Official Series Description


Lab Data Summary

Aggregate lab data for the WOODWARD soil series. This aggregation is based on all pedons with a current taxon name of WOODWARD, 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 WOODWARD 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
78B80P0281MLRA78-Obaro-TX263-002Woodward8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.1791649,-100.7069473
78B80P0280MLRA78-Woodward-TX263-001Woodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0991669,-100.5455551
78C75-OK-75-175-OK149-75-1Woodward4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.2572667,-98.8338
78C87P043287OK059002CWoodward6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8255539,-99.6036148
78C87P043387OK059002DWoodward8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8255539,-99.6036148
78C87P043487OK059002EWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8255539,-99.6036148
78C88P073488OK151001Woodward8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P073588OK151001AWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P073688OK151001BWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P073788OK151001CWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P073888OK151001DWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P073988OK151001EWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P074088OK151001FWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C88P074188OK151001GWoodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.875,-99.1397247
78C87P0435S1987OK153001Woodward7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6701317,-99.2128372
80A88P046188OK003002Woodward4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.663887,-98.25
80A88P046288OK003003Woodward4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.663887,-98.2508316

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WOODWARD 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 WOODWARD 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 WOODWARD 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 WOODWARD series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Click the image to view it full size.

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

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

Competing Series

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

Click the image to view it full size.

Click the image to view it full size.

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

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 WOODWARD, 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-2012-01-20-24 | Clark County - December 1982

    Typical pattern of soils in the Carey-Woodward-Quinlan association (Soil Survey of Clark County, Kansas; 1982).

  2. KS-2012-01-20-37 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Quinlan-Woodward-Carey association (Soil Survey of Comanche County, Kansas; 1989).

  3. KS-2012-01-20-38 | Comanche County - June 1989

    Typical pattern of soils and parent material in the Obaro-Abilen association (Soil Survey of Comanche County, Kansas; 1989).

  4. OK-2010-09-29-20 | Woods County - 2003

    Typical pattern of soils and underlying material in the Quinlan-Woodward-Deepwood general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

  5. OK-2012-02-16-03 | Beaver County - August 1962

    Parent material and parent rock of most of the soils in Beaver County, and their position on the landscape (Soil Survey of Beaver County, Oklahoma; August 1962).

  6. OK-2012-02-16-24 | Dewey County - December 1963

    Typical pattern of the soils in associations 1 and 2 (Soil Survey of Dewey County, Oklahoma; December 1963).

  7. OK-2012-02-16-27 | Dewey County - December 1963

    Typical pattern of most of the soils in association 5 (Soil Survey of Dewey County, Oklahoma; December 1963).

  8. OK-2012-02-16-28 | Ellis County - April 1966

    Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

  9. OK-2012-02-16-36 | Greer County - March 1967

    Major soils in soil association 2, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

  10. OK-2012-02-16-39 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Woodward-Quinlan map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  11. OK-2012-02-16-40 | Harmon County - September 1984

    Typical pattern of soils and underlying material in the Madge-Abilene-Shrewder map unit (Soil Survey of Harmon County, Oklahoma; September 1984).

  12. OK-2012-02-16-45 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed over Permian redbeds. The typical slope range is given for each soil. Alternating layers of sandstone and shale underlie these soils (Soil Survey of Harper County, Oklahoma; June 1960).

  13. OK-2012-02-17-41 | Roger Mills County - August 1963

    Typical pattern of soils in associations 6, 7, and 9 (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  14. OK-2012-02-17-42 | Roger Mills County - August 1963

    Typical pattern of soils in association 8. Woodward silt loam is a variation, which is described in the section "Descriptions of Soils" (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  15. OK-2012-02-17-58 | Woodward County - November 1963

    Typical pattern of soils of the St. Paul-Carey-Woodward association (Soil Survey of Woodward County, Oklahoma; November 1963).

  16. TX-2012-03-20-17 | Childress County - July 1963

    Soils developed in sandstone material (Soil Survey of Childress County, TX; 1963).

  17. TX-2012-03-21-88 | Stonewall County - January 1975

    Quinlan-Woodward soil association (Soil Survey of Stonewall County, TX; 1975).

Map Units

Map units containing WOODWARD 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
Quinlan-Woodward loams, 6 to 15 percent slopes54576388813825192t6qpks00719731:24000
Woodward-Quinlan complex, 3 to 5 percent slopes54963238513825352w5qnks00719731:24000
Woodward-Quinlan loams, 1 to 3 percent slopes5495544913825342w5qpks00719731:24000
Quinlan-Woodward loams, 15 to 30 percent slopes545852813825182t6qmks00719731:24000
Woodward-Port complex, 0 to 20 percent slopes54923213825332w5qlks00719731:24000
Quinlan-Woodward loams, 6 to 15 percent slopes54574226013817392t6qpks02519801:24000
Woodward-Quinlan complex, 3 to 5 percent slopes54961986913817572w5qnks02519801:24000
Woodward loam, 1 to 3 percent slopes54901013013817562vytxks02519801:24000
Badland-Woodward complex, 1 to 50 percent slopes5405132813816981hcrxks02519801:24000
Quinlan-Woodward loams, 6 to 15 percent slopes54574912413812862t6qpks03319871:24000
Quinlan-Woodward loams, 15 to 30 percent slopes54581742113812852t6qmks03319871:24000
Woodward-Quinlan complex, 3 to 5 percent slopes54961483213813002w5qnks03319871:24000
Woodward loam, 1 to 3 percent slopes5490460313812992vytxks03319871:24000
Woodward-Port complex, 0 to 20 percent slopes54922560613827512w5qlks07719651:24000
Woodward-Quinlan loams, 1 to 3 percent slopes54951548613827531hdvyks07719651:24000
Woodward-Quinlan loams, 0 to 1 percent slopes5494544313827521hdvxks07719651:24000
Woodward-Quinlan loams, 3 to 6 percent slopes549659313827541hdvzks07719651:24000
Quinlan-Woodward loams, 6 to 15 percent slopes5457405813805401hbkkks09719831:24000
Woodward-Port complex, 0 to 20 percent slopes5492314446112w5qlks19119741:24000
Quinlan-Woodward complex, 5 to 30 percent slopesQwE13869381440dsxjok00319711:24000
Woodward-Quinlan complex, 1 to 3 percent slopesWuB10199381449dsxtok00319711:24000
Quinlan-Woodward complex, 3 to 5 percent slopesQwC9380381439dsxhok00319711:24000
Woodward-Deepwood complex, 1 to 3 percent slopesWoDB566225452w5q3ok00319711:24000
Woodward-Quinlan-Burson complex, 3 to 5 percent slopes, erodedWQBC2456225462w5qqok00319711:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE42731012762t6qrok00720211:24000
Quinlan-Woodward complex, 5 to 12 percent slopes48147903816862t6qhok00919781:24000
Woodward-Quinlan complex, 3 to 5 percent slopes64106113817042w5qnok00919781:24000
Woodward loam, 1 to 3 percent slopes6190883817012vytxok00919781:24000
Woodward loam, 3 to 5 percent slopes6239823817022w5pvok00919781:24000
Woodward-Quinlan complex, 1 to 3 percent slopes6328623817032w5qmok00919781:24000
Woodward variant fine sandy loam, 1 to 3 percent slopes651946381705dt62ok00919781:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded4711663816852t6qfok00919781:24000
Quinlan-Woodward complex, 5 to 20 percent slopesQwF178923817622t6qjok01119651:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWuC99663819292w5qnok01519671:24000
Quinlan-Woodward complex, 5 to 12 percent slopesWwE1350253823512t6qhok03919731:24000
Carey and Woodward soils, 3 to 5 percent slopesCaC45869382310dttlok03919731:24000
Woodward silt loam, 5 to 8 percent slopesWoD359353823482w5q1ok03919731:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWwC324433823502w5qnok03919731:24000
Quinlan and Woodward soils, 3 to 8 percent slopes, severely erodedQwE3169563823392t6qkok03919731:24000
Woodward-Clairemont complex, 0 to 12 percent slopesWt75653823492w5q2ok03919731:24000
Woodward silt loam, 3 to 5 percent slopesWoC55513823472w5pzok03919731:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, erodedQwC244073823382t6qfok03919731:24000
Carey and Woodward soils, 3 to 5 percent slopes, severely erodedCbC31135382311dttmok03919731:24000
Woodward silt loam, 1 to 3 percent slopesWoB11093823462w5q0ok03919731:24000
Quinlan-Woodward complex, 5 to 20 percent slopesQwE1087593823952t6qjok04319611:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, erodedQwC2161003823942t6qfok04319611:24000
Woodward loam, 3 to 5 percent slopesWbC97303824082w5pvok04319611:24000
Woodward-Carey complex, 3 to 5 percent slopes, erodedWcC28661382410dtxtok04319611:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWwC47513824132w5qnok04319611:24000
Woodward-Carey complex, 5 to 8 percent slopes, erodedWcD22908382411dtxvok04319611:24000
Woodward-Carey complex, 1 to 3 percent slopesWcB2026382409dtxsok04319611:24000
Quinlan-Woodward complex, 8 to 20 percent slopesQwE19124382463dtzjok04519631:24000
Woodward-Quinlan complex, 5 to 12 percent slopesWwE17243382480dv02ok04519631:24000
Woodward loam, 3 to 5 percent slopesWoC63943824782w5pvok04519631:24000
Woodward-Quinlan complex, 3 to 8 percent slopes, erodedWwD24198382479dv01ok04519631:24000
Woodward loam, 1 to 3 percent slopesWoB21783824772vytxok04519631:24000
Woodward-Quinlan complex, 5 to 12 percent slopesWoQE20676366442w5qrok05520051:24000
Woodward loam, 3 to 5 percent slopes, warmWooC12566366432w5pwok05520051:24000
Woodward loam, 1 to 3 percent slopes, warmWooB9256366422w5ptok05520051:24000
Woodward-Quinlan complex, 5 to 12 percent slopes71191859755082w5qrok05719821:24000
Woodward-Quinlan complex, 3 to 5 percent slopes7083629755072w5qsok05719821:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded4945659754832t6qfok05719821:24000
Woodward loam, 1 to 3 percent slopes, warm6728619755032w5ptok05719821:24000
Woodward-Quinlan complex, 1 to 3 percent slopes69208097550511r2xok05719821:24000
Woodward loam, 3 to 5 percent slopes, warm685099755042w5pwok05719821:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE479233831072t6qrok05919981:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWQnC353593830482w5qnok05919981:24000
Woodward-Quinlan complex, 1 to 3 percent slopesWQnB167513830472w5qmok05919981:24000
Quinlan-Woodward complex, 5 to 8 percent slopesQnWD8552383049dvlfok05919981:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, severely erodedQnWC33514383111dvnfok05919981:24000
Quinlan-Rock outcrop-Woodward complex, 5 to 45 percent slopesQRWG2789383110dvndok05919981:24000
Quinlan-Woodward-Rock outcrop complex, 1 to 5 percent slopesQWRC1150383105dvn7ok05919981:24000
Quinlan-Woodward complex, 5 to 12 percent slopesQnWE6563831122t6qhok05919981:24000
Quinlan-Woodward complex, 5 to 20 percent slopesQnWE96979432t6qjok09319651:24000
Quinlan-Woodward complex, 5 to 12 percent slopesQwE1761933847692t6qhok12919611:24000
Woodward loam, 3 to 5 percent slopesWoC130993847862w5pvok12919611:24000
Quinlan and Woodward soils, 3 to 8 percent slopes, severely erodedQu3112333847672t6qkok12919611:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWwC97363847912w5qnok12919611:24000
Woodward loam, 1 to 3 percent slopesWoB68283847852vytxok12919611:24000
Woodward loam, 5 to 8 percent slopesWoD51753847872w5pxok12919611:24000
Woodward-Quinlan complex, 1 to 3 percent slopesWsB41993847882w5qmok12919611:24000
Woodward-Quinlan loams, 1 to 3 percent slopesWwB39003847902w5qpok12919611:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, erodedQwC230863847682t6qfok12919611:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWsC2782384789dxdkok12919611:24000
Woodward fine sandy loam, 1 to 3 percent slopesWdB1227384783dxdcok12919611:24000
Woodward fine sandy loam, 3 to 5 percent slopesWdC1018384784dxddok12919611:24000
Woodward loam, 1 to 3 percent slopesWwB3350384932dxk5ok13919591:24000
Woodward-Quinlan complex, 3 to 5 percent slopes55264633850422w5qnok14919761:24000
Quinlan-Woodward complex, 5 to 12 percent slopes40167313850262t6qhok14919761:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, eroded39106173850242t6qfok14919761:24000
Woodward-Clairemont complex, 0 to 12 percent slopes5399873850402w5q2ok14919761:24000
Woodward silt loam, 3 to 5 percent slopes5167893850382w5pzok14919761:24000
Woodward silt loam, 1 to 3 percent slopes5033953850372w5q0ok14919761:24000
Woodward silt loam, 5 to 8 percent slopes5231863850392w5q1ok14919761:24000
Woodward-Quinlan complex, 1 to 3 percent slopes5426603850412w5qmok14919761:24000
Quinlan-Woodward-Burson complex, 12 to 45 percent slopesQWBG32555385225dxvmok15119951:24000
Quinlan-Woodward-Deepwood complex, 5 to 12 percent slopesQWDE267433852262t6qrok15119951:24000
Woodward-Quinlan-Burson complex, 3 to 5 percent slopes, erodedWQBC293933852492w5qqok15119951:24000
Woodward-Deepwood complex, 3 to 5 percent slopesWoDC8042385256dxwmok15119951:24000
Quinlan-Woodward-Burson complex, 5 to 12 percent slopes, erodedQWBE27290385224dxvlok15119951:24000
Woodward-Deepwood complex, 1 to 3 percent slopesWoDB47763852552w5q3ok15119951:24000
Quinlan-Woodward complex, 5 to 12 percent slopesQwD41907385297dxxyok15319611:24000
Woodward loam, 3 to 5 percent slopesWoC110173853142w5pvok15319611:24000
Quinlan-Woodward complex, 3 to 5 percent slopes, erodedQwC2100793852962t6qfok15319611:24000
Quinlan-Woodward complex, 5 to 12 percent slopes, erodedQwD28982385298dxxzok15319611:24000
Woodward loam, 1 to 3 percent slopesWoB88363853132vytxok15319611:24000
Woodward loam, 5 to 8 percent slopesWoD76793853152w5pxok15319611:24000
Woodward-Quinlan complex, 3 to 5 percent slopesWwC22173853162w5qnok15319611:24000
Woodward loam, 3 to 5 percent slopes, warmWoC60963625072w5pwtx01119631:20000
Woodward loam, 5 to 8 percent slopes, warmWoD40433625082w5pytx01119631:20000
Woodward loam, 1 to 3 percent slopes, warmWoB13493625062w5pttx01119631:20000
Quinlan-Woodward loams, 8 to 20 percent slopesQuE213783638362t6qntx07519611:20000
Woodward loam, 3 to 5 percent slopes, warmWoC197893638582w5pwtx07519611:20000
Woodward-Quinlan complex, 5 to 12 percent slopesWwD99903638592w5qrtx07519611:20000
Woodward loam, 1 to 3 percent slopes, warmWoB25973638572w5pttx07519611:20000
Quinlan-Woodward loamsQw74607364120d6wttx08719651:20000
Woodward-Yahola-Breaks complexWy32727364138d6xdtx08719651:20000
Veal-Woodward complexMd12317364112d6wktx08719651:20000
Woodward loam, 1 to 3 percent slopes, warmWoB104203641352w5pttx08719651:20000
Woodward loam, 3 to 5 percent slopes, warmWoC98503641362w5pwtx08719651:20000
Woodward-Quinlan complex, 3 to 5 percent slopesWuC92003641372w5qstx08719651:20000
Rough broken land-Woodward complexRw2484364121d6wvtx08719651:20000
Woodward and Quinlan loams, 3 to 12 percent slopesWu339303646362w5q4tx10119691:20000
Woodward soils and rough broken landWr28524364635d7fftx10119691:20000
Woodward loam, 3 to 5 percent slopes, warmWoC234643646342w5pwtx10119691:20000
Woodward loam, 1 to 3 percent slopes, warmWoB111593646332w5pttx10119691:20000
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopesWQE411853651612wt7jtx12519651:20000
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopesDQG191093651122y7bdtx12519651:20000
Deepwood-Woodward-Rock outcrop complex, warm, 12 to 50 percent slopesDRG1893631007422y7bftx12519651:20000
Woodward-Deepwood complex, warm, 3 to 5 percent slopesWoC86783651602wt7ftx12519651:20000
Woodward, warm-Obaro complex, 1 to 3 percent slopesWoB46173651592wt7dtx12519651:20000
Woodward-Quinlan complex, 3 to 5 percent slopesWwC277903658292w5qstx15119641:24000
Woodward loam, 3 to 5 percent slopes, warmWoC240703658272w5pwtx15119641:24000
Quinlan-Woodward complexQw21168365803d8n3tx15119641:24000
Woodward-Quinlan complex, 5 to 12 percent slopesWwD147793658302w5qrtx15119641:24000
Woodward loam, 1 to 3 percent slopes, warmWoB50293658262w5pttx15119641:24000
Woodward-Quinlan loams, 1 to 3 percent slopesWwB4993365828d8nxtx15119641:24000
Woodward-Quinlan complex, 5 to 50 percent slopesWcF1308391959f4vvtx17919651:20000
Woodward-Quinlan complex, 5 to 12 percent slopesWwD1212253669742w5qrtx19119651:20000
Quinlan-Woodward complexQw85576366956d9v9tx19119651:20000
Woodward loam, 3 to 5 percent slopes, warmWoC283383669732w5pwtx19119651:20000
Woodward loam, 1 to 3 percent slopes, warmWoB61623669722w5pttx19119651:20000
Woodward and Quinlan loams, 3 to 12 percent slopesWoC368813685142w5q4tx26319681:31680
Woodward-Deepwood complex, warm, 3 to 5 percent slopesWoC381263686152wt7ftx26919991:31680
Woodward-Deepwood-Quinlan complex, warm, 2 to 12 percent slopesWQE350333686172wt7jtx26919991:31680
Deepwood-Woodward-Quinlan complex, warm, 2 to 45 percent slopesDQG287703686072y7bdtx26919991:31680
Woodward-Deepwood complex, warm, 5 to 8 percent slopesWoD112583686162wt7gtx26919991:31680
Woodward, warm-Obaro complex, 1 to 3 percent slopesWoB26163686012wt7dtx26919991:31680
Woodward and Quinlan loams, 3 to 12 percent slopesWQD689493709002w5q4tx34519721:24000
Woodward-Yomont complex, 0 to 15 percent slopesWoD32679370903dfymtx34519721:24000
Woodward loam, 3 to 5 percent slopes, warmWlC92743709022w5pwtx34519721:24000
Woodward loam, 1 to 3 percent slopes, warmWlB25573709012w5pttx34519721:24000
Woodward loam, 1 to 3 percent slopes, warm57103843710282w5pttx35319791:24000
Woodward loam, 3 to 5 percent slopes, warm58101213710292w5pwtx35319791:24000
Quinlan-Burson-Woodward association, rolling324686371001dg1stx35319791:24000
Quinlan-Woodward complex, 5 to 30 percent slopesQwE2345371410dggztx38119991:24000
Woodward loam, 1 to 3 percent slopes, warmWwB19883720462w5pttx41519661:24000
Woodward-Quinlan complex, 5 to 12 percent slopesWoD391273723142w5qrtx43319701:24000

Map of Series Extent

Approximate geographic distribution of the WOODWARD 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 .