Official Series Description


Lab Data Summary

Aggregate lab data for the HOBBS soil series. This aggregation is based on all pedons with a current taxon name of HOBBS, 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 HOBBS 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
102C81P03551980NE141053Hobbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5458346,-97.5209016
7379P01481979NE073003Hobbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6025009,-99.8891678
7401KS20100301KS201003Hobbs3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7243576,-97.2748184
7401KS20101601KS201016Hobbs3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7219696,-97.2716599
7491KS06100291KS061002ksuHobbs3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1472282,-96.958725
7501KS20103901KS201039Hobbs3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.891304,-97.1795425
7503N0358S2002NE095001Hobbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0608521,-97.3664474
7503N0359S2002NE095002Hobbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0743523,-97.0996017
7602N0462S2001KS027016Hobbs7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2866898,-96.9958878

Water Balance

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the HOBBS 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

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

Soil series sharing subgroup-level classification with HOBBS, 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. KS-2012-01-20-30 | Clay County - September 1984

    Typical pattern of soils and underlying material in the Crete-Lancaster-Hedville association (Soil Survey of Clay County, Kansas; 1984).

  2. KS-2012-01-23-06 | Geary County - February 1960

    Diagram showing the relationship of the soils in the southeastern part of Geary County (Soil Survey of Geary County, Kansas; 1960).

  3. KS-2012-01-23-07 | Geary County - February 1960

    Diagram showing the relationship of the soils in the Flint Hills (Soil Survey of Geary County, Kansas; 1960).

  4. KS-2012-01-23-29 | Harvey County - November 1974

    Typical pattern of soils in the Irwin-Rosehill-Clime association (Soil Survey of Harvey County, Kansas; 1974).

  5. KS-2012-01-25-05 | Phillips County - September 1987

    Pattern of soils and parent material in the Holdrege-Uly association (Soil Survey of Phillips County, Kansas; 1987).

  6. KS-2012-01-25-08 | Phillips County - September 1987

    Pattern of soils and parent material in the Harney-Holdrege-Uly association (Soil Survey of Phillips County, Kansas; 1987).

  7. KS-2012-01-25-19 | Republic County - November 1967

    Distribution of the soils in the Crete-Butler-Hastings association (Soil Survey of Republic County, Kansas; 1967).

  8. KS-2012-01-25-24 | Rice County - December 1974

    Distribution of the soils in the Crete-Geary association (Soil Survey of Rice County, Kansas; 1974).

  9. KS-2012-01-25-25 | Rice County - December 1974

    Distribution of the soils in the Smolan-Crete-Hobbs association (Soil Survey of Rice County, Kansas; 1974).

  10. KS-2012-01-25-26 | Rice County - December 1974

    Distribution of the soils in the Hedville-Lancaster-Smolan association (Soil Survey of Rice County, Kansas; 1974).

  11. KS-2012-01-25-27 | Rice County - December 1974

    Distribution of the soils in the Carwile-Farnum-Tabler and Canadian-Kaski-Platte associations (Soil Survey of Rice County, Kansas; 1974).

  12. KS-2012-01-26-26 | Washington County - August 1993

    Typical pattern of soils and parent material in the Crete-Longford association (Soil Survey of Washington County, Kansas; 1993).

  13. KS-2012-01-26-28 | Washington County - August 1993

    Typical pattern of soils and parent material in the Crete-Mayberry-Morrill association (Soil Survey of Washington County, Kansas; 1993).

  14. KS-2012-01-26-29 | Washington County - August 1993

    Typical pattern of soils and parent material in the Crete-Kipson-Tully association (Soil Survey of Washington County, Kansas; 1993).

  15. NE-2012-02-08-13 | Butler County - February 1982

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

  16. NE-2012-02-08-14 | Butler County - February 1982

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

  17. 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).

  18. 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).

  19. NE-2012-02-10-10 | Clay County - March 1981

    Typical pattern of soils in the Hastings-Crete-Butler association showing the relationship of the soils to topography and parent material (Soil Survey of Clay County, Nebraska; March 1981).

  20. NE-2012-02-10-13 | Clay County - March 1981

    Typical pattern of soils in the Geary-Holder-Uly and the Hord-Cass-Hobbs associations showing the relationship of the soils to topography and parent material (Soil Survey of Clay County, Nebraska; March 1981).

  21. NE-2012-02-10-14 | Colfax County - January 1982

    Typical pattern of soils and parent material in the Nora-Crofton-Moody association (Soil Survey of Colfax County, Nebraska; January 1982).

  22. NE-2012-02-10-18 | Colfax County - January 1982

    Typical pattern of soils and parent material in the Zook-Shell-Hobbs association (Soil Survey of Colfax County, Nebraska; January 1982).

  23. NE-2012-02-10-20 | Custer County - July 1982

    Typical pattern of soils in the Uly-Coly association and relationship of soils to topography and parent material (Soil Survey of Custer County, Nebraska; July 1982).

  24. NE-2012-02-10-21 | Custer County - July 1982

    Typical pattern of soils in the Holdrege-Hall-Hord association and relationship of soils to topography and parent material (Soil Survey of Custer County, Nebraska; July 1982).

  25. NE-2012-02-10-30 | Fillmore County - July 1986

    Typical pattern of soils, topography, and parent material in the Hastings-Crete association (Soil Survey of Fillmore County, Nebraska; July 1986).

  26. NE-2012-02-10-31 | Fillmore County - July 1986

    Typical pattern of soils, topography, and parent material in the Hastings-Uly-Geary and Muir-Hobbs-Butler associations (Soil Survey of Fillmore County, Nebraska; July 1986).

  27. NE-2012-02-10-32 | Fillmore County - July 1986

    Typical pattern of soils, topography, and parent material in the Crete-Butler association (Soil Survey of Fillmore County, Nebraska; July 1986).

  28. NE-2012-02-10-33 | Fillmore County - July 1986

    Typical pattern of soils, topography, and parent material in the Hastings-Crete-Geary association (Soil Survey of Fillmore County, Nebraska; July 1986).

  29. NE-2012-02-13-09 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Hersh-Valentine-Gates association (Soil Survey of Garfield County, Nebraska; February 1988).

  30. NE-2012-02-13-10 | Garfield County - February 1988

    Typical pattern of soils and parent material in the Uly-Coly association (Soil Survey of Garfield County, Nebraska; February 1988).

  31. NE-2012-02-13-11 | Gosper County - February 1981

    Typical pattern of soils and parent material in the Holdrege-Uly-Coly association (Soil Survey of Gosper County, Nebraska; February 1981).

  32. NE-2012-02-13-13 | Gosper County - February 1981

    Typical pattern of soils and parent material in the Uly-Coly association (Soil Survey of Gosper County, Nebraska; February 1981).

  33. NE-2012-02-13-14 | Gosper County - February 1981

    Typical pattern of soils and parent material in the Coly-Uly-Hobbs association (Soil Survey of Gosper County, Nebraska; February 1981).

  34. NE-2012-02-13-15 | Gosper County - February 1981

    Typical pattern of soils and parent material in the Hobbs-Cozad-Hord association (Soil Survey of Gosper County, Nebraska; February 1981).

  35. NE-2012-02-13-18 | Greeley County - April 1993

    Typical pattern of soils and parent material in the Hord-Cozad and the Boel-Loup-Leshara associations (Soil Survey of Greeley County, Nebraska; April 1993).

  36. NE-2012-02-13-19 | Hall County - January 1962

    Topography, soils, and parent materials, in the southeastern part of Hall County (Soil Survey of Hall County, Nebraska; January 1962).

  37. NE-2012-02-13-22 | Hamilton County - March 1985

    Typical pattern of soils and relationship to topography and parent material in the Hord-Hobbs association (3) and the Holder-Geary association (8) (Soil Survey of Hamilton County, Nebraska; March 1985).

  38. NE-2012-02-13-69 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Nora-Crofton-Moody association (Soil Survey of Platte County, Nebraska; September 1988).

  39. NE-2012-02-13-72 | Platte County - September 1988

    Typical landscape pattern of the soils and the underlying material in the Shell-Hobbs-Muir association (Soil Survey of Platte County, Nebraska; September 1988).

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

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

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

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

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

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

  43. NE-2012-02-13-97 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Uly-Coly-Holdrege association (Soil Survey of Sherman County, Nebraska; May 1990).

  44. NE-2012-02-13-98 | Sherman County - May 1990

    Typical pattern of soils and parent material in the Hord-Hobbs association (Soil Survey of Sherman County, Nebraska; May 1990).

  45. NE-2012-02-14-08 | Valley County - October 1985

    Typical pattern of soils and parent material in the Coly-Uly association (Soil Survey of Valley County, Nebraska; October 1985).

  46. NE-2012-02-14-09 | Valley County - October 1985

    Typical pattern of soils and parent material in the Holdrege-Uly-Cozad association (Soil Survey of Valley County, Nebraska; October 1985).

  47. NE-2012-02-14-19 | Wheeler County - September 1988

    Pattern of soils and parent material in the Coly-Uly association (Soil Survey of Wheeler County, Nebraska; September 1988).

Map Units

Map units containing HOBBS 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
Hobbs silt loam, occasionally flooded3561104713828762wtv4ks01519701:24000
Hobbs silt loam, occasionally flooded35611609814546452wtv4ks02719831:24000
Hobbs silt loam, channeled, frequently flooded3545796414546432wtwmks02719831:24000
Hobbs-Geary silt loams, 0 to 15 percent slopes35691327333112r9d4ks02719831:24000
Hastings-Hobbs complex, 0 to 25 percent slopes38742007713820622wtxrks02919721:24000
Hobbs silt loam, occasionally flooded3561853613820412wtv4ks02919721:24000
Hobbs silt loam, channeled, frequently flooded3545772826057462wtwmks02919721:24000
Hobbs silt loam, frequently flooded3553255413820402zt60ks02919721:24000
Geary-Hobbs silt loams, 0 to 30 percent slopes385186527333192r9d6ks02919721:24000
Hobbs-Geary silt loams, 0 to 15 percent slopes356983027333152r9d4ks02919721:24000
Hobbs silt loam, occasionally flooded35616511505732yjnbks03919851:24000
Hobbs silt loam, occasionally flooded35612873514545302wtv4ks04119771:24000
Hobbs silt loam, channeled, frequently flooded35451305814545292wtwmks04119771:24000
Hobbs silt loam, occasionally flooded3561211913871642wtv4ks06119911:24000
Hobbs silt loam, channeled, frequently flooded354541713871632wtwmks06119911:24000
Hobbs silt loam, occasionally flooded35611457011554032wtv4ks07919701:24000
Clime-Hobbs complex, 0 to 20 percent slopes4585535611554252tt72ks07919701:24000
Hobbs silt loam, channeled, frequently flooded35454026057572wtwmks08919811:24000
Hobbs silt loam, occasionally flooded356161813827762wtv4ks11519811:24000
Hobbs silt loam, channeled, frequently flooded354527913827752wtwmks11519811:24000
Hobbs silt loam, occasionally flooded356113514570602wtv4ks11719771:24000
Hobbs silt loam, channeled, frequently flooded354545114544812wtwmks12719701:24000
Hobbs silt loam, occasionally flooded356118214544822wtv4ks12719701:24000
Hobbs silt loam, occasionally flooded35611242311507572yjnbks13719731:24000
Hobbs silt loam, occasionally flooded35611260613821312wtv4ks14319781:24000
Hobbs-Geary silt loams, 0 to 15 percent slopes3569635227333462r9d4ks14319781:24000
Hobbs silt loam, frequently flooded3553315713821302zt60ks14319781:24000
Hobbs silt loam, channeled, frequently flooded354532013821292wtwmks14319781:24000
Hobbs silt loam, occasionally flooded35611031811509072yjnbks14719851:24000
Hobbs silt loam, channeled, frequently flooded354528811150906307p8ks14719851:24000
Hastings-Hobbs complex, 0 to 25 percent slopes38744872913819162wtxrks15719651:24000
Geary-Hobbs silt loams, 0 to 30 percent slopes38513833927334142r9d6ks15719651:24000
Hobbs silt loam, channeled, frequently flooded3545568226056452wtwmks15719651:24000
Hobbs silt loam, occasionally flooded3561227013819202wtv4ks15719651:24000
Hobbs silt loam, occasionally flooded3561877414332362wtv4ks15919711:24000
Hobbs silt loam, occasionally flooded356159714722802wtv4ks16119701:24000
Hobbs silt loam, channeled, frequently flooded354530414722792wtwmks16119701:24000
Hobbs silt loam, occasionally flooded356179013821702wtv4ks16919891:24000
Hobbs silt loam, channeled, frequently flooded35454531151116307p8ks18319741:24000
Hobbs silt loam, occasionally flooded35613611511172yjnbks18319741:24000
Hobbs silt loam, occasionally flooded35613460014548772wtv4ks20119881:24000
Hobbs silt loam, channeled, frequently flooded3545373526057202wtwmks20119881:24000
Hobbs silt loam, occasionally flooded3561656327330512rdfjne00119701:20000
Hobbs silt loam, frequently flooded3553429827458052rdfpne00119701:20000
Hobbs silt loam, channeled, frequently flooded3545250227458042rdfrne00119701:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes2834113916918932rdg0ne00119701:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes252134622161112rdfzne00119701:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes38511427333642r9d5ne00119701:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25606221611231658ne00119701:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356163604269562vwbyne00319751:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354525784269572vwc0ne00319751:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool35612555327330582vwbyne01119661:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool355365827458072vwbzne01119661:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded35458527458062vwc0ne01119661:20000
Coly, Uly and Hobbs soils, 3 to 30 percent slopes25446644017000442vzkjne01919671:20000
Hobbs silt loam, occasionally flooded, cool35622478027330522rdfhne01919671:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes2521504817000352rdffne01919671:20000
Hobbs silt loam, channeled, frequently flooded3545492027458082rdfsne01919671:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes25397326058672rdfcne01919671:20000
Uly, eroded-Hobbs silt loams, 2 to 40 percent slopes28265922281942vzl3ne01919671:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded35452922166982vwc0ne02119781:20000
Hobbs silt loam, occasionally flooded35611056027330532rdfjne02319791:20000
Hobbs silt loam, channeled, frequently flooded3545547727458092rdfrne02319791:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes, eroded2835447616913341trz5ne02319791:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356194314271052vwbyne02719821:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool35533722169212vwbzne02719821:20000
Hobbs silt loam, channeled, frequently flooded3545725427458142rdfrne03519791:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes2834661016921352rdg0ne03519791:20000
Hobbs silt loam, occasionally flooded3561496527330542rdfjne03519791:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes3851303927333672r9d5ne03519791:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356169714278902vwbyne03719801:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354515434278912vwc0ne03719801:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356110522169822vwbyne03919731:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes253913785826058682rdfcne04119801:20000
Hobbs silt loam, occasionally flooded, cool35623049527330552rdfhne04119801:20000
Hobbs silt loam, channeled, frequently flooded35451551527458152rdfsne04119801:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25602278222816031658ne04119801:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes2521105122281652rdffne04119801:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool35531322170452vwbzne04319721:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256029215169966431658ne04719751:20000
Hobbs silt loam, occasionally flooded, cool35621196327330562rdfhne04719751:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes25211087616996742rdffne04719751:20000
Coly, Uly and Hobbs soils, 3 to 30 percent slopes2544186522288142vzkjne04719751:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes253953626058692rdfcne04719751:20000
Hobbs silt loam, frequently flooded355344927458162rdfqne04719751:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded35451822170752vwc0ne05319751:20000
Hobbs silt loam, channeled, frequently flooded3545757927458172rdfrne05919841:20000
Hobbs silt loam, occasionally flooded3561467127330572rdfjne05919841:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes2834297616923922rdg0ne05919841:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes3851218127333692r9d5ne05919841:20000
Hobbs silt loam, channeled, occasionally flooded355733822188102dgvjne05919841:20000
Nuckolls-Hobbs complex, 11 to 30 percent slopes25836297016919772twlnne06119741:20000
Hobbs silt loam, frequently flooded3553863627458182rdfpne06119741:20000
Hobbs silt loam, occasionally flooded3561513727330592rdfjne06119741:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256058221930831658ne06119741:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256014579169942031658ne06319731:20000
Hobbs silt loam, frequently flooded3553437327458192rdfqne06319731:20000
Hobbs silt loam, channeled, frequently flooded354525302219355307p9ne06319731:20000
Hobbs silt loam, occasionally flooded, cool3562172127330602rdfhne06319731:20000
Hobbs-McCook silt loams, occasionally flooded35631279316997462yl4dne06519751:20000
Hobbs silt loam, channeled, frequently flooded354575151699745307p9ne06519751:20000
Hobbs silt loam, occasionally flooded3561100027330612rdfjne06519751:20000
Hobbs silt loam, occasionally flooded, cool356290727330622rdfhne06519751:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256013221943331658ne06519751:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes, moist2540683126060512pf1pne07119841:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes2539218526058702rdfcne07119841:20000
Hobbs silt loam, occasionally flooded, cool356252527330632rdfhne07119841:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256035760169220131658ne07319781:20000
Hobbs silt loam, channeled, frequently flooded354563311692212307p9ne07319781:20000
Hobbs silt loam, occasionally flooded3561200027330642rdfjne07319781:20000
Hobbs silt loam, occasionally flooded, cool356298227330652rdfhne07319781:20000
Hobbs silt loam, occasionally flooded, cool35621325927330662rdfhne07719871:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes, moist2540716326060392pf1pne07719871:20000
Hobbs silt loam, channeled, frequently flooded3545347127458202rdfsne07719871:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes2539203526058712rdfcne07719871:20000
Hobbs silt loam, occasionally flooded356141016999491v1y2ne07719871:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool35531027458212vwbzne07719871:20000
Hobbs silt loam, channeled, frequently flooded3545323227458222rdfsne07920031:12000
Hall, eroded-Hobbs, silt loams, 0 to 3 perent slopes8849236717001341v241ne07920031:12000
Hobbs silt loam, occasionally flooded3561200027330672rdfjne07920031:12000
Uly, eroded-Hobbs silt loams, 2 to 40 percent slopes2826160317001842vzl3ne07920031:12000
Cozad, sand substratum-Hobbs, occasionally flooded, silt loams, 0 to 3 percent slopes844768517001141v23dne07920031:12000
Hobbs silt loam, occasionally flooded, cool356230227330682rdfhne07920031:12000
Hobbs silt loam, occasionally flooded3561846627330692rdfjne08119821:20000
Hobbs silt loam, channeled, frequently flooded3545497927458232rdfrne08119821:20000
Hobbs silt loam, frequently flooded3553827458242rdfpne08119821:20000
Hobbs silt loam, frequently flooded35531207627458252rdfpne08319671:20000
Hobbs and McCook silt loams, occasionally flooded3541590416922412zwjkne08319671:20000
Coly and Hobbs silt loams2520109916922332yd3wne08319671:20000
Hobbs silt loam, channeled, frequently flooded35459472219520307p9ne08319671:20000
Hobbs silt loam, occasionally flooded356173827330702rdfjne08319671:20000
Hobbs-McCook silt loams, occasionally flooded356311422195222yl4dne08319671:20000
Nuckolls-Hobbs complex, 11 to 30 percent slopes2583522195352twlnne08319671:20000
Hobbs silt loam, occasionally flooded, cool3562527627330712rdfhne09319681:12000
Hobbs silt loam, frequently flooded3553250427458272rdfqne09319681:12000
Hobbs silt loam, channeled, frequently flooded3545198827458262rdfsne09319681:12000
Coly-Hobbs silt loams, 3 to 60 percent slopes25392226058722rdfcne09319681:12000
Hobbs silt loam, occasionally flooded3561685427330722rdfjne09519701:20000
Hobbs silt loam, channeled, occasionally flooded3557683216917661tsf3ne09519701:20000
Hobbs silt loam, channeled, frequently flooded35451527458282rdfrne09519701:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes2834922192122rdg0ne09519701:20000
Hobbs silt loam, occasionally flooded3561200027330732rdfjne09919821:20000
Hobbs silt loam, channeled, frequently flooded3545120727458292rdfrne09919821:20000
Hobbs silt loam, frequently flooded35531127458302rdfpne09919821:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool3561296711442442vwbyne10719891:20000
Hobbs silt loam, frequently flooded, wet3554625704692r989ne10719891:20000
Hobbs silt loam, occasionally flooded35617422192282dh90ne10919771:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes25399979326058732rdfcne11119711:24000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes256013407221976831658ne11119711:24000
Hobbs and McCook silt loams, occasionally flooded3541606016991822yl4cne11119711:24000
Hobbs silt loam, occasionally flooded, cool3562374727330742rdfhne11119711:24000
Coly-Hobbs silt loams, 3 to 60 percent slopes2539401126058742rdfcne11519861:20000
Hobbs silt loam, channeled, frequently flooded354527127458322rdfsne11519861:20000
Hobbs silt loam, occasionally flooded, cool35623827330752rdfhne11519861:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool3561159644274052vwbyne11919811:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354551534274062vwc0ne11919811:20000
Hobbs silt loam, channeled, frequently flooded3545133527458332rdfsne12119781:20000
Hobbs silt loam, occasionally flooded, cool356227127330762rdfhne12119781:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool35533427458342vwbzne12119781:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool3561799427330772vwbyne12519581:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool3553579827458362vwbzne12519581:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded35457827458352vwc0ne12519581:20000
Hobbs silt loam, channeled, frequently flooded3545886627458372rdfrne12919741:20000
Hobbs silt loam, occasionally flooded3561801827330782rdfjne12919741:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes385187127333732r9d5ne12919741:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes252111022187462rdfzne12919741:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes28346722187582rdg0ne12919741:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25607221874731658ne12919741:20000
Geary and Hobbs soils3852327683362r9dvne12919741:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25606234169175631658ne13719671:20000
Hobbs silt loam, occasionally flooded356152027330792rdfjne13719671:20000
Hobbs silt loam, overwash, occasionally flooded356047816917131tscdne13719671:20000
Hord-Hobbs silt loams, 0 to 6 percent slopes888213756427571gbxmne13919701:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356136644275692vwbyne13919701:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool355322754276042vwbzne13919701:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354536122171342vwc0ne13919701:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool3561222574276412vwbyne14119841:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354550164276422vwc0ne14119841:20000
Hobbs silt loam, occasionally flooded3561375527330802rdfjne14319671:20000
Hobbs silt loam, channeled, frequently flooded3545195727458382rdfrne14319671:20000
Hobbs silt loam, frequently flooded355316527458392rdfpne14319671:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25608236169944331658ne14519651:20000
Hobbs-McCook silt loams, occasionally flooded3563631322191162yl4dne14519651:20000
Hobbs silt loam, channeled, frequently flooded354514241699465307p9ne14519651:20000
Hobbs silt loam, channeled, frequently flooded35451503227458402rdfrne15119851:20000
Hobbs silt loam, occasionally flooded35611106127330812rdfjne15119851:20000
Hobbs silt loam, frequently flooded3553364527458412rdfpne15119851:20000
Hobbs silt loam, channeled, occasionally flooded355722522191832dh7kne15119851:20000
Hobbs silt loam, frequently flooded35531691927458442rdfpne15919671:20000
Hobbs silt loam, occasionally flooded3561904227330822rdfjne15919671:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes2521519216911992rdfzne15919671:20000
Hobbs silt loam, channeled, frequently flooded3545109627458432rdfrne15919671:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes, eroded283515022191592dh6sne15919671:20000
Uly-Hobbs silt loams, 11 to 30 percent slopes28361622191642dh6yne15919671:20000
Hobbs silt loam, occasionally flooded, cool35621264427330852rdfhne16319871:20000
Hobbs silt loam, channeled, frequently flooded3545655527458452rdfsne16319871:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes2539637526058752rdfcne16319871:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool3561146354268302vwbyne16719801:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354545504268312vwc0ne16719801:20000
Hobbs silt loam, occasionally flooded35611206327330842rdfjne16919651:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes2834500516923982rdg0ne16919651:20000
Hobbs silt loam, frequently flooded3553224127458472rdfpne16919651:20000
Hobbs silt loam, channeled, frequently flooded3545131627458462rdfrne16919651:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes385122827333762r9d5ne16919651:20000
Hobbs silt loam, channeled, occasionally flooded355721922187392dgs7ne16919651:20000
Hobbs silt loam, 0 to 2 percent slopes, frequently flooded, cool355320954277492vwbzne17319661:20000
Hobbs silt loam, channeled, 0 to 2 percent slopes, frequently flooded354519222172852vwc0ne17319661:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes25394730126058762rdfcne17519831:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes, moist25401364226060482pf1pne17519831:20000
Hobbs silt loam, occasionally flooded, cool3562747327330862rdfhne17519831:20000
Hobbs silt loam, channeled, frequently flooded3545673427458482rdfsne17519831:20000
Coly-Hobbs silt loams, 3 to 17 percent slopes, eroded2545599616998752wtjzne17519831:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356126122173202vwbyne17919701:20000
Geary and Hobbs soils38524439127683652r9dvne18119671:20000
Coly-Hobbs silt loams, 0 to 30 percent slopes25213109916920022rdfzne18119671:20000
Hobbs silt loam, occasionally flooded35611707027330872rdfjne18119671:20000
Hobbs silt loam, frequently flooded35531002127458502rdfpne18119671:20000
Coly-Uly-Hobbs silt loams, 3 to 60 percent slopes25601845169203631658ne18119671:20000
Nuckolls-Hobbs complex, 11 to 30 percent slopes258395522290792twlnne18119671:20000
Hobbs silt loam, channeled, frequently flooded354543227458492rdfrne18119671:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes38513827333782r9d5ne18119671:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes28342122290682rdg0ne18119671:20000
Coly-Hobbs silt loams, 3 to 60 percent slopes2539124816998281v1t5ne18319841:20000
Hobbs silt loam, 0 to 2 percent slopes, occasionally flooded, cool356175616998452vwbyne18319841:20000
Uly-Hobbs silt loams, 11 to 30 percent slopes28361093516923501tt0yne18519741:20000
Hobbs silt loam, channeled, frequently flooded3545723327458512rdfrne18519741:20000
Hobbs silt loam, occasionally flooded3561399427330882rdfjne18519741:20000
Hobbs silt loam, frequently flooded3553384127458522rdfpne18519741:20000
Geary-Hobbs silt loams, 0 to 30 percent slopes3851246627333802r9d5ne18519741:20000
Uly-Hobbs silt loams, 0 to 30 percent slopes283422922188142rdg0ne18519741:20000

Map of Series Extent

Approximate geographic distribution of the HOBBS 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 .