Official Series Description


Lab Data Summary

Aggregate lab data for the ENDERS soil series. This aggregation is based on all pedons with a current taxon name of ENDERS, 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 ENDERS 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
11777-OK-51-1577-OK101-51-15Enders4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5658722,-95.2111333
11785P0065S1980AR047001Enders2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6472015,-93.7316971
11975-OK-3-375-OK005-3-3Enders4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.3526389,-95.9931139
n/a81KY-231-00481KY-231-004Enders3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4293S1963KY085004Enders4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4300S1963KY085011Enders5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ENDERS 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 ENDERS 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 ENDERS 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 ENDERS 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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Competing Series

Soil series competing with ENDERS 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 ENDERS 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 ENDERS 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 ENDERS, 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. AL-2012-04-24-07 | Fayette County - November 1965

    Block diagram showing typical topography and the major soils in the Montevallo-Enders-Townley association (Soil Survey of Fayette County, Alabama; November 1965).

  2. AR-2011-05-27-01 | Boone County - 1981

    Pattern of soils and parent materials in Enders-Nella-Mountainburg unit (Soil Survey of Boone County, Arkansas; 1981).

  3. AR-2011-05-27-03 | Newton County - 1988

    Pattern of soils and parent material in Nella-Enders-Steprock general soil map unit (Soil Survey of Newton County, Arkansas; 1988)

  4. AR-2012-05-08-01 | Boone County - June 1981

    Pattern of soils and parent material in Enders-Nella-Mountburg unit (Soil Survey of Boone County, Arkansas; June 1981).

  5. AR-2012-05-08-04 | Newton County - March 1988

    Pattern of soils and parent material in Nella-Enders-Steprock general soil map unit (Soil Survey of Newton County, Arkansas; March 1988).

  6. OK-2012-02-17-32 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 1, 2, 3, and 7 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

  7. OK-2012-02-17-33 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 3 and 4 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

  8. OK-2012-02-17-45 | Sequoyah County - June 1970

    Typical pattern of soils in associations 1, 2, and 5 (Soil Survey of Sequoyah County, Oklahoma; June 1970).

Map Units

Map units containing ENDERS 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
Enders gravelly fine sandy loam, 10 to 15 percent slopesEnD393523321kkkbal01519591:20000
Enders gravelly fine sandy loam, 6 to 10 percent slopes , erodedEnC2368523320kkk9al01519591:20000
Enders gravelly fine sandy loam, 2 to 6 percent slopes erodedEnB2208523319kkk8al01519591:20000
Enders and albertville soils, shallow, 10 to 15 percent slopes, erodedEsD27637328899c17nal04319601:20000
Enders and albertville soils, shallow, 6 to 10 percent slopes, erodedEsC24354328896c17kal04319601:20000
Enders and albertville silty clay loams, shallow, 10 to 15 percent slopes, severely erodedErD32377328894c17hal04319601:20000
Enders (Townley) silt loam, 2 to 6 percent slopes, erodedEnB220163288912ykf6al04319601:20000
Enders (Townley) silt loam, 6 to 10 percent slopes, erodedEnC213103288922ykf4al04319601:20000
Enders and albertville silty clay loams, shallow, 6 to 10 percent slopes, severely erodedErC31303328893c17gal04319601:20000
Enders and albertville soils, shallow, 2 to 6 percent slopes, erodedEsB2988328895c17jal04319601:20000
Enders and albertville soils, shallow, 10 to 15 percent slopesEsD704328898c17mal04319601:20000
Enders and Muse soils, 6 to 15 percent slopes, severely erodedEsC3597328897c17lal04319601:20000
Enders loam, 6 to 10 percent slopes, erodedEdC25138329453c1tjal05719631:15840
Enders loam, 2 to 6 percent slopes, erodedEdB24237329451c1tgal05719631:15840
Enders loam, 6 to 10 percent slopesEdC2528329452c1thal05719631:15840
Enders clay loam, 6 to 10 percent slopes, severely erodedEcC31258329448c1tcal05719631:15840
Enders loam, 2 to 6 percent slopesEdB5163294502ykdyal05719631:15840
Enders loam, 10 to 15 percent slopes, erodedEdD2471329455c1tlal05719631:15840
Enders clay loam, 2 to 6 percent slopes, severely erodedEcB3349329447c1tbal05719631:15840
Enders clay loam, 10 to 15 percent slopes, severely erodedEcD3349329449c1tdal05719631:15840
Enders loam, 10 to 15 percent slopesEdD348329454c1tkal05719631:15840
Enders (Albertville) silt loam, 2 to 5 percent slopesEdu23375228642zpq6al07119431:24000
Enders (Albertville) silt loam, 5 to 10 percent slopesEdo22335228632zn17al07119431:24000
Enders (Albertville) silt loam, 5 to 10 percent slopes, erodedEdn15095228622ykf3al07119431:24000
Enders (Albertville) silt loam, 2 to 5 percent slopes, erodedEde4855228602ykf5al07119431:24000
Enders (Townley) silt loam, 5 to 10 percent slopes, eroded, shallowEda4225228592zjxpal07119431:24000
Enders (Townley) silt loam, 5 to 10 percent slopes, shallowEdg2035228612zjxnal07119431:24000
Enders loam, 5 to 12 percent slopesEc136223301162ykf0al07919501:20000
Enders loam, 5 to 12 percent slopes, erodedEa20643301142ykdzal07919501:20000
Enders loam, 2 to 5 percent slopes, erodedEb4383301152ykdxal07919501:20000
Enders (Townley) loam, 5 to 10 percent slopes, erodedEb82673310692ykf1al10319491:15840
Enders (Townley) loam, 5 to 10 percent slopesEd31273310712ykf2al10319491:15840
Enders loam, 2 to 5 percent slopes, erodedEc20843310702ykdxal10319491:15840
Enders loam, 2 to 5 percent slopesEe13193310722zpq7al10319491:15840
Enders-Montevallo association, steepEmE3356523234kkgjal12119691:20000
Enders-Townley-Montevallo complex, 6 to 15 percent slopesEtD1432523235kkgkal12119691:20000
Enders very stony loam, 12 to 30 percent slopesEoF19495650302s1y9ar00719731:20000
Enders very gravelly loam, 3 to 12 percent slopesEnD1648565028lyyqar00719731:20000
Enders very stony loam, 3 to 12 percent slopesEoD6815650292s1y8ar00719731:20000
Enders-Nella complex, 8 to 20 percent slopes16105275651012s1ybar00919771:20000
Enders-Nella complex, 20 to 40 percent slopes1763875651022rxhfar00919771:20000
Enders gravelly loam, 3 to 8 percent slopes1520255651002rxhbar00919771:20000
Enders-Leesburg complex, 8 to 20 percent slopes14179205652182rxhcar01519811:20000
Enders-Mountainburg association, 20 to 40 percent slopes1573505652192s1yvar01519811:20000
Enders gravelly loam, 3 to 8 percent slopes1224305652162rxhbar01519811:20000
Enders gravelly loam, 8 to 15 percent slopes1313205652172s1ynar01519811:20000
Enders-Steprock complex, 8 to 20 percent slopes93408030860632s1xzar02319831:20000
Enders-Nella-Steprock complex, 8 to 20 percent slopes71442930860612s1y2ar02319831:20000
Enders-Steprock complex, 20 to 40 percent slopes101310530860312s1y0ar02319831:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes47865308605830x8dar02319831:20000
Enders-Nella-Steprock complex, 20 to 40 percent slopes8519030860622s1y3ar02319831:20000
Enders stony fine sandy loam, 8 to 15 percent slopes63325308606030x8mar02319831:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes51370308605930x8har02319831:20000
Enders gravelly fine sandy loam, 12 to 45 percent slopes101152356537630x8gar02919771:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes983535654102s1ydar02919771:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes878905654092s1yfar02919771:20000
Enders gravelly fine sandy loam, 1 to 3 percent slopes758856540830x8nar02919771:20000
Nella-Enders complex, 20 to 40 percent slopes221123825654262y1ktar03319751:20000
Enders stony fine sandy loam, 12 to 50 percent slopes7428845654392s1ypar03319751:20000
Enders gravelly fine sandy loam, 8 to 20 percent slopes63070556543830x8qar03319751:20000
Nella-Enders association, very steep2311838565427lzclar03319751:20000
Enders-Mountainburg association, 8 to 20 percent slopes877385654402s1ytar03319751:20000
Enders-Mountainburg association, 20 to 40 percent slopes942335654412s1yvar03319751:20000
Enders fine sandy loam, 3 to 8 percent slopes532185654372s1yqar03319751:20000
Nella-Enders complex, 8 to 20 percent slopes2120975654252y1kwar03319751:20000
Enders gravelly fine sandy loam, 12 to 45 percent slopes51554256551230x8gar04519751:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes4992956551130x8har04519751:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes3557756550630x8dar04519751:20000
Allen-Enders association, steep, (nella)AEE24282565522lzgnar04719671:20000
Allen-Enders association, rolling, (nella)AED15414565521lzgmar04719671:20000
Enders-Mountainburg association, 20 to 40 percent slopesEME113975655412s1yvar04719671:20000
Allen-Enders association, very steep, (nella)AEF5494565523lzgpar04719671:20000
Enders-Mountainburg association, 8 to 20 percent slopesEMD54605655402s1ytar04719671:20000
Holston-Enders association, very steep, (nella, enders)HOF3636565555lzhqar04719671:20000
Holston-Enders association, steep, (nella, enders)HOE2753565554lzhpar04719671:20000
Enders gravelly silt loam, 8 to 20 percent slopes, erodedEnD225675655432s1yhar04719671:20000
Enders gravelly silt loam, 3 to 8 percent slopes, erodedEnC218505655422s1yjar04719671:20000
Enders stony fine sandy loam, 12 to 50 percent slopesEsF14205655442s1ypar04719671:20000
Holston-Enders association, rolling, (nella, enders)HOD1251565553lzhnar04719671:20000
Enders stony fine sandy loam, 20 to 45 percent slopes22291595657422s1ygar06319801:20000
Enders stony fine sandy loam, 8 to 20 percent slopes21122685657412s1ycar06319801:20000
Enders fine sandy loam, 8 to 12 percent slopes2060145657402s1ymar06319801:20000
Enders fine sandy loam, 3 to 8 percent slopes1936005657382s1yqar06319801:20000
Enders stony silt loam, 12 to 25 percent slopesEsE2957565805lzrsar06719711:20000
Enders silt loam, 3 to 12 percent slopesEnD122956580430x8var06719711:20000
Nella-Enders complex, 20 to 40 percent slopesNEE535905658552y1ktar07119731:24000
Nella-Enders complex, 8 to 20 percent slopesNED161115658542y1kwar07119731:24000
Nella-Enders association, very steepNEF10836565856lztfar07119731:24000
Leesburg-Enders association, very steepLEF8014565835lzsrar07119731:24000
Leesburg-Enders association, steepLEE3060565834lzsqar07119731:24000
Mountainburg-Enders association, steepMEE2920565844lzt1ar07119731:24000
Enders gravelly fine sandy loam, 5 to 15 percent slopesEnD282556583030x8par07119731:24000
Enders-Mountainburg association, 8 to 20 percent slopesEMD23335658282s1ytar07119731:24000
Enders-Mountainburg association, 20 to 40 percent slopesEME21355658292s1yvar07119731:24000
Mountainburg-Enders association, rollingMED2083565843lzt0ar07119731:24000
Mountainburg-Enders association, very steepMEF806565845lzt2ar07119731:24000
Enders-Mountainburg complex, 20 to 40 percent slopes14533205658772xhyvar08319771:20000
Enders stony silt loam, 12 to 45 percent slopes1236739565875lzv1ar08319771:20000
Enders gravelly silt loam, 8 to 20 percent slopes103210356587330x8kar08319771:20000
Nella-Enders complex, 20 to 40 percent slopes28215845658922y1kvar08319771:20000
Enders-Mountainburg complex, 8 to 20 percent slopes13181255658762xhywar08319771:20000
Nella-Enders complex, 8 to 20 percent slopes27168935658912y1ksar08319771:20000
Enders silt loam, 8 to 20 percent slopes8732356590530x8tar08319771:20000
Enders silt loam, 3 to 8 percent slopes7610456590430x8far08319771:20000
Enders gravelly silt loam, 3 to 8 percent slopes9328056590630x8jar08319771:20000
Enders gravelly silt loam, 20 to 45 percent slopes1184956587430x8rar08319771:20000
Enders-Leesburg complex, 8 to 20 percent slopes151011915659142rxhcar08719821:20000
Enders-Leesburg complex, 20 to 40 percent slopes16943255659152rxhdar08719821:20000
Enders stony loam, 3 to 15 percent slopes14142025659132s1yrar08719821:20000
Enders gravelly loam, 3 to 8 percent slopes1231465659112rxhbar08719821:20000
Enders gravelly loam, 8 to 15 percent slopes1322915659122s1ynar08719821:20000
Nella-Enders complex, 8 to 20 percent slopes35525245660172y1kwar10119841:20000
Nella-Enders stony loams, 20 to 40 percent slopes3635718566018lzznar10119841:20000
Enders-Leesburg complex, 8 to 20 percent slopes15274785659952rxhcar10119841:20000
Enders-Leesburg complex, 20 to 40 percent slopes16140765659962rxhdar10119841:20000
Enders stony loam, 3 to 15 percent slopes13134565659932s1yrar10119841:20000
Enders gravelly loam, 8 to 15 percent slopes1253655659922s1ynar10119841:20000
Enders gravelly loam, 3 to 8 percent slopes1146265659912rxhbar10119841:20000
Enders stony loam, 15 to 40 percent slopes1437105659942s1xwar10119841:20000
Enders stony fine sandy loam, 12 to 20 percent slopes12449056608330x8lar10519801:20000
Enders stony fine sandy loam, 20 to 45 percent slopes134210566084m01sar10519801:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes11186056608230x8har10519801:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes10152056608130x8dar10519801:20000
Nella-Enders-Mountainburg association, very steep3451174566140m03lar11519781:20000
Nella-Enders complex, 20 to 40 percent slopes33348285661392y1ktar11519781:20000
Enders-Mountainburg association, steep1121224566115m02sar11519781:20000
Enders stony fine sandy loam, 12 to 45 percent slopes915996566160m047ar11519781:20000
Nella-Enders complex, 8 to 20 percent slopes32131605661382y1kwar11519781:20000
Enders-Mountainburg association, rolling109348566114m02rar11519781:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes8478056615930x8har11519781:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes7249756615830x8dar11519781:20000
Leesburg-Enders association, steep151756566119m02xar11519781:20000
Enders-Mountainburg complex, 20 to 40 percent slopesEMF356005663352xhyvar12719931:20000
Enders-Mountainburg complex, 8 to 20 percent slopesEME303375663342xhywar12719931:20000
Nella-Enders complex, 20 to 40 percent slopesNEF205195663562y1kvar12719931:20000
Nella-Enders complex, 8 to 20 percent slopesNEE102095663552y1ksar12719931:20000
Enders-Mountainburg complex, 40 to 65 percent slopesEMG9550566336m09xar12719931:20000
Enders gravelly silt loam, 8 to 20 percent slopesEdE458256633830x8kar12719931:20000
Enders gravelly silt loam, 3 to 8 percent slopesEdC155456633730x8jar12719931:20000
Enders stony silt loam, 20 to 40 percent slopesEdF977566339m0b0ar12719931:20000
Enders-Nella complex, 3 to 20 percent slopes24CD243185664592s1y4ar12919871:20000
Enders stony loam, 3 to 15 percent slopes22CD220075664572s1yrar12919871:20000
Enders-Nella complex, 20 to 40 percent slopes24EF91205664602rxhfar12919871:20000
Enders gravelly loam, 3 to 8 percent slopes20C69535664552rxhbar12919871:20000
Enders stony loam, 15 to 40 percent slopes22EF34115664582s1xwar12919871:20000
Enders gravelly loam, 8 to 15 percent slopes20DE16125664562s1ynar12919871:20000
Enders-Mountainburg complex, 20 to 40 percent slopesEmE495525663782xhyvar13119711:20000
Enders-Mountainburg complex, 8 to 20 percent slopesEmC311765663772xhywar13119711:20000
Enders stony silt loam, 12 to 30 percent slopesEeE9000566376m0c6ar13119711:20000
Enders silt loam, 8 to 12 percent slopesEdD130456637530x8sar13119711:20000
Enders silt loam, 3 to 8 percent slopesEdC126256637430x8far13119711:20000
Nella-Enders complex, 8 to 20 percent slopes24157445664162y1kwar13719811:20000
Nella-Enders complex, 20 to 40 percent slopes25109505664172y1ktar13719811:20000
Enders very stony sandy loam, 20 to 40 percent slopes1198385664022s1y7ar13719811:20000
Enders very stony loam, 8 to 20 percent slopes1063505664012s1y6ar13719811:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes9394456644830x8dar13719811:20000
Enders-Steprock complex, 8 to 20 percent slopes94639730862102s1xzar14119831:20000
Enders-Nella-Steprock complex, 8 to 20 percent slopes74062130862082s1y2ar14119831:20000
Enders-Steprock complex, 20 to 40 percent slopes103480230861782s1y0ar14119831:20000
Enders-Nella-Steprock complex, 20 to 40 percent slopes82963530862092s1y3ar14119831:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes413910308620530x8dar14119831:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes59464308620630x8har14119831:20000
Enders stony fine sandy loam, 8 to 15 percent slopes63587308620730x8mar14119831:20000
Enders-Leesburg complex, 20 to 40 percent slopesErF952685665802rxhdar14319661:20000
Enders-Leesburg complex, 8 to 20 percent slopesErE694645665792rxhcar14319661:20000
Enders stony loam, 3 to 15 percent slopesEoD99345665782s1yrar14319661:20000
Enders gravelly loam, 3 to 8 percent slopes, erodedEnC23455566575m0kmar14319661:20000
Enders gravelly loam, 8 to 12 percent slopes, erodedEnD22349566577m0kpar14319661:20000
Enders gravelly loam, 3 to 8 percent slopesEnC11715665742rxhbar14319661:20000
Enders gravelly loam, 8 to 15 percent slopesEnD8555665762s1ynar14319661:20000
Steprock-Enders complex, 12 to 30 percent slopes32365785666602sp1var14519801:20000
Enders-Steprock complex, 12 to 30 percent slopes1121686566637m0mmar14519801:20000
Enders stony fine sandy loam, 3 to 12 percent slopes105251566636m0mlar14519801:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes9367756667030x8har14519801:20000
Enders fine sandy loam, 3 to 8 percent slopes83315566669m0nnar14519801:20000
Nella-Enders complex, 8 to 20 percent slopes39218855649982y1ksar14919851:20000
Nella-Enders complex, 20 to 40 percent slopes40177875650002y1kvar14919851:20000
Enders-Mountainburg complex, 8 to 20 percent slopes21105435649792xhywar14919851:20000
Enders-Mountainburg complex, 20 to 40 percent slopes22100255649802xhyvar14919851:20000
Nella-Enders-Mountainburg stony fine sandy loams, 40 to 65 percent slopes413856565001lyxvar14919851:20000
Enders gravelly fine sandy loam, 8 to 12 percent slopes19294256497630x8har14919851:20000
Enders stony fine sandy loam, 12 to 20 percent slopes20235856497830x8lar14919851:20000
Enders gravelly fine sandy loam, 3 to 8 percent slopes18227756497530x8dar14919851:20000
Nella-Enders complex 8 to 15 percent slopesND3801625778441qfxxar14919851:20000
Enders stony fine sandy loam, 8 to 15 percent slopes10543056429230x8mar68019801:20000
Linker-Enders-Mountainburg complex, 12 to 25 percent slopes204232564303ly6bar68019801:20000
Enders-Sunlight complex, 15 to 30 percent slopesEsE3365202381925xyhga12920071:12000
Enders loam, 6 to 15 percent slopesEnD1005202383225xyxga12920071:12000
Enders loam, 15 to 30 percent slopesEnE235202383325xyyga12920071:12000
Enders silt loam, 6 to 15 percent slopesEnD2155562850lwpgga64820011:12000
Enders silt loam, 2 to 6 percent slopesEnB645562849lwpfga64820011:12000
Enders-Urban land complex, 2 to 15 percent slopesEuC360562942lwsfga64820011:12000
Enders-Linker-Hector association, 5 to 30 percent slopesHc810105717862pwxmok00119631:24000
Enders-Linker-Hector association, 5 to 30 percent slopesHlE895705718162pwxmok02119671:24000
Endsaw-Hector association, 12 to 20 percent slopes1766005571726m5xsok09119801:24000
Hector-Enders complex, 5 to 20 percent slopesHeE177251065572ydtcok09719721:24000
Hector-Enders-Linker complex, 1 to 5 percent slopesHeC61201065562ydtfok09719721:24000
Enders-Linker-Hector association, 5 to 30 percent slopes18408861063783kpkok10119841:24000
Hector-Linker-Enders complex, 5 to 40 percent slopes, extremely stonyHeF2124935718872vz7tok13519661:24000
Hector-Enders complex, 5 to 30 percent slopesHeF253001067622ydtdok14519721:24000
Enders silt loam, 20 to 50 percent slopesEnE2871526659kp10tn00719871:24000
Enders silt loam, 12 to 20 percent slopesEnD810526658kp0ztn00719871:24000
Enders silt loam, 6 to 12 percent slopesEnC450526657kp0ytn00719871:24000
Enders silt loam, 2 to 12 percent slopesEdC559810178471354stn06519801:15840
Enders silty clay loam, 12 to 25 percent slopes, erodedEeD166210178481354ttn06519801:15840
Enders gravelly loam, 2 to 12 percent slopesEgC121010178491354vtn06519801:15840
Enders-Urban land complex, 2 to 12 percent slopesEhC117110178501354wtn06519801:15840
Enders silt loam, 20 to 50 percent slopesEnE459529609ks35tn15319951:24000

Map of Series Extent

Approximate geographic distribution of the ENDERS 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 .