butler County - February 1982

    Typical pattern of soils in the Sharpsburg-Steinauer-Pawnee association and relationship of the soils to topography and parent material (Soil Survey of Butler County, Nebraska; February 1982).

  26. NE-2012-02-08-17 | Gage County - May 1964

    Schematic diagram showing the relationship of major soil series to parent materials in Gage County, Nebraska (Soil Survey of Gage County, Nebraska; May 1964).

  27. NE-2012-02-13-62 | Nance County - July 1960

    Principal soils of Nance County (Soil Survey of Nance County, Nebraska; July 1960).

  28. NE-2012-02-13-63 | Nance County - July 1960

    A cross section along the eastern side of Nance County showing the relationship of the soils to the geological materials (Soil Survey of Nance County, Nebraska; July 1960).

  29. NE-2012-02-13-65 | Nemaha County - December 1985

    Typical pattern of soils and parent material in the Sharpsburg association (Soil Survey of Nemaha County, Nebraska; December 1985).

  30. NE-2012-02-13-66 | Nemaha County - December 1985

    Typical pattern of soils and parent material in the Pawnee-Nodaway-Gymer association (Soil Survey of Nemaha County, Nebraska; December 1985).

  31. NE-2012-02-13-67 | Nemaha County - December 1985

    Typical pattern of soils and parent material in the Monona-Ida and Onawa-Haynie-Albaton associations (Soil Survey of Nemaha County, Nebraska; December 1985).

  32. NE-2012-02-13-84 | Saunders County - January 1965

    Soils in the Lamoure-Rauville association (Soil Survey of Saunders County, Nebraska; January 1965).

  33. NE-2012-02-13-85 | Saunders County - January 1965

    Soils in the Colo-Lamoure association (Soil Survey of Saunders County, Nebraska; January 1965).

  34. NE-2012-02-13-87 | Saunders County - January 1965

    Soils in the Sharpsburg association (Soil Survey of Saunders County, Nebraska; January 1965).

  35. NE-2012-02-13-88 | Saunders County - January 1965

    Soils in the Monona-Sharpsburg association (Soil Survey of Saunders County, Nebraska; January 1965).

  36. NE-2012-02-13-89 | Saunders County - January 1965

    Soils in the Sharpsburg-Burchard association (Soil Survey of Saunders County, Nebraska; January 1965).

  37. NE-2012-02-13-90 | Saunders County - January 1965

    Soils in the Burchard-Shelby association (Soil Survey of Saunders County, Nebraska; January 1965).

  38. NE-2012-02-13-91 | Saunders County - January 1965

    Soils in the Monona association (Soil Survey of Saunders County, Nebraska; January 1965).

  39. NE-2012-02-13-92 | Saunders County - January 1965

    Soils in the Muir-Hobbs association (Soil Survey of Saunders County, Nebraska; January 1965).

  40. NE-2012-02-14-12 | Washington County - September 1964

    Soil pattern of the Sharpsburg-Marshall association (Soil Survey of Washington County, Nebraska; September 1964).

  41. NE-2012-02-14-13 | Washington County - September 1964

    Soil pattern of the Monona-Crofton association (Soil Survey of Washington County, Nebraska; September 1964).

  42. NE-2012-02-14-14 | Washington County - September 1964

    Soil pattern of the Luton-Volin and Albaton-Haynie associations (Soil Survey of Washington County, Nebraska; September 1964).

  43. WI-2012-03-22-06 | Grant County - June 1961

    Landscape of Grant County showing the relationship of the major soil series (Soil Survey of Grant County, WI; 1961).

  44. WI-2012-03-23-30 | Pepin County - March 1964

    Cross section showing the geology and the associated soils in Pepin County (Soil Survey of Pepin County, WI; 1964).

Map Units

Map units containing JUDSON 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
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B9554022152sy6zia00119761:15840
Judson silty clay loam, dissected till plain, 5 to 9 percent slopes8C4364022162sy72ia00119761:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B274714048732sy6zia00320081:12000
Judson-Colo-Ackmore complex, 2 to 5 percent slopes11B5212240274830kfwia00919821:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B52744027862sy6yia00919821:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C12544027872sy71ia00919821:15840
Gullied land-Judson complex, 5 to 40 percent slopes980G8124027932sy74ia00919821:15840
Judson silty clay loam, 2 to 5 percent slopes8B22247479131170ia02319781:15840
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B400194035042sy7jia02719791:15840
Ackmore-Judson complex, 1 to 5 percent slopes5B9274035532zsp7ia02719791:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B8744035682sy6yia02719791:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C5824035692sy71ia02719791:15840
Judson-Ackmore-Colo, overwash complex, 1 to 5 percent slopes431B3578124230072y6b2ia02920101:12000
Judson silty clay loam, deep loess, 2 to 5 percent slopesZ8B1151718679792sy6yia02920101:12000
Judson silty clay loam, dissected till plain, 2 to 5 percent slopesY8B290824861792sy6zia02920101:12000
Judson silty clay loam, deep loess, 5 to 9 percent slopesZ8C27918679802sy71ia02920101:12000
Judson silty clay loam, dissected till plain, 5 to 9 percent slopesY8C20824864502sy72ia02920101:12000
Judson silty clay loam, 2 to 5 percent slopes8B1616139714231170ia03120081:12000
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B209014039022sy7jia03519871:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B3474039682sy6yia03519871:15840
Judson-Ackmore-Colo, overwash complex, 1 to 5 percent slopes431B522093997902y6b2ia04720041:12000
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B207013998532sy6yia04720041:12000
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C73953998542sy71ia04720041:12000
Judson-Gullied land, frequently flooded, complex, 5 to 9 percent slopes980C136913868872sy73ia04720041:12000
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B4274046342sy6zia04919801:15840
Judson silty clay loam, 2 to 5 percent slopes8B216340496431170ia06919771:15840
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B244504060902sy7jia07119681:20000
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B57104061702sy6yia07119681:20000
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B145664063362sy7jia07719681:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B22404064332sy6zia07719681:15840
Judson silty clay loam, dissected till plain, 5 to 9 percent slopes8C8154064342sy72ia07719681:15840
Judson silty clay loam, 2 to 5 percent slopes8B61540670531170ia08319821:15840
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B227364070672sy7jia09319891:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C60744072282sy71ia09319891:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B37564072272sy6yia09319891:15840
Judson silty clay loam, 2 to 5 percent slopes8B338645294831170ia09520051:12000
Judson silty clay loam, 2 to 5 percent slopes8B511640770131170ia09919751:15840
Judson silty clay loam, 0 to 2 percent slopes899340769331173ia09919751:15840
Judson silty clay loam, 5 to 9 percent slopes8C72940770231174ia09919751:15840
Judson silty clay loam, 2 to 5 percent slopes8B97840821831170ia10519881:15840
Judson silty clay loam, 5 to 9 percent slopes8C37140821931174ia10519881:15840
Judson silty clay loam, 2 to 5 percent slopes8B36244724331170ia10719981:12000
Judson silty clay loam, 5 to 9 percent slopes8C32644724431174ia10719981:12000
Judson silty clay loam, 2 to 5 percent slopes8B275340869031170ia11319701:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B3944092032sy6zia12119681:15840
Judson silty clay loam, 2 to 5 percent slopes8B137040938531170ia12319711:15840
Judson silty clay loam, 5 to 9 percent slopes8C50240938631174ia12319711:15840
Judson silty clay loam, dissected till plain, 5 to 9 percent slopes8C6244128122sy72ia12519761:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B6194128112sy6zia12519761:15840
Judson silty clay loam, 2 to 5 percent slopes8B141640951131170ia12719781:15840
Judson silty clay loam, 5 to 9 percent slopes8C84640951231174ia12719781:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B151804095962sy6yia12919791:15840
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B53824095292sy7jia12919791:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C2874095972sy71ia12919791:15840
Ackmore-Colo-Judson complex, 0 to 5 percent slopes11B393914098292zsp6ia13719871:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopesZ8B1009629964542sy6yia13719871:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopesY8B11394098912sy6zia13719871:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopesZ8C6514098922sy71ia13719871:15840
Judson silty clay loam, dissected till plain, 5 to 9 percent slopesY8C11530070202sy72ia13719871:15840
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B658664101842sy7jia14519751:20000
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B38724102332sy6zia14519751:20000
Judson silty clay loam, deep loess, 2 to 5 percent slopesZ8B350929964552sy6yia14519751:20000
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded11B62304128222sy7jia15319931:12000
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B6894129862sy6zia15319931:12000
Colo, rarely flooded-Judson-Urban land complex, 2 to 5 percent slopes4011B694128962wnydia15319931:12000
Ackmore-Colo-Judson complex, 0 to 5 percent slopes11B531104104352zsp6ia15519861:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B292244105172sy6yia15519861:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C51334105182sy71ia15519861:15840
Judson silty clay loam, 2 to 5 percent slopes8B231641063931170ia15719781:15840
Judson silty clay loam, 5 to 9 percent slopes8C43141064031174ia15719781:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C4074108402sy71ia16119751:15840
Judson-Ackmore-Colo, overwash complex, 1 to 5 percent slopes431B733279916112y6b2ia16520051:12000
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C59774374582sy71ia16520051:12000
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B52104374572sy6yia16520051:12000
Radford-Judson complex, 0 to 5 percent slopes11B100694111952zv9mia16719871:15840
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B70684112692sy6yia16719871:15840
Judson silty clay loam, 2 to 5 percent slopes8B183441156631170ia17119891:15840
Colo-Judson-Nodaway complex, 0 to 5 percent slopes286B315114116122wxshia17319891:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B4044116612sy6zia17319891:15840
Judson silty clay loam, dissected till plain, 5 to 9 percent slopes8C1514116622sy72ia17319891:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B4364117372sy6zia17519751:15840
Judson silty clay loam, dissected till plain, 2 to 5 percent slopes8B5664119772sy6zia18119751:15840
Judson silty clay loam, deep loess, 5 to 9 percent slopes8C149154018852sy71ia19320031:12000
Judson silty clay loam, deep loess, 2 to 5 percent slopes8B110624019822sy6yia19320031:12000
Smithland-Danbury-Judson complex, 0 to 5 percent slopes666B50227416292zv9nia19320031:12000
Judson-Rawles complex, 0 to 5 percent slopes847B36174021382zv9gia19320031:12000
Judson silt loam, 1 to 5 percent slopes7851181714753882x6bpks00519981:24000
Judson silt loam, 1 to 5 percent slopes7851273111521912x6bpks01319941:24000
Judson silt loam, 1 to 5 percent slopes785137047471612x6bpks04319771:24000
Judson silt loam, rarely flooded7852514688591l9gkks04519741:24000
Judson silt loam, 0 to 1 percent slopes78501433186240920hzqks10319731:24000
Judson silt loam, 1 to 5 percent slopes78518314060372x6bpks13119801:24000
Judson silt loam, 2 to 6 percent slopes7231325051502x6bqks13119801:24000
Judson silt loam, 2 to 6 percent slopes7231625594302x6bqks20119881:24000
Judson silt loam, 0 to 1 percent slopes7850410186229720hw3ks20919731:24000
Chaseburg and Judson silt loams, 2 to 6 percent slopesCb1255322167052ddnmmn04520081:12000
Chaseburg and Judson silt loams, 0 to 1 percent slopesCa338122167042ddnlmn04520081:12000
Judson silty clay loam, 3 to 8 percent slopesP20B3257256952zv9dmn10120081:12000
Judson silty clay loam, 3 to 8 percent slopesP20B2386300672zv9dmn10520041:12000
Judson silt loam, 2 to 7 percent slopes10037435525210982qkydmo00319861:24000
Colo, frequently flooded-Judson silty clay loams, 0 to 5 percent slopes13627175126076932sy7kmo00319861:24000
Colo, frequently flooded-Judson silty clay loams, 0 to 5 percent slopes136271081626718412sy7kmo00519881:24000
Colo-Judson silty clay loams, 0 to 5 percent slopes, occasionally flooded13511495325283672sy7jmo00519881:24000
Judson silty clay loam, deep loess, 2 to 5 percent slopes10187368125210972sy6ymo00519881:24000
Kenridge-Judson complex, 1 to 7 percent slopes1003943625211012qkyfmo00519881:24000
Judson-Colo complex, 1 to 5 percent slopes100383201913496znkmmo02119841:24000
Judson silt loam, 2 to 7 percent slopes10037200525210962qkydmo02119841:24000
Colo-Judson silty clay loams, 0 to 5 percent slopes1362711726076962qhz5mo07519821:24000
Colo, frequently flooded-Judson silty clay loams, 0 to 5 percent slopes136271507726718422sy7kmo08719921:24000
Kenridge-Judson complex, 1 to 7 percent slopes10039678225211002qkyfmo08719921:24000
Nodaway-Judson silt loams, 1 to 7 percent slopes135642958887524ysjtmo08719921:24000
Colo, frequently flooded-Judson silty clay loams, 0 to 5 percent slopes136271495126718432sy7kmo14719831:24000
Judson silt loam, 2 to 6 percent slopes7231755616912942x6bqne02319791:20000
Yutan, eroded-Judson complex, 6 to 11 percent slopes7646130922190452scynne02319791:20000
Judson silt loam, 0 to 2 percent slopes72302922190402dh2yne02319791:20000
Judson silt loam, 2 to 6 percent slopes72311650016914712x6bqne02519811:20000
Yutan, eroded-Judson complex, 6 to 11 percent slopes7646195022160322scynne02519811:20000
Judson silt loam, 0 to 2 percent slopes7230139416914701ts3kne02519811:20000
Judson silty clay loam, 2 to 6 percent slopes7234826417109502sy70ne05520071:12000
Urban land-Udorthents-Judson complex, 0 to 11 percent slopes9718504617109792sy75ne05520071:12000
Pohocco-Judson complex, 1 to 30 percent slopes8140116917109642zv9hne05520071:12000
Judson-Nodaway channeled-Contrary complex, 0 to 12 percent slopes723549217109512zv9fne05520071:12000
Judson silt loam, 2 to 6 percent slopes72311777016911042x6bqne06720001:12000
Judson silt loam, 2 to 6 percent slopes7231371816917671tsf4ne09519701:20000
Judson silt loam, 2 to 6 percent slopes72311065916915742x6bqne09719841:20000
Judson silt loam, 2 to 6 percent slopes72312743516913602x6bqne10919771:20000
Urban land-Judson complex, 1 to 3 percent slopes9708130416913951ts14ne10919771:20000
Yutan, eroded-Judson complex, 6 to 11 percent slopes764688922192432scynne10919771:20000
Judson fine sandy loam, 2 to 6 percent slopes723230716913591trzzne10919771:20000
Judson silt loam, 2 to 6 percent slopes72311157216916642x6bqne12719831:20000
Judson silt loam, 0 to 2 percent slopes723079516916631ts9sne12719831:20000
Judson silt loam, 2 to 6 percent slopes72311863816915272x6bqne13119791:20000
Judson silt loam, 0 to 2 percent slopes723073216915261ts5cne13119791:20000
Judson silt loam, 2 to 6 percent slopes72311445016916152x6bqne13319691:15840
Judson silt loam, 2 to 6 percent slopes72311824416910412x6bqne14719671:20000
Judson silt loam, 2 to 6 percent slopes723151722191852x6bqne15119851:20000
Judson silty clay loam, 2 to 6 percent slopes7234989917110142sy70ne15320071:12000
Judson-Nodaway channeled-Contrary complex, 0 to 12 percent slopes7235278217110152zv9fne15320071:12000
Urban land-Udorthents-Judson complex, 0 to 11 percent slopes9718128117110432sy75ne15320071:12000
Pohocco-Judson complex, 1 to 30 percent slopes814083817110282zv9hne15320071:12000
Yutan, eroded-Judson complex, 6 to 11 percent slopes764610674516914542scynne15519951:12000
Judson silt loam, 2 to 6 percent slopes72312453416914262x6bqne15519951:12000
Judson silt loam, 0 to 2 percent slopes7230351116914251ts23ne15519951:12000
Judson silt loam, 2 to 6 percent slopes723143822191272x6bqne15919671:20000
Judson silty clay loam, 2 to 6 percent slopes7234194993955412sy70ne17720001:12000
Judson-Nodaway channeled-Contrary complex, 0 to 12 percent slopes723519222173032zv9fne17720001:12000
Judson silt loam, 3 to 10 percent slopesJuB3006424283g7hkwi04319591:20000
Judson silt loam, 0 to 3 percent slopesJuA2163424282g7hjwi04319591:20000
Judson silt loam, 2 to 6 percent slopesJuB3631424645g7w7wi04919601:20000
Judson silt loam, 0 to 2 percent slopesJuA2092424644g7w6wi04919601:20000
Judson silt loam, 6 to 12 percent slopesJuC287424646g7w8wi04919601:20000

Map of Series Extent

Approximate geographic distribution of the JUDSON 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 .