Official Series Description


Lab Data Summary

Aggregate lab data for the ETHAN soil series. This aggregation is based on all pedons with a current taxon name of ETHAN, 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 ETHAN 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
102B05N0473S2004SD099002Ethan7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.6134109,-97.1284256

Water Balance

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

Click the image to view it full size.

Geomorphic description summaries for the ETHAN 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.

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 ETHAN, 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. SD-2010-11-01-06 | Clay County - 2003

    Typical pattern of soils and underlying material in the Egan-Ethan-Trent association (Soil Survey of Clay County, South Dakota; 2003).

  2. SD-2010-11-01-10 | Minnehaha County - 2004

    Typical pattern of soils and parent material in the Egan-Ethan-Trent association (Soil Survey of Minnehaha County, South Dakota; 2004).

  3. SD-2010-11-01-16 | Spink County - 2009

    Pattern of soils and underlying materials in the Hand-Carthage-Forestburg association (Soil Survey of Spink County, South Dakota; 2009).

  4. SD-2010-11-01-17 | Spink County - 2009

    Pattern of soils and underlying materials in the Hand-Ethan-Bonilla and Northville-Farmsworth-Durrstein associations (Soil Survey of Spink County, South Dakota; 2009).

  5. SD-2012-03-14-04 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Clarno-Ethan-Bonilla association (Soil Survey of Bon Homme County, SD; 1983).

  6. SD-2012-03-14-05 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Homme-Ethan-Onita association (Soil Survey of Bon Homme County, SD; 1983).

  7. SD-2012-03-14-06 | Bon Homme County - January 1983

    Pattern of soils and underlying material in the Eltree-Yankton-Alcester association (Soil Survey of Bon Homme County, SD; 1983).

  8. SD-2012-03-14-12 | Charles Mix County - February 1982

    Pattern of soils and parent material in the Eakin-Highmore-Ethan association (Soil Survey of Charles Mix County, SD; 1982).

  9. SD-2012-03-14-15 | Clark County - 1999

    Typical pattern of soils and underlying material in the Clarno-Bonilla-Ethan association (Soil Survey of Clark County, SD; 1999).

  10. SD-2012-03-15-16 | Davison County - January 1974

    Typical pattern of soils in associations 5 and 7 near the James River and Firesteel Creek (Soil Survey of Davison County, SD; 1974).

  11. SD-2012-03-15-22 | Douglas County - June 1981

    Pattern of soils and underlying material in the Eakin-Highmore-Ethan association (Soil Survey of Douglas County, SD; 1981).

  12. SD-2012-03-15-23 | Douglas County - June 1981

    Pattern of soils and underlying material in the Highmore-Walke association (Soil Survey of Douglas County, SD; 1981).

  13. SD-2012-03-15-24 | Douglas County - June 1981

    Pattern of soils and underlying material in the Clarno-Ethan-Prosper association (Soil Survey of Douglas County, SD; 1981).

  14. SD-2012-03-15-58 | Jerauld County - September 1994

    Pattern of soils and parent material in the Clarno-Ethan-Prosper association (Soil Survey of Jerauld County, SD; 1994).

  15. SD-2012-03-15-65 | Kingsbury County - November 1997

    Typical pattern of soils and underlying material in the Clarno-Bonilla-Ethan association (Soil Survey of Kingsbury County, SD; 1997).

  16. SD-2012-03-15-66 | Lake County - December 1973

    Relationship of soils to topography and the underlying materials in the Lamo-Rauville association (Soil Survey of Lake County, SD; 1973).

  17. SD-2012-03-15-77 | Miner County - December 1984

    Pattern of soils and parent material in the Clarno-Bonilla-Crossplain association (Soil Survey of Miner County, SD; 1984).

  18. SD-2012-03-15-83 | Moody County - April 1989

    Pattern of soils and parent material in the Egan-Baltic association (Soil Survey of Moody County, SD; 1989).

  19. SD-2012-03-16-02 | Turner County - November 1982

    Pattern of soils and parent material in the Egan-Ethan association (Soil Survey of Turner County, SD; 1982).

Map Units

Map units containing ETHAN 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
Houdek-Ethan loams, 2 to 6 percent slopesHeB479413548532tlbmsd00319791:20000
Houdek-Ethan loams, 6 to 9 percent slopesHeC158273548542wkqksd00319791:20000
Eakin-Ethan complex, 2 to 6 percent slopesEeB95283548472xhbvsd00319791:20000
Ethan-Betts loams, 9 to 15 percent slopesEtD47173548492wkq8sd00319791:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC29813548362wknzsd00319791:20000
Betts-Ethan loams, 15 to 40 percent slopesBeE7413548292wkq9sd00319791:20000
Houdek-Ethan loams, 6 to 9 percent slopesHeC132653545852wkqksd00519761:20000
Ethan-Betts loams, 9 to 15 percent slopesBfD102033545512wkq8sd00519761:20000
Hand-Ethan loams, 6 to 9 percent slopesHbC88343545812xhd2sd00519761:20000
Houdek-Ethan loams, 2 to 6 percent slopesHeB11203545842tlbmsd00519761:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHnB368114182762yyfxsd00919811:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCsB289534182552wknysd00919811:20000
Homme-Ethan-Tetonka complex, 0 to 6 percent slopesHpB23677418277g17tsd00919811:20000
Ethan-Homme complex, 6 to 9 percent slopesEpC141264182712yyfysd00919811:20000
Betts-Ethan loams, 15 to 40 percent slopesEmE133364182682wkq9sd00919811:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesEnC79914182692wknzsd00919811:20000
Ethan-Davis loams, 9 to 15 percent slopesEoD7824418270g17lsd00919811:20000
Homme-Ethan-Tetonka complex, 0 to 9 percent slopesHpC3419418278g17vsd00919811:20000
Ethan-Alcester complex, 1 to 6 percent slopesEhB2335418266g17gsd00919811:20000
Ethan-Alcester complex, 1 to 9 percent slopesEhC1862418267g17hsd00919811:20000
Gavins-Ethan loams, 15 to 40 percent slopesGeE1461418273g17psd00919811:20000
Talmo-Ethan very stony complex, 6 to 40 percent slopesTbE1334418288g185sd00919811:20000
Eltree-Ethan complex, 6 to 9 percent slopesEbC653418261g179sd00919811:20000
Eltree-Ethan complex, 9 to 40 percent slopesEbE577418262g17bsd00919811:20000
Egan-Ethan complex, 2 to 6 percent slopesEaB39341874731c3psd01119951:24000
Ethan-Egan complex, 5 to 9 percent slopesEwC22841875631c3ksd01119951:24000
Ethan-Clarno loams, 9 to 15 percent slopesEvD140418755g1r7sd01119951:24000
Eakin-Ethan complex, 2 to 6 percent slopesEeB856723550202xhbvsd02319801:20000
Eakin-Ethan complex, 6 to 9 percent slopesEeC442763550212xhc0sd02319801:20000
Betts-Ethan loams, 15 to 40 percent slopesBdF226563550052wkq9sd02319801:20000
Ethan-Betts loams, 9 to 15 percent slopesBeE194133550062wkq8sd02319801:20000
Ethan-Clarno loams, 9 to 15 percent slopesEtD17418355024cxfdsd02319801:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHmB166793550362wkqdsd02319801:20000
Ethan-Homme complex, 6 to 9 percent slopesEuC42763550252wkprsd02319801:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCeB36583550102wknysd02319801:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC17623550112wknzsd02319801:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCeB28564177052wknysd02519921:20000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHnB16584177402tlb9sd02519921:20000
Ethan-Betts loams, 9 to 15 percent slopesBkD2074176932wkq8sd02519921:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC1594177062wknzsd02519921:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopesEoD101417723g0nysd02519921:20000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHnC594177412tlbbsd02519921:20000
Egan-Ethan-Trent complex, 1 to 6 percent slopesEgB1864644555531c3lsd02719951:24000
Egan-Ethan-Tetonka complex, 0 to 6 percent slopesEfB7382445554gymqsd02719951:24000
Betts-Ethan loams, 15 to 40 percent slopesEoE30604455622wkq9sd02719951:24000
Ethan-Bon, channeled, loams, 0 to 20 percent slopesEpD2876445563gyn0sd02719951:24000
Ethan-Clarno loams, 9 to 15 percent slopesErD2281445566gyn3sd02719951:24000
Ethan-Clarno-Bon, channeled, loams, 0 to 9 percent slopesEtC2160445568gyn5sd02719951:24000
Ethan-Clarno loams, 6 to 9 percent slopesErC20234455652wkp0sd02719951:24000
Ethan-Clarno-Bon loams 0 to 6 percent slopesEsB1500445567gyn4sd02719951:24000
Ethan-Bon, channeled, loams, 0 to 40 percent slopesEpE1495445564gyn1sd02719951:24000
Ethan-Davison-Tetonka complex, 0 to 6 percent slopesEuB1013445569gyn6sd02719951:24000
Ethan-Betts loams, 9 to 15 percent slopesEoD5714455612wkq8sd02719951:24000
Egan-Ethan complex, 2 to 6 percent slopesEeB18044555331c3psd02719951:24000
Ethan-Egan complex, 5 to 9 percent slopesEvC17644557031c3ksd02719951:24000
Ethan-Talmo complex, 15 to 40 percent slopesEzE89445571gyn8sd02719951:24000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesChB386783529112wknysd03519661:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC66673529092wknzsd03519661:20000
Betts-Ethan loams, 15 to 40 percent slopesBeE62743529002wkq9sd03519661:20000
Ethan-Betts loams, 9 to 15 percent slopesBhD36663529012wkq8sd03519661:20000
Ethan-Betts loams, 5 to 9 percent slopes, erodedEtC22145352918cv7gsd03519661:20000
Eakin-Ethan complex, 2 to 6 percent slopesEaB525433548932xhbvsd04319791:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCnB324273548832wknysd04319791:20000
Clarno-Ethan-Prosper loams, 0 to 3 percent slopesCnA9781354882cx8tsd04319791:20000
Eakin-Ethan complex, 0 to 3 percent slopesEaA82323548922yyhzsd04319791:20000
Eakin-Ethan complex, 6 to 9 percent slopesEaC69293548942xhc0sd04319791:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC41073548812wknzsd04319791:20000
Ethan-Clarno loams, 9 to 15 percent slopesEtD1801354896cx98sd04319791:20000
Betts-Ethan loams, 15 to 40 percent slopesBeE17303548782wkq9sd04319791:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHmB11393549042yyfxsd04319791:20000
Ethan-Homme complex, 6 to 9 percent slopesEwC18531192112yyfysd04319791:20000
Houdek-Ethan loams, 6 to 9 percent slopesHuD146213526272wkqksd05919591:20000
Ethan-Houdek loams, hillyZhD50193527042yyhjsd05919591:20000
Betts-Ethan loams, 15 to 40 percent slopesZhE15053527052wkq9sd05919591:20000
Ethan-Houdek loams, hillyZaD10433527032yyhhsd05919591:20000
Ethan-Glenham loams, 6 to 9 percent slopesJgC456035329530t33sd06519701:20000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHwB310433564462tlb9sd07319871:20000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHwC279293564472tlbbsd07319871:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCpB257973564132wknysd07319871:20000
Ethan-Betts loams, 9 to 15 percent slopesEtD185503564302wkq8sd07319871:20000
Eakin-Ethan-Onita complex, 2 to 6 percent slopesEaB112333564272yyj0sd07319871:20000
Betts-Ethan loams, 6 to 40 percent slopes, stonyBmD9341356407cyw0sd07319871:20000
Hand-Ethan-Prosper loams, 1 to 5 percent slopesHaB79993564352yyghsd07319871:20000
Betts-Ethan loams, 15 to 40 percent slopesBoE64263564082wkq9sd07319871:20000
Hand-Ethan-Prosper loams, 2 to 9 percent slopesHaC47623564362yygjsd07319871:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCpC42003564142wknzsd07319871:20000
Delmont-Ethan loams, 9 to 20 percent slopesDkD2336356421cywgsd07319871:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCeB450244174652wknysd07719921:20000
Ethan-Clarno loams, 6 to 9 percent slopesEtC58724174822wkp0sd07719921:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopesEoD4554417481g0f4sd07719921:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC34494174662wknzsd07719921:20000
Ethan-Clarno loams, 9 to 15 percent slopesEtD1255417483g0f6sd07719921:20000
Ethan-Betts loams, 9 to 15 percent slopesEnD10004174802wkq8sd07719921:20000
Egan-Ethan complex, 6 to 9 percent slopes, erodedEeC219515416491fzd6sd07919671:20000
Clarno-Ethan loams, 9 to 16 percent slopesCeD8098416479fzctsd07919671:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCeC31074164782wknzsd07919671:20000
Ethan-Clarno stony complex, 6 to 25 percent slopesEsE2102416497fzddsd07919671:20000
Egan-Ethan complex, 2 to 6 percent slopesEeB197841649031c3psd07919671:20000
Ethan-Clarno loams, 16 to 21 percent slopesErE1382416496fzdcsd07919671:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCeB11214164772wknysd07919671:20000
Betts-Ethan loams, 15 to 40 percent slopesEoF10424164952wkq9sd07919671:20000
Ethan-Davis stony complex, 3 to 21 percent slopesEtD966416498fzdfsd07919671:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesEbC164684180252wknzsd08719761:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesChB114784180162wknysd08719761:20000
Hand-Ethan loams, 3 to 6 percent slopesHeB111264180312yyhlsd08719761:20000
Ethan-Betts loams, 9 to 15 percent slopesEcD105954180262wkq8sd08719761:20000
Betts-Ethan loams, 15 to 40 percent slopesBcE87544180062wkq9sd08719761:20000
Egan-Ethan complex, 5 to 9 percent slopesEaC8298418024g0znsd08719761:20000
Wentworth-Ethan complex, 2 to 5 percent slopesWcB4812418041g106sd08719761:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCkB234743553892wknysd09719831:20000
Ethan-Clarno loams, 6 to 9 percent slopesEgC42963553982wkp0sd09719831:20000
Ethan-Clarno complex, 9 to 15 percent slopesEgD970355399cxthsd09719831:20000
Ethan-Egan complex, 3 to 7 percent slopesEmB527355400cxtjsd09719831:20000
Egan-Ethan-Trent complex, 1 to 6 percent slopesEeB4950244603331c3lsd09919951:24000
Ethan-Egan complex, 5 to 9 percent slopesEuC2793444604131c3ksd09919951:24000
Ethan-Clarno loams, 9 to 15 percent slopesEtD4433446040gz4dsd09919951:24000
Ethan-Betts loams, 9 to 15 percent slopesEpD13904460382wkq8sd09919951:24000
Betts-Ethan loams, 15 to 40 percent slopesBeE12304460022wkq9sd09919951:24000
Egan-Ethan complex, 2 to 6 percent slopesEaB117844603131c3psd09919951:24000
Ethan-Clarno loams, 6 to 25 percent slopes, very stonyEsE938446039gz4csd09919951:24000
Ethan, very stony-Egan complex, 2 to 9 percent slopesExC464446042gz4gsd09919951:24000
Egan-Ethan complex, 2 to 6 percent slopesEeB1806241832131c3psd10119851:20000
Ethan-Egan complex, 5 to 9 percent slopesEtC630341832631c3ksd10119851:20000
Ethan-Egan complex, 2 to 9 percent slopes, very stonyExC1158418327g19fsd10119851:20000
Ethan-Clarno loams, 6 to 25 percent slopesErD967418324g19bsd10119851:20000
Ethan-Clarno loams, 6 to 25 percent slopes, very boulderyEsD713418325g19csd10119851:20000
Glenham-Ethan-Prosper loams, 1 to 6 percent slopesJgB1584635534230t2ysd10719831:20000
Ethan-Glenham loams, 6 to 9 percent slopesJgC451341156230t33sd10719831:20000
Glenham-Ethan, very stony-Prosper loams, 2 to 9 percent slopesJaC196341156130t39sd10719831:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCmB261793547702wknysd11119781:20000
Hand-Ethan loams, 2 to 6 percent slopesHbB140593547912xhd1sd11119781:20000
Ethan-Clarno loams, 6 to 9 percent slopesEeC117493547852wkp0sd11119781:20000
Forestburg-Ethan loamy fine sands, 2 to 6 percent slopesFcB5622354788cx5ssd11119781:20000
Houdek-Ethan loams, 2 to 6 percent slopesHdB49293547932tlbmsd11119781:20000
Betts-Ethan loams, 15 to 40 percent slopesBaE48783547552wkq9sd11119781:20000
Ethan-Betts loams, 9 to 15 percent slopesBbD16583547562wkq8sd11119781:20000
Forestburg-Ethan loamy fine sands, 6 to 9 percent slopesFcC533354789cx5tsd11119781:20000
Hand-Ethan-Bonilla loams, 1 to 6 percent slopesHgB266573566422yygxsd11519971:24000
Hand-Ethan-Carthage complex, 1 to 6 percent slopesHhB60593566442yyh0sd11519971:24000
Hand-Ethan-Bonilla loams, 2 to 9 percent slopesHgC52913566432yygysd11519971:24000
Houdek-Ethan-Prosper loams, 1 to 6 percent slopesHtB52103566552tlb9sd11519971:24000
Ethan-Hand loams, 9 to 20 percent slopesEnD30743566052yygzsd11519971:24000
Hand-Ethan loams, 6 to 9 percent slopesHfC7313566412yyhmsd11519971:24000
Talmo-Ethan complex, 9 to 40 percent slopes, very stonyTbE448356711cz5tsd11519971:24000
Betts-Ethan loams, 15 to 40 percent slopesEmE1793566042wkq9sd11519971:24000
Houdek-Ethan-Prosper loams, 2 to 9 percent slopesHtC523566562tlbbsd11519971:24000
Glenham-Ethan-Prosper loams, 1 to 6 percent slopesGlB1105335307830t2ysd11919671:20000
Ethan-Glenham loams, 6 to 9 percent slopesJgC908535309030t33sd11919671:20000
Egan-Ethan complex, 2 to 6 percent slopesEeB5402941822831c3psd12519801:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesCoB211804182172wknysd12519801:20000
Ethan-Egan complex, 5 to 9 percent slopesEtC1006841823431c3ksd12519801:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCoC70064182182wknzsd12519801:20000
Ethan-Betts loams, 9 to 15 percent slopesEsD68334182322wkq8sd12519801:20000
Ethan-Egan complex, 2 to 6 percent slopesEtB3053418233g16dsd12519801:20000
Betts-Ethan loams, 15 to 40 percent slopesBeE16684182052wkq9sd12519801:20000
Egan-Ethan complex, 0 to 2 percent slopesEeA923418227g166sd12519801:20000
Glenham-Ethan-Prosper loams, 1 to 6 percent slopesGmB10341157330t2ysd12919751:20000
Betts-Ethan loams, 15 to 40 percent slopesEmE225104180812wkq9sd13519771:20000
Egan-Ethan-Trent complex, 1 to 6 percent slopesEbB22115311920631c3lsd13519771:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesEnC125744180822wknzsd13519771:20000
Egan-Ethan-Trent complex, 2 to 9 percent slopesEbC1184041807431c3msd13519771:20000
Ethan-Davis loams, 9 to 15 percent slopesEoD10358418083g11ksd13519771:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHnB86224180732yyfxsd13519771:20000
Boyd-Ethan association, 15 to 40 percent slopesBoE1386418060g10tsd13519771:20000
Thurman-Ethan complex, 2 to 9 percent slopesTcC1098418108g12csd13519771:20000
Ethan-Talmo loams, 6 to 15 percent slopesEpD748418084g11lsd13519771:20000
Ethan stony loam, 3 to 25 percent slopesEkD687418080g11gsd13519771:20000
Ethan-Clarno loams, 9 to 15 percent slopesErD80418123g12vsd13519771:20000
Ethan-Egan complex, 5 to 9 percent slopesEtC5641812531c3ksd13519771:20000
Ethan-Bon, channeled, loams, 0 to 20 percent slopesEsD14418124g12wsd13519771:20000
Betts-Ethan loams, 15 to 40 percent slopesBeE339744179382wkq9sd60219751:20000
Clarno-Ethan-Bonilla loams, 2 to 9 percent slopesCnC185744179472wknzsd60219751:20000
Ethan-Betts loams, 9 to 15 percent slopesEtD120444179672wkq8sd60219751:20000
Ethan-Betts loams, 6 to 9 percent slopes, erodedEtC28231417966g0xssd60219751:20000
Ethan-Betts loams, 3 to 6 percent slopesEtB4795417965g0xrsd60219751:20000
Ethan-Clarno loams, 6 to 9 percent slopesEuC38184179692wkp0sd60219751:20000
Ethan-Homme complex, 6 to 9 percent slopesHoC32324179822yyfysd60219751:20000
Homme-Ethan-Onita complex, 1 to 6 percent slopesHoB10514179532yyfxsd60219751:20000
Clarno-Ethan-Bonilla loams, 1 to 6 percent slopesEuB6184179682wknysd60219751:20000

Map of Series Extent

Approximate geographic distribution of the ETHAN 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 .