Official Series Description


Lab Data Summary

Aggregate lab data for the HAVERSON soil series. This aggregation is based on all pedons with a current taxon name of HAVERSON, 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 HAVERSON 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
67A40A3448S1950WY015007Haverson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.060833,-104.1725006
6910N077610CO055002Haverson8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6553722,-104.6907944

Water Balance

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

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Competing Series

Soil series competing with HAVERSON 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 HAVERSON 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 HAVERSON series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with HAVERSON, 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. CO-2011-05-27-07 | Otero County - 1972

    Volney-Olney-Dwyer association; part of Minnequa-Penrose soil association in background (Soil Survey of Otero County, Colorado; 1972).

  2. CO-2011-05-27-09 | Otero County - 1972

    Travessilla-Kim-Wiley soil association (Soil Survey of Otero County, Colorado; 1972).

  3. NE-2012-02-13-75 | Red Willow County - April 1967

    Typical pattern of soils in the Hord, terrace-McCook-Bridgeport association (Soil Survey of Red Willow County, Nebraska; April 1967).

  4. NE-2012-02-13-76 | Red Willow County - April 1967

    Typical pattern of soils in the Sandy alluvial land-Las-Glenberg association (Soil Survey of Red Willow County, Nebraska; April 1967).

  5. SD-2012-03-15-12 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils and underlying material in the Bankard-Haverson-Lohmiller and the Samsil-Pierre associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

  6. SD-2012-03-15-28 | Fall River County - April 1982

    Pattern of soils in the Mathias-Butche-Rockoa association (Soil Survey of Fall River County, SD; 1982).

  7. SD-2012-03-15-53 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Samsil-Pierre and Haverson associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

Map Units

Map units containing HAVERSON 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
Haverson loam, 0 to 1 percent slopes177695943043542co01719851:24000
Haverson clay loam158472933375357xco06119771:24000
Haverson loam, 0 to 1 percent slopes, occasionally flooded2712969682437rcco06319961:24000
Haverson loam, 0 to 3 percent slopes, rarely flooded13450711052153jh1co07320011:24000
Haverson loam, 0 to 1 percent slopes3293979451335btco07519741:24000
Haverson loam, frequently flooded3436579451535bwco07519741:24000
Haverson loam, saline3520909451635bxco07519741:24000
Haverson loam, 1 to 3 percent slopes3310069451435bvco07519741:24000
Haverson loam, 1 to 3 percent slopesHeB67441104312tlq0co08719651:24000
Haverson loam, 0 to 1 percent slopesHeA48841104303px8co08719651:24000
Haverson clay loam, 0 to 1 percent slopesHaA38041104293px7co08719651:24000
Haverson sandy loam, 0 to 1 percent slopesHhA16521104323pxbco08719651:24000
Haverson sandy loam, 1 to 3 percent slopesHhB15941104333pxcco08719651:24000
Haverson sandy loam, 3 to 5 percent slopesHhC6061104343pxdco08719651:24000
Glenberg and Haverson soils, sand substrataGnAB393124843302pd4pco09919631:15840
Glenberg and Haverson fine sandy loamsGhAB248024843272pd4lco09919631:15840
Glenberg and Haverson soils, sand substrata, 0 to 1 percent slopesGnA167724843292pd4nco09919631:15840
Glenberg and Haverson fine sandy loams, 0 to 1 percent slopesGhA81624843262pd4kco09919631:15840
Haverson loamHm29029333822pd4rco09919631:15840
Glenberg and Haverson soils, sand substrata, 1 to 3 percent slopesGnB25924843312pd4qco09919631:15840
Glenberg and Haverson fine sandy loams, 1 to 3 percent slopesGhB19624843282pd4mco09919631:15840
Haverson loam, 0 to 1 percent slopesHaA4929493635sgco11519691:15840
Haverson loam, 1 to 3 percent slopesHaB213949372tlq1co11519691:15840
Haverson silty clay loam2694739498635v2co12119821:24000
Haverson loam2458829498435v0co12119821:24000
Haverson loam, terrace254639498535v1co12119821:24000
Haverson loam1775659505935xfco12519761:24000
Haverson loam, 0 to 3 percent slopes29347379512035zdco61719801:24000
Haverson loam, 0 to 1 percent slopes2510857952033622co61819761:24000
Haverson loam, 1 to 3 percent slopes269371952042tlq0co61819761:24000
Haverson clay loam, 0 to 3 percent slopes, rarely flooded2427124964592tqysco62719801:24000
Haverson clay loam, 0 to 3 percent slopes, rarely floodedHvC557429333912tqysco62820081:24000
Haverson loam, 0 to 3 percent slopes604040497506jpplco64119801:24000
Haverson loam, 3 to 9 percent slopes61788497507jppmco64119801:24000
Haverson fine sandy loam, occasionally flooded1178228513826041hdq4ks12919951:24000
Haverson fine sandy loam, occasionally flooded11781724418132myx5ks18719591:24000
Haverson fine sandy loam, occasionally flooded11787615398071np96ks18920051:24000
Haverson and Lohmiller soils, 0 to 4 percent slopesHl17050345731clrmmt11119661:20000
Haverson loam, 0 to 1 percent slopesHa15937345725clrfmt11119661:20000
Haverson silty clay loam, 0 to 1 percent slopesHd11303345728clrjmt11119661:20000
Haverson and Lohmiller soils, channeled, 0 to 35 percent slopesHm10911345732clrnmt11119661:20000
Haverson silty clay loam, 1 to 3 percent slopesHe9074345729clrkmt11119661:20000
Hysham and Haverson soils, 0 to 4 percent slopesHz7317345744cls1mt11119661:20000
Haverson-Hysham loams, 0 to 1 percent slopesHh2993345730clrlmt11119661:20000
McRae-Hysham loams, 1 to 3 percent slopesMu2954345778clt4mt11119661:20000
Haverson clay loam, 0 to 1 percent slopesHc1858345727clrhmt11119661:20000
Haverson loam, gravelly variant, 0 to 1 percent slopesHn1200345733clrpmt11119661:20000
Lohmiller silty clay, gravelly variant, 0 to 1 percent slopesLv1002345767clssmt11119661:20000
Haverson loam, clay substratum, 0 to 1 percent slopesHb387345726clrgmt11119661:20000
Haverson and Lohmiller soils, channeledHGb21426345972cm0dmt60719701:24000
Haverson loam, 0 to 2 percent slopesHfa14154345982cm0qmt60719701:24000
Haverson and Glenberg soilsHGa10136345971cm0cmt60719701:24000
Haverson-Hysham silty clay loamsHfh7718345988cm0xmt60719701:24000
Haverson and Lohmiller soils, frequently floodedHGc5915345973cm0fmt60719701:24000
Haverson silty clay loamHfd5308345985cm0tmt60719701:24000
Haverson and Lohmiller soils, wetHh3098345989cm0ymt60719701:24000
Haverson soils, salineHK2116345974cm0gmt60719701:24000
Hysham loam, 0 to 2 percent slopesHo1785346009cm1lmt60719701:24000
Haverson loam, salineHfc1563345984cm0smt60719701:24000
Haverson silty clay, thick surfaceHff1547345987cm0wmt60719701:24000
Haverson loam, 2 to 4 percent slopesHfb1269345983cm0rmt60719701:24000
Haverson silty clayHfe646345986cm0vmt60719701:24000
Stormitt complex, 4 to 15 percent slopesSX336346149cm63mt60719701:24000
Haverson-Heldt silty clay loams, 0 to 4 percent slopesHn8319347066cn4pmt61119711:24000
Haverson silty clay loam, 0 to 2 percent slopesHm3851347065cn4nmt61119711:24000
Glenberg-Haverson complexGh1672347055cn4bmt61119711:24000
Haverson silt loamHc27298347862cnzcmt64319671:20000
Haverson soils, channeledHf24057347865cnzgmt64319671:20000
Haverson silty clay loamHd19005347863cnzdmt64319671:20000
Haverson silty clayHe9551347864cnzfmt64319671:20000
Haverson soils, salineHg6280347866cnzhmt64319671:20000
Haverson loamHa5061347861cnzbmt64319671:20000
Haverson loam, 0 to 3 percent slopes, frequently flooded5640115543581262wcb0ne04519731:20000
Sulco-Haverson loams, 0 to 50 percent slopes15354658358074d0lsne04519731:20000
Haverson silt loam, occasionally flooded56384398358107d0mvne04519731:20000
Haverson silty clay loam, occasionally flooded56391678358108d0mwne04519731:20000
Haverson silt loam, 0 to 3 percent slopes5637972358106d0mtne04519731:20000
Haverson fine sandy loam, rarely flooded563617416993011v185ne08719651:20000
Haverson fine sandy loam, rarely flooded5636295116537451shvmne15719651:20000
Haverson loam, 0 to 3 percent slopes, frequently flooded5640422198552wcb0ne16119921:20000
Haverson loam, 0 to 3 percent slopes, frequently flooded5640627845592wcb0ne16519931:20000
Haverson silty clay loam, 0 to 1 percent slopes191792592851zpfnm66219791:48000
Haverson loam, 0 to 3 percent slopes, occasionally floodedHaA12013527402wcb3sd00720041:20000
Glenberg and Haverson soilsGh7465353175cvhrsd01919701:24000
Haverson loam, 0 to 2 percent slopes, rarely floodedHeA63943531792wcb1sd01919701:24000
Haverson loam, channeled, 0 to 3 percent slopesLm3435353194cvjcsd01919701:24000
Haverson loam, 2 to 6 percent slopesHeB429353180cvhxsd01919701:24000
Haverson loam, 0 to 2 percent slopes, rarely floodedHa92173551082wcb1sd04719801:24000
Haverson-Craft complex, 0 to 3 percent slopes, rarely floodedHc15673540902zzw6sd05519921:24000
Haverson silt loam, channeled, 0 to 3 percent slopes, occasionally floodedHbA9343540892zzw8sd05519921:24000
Haverson silt loamHa420354088cwg6sd05519921:24000
Haverson silt loam, channeled, 0 to 3 percent slopes, occasionally floodedHbA14163558452zzw8sd13719851:24000
Haverson silt loamHa54542580905cyh8sd60620111:24000
Haverson loam, channeledHc36112580906cyh9sd60620111:24000
Haverson loam, 0 to 2 percent slopes, rarely floodedHaA82425864512wcb1sd60720111:24000
Haverson loam, 0 to 3 percent slopes, occasionally floodedHlA378229254852wcb3sd61019651:20000
Haverson loam, 0 to 2 percent slopes, rarely floodedHhA324529255212wcb2sd61019651:20000
Haverson silty clay loam, 0 to 3 percent slopesHoA11532925507cv5ksd61019651:20000
Haverson loam, 0 to 2 percent slopes, rarely floodedHa372025810202wcb2sd61120111:24000
Haverson-Craft complex, 0 to 3 percent slopes, rarely floodedHc351225810212zzw6sd61120111:24000
Haverson loam, 0 to 3 percent slopes, occasionally floodedHlA1137025826972wcb3sd61320111:24000
Haverson loam, 0 to 2 percent slopes, rarely floodedHhA394525826962wcb2sd61320111:24000
Haverson silty clay loam, 0 to 3 percent slopesHoA35482582698cv3csd61320111:24000
Haverson loam, 0 to 2 percent slopes, rarely flooded7755723493572wcb1wy01119781:24000
Haverson loam, saline, 0 to 3 percent slopes793920349359cqjnwy01119781:24000
Haverson silty clay loam, 0 to 2 percent slopes802919349360cqjpwy01119781:24000
Haverson loam, 1 to 6 percent slopes782649349358cqjmwy01119781:24000
Haverson silty clay loam, 2 to 6 percent slopes81665349361cqjqwy01119781:24000
Haverson and McCook loams, 0 to 3 percent slopesHnA58991047033hyjwy61519651:20000
Haverson fine sandy loam, 0 to 3 percent slopesHaA46601047013hygwy61519651:20000
Haverson loam, gravel substratum variant, 0-3 percent slopesHgA8151047023hyhwy61519651:20000
Kim-Haverson associationKH10251350867cs39wy61919711:24000
Haverson-Glenberg association, salineHK6369350854cs2wwy61919711:24000
Haverson-Glenberg associationHH5641350853cs2vwy61919711:24000
Haverson silt loamHe3308350857cs2zwy61919711:24000
Haverson silt loam, sandy subsoil variantHm1606350860cs32wy61919711:24000
Haverson clay loamHg788350859cs31wy61919711:24000
Haverson silt loam, wetHf664350858cs30wy61919711:24000
Haverson loam, 0 to 3 percent slopes136531049373j62wy72119941:24000

Map of Series Extent

Approximate geographic distribution of the HAVERSON 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 .