Official Series Description


Lab Data Summary

Aggregate lab data for the SHELBY soil series. This aggregation is based on all pedons with a current taxon name of SHELBY, 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 SHELBY 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
10606KS00560406KS005604Shelby3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.5113907,-95.3686142
10640A186071KS087004Shelby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2150002,-95.2055588
10640A186171KS087005Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1822205,-95.2005539
10692P064492NE109001DShelby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5374985,-96.8333359
10606N0950S2006KS005002Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4925804138184,-95.4089584350586
10606N0951S2006KS005003Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4789123535156,-95.4799728393555
10606N0952S2006KS005004Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4770927429199,-95.2811050415039
10606N0953S2006KS005005Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.426643371582,-95.4226913452148
10606N0954S2006KS005006Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6446266174316,-95.5087051391602
107BM87005171987MO005017Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5469437,-95.2591629
107BM90087551990MO087055mShelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.231945,-95.2663879
107BM90087561990MO087056mShelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2316666,-95.2663879
107BM91087621991MO087062mShelby3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1744461,-95.1711121
107BM91087631991MO087063mShelby3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2224998,-95.2372208
107B85P057184IA0090011Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7194443,-94.7694473
107B85P057284IA0090012Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.7194443,-94.7694473
107B87P032487IA0090031Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6219444,-94.9552765
107B87P032587IA0090032Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.621666,-94.9547195
108C85P047784IA0990011Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8166656,-92.8888855
108C85P047884IA0990012Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8166656,-92.8888855
108C87P034386IA0990042Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8211098,-92.8883362
108C87P034486IA0990043Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8208351,-92.8894424
108C88P060087IA099001Shelby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8277779,-92.8888855
108C88P060187IA099002Shelby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8277779,-92.8888855
108DM89087441989MO087044mShelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2324982,-95.0858307
108D84P038183IA003002Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0763893,-94.6627808
108D85P050084IA0030041Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.942791,-94.735527
108D85P050184IA0030042Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9425125,-94.7352524
108D85P050484IA0030045Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9422379,-94.736084
108D85P056684IA1730013Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8194427,-94.8616638
108D85P056784IA1730014Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8194427,-94.8616638
108D86P031785IA0030051Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9472237,-94.6647186
108D86P031885IA0030052Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9472237,-94.6641693
108D87P038887IA1730063Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8333321,-94.8666687
108D87P038987IA1730064Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8333321,-94.8666687
108D40A1463S1956IA001006SHELBY4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3827782,-94.4658356
109M82079061982MO079006Shelby2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1225014,-93.5397186
10984P08331984MO171005Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5719452,-93.1530533
10987P03731987IA159002Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.85796,-94.2374
109M88129081988MO129008Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5772209,-93.3897247
109M88129111988MO129011Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4308319,-93.6755524
109M89129061989MO129006Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4275017,-93.6761093
109M89129131989MO129013Shelby3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4363899,-93.3675003
109M89129181989MO129018Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3022232,-93.7183304
109M89129231989MO129023Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.292244,-93.6707687
10984P043083IA185002Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7311096,-93.378334
10985P051884IA1590021Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8250008,-94.0638885
10985P051984IA1590022Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8250008,-94.0638885
10987P037487IA1590072Shelby5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8333321,-94.0500031
115BM90001371990MO001037Shelby4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHELBY 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 SHELBY 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 SHELBY 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 SHELBY 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with SHELBY 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 SHELBY 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 SHELBY 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 .

Click the image to view it full size.

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 SHELBY, 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-2010-09-02-21 | Keokuk County - 2003

    Typical pattern of soils and parent material in the Otley-Mahaska-Nira association (Soil Survey of Keokuk County, Iowa; 2003).

  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-2010-09-09-02 | Adams County - 2008

    Typical pattern of soils and parent material in the Sharpsburg-Macksburg association (Soil Survey of Adams County, Iowa; 2008).

  4. IA-2010-09-09-03 | Adams County - 2008

    Typical pattern of soils and parent material in the Sharpsburg-Shelby association (Soil Survey of Adams County, Iowa; 2008).

  5. IA-2010-09-09-18 | Iowa County - 2007

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

  6. IA-2010-09-09-20 | Iowa County - 2007

    Typical pattern of soils and parent material in the Otley-Mahaska-Shelby association (Soil Survey of Iowa County, Iowa; 2007).

  7. IA-2010-09-09-21 | Shelby County - 2007

    Diagram showing the relationships of the upland soils in the eastern part of Shelby County to parent material and landforms (Soil Survey of Shelby County, Iowa; 2007).

  8. 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).

  9. 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).

  10. IA-2011-05-31-08 | Audubon County - 1984

    Relationship of the major soils in Audubon County to the parent material (Soil Survey of Audubon County, Iowa; 1984).

  11. IA-2011-06-01-13 | Lucas County - 1999

    Typical pattern of soils and parent material in the Arispe-Lamoni-Shelby association (Soil Survey of Lucas County, Iowa; 1999).

  12. 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).

  13. 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).

  14. IA-2011-06-01-38 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Nira-Sharpsburg-Shelby association (Soil Survey of Ringgold County, Iowa; 1992).

  15. IA-2011-06-01-41 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Arispe-Shelby-Lamoni association (Soil Survey of Ringgold County, Iowa; 1992).

  16. IA-2011-06-01-48 | Washington County - 1986

    Pattern of soils and parent material in the Otley-Nira association (Soil Survey of Washington County, Iowa; 1986).

  17. KS-2012-01-20-01 | Atchison County - February 1984

    Typical pattern of soils in the Grundy-Pawnee association (Soil Survey of Atchison County, Kansas; 1984).

  18. KS-2012-01-20-02 | Atchison County - February 1984

    Typical pattern of soils in the Shelby-Pawnee-Grundy association (Soil Survey of Atchison County, Kansas; 1984).

  19. KS-2012-01-20-03 | Atchison County - February 1984

    Typical pattern of soils in the Sharpsburg-Shelby association (Soil Survey of Atchison County, Kansas; 1984).

  20. KS-2012-01-20-05 | Atchison County - February 1984

    Typical pattern of soils in the Martin-Vinland-Pawnee association (Soil Survey of Atchison County, Kansas; 1984).

  21. 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).

  22. KS-2012-01-20-08 | Brown County - September 1960

    Typical cross section of the smooth, sloping, loess-till uplands (Soil Survey of Brown County, Kansas; 1960).

  23. KS-2012-01-25-36 | Shawnee County - June 1970

    Loess-till area in the northern part of Shawnee County showing the relation of soils to the landscape in soil association 3 (Soil Survey of Shawnee County, Kansas; 1970).

  24. MO-2010-09-08-02 | Gentry County - 1985

    Relationship of soils, topography, and underlying material in the Lamoni-Shelby association (Soil Survey of Gentry County, Missouri; 1985).

  25. 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).

  26. 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).

  27. MO-2012-02-06-04 | Atchison County - May 1994

    Typical pattern of soils and parent material in the Marshall-Contrary association (Soil Survey of Atchison County, Missouri; May 1994).

  28. MO-2012-02-06-05 | Atchison County - May 1994

    Typical pattern of soils and parent material in the Marshall-Shelby association (Soil Survey of Atchison County, Missouri; May 1994).

  29. MO-2012-02-06-06 | Atchison County - May 1994

    Typical pattern of soils and parent material in the Higginsville-Sharpsburg-Shelby association (Soil Survey of Atchison County, Missouri; May 1994).

  30. 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).

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

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

Map Units

Map units containing SHELBY 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
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D2280224021632sqs5ia00119761:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E2143204021652sqrvia00119761:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D269234022172wxrzia00119761:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E219164022182wxs3ia00119761:15840
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D18614021622sqs3ia00119761:15840
Shelby clay loam, dissected till plain, 5 to 9 percent slopes, erodedY24C213404021612sqscia00119761:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F210604021662sqs1ia00119761:15840
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E7284021642sqrxia00119761:15840
Shelby loam, dissected till plain, 5 to 9 percent slopesY24C2544021602sqsgia00119761:15840
Lamoni-Shelby complex, 9 to 14 percent slopes, eroded470D22254917118532zsp0ia00320081:12000
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D21014214049042sqs5ia00320081:12000
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E2977714049062sqrvia00320081:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, eroded469C2595317118512y6bwia00320081:12000
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E2360714048362wxs3ia00320081:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D2344214048342wxrzia00320081:12000
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E211614049052sqrxia00320081:12000
Shelby loam, dissected till plain, 18 to 25 percent slopesY24F123923929482sqsfia00320081:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, severely eroded469C321819078652y6bxia00320081:12000
Shelby clay loam, dissected till plain, 5 to 9 percent slopes, erodedY24C218614049022sqscia00320081:12000
Shelby loam, 9 to 14 percent slopes, moderately eroded24D236854026642tk98ia00719701:15840
Adair-Shelby complex, 9 to 14 percent slopes, moderately eroded93D236384027332wjfbia00719701:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E225554026662tkc6ia00719701:15840
Adair-Shelby complex, 9 to 14 percent slopes, severely eroded93D3806402734fj2fia00719701:15840
Shelby soils, 9 to 14 percent slopes, severely eroded24D3667402665fj06ia00719701:15840
Shelby soils, 14 to 18 percent slopes, severely eroded24E3312402667fj08ia00719701:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D296564027892wxryia00919821:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, severely erodedZ24E361624027642sqryia00919821:15840
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, erodedZ93E247414027912wxs2ia00919821:15840
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, severely erodedZ93E339554027922wxs4ia00919821:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, severely erodedZ93D335734027902wxs0ia00919821:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D232874027622sqs4ia00919821:15840
Shelby clay loam, deep loess, 18 to 25 percent slopes, severely erodedZ24F328954027652sqs8ia00919821:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, severely erodedZ24D318054027632sqs6ia00919821:15840
Shelby clay loam, deep loess, 5 to 9 percent slopes, severely erodedZ24C39974027612sqshia00919821:15840
Adair-Shelby complex, MLRA 107B, 9 to 14 percent slopes, severely erodedZ82D31320324849122pdrgia02920101:12000
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E2587618679862sqrvia02920101:12000
Lamoni-Shelby complex, 9 to 14 percent slopes, eroded470D2498518680612zsp0ia02920101:12000
Shelby clay loam, deep loess, 14 to 18 percent slopes, severely erodedZ24E3397124849182sqryia02920101:12000
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E2293624849152sqrtia02920101:12000
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D2286518679832sqs4ia02920101:12000
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D2245924992152sqs5ia02920101:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, severely erodedY93D3219118680062wxs1ia02920101:12000
Shelby-Lamoni complex, 14 to 18 percent slopes, severely eroded824E3147724992142zv94ia02920101:12000
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, severely erodedY24E3120018679872sqrzia02920101:12000
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F2119518679882sqs1ia02920101:12000
Shelby-Adair complex, MLRA 107B, 5 to 9 percent slopes, moderately erodedZ93C2112824849252pdrwia02920101:12000
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, severely erodedY24D386218679842sqs7ia02920101:12000
Shelby clay loam, deep loess, 18 to 25 percent slopes, erodedZ24F279124849132sqs0ia02920101:12000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D277918680052wxrzia02920101:12000
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, severely erodedY24F340024228262sqs9ia02920101:12000
Shelby clay loam, deep loess, 9 to 14 percent slopes, severely erodedZ24D336224849212sqs6ia02920101:12000
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, erodedZ93E234124849282wxs2ia02920101:12000
Shelby clay loam, dissected till plain, 5 to 9 percent slopes, erodedY24C229124864262sqscia02920101:12000
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E224118680072wxs3ia02920101:12000
Adair-Shelby complex, MLRA 108D, 5 to 9 percent slopes, severely erodedY82C319724228272mb4qia02920101:12000
Shelby, sandy substratum-Hesch, deep-Hesch complex, 9 to 14 percent slopes, moderately eroded247D29224849082pdrbia02920101:12000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D21225065902wxryia02920101:12000
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E825070122sqrxia02920101:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, eroded469C2125070142y6bwia02920101:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, severely eroded469C3125070132y6bxia02920101:12000
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E2108344041282tk96ia03919871:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E2353529595732sqrvia03919871:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D228714041852tkbwia03919871:15840
Shelby loam, 14 to 18 percent slopes24E19604041272tk97ia03919871:15840
Shelby clay loam, 18 to 25 percent slopes, moderately eroded24F212044041312tkc5ia03919871:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D21168404126fkjbia03919871:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D2101629859152wxrzia03919871:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F289429594862sqs1ia03919871:15840
Shelby-Adair clay loams, 9 to 14 percent slopes, severely eroded93D3855404186fkl8ia03919871:15840
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E34414041292tkbvia03919871:15840
Shelby loam, 9 to 14 percent slopes24D4124041252tk8zia03919871:15840
Shelby-Adair loams, 9 to 14 percent slopes93D278404184fkl6ia03919871:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, severely erodedY24E323629595532sqrzia03919871:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D219829596162sqs5ia03919871:15840
Shelby loam, 18 to 25 percent slopes24F180404130fkjgia03919871:15840
Shelby loam, dissected till plain, 18 to 25 percent slopesY24F15829595422sqsfia03919871:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D221884046362wxrzia04919801:15840
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E9904045862sqrxia04919801:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D24894045852sqs5ia04919801:15840
Shelby-Adair complex, 14 to 18 percent slopes93E290404637fl1tia04919801:15840
Adair-Shelby complex, 9 to 14 percent slopes, moderately eroded93D28674047472wjfbia05119881:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E26194046702tkc6ia05119881:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D26124046692tk98ia05119881:15840
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E257494047872tk96ia05319861:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D248624047862tk93ia05319861:15840
Shelby clay loam, 18 to 25 percent slopes, moderately eroded24F25504047882tkc5ia05319861:15840
Shelby loam, 9 to 14 percent slopes24D2274047852tk8zia05319861:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D29164061242sqs4ia07119681:20000
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E25004061252sqrtia07119681:20000
Shelby clay loam, deep loess, 18 to 25 percent slopes, erodedZ24F21274061262sqs0ia07119681:20000
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E2150564063662sqrvia07719681:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D294804063652sqs5ia07719681:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D278264064352wxrzia07719681:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E258394064372wxs3ia07719681:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F243944063682sqs1ia07719681:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, severely erodedY93E318734064382wxs5ia07719681:15840
Shelby, moderately eroded-Dickinson, loamy substratum complex, 14 to 25 percent slopes176F2133625070392qhz1ia07719681:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, severely erodedY24E36354063672sqrzia07719681:15840
Shelby clay loam, dissected till plain, 5 to 9 percent slopes, erodedY24C26284063642sqscia07719681:15840
Shelby loam, dissected till plain, 2 to 5 percent slopesY24B5064063632sqsjia07719681:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, severely erodedY24F33144063692sqs9ia07719681:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, severely erodedY93D33024064362wxs1ia07719681:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D21534628331p2tria09520051:12000
Shelby loam, 9 to 14 percent slopes, moderately eroded24D21485452996h6csia09520051:12000
Shelby-Adair complex, 14 to 18 percent slopes, moderately eroded93E2941628332p2tsia09520051:12000
Shelby loam, 14 to 18 percent slopes, moderately eroded24E2822452997h6ctia09520051:12000
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E3597114445017dwria09520051:12000
Shelby-Adair complex, 9 to 14 percent slopes, severely eroded93D3349114445117dwsia09520051:12000
Shelby loam, 5 to 9 percent slopes, moderately eroded24C2321114444817dwpia09520051:12000
Shelby clay loam, 9 to 14 percent slopes, severely eroded24D3279114444917dwqia09520051:12000
Shelby loam, 14 to 18 percent slopes, moderately eroded24E27316407643fp5sia09919751:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D27306407703fp7qia09919751:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately erode93E24323407704fp7ria09919751:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D23435407642fp5ria09919751:15840
Shelby loam, 18 to 25 percent slopes, moderately eroded24F22004407644fp5tia09919751:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D21536407765fp9qia10119921:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D22173447246h0d9ia10719981:12000
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E2495447060h069ia10719981:12000
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D2285447059h068ia10719981:12000
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E240634089062tk96ia11719911:15840
Lamoni-Shelby complex, 9 to 14 percent slopes, moderately eroded470D231214089662wjfcia11719911:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D22792408903fqhfia11719911:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D216264090582tkbwia11719911:15840
Shelby clay loam, 18 to 25 percent slopes, moderately eroded24F28954089092tkc5ia11719911:15840
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E32034089072tkbvia11719911:15840
Shelby clay loam, 9 to 14 percent slopes24D1824089022xjcria11719911:15840
Shelby-Lamoni complex, 9 to 14 percent slopes, eroded824D289204092542zv91ia12119681:15840
Shelby-Lamoni complex, 14 to 18 percent slopes, eroded824E278914092562zv93ia12119681:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, eroded24E267134092492sqrvia12119681:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, eroded24F239914092502sqs1ia12119681:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, eroded24D223634092472sqs5ia12119681:15840
Shelby loam, dissected till plain, 14 to 18 percent slopes24E4144092482sqrxia12119681:15840
Shelby-Lamoni complex, 14 to 18 percent slopes, severely eroded824E33944092572zv94ia12119681:15840
Shelby-Lamoni complex, 9 to 14 percent slopes824D3564092532zv90ia12119681:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, severely eroded24E33284092512sqrzia12119681:15840
Shelby-Lamoni complex, 9 to 14 percent slopes, severely eroded824D32644092552zv92ia12119681:15840
Shelby-Lamoni complex, 5 to 9 percent slopes, eroded824C21174092522zv8zia12119681:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D2536409296fqx3ia12319711:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E2375409297fqx4ia12319711:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D242684127542tk98ia12519761:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E22262412755fvhpia12519761:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D2142429596202sqs5ia12519761:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D2108429859242wxrzia12519761:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D2431412813fvkkia12519761:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E26614409462fr2gia12719781:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D23905409460fr2dia12719781:15840
Shelby loam, 18 to 25 percent slopes, moderately eroded24F21057409464fr2jia12719781:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately erode93E2969409514fr44ia12719781:15840
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E3605409463fr2hia12719781:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D2536409513fr43ia12719781:15840
Shelby clay loam, 9 to 14 percent slopes, severely eroded24D3200409461fr2fia12719781:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D27604095592sqs4ia12919791:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D25014095992wxryia12919791:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E22104095602sqrtia12919791:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D2979409763frd5ia13519821:15840
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E24654097642tk96ia13519821:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D2964029595012sqs4ia13719871:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D2478729859042wxryia13719871:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D231694098502sqs5ia13719871:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E224854098522sqrtia13719871:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E297929594412sqrvia13719871:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D26904098942wxrzia13719871:15840
Shelby, sandy substratum-Hesch, deep-Hesch complex, 9 to 14 percent slopes, moderately eroded247D240425412302qhz3ia13719871:15840
Shelby loam, deep loess, 9 to 14 percent slopesZ24D37629594942sqs2ia13719871:15840
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E3494098512sqrxia13719871:15840
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D3294098492sqs3ia13719871:15840
Shelby loam, dissected till plain, 18 to 25 percent slopesY24F2484098532sqsfia13719871:15840
Shelby loam, deep loess, 18 to 25 percent slopesZ24F19729595402sqsdia13719871:15840
Shelby loam, deep loess, 14 to 18 percent slopesZ24E15729594922sqrwia13719871:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D261084102022sqs5ia14519751:20000
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D60204102012sqs3ia14519751:20000
Shelby loam, deep loess, 9 to 14 percent slopesZ24D149929594952sqs2ia14519751:20000
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D2148829595022sqs4ia14519751:20000
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E13794102032sqrxia14519751:20000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D2100329859052wxryia14519751:20000
Shelby-Adair clay loams, 9 to 14 percent slopes93D915410234frwcia14519751:20000
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E263829594362sqrvia14519751:20000
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D25694102352wxrzia14519751:20000
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E24204102042sqrtia14519751:20000
Shelby loam, deep loess, 14 to 18 percent slopesZ24E32629594932sqrwia14519751:20000
Shelby-Adair clay loams, deep loess, 14 to 18 percent slopes, erodedZ93E219729859272wxs2ia14519751:20000
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F21874102052sqs1ia14519751:20000
Shelby clay loam, deep loess, 18 to 25 percent slopes, erodedZ24F216429594822sqs0ia14519751:20000
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E2294102362wxs3ia14519751:20000
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D2848412878fvmnia15319931:12000
Shelby clay loam, 14 to 18 percent slopes24E237412879fvmpia15319931:12000
Shelby-Urban land complex, 9 to 14 percent slopes4024D184128972sqskia15319931:12000
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D258334105202wxryia15519861:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D227184104702sqs4ia15519861:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E211484104712sqrtia15519861:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, severely erodedZ93D38024105212wxs0ia15519861:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, severely erodedZ24E32624104722sqryia15519861:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D29441410641fs9hia15719781:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E28902410568fs74ia15719781:15840
Shelby loam, 9 to 14 percent slopes, moderately eroded24D25405410566fs72ia15719781:15840
Shelby-Adair complex, 14 to 18 percent slopes, moderately eroded93E21251410642fs9jia15719781:15840
Shelby loam, 18 to 40 percent slopes24F456410569fs75ia15719781:15840
Shelby loam, 14 to 18 percent slopes24E447410567fs73ia15719781:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D2101044106782tk93ia15919871:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D2276429596232sqs5ia15919871:15840
Lamoni-Shelby complex, 9 to 14 percent slopes, moderately eroded470D227614107092wjfcia15919871:15840
Shelby clay loam, 14 to 18 percent slopes, moderately eroded24E226914106802tk96ia15919871:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D216294107482tkbwia15919871:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D2160529859202wxrzia15919871:15840
Shelby clay loam, 9 to 14 percent slopes24D14834106772xjcria15919871:15840
Shelby clay loam, 14 to 18 percent slopes24E885410679fsbqia15919871:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E257629595782sqrvia15919871:15840
Lamoni-Shelby complex, 9 to 14 percent slopes470D4044107082zsnzia15919871:15840
Shelby-Adair clay loams, 9 to 14 percent slopes93D365410747fsdxia15919871:15840
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D25529596072sqs3ia15919871:15840
Shelby clay loam, deep loess, 5 to 9 percent slopes, erodedZ24C28344107812sqsbia16119751:15840
Shelby clay loam, deep loess, 9 to 14 percent slopes, erodedZ24D25474107822sqs4ia16119751:15840
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E22414107832sqrtia16119751:15840
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E3519410946fsmbia16319891:15840
Shelby clay loam, 9 to 14 percent slopes, severely eroded24D3217410944fsm8ia16319891:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E2205410945fsm9ia16319891:15840
Shelby-Adair clay loams, deep loess, 9 to 14 percent slopes, erodedZ93D263489916792wxryia16520051:12000
Shelby clay loam, deep loess, 14 to 18 percent slopes, erodedZ24E243244375052sqrtia16520051:12000
Shelby clay loam, deep loess, 18 to 25 percent slopes, erodedZ24F212284375062sqs0ia16520051:12000
Shelby loam, 9 to 14 percent slopes, moderately eroded24D2699411434ft42ia17119891:15840
Shelby clay loam, 14 to 18 percent slopes, severely eroded24E3590411437ft45ia17119891:15840
Shelby loam, 14 to 18 percent slopes, moderately eroded24E2559411436ft44ia17119891:15840
Shelby clay loam, 9 to 14 percent slopes, severely eroded24D3264411435ft43ia17119891:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D2143984116052sqs5ia17319891:15840
Lamoni-Shelby complex, 9 to 14 percent slopes, eroded470D2127824116282zsp0ia17319891:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D268274116642wxrzia17319891:15840
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D22764116042sqs3ia17319891:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E216704116072sqrvia17319891:15840
Lamoni-Shelby complex, 9 to 14 percent slopes470D8234116272zsnzia17319891:15840
Shelby-Adair complex, 9 to 14 percent slopes93D697411663ftcgia17319891:15840
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E3084116062sqrxia17319891:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, erodedY24D21138229596252sqs5ia17519751:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D21092629859222wxrzia17519751:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E233044117002sqrvia17519751:15840
Adair-Shelby clay loams, 9 to 14 percent slopes93D2707411738ftfwia17519751:15840
Shelby loam, dissected till plain, 9 to 14 percent slopesY24D22174116962sqs3ia17519751:15840
Shelby clay loam, 9 to 14 percent slopes, moderately eroded24D21816411697ftdkia17519751:15840
Adair-Shelby clay loams, 9 to 14 percent slopes, moderately eroded93D21667411739ftfxia17519751:15840
Shelby loam, dissected till plain, 14 to 18 percent slopesY24E15634116992sqrxia17519751:15840
Shelby clay loam, dissected till plain, 5 to 9 percent slopes, erodedY24C210324116952sqscia17519751:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E26434117402wxs3ia17519751:15840
Shelby clay loam, dissected till plain, 9 to 14 percent slopes, severely erodedY24D33984116982sqs7ia17519751:15840
Shelby loam, dissected till plain, 5 to 9 percent slopesY24C3804116942sqsgia17519751:15840
Shelby clay loam, dissected till plain, 18 to 25 percent slopes, erodedY24F228629594902sqs1ia17519751:15840
Shelby clay loam, 18 to 25 percent slopes, moderately eroded24F241411701ftdpia17519751:15840
Shelby-Adair complex, 9 to 14 percent slopes, moderately eroded93D24944118692tkbwia17919781:15840
Shelby-Adair clay loams, dissected till plain, 9 to 14 percent slopes, erodedY93D2554829859232wxrzia18119751:15840
Shelby-Adair clay loams, dissected till plain, 14 to 18 percent slopes, erodedY93E2294829859362wxs3ia18119751:15840
Shelby clay loam, dissected till plain, 14 to 18 percent slopes, erodedY24E217324119152sqrvia18119751:15840
Adair-Shelby clay loams, 9 to 14 percent slopes, moderately eroded93D21272411978ftpmia18119751:15840

Map of Series Extent

Approximate geographic distribution of the SHELBY 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 .