Official Series Description


Lab Data Summary

Aggregate lab data for the ADEL soil series. This aggregation is based on all pedons with a current taxon name of ADEL, 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 ADEL were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ADEL 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 ADEL 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 ADEL 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 ADEL 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 ADEL 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 ADEL 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 ADEL 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 flats position figure.

Soil series sharing subgroup-level classification with ADEL, 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

No block diagrams are available.

Map Units

Map units containing ADEL 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
Adel-Teton family association, 25 to 50 percent slopes83755509401k329co6471:24000
Nimerick family-Secondset-Adel complex, 15 to 45 percent slopes453293509344k30gco6471:24000
Northwater-Adel complex, 5 to 50 percent slopes1712725095332w4zkco66019941:24000
Adel loam, 4 to 25 percent slopes1D4495500883jt6jco66619741:31680
Adel loam, 25 to 65 percent slopes1E354500884jt6kco66619741:31680
Ryman-Adel complex, 1 to 15 percent slopes7314840507250k0txco67220031:24000
Adel-Quazar complex, 5 to 30 percent slopes732878507251k0tyco67220031:24000
Adel-Bucklon complex, 10 to 30 percent slopes733859507252k0tzco67220031:24000
Adel loam, moist, 15 to 50 percent slopes909218507291k0w7co67220031:24000
Adel loam, 5 to 30 percent slopes90864507290k0w6co67220031:24000
Adel loam, moist, 15 to 50 percent slopes101123505149jyn4co67419981:24000
Ryman-Adel, moist complex, 1 to 15 percent slopes15333505210jyq3co67419981:24000
Ryman-Adel, moist complex, 1 to 15 percent slopes9112906502149jvjcco67519861:24000
Adel loam, moist, 15 to 50 percent slopes912481502143jvj5co67519861:24000
Adel loam, 5 to 30 percent slopes81749502124jvhkco67519861:24000
Northwater-Adel complex, 5 to 50 percent slopes52265384967152w4zkco68219861:24000
Cochetopa-Adel-Hapgood loams, 5 to 25 percent slopes1817025496857jp0nco68419841:24000
Hapgood-Adel-Clayburn loams, 5 to 25 percent slopes5314044496896jp1xco68419841:24000
Lespate-Adel-Starley complex, 3 to 25 percent slopes6811937496912jp2fco68419841:24000
Cochetopa-Adel-Hapgood loams, 25 to 45 percent slopes198845496858jp0pco68419841:24000
Parachute-Secondset-Adel, cool loams, 3 to 35 percent slopes878838496933jp33co68419841:24000
Hapgood-Adel-Clayburn loams, 25 to 65 percent slopes547632496897jp1yco68419841:24000
Clayburn-Mayoworth-Adel loams, 5 to 30 percent slopes165680496855jp0lco68419841:24000
Adel-Namela-Splitro complex, 5 to 25 percent slopes35567496870jp12co68419841:24000
Adel-Cochetopa-Mayoworth loams, 25 to 65 percent slopes24908496859jp0qco68419841:24000
Adel-Cochetopa-Mayoworth loams, 5 to 25 percent slopes14851496821jnzhco68419841:24000
Quander-Clayburn-Adel loams, 3 to 25 percent slopes994233496946jp3jco68419841:24000
Adel-Namela-Splitro complex, 25 to 65 percent slopes42715496881jp1fco68419841:24000
Namela-Adel-Hapgood complex, 5 to 25 percent slopes79787496924jp2tco68419841:24000
Yellowmule-Elve-Adel families, complex, landslide deposits704X60202406925y6kid75819981:24000
Teton-Adel loams, 8 to 15 percent slopes2292747342467chcbmt02719791:24000
Adel-Cheadle complex, 15 to 45 percent slopes111832342335ch72mt02719791:24000
Adel loam, 2 to 15 percent slopes1013323423241ndtlmt02719791:24000
Adel loam, 2 to 15 percent slopes410D29717156901vl9vmt02719791:24000
Pishkun-Adel association, steepPH651591469004xvqmt60019691:24000
Fifer-Adel association, hillyAF190411467534xpzmt60019691:24000
Adel-Babb complex, hillyAB183301467524xpymt60019691:24000
Burnette-Adel association, rollingBW45541467714xqkmt60019691:24000
Adel-Hanson complex, hillyAL33371467544xq0mt60019691:24000
Adel loam, 4 to 10 percent slopesAe16721467574xq3mt60019691:24000
Libeg-Adel complex, rollingLH16721468534xt6mt60019691:24000
Adel loam, 0 to 4 percent slopesAd15931467564xq2mt60019691:24000
Teton-Adel stony loamsTh147871474414yf5mt60219631:20000
Raynesford and Adel loams, 4 to 8 percent slopesRd35091474064yd1mt60219631:20000
Raynesford and Adel stony loams, 4 to 15 percent slopesRn14101474084yd3mt60219631:20000
Adel silt loam, terraceAm11441472884y87mt60219631:20000
Raynesford and Adel loams, 2 to 4 percent slopesRa9351474054yd0mt60219631:20000
Raynesford and Adel loams, 8 to 15 percent slopesRf7641474074yd2mt60219631:20000
Adel loam, 8 to 18 percent slopesAl4291472874y86mt60219631:20000
Adel loam, 2 to 8 percent slopesAk4211472864y85mt60219631:20000
Adel-Garlet-Yellowmule families, complex, landslide deposits704T245861487654zswmt60520071:24000
Yellowmule-Elve-Adel families, complex, landslide deposits704X164031487664zsxmt60520071:24000
Adel-Redchief-Woodhurst families, complex, gentle mountain slopes522E141481486024zmmmt60520071:24000
Adel-Wesdy-Woodhurst families, complex, landslide deposits704C90121487574zsmmt60520071:24000
Tibson-Adel-Tiban families, complex, ice-margin slopes464E56361485924zm9mt60520071:24000
Adel-Levengood-Groomer families, complex, gentle mountain slopes524C39621486064zmrmt60520071:24000
Maciver-Tibson-Adel families, complex pediment slopes624E37841487314zrsmt60520071:24000
Philipsburg-Adel families, complex, cirque basins2510C3191625761p04vmt60520071:24000
Adel-Dunkleber, rarely flooded-Wetopa families, complex, alluvial-colluvial deposits613G215714932050csmt60520071:24000
Bridger-Adel-Wetopa families, complex, alluvial-colluvial deposits613E193314932250cvmt60520071:24000
Adel-Libeg-Tiban families, complex, glacial moraines3410E169314931350ckmt60520071:24000
Adel-Libeg-Woodhurst families, complex, alluvial-colluvial deposits611E16891487204zrfmt60520071:24000
Adel-Libeg-Marcetta families, complex, alluvial fans6810E124714931750cpmt60520071:24000
Elkpeak, stony-Booneville-Adel complex, 4 to 25 percent slopes920E43925980152ppb5mt60520071:24000
Hanson-Adel complex, 4 to 45 percent slopes51399185962720f2zmt60520071:24000
Libeg-Adel complex, 2 to 8 percent slopes47C134185952720dzrmt60520071:24000
Adel loam, 4 to 15 percent slopes25818596154xcxmt60520071:24000
Boatman, stony-Adel complex, 8 to 35 percent slopes729E5226334562ppjgmt60520071:24000
Sebud, stony-Adel complex, 12 to 30 percent slopes911E22185972520f64mt60520071:24000
Libeg-Adel complex, 8 to 15 percent slopes47D17185952820dzsmt60520071:24000
Adel loam, 0 to 4 percent slopes15185961420f2kmt60520071:24000
Adel-Mayflower association, slopingAO5816345843clw7mt60719701:24000
Adel loam, cool, 4 to 15 percent slopes614D31476714ynlmt60919711:24000
Libeg-Adel complex, 2 to 8 percent slopes47C3499817734wfxjmt61020051:24000
Libeg-Adel complex, 8 to 15 percent slopes47D2719817736wfxlmt61020051:24000
Libeg-Adel complex, 0 to 2 percent slopes51A781115134717n27mt61020051:24000
Adel silt loam, 8 to 15 percent slopes59D52312925601dd0hmt61020051:24000
Yellowmule-Elve-Adel families, complex, landslide deposits704X14615312271ndcfmt61020051:24000
Adel-Dunkleber-Wetopa families, complex, alluvial-colluvial deposits613G5715312181ndc4mt61020051:24000
Adel silty clay loam, 0 to 4 percent slopesAn6170347029cn3hmt61119711:24000
Redlodge-Adel silty clay loamsRc3901347120cn6fmt61119711:24000
Adel silty clay loam, 4 to 8 percent slopesAo1622347030cn3jmt61119711:24000
Redlodge-Adel silty clay loams, wetRd1214347121cn6gmt61119711:24000
Burnette-Adel complex, 15 to 50 percent slopes, landslides738F274925153842ppjfmt61220111:24000
Arrowpeak, extremely stony-Elkpeak, stony-Adel complex, 4 to 15 percent823D103824853902pf7wmt61220111:24000
Yellowmule-Elve-Adel families, complex, landslide deposits704X35325977324zsxmt61220111:24000
Boatman, stony-Adel complex, 8 to 35 percent slopes729E7125153852ppjgmt61220111:24000
Adel loam, 4 to 15 percent133271341790cgnhmt61319751:24000
Elkpeak, stony-Booneville-Adel complex, 4 to 25 percent slopes920E131725187222ppb5mt61420121:24000
Boatman, stony-Adel complex, 8 to 35 percent slopes729E10725416502ppjgmt61420121:24000
Burnette-Adel complex, 15 to 50 percent slopes, landslides738F625416492ppjfmt61420121:24000
Adel-Mooseflat complex, 8 to 35 percent slopes437E7741547855622mt61620031:24000
Adel loam, 2 to 8 percent slopes37C71154748560wmt61620031:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes879E6288155760572jmt62219971:24000
Tolbert-Blaincreek-Adel complex, 15 to 45 percent slopes439E452115547856sfmt62219971:24000
Reedwest-Adel-Castner complex, 15 to 45 percent slopes447E287815548656spmt62219971:24000
Bangtail-Adel loams, 4 to 25 percent slopes679D241915565456z3mt62219971:24000
Adel loam, cool, 4 to 15 percent slopes614D155615562356y3mt62219971:24000
Adel loam, 8 to 25 percent slopes314E143015539056plmt62219971:24000
Bigbear-Storyhill-Adel complex, 15 to 45 percent slopes665E142815564756ywmt62219971:24000
Adel loam, 2 to 8 percent slopes314C108215538956pkmt62219971:24000
Billman-Adel-Tolbert complex, 25 to 60 percent slopes860F8311557535729mt62219971:24000
Adel loam, 15 to 60 percent slopes614F79915562456y4mt62219971:24000
Adel-Copenhaver complex, 4 to 15 percent slopes814D597155738571tmt62219971:24000
Hoppers-Adel-Tolbert, very stony complex, 15 to 45 percent slopes547E59615558956x0mt62219971:24000
Adel-Uinta loams, 8 to 35 percent slopes714E59215567656ztmt62219971:24000
Libeg, very stony-Copenhaver, extremely stony-Adel complex, 15 to 45 percent slopes580E54315560456xhmt62219971:24000
Zade-Adel complex, 15 to 45 percent slopes283E48215537156nzmt62219971:24000
Storyhill, very stony-Bigbear, stony-Adel complex, 15 to 45 percent slopes365E42715543156qxmt62219971:24000
Adel-Copenhaver complex, 15 to 35 percent slopes814E409155739571vmt62219971:24000
Adel-Libeg complex, 15 to 35 percent slopes414E32715546556s0mt62219971:24000
Bangtail-Adel, cool, loams, 8 to 25 percent slopes579E31915560056xcmt62219971:24000
Tiban-Adel complex, 40 to 70 percent slopes461G29215551256tjmt62219971:24000
Libeg, stony-Monaberg-Adel complex, 15 to 35 percent slopes997E18615164152snmt62719981:24000
Adel-Libeg complex, 4 to 15 percent slopes, stony1103D16715048051l6mt62719981:24000
Adel loam, 2 to 8 percent slopes1104C8015048151l7mt62719981:24000
Adel-Libeg, stony, complex, 1 to 4 percent slopes1102B2415047951l5mt62719981:24000
Booneville-Lingshire-Adel complex, 15 to 60 percent slopes335F410624862532pg4qmt6321:24000
Sawpit, stony-Adel families-Rubble land complex, 30 to 65 percent slopes1260G250228324432v10vmt6321:24000
Medicinelodge-Adel-Mooseflat complex, 4 to 15 percent slopes23D6622512883pdnqmt6321:24000
Mollet-Adel complex, 8 to 35 percent slopes270E60123927992l9x2mt6321:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E3732496365swkymt6321:24000
Adel-Dailybasin, very stony complex, 8 to 25 percent slopes5405E223249636357tfmt6321:24000
Adel loam, 2 to 15 percent slopes410D325120051ndtlmt6321:24000
Sebud, stony-Adel complex, 12 to 30 percent slopes911E21717032201v5blmt63520061:24000
Libeg, stony-Monaberg-Adel complex, 15 to 35 percent slopes997E10317030481v551mt63520061:24000
Libeg-Adel complex, 4 to 25 percent slopes7062141464974xfqmt63619831:24000
Adel loam, 4 to 15 percent slopes236371464414xcxmt63619831:24000
Hanson-Adel complex, 4 to 45 percent slopes5132561464764xf1mt63619831:24000
Bridger-Tiban-Adel complex, 8 to 25 percent slopes2626471464484xd4mt63619831:24000
Adel loam, 0 to 4 percent slopes112621463694x9lmt63619831:24000
Leavitt, moist-Adel complex, 4 to 15 percent slopes699161464954xfnmt63619831:24000
Yellowmule-Elve-Adel families, complex, landslide deposits310817101671vdkpmt63619831:24000
Medicinelodge-Adel-Mooseflat complex, 4 to 15 percent slopes23D3436637785pdnqmt63720141:24000
Booneville-Lingshire-Adel complex, 15 to 60 percent slopes335F297923982562lhl3mt63720141:24000
Bangtail-Copenhaver-Adel complex, 15 to 35 percent slopes879E17222493522572jmt63720141:24000
Bangtail-Adel complex, 4 to 25 percent slopes679D1628185853820cyvmt63720141:24000
Mollet-Adel complex, 8 to 35 percent slopes270E1443814093wb42mt63720141:24000
Bachus-Mayflower-Adel complex, 4 to 25 percent slopes435E116323982502lhkxmt63720141:24000
Adel-Dailybasin, very stony complex, 8 to 25 percent slopes5405E933249352857tfmt63720141:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E5712493530swkymt63720141:24000
Billman-Adel-Tolbert complex, 25 to 60 percent slopes860F50123778082kt9hmt63720141:24000
Adel loam, 2 to 8 percent slopes314C148249351856pkmt63720141:24000
Adel loam, cool, 4 to 15 percent slopes614D144249352556y3mt63720141:24000
Libeg-Libeg, extremely bouldery-Adel complex, 15 to 60 percent slopes414F16441499785120mt63920001:24000
Tibson, extremely bouldery-Bridger, extremely bouldery-Adel complex, 8 to 35 percent slopes420E15691499845126mt63920001:24000
Bridger, very stony-Adel complex, 8 to 35 percent slopes424E1504149990512dmt63920001:24000
Tongue River-Cabba, moist-Adel loams, 15 to 60 percent slopes377F1330149940510smt63920001:24000
Lymanson-Cheadle-Adel complex, 8 to 35 percent slopes348E132814990450zmmt63920001:24000
Rocko-Adel complex, 15 to 45 percent slopes415F10311499795121mt63920001:24000
Millerlake-Arrowpeak-Adel complex, 8 to 35 percent slopes385E8411499475110mt63920001:24000
Libeg, extremely bouldery-Adel complex, 4 to 15 percent slopes414D613149977511zmt63920001:24000
Adel loam, 2 to 15 percent slopes388D4321499505113mt63920001:24000
Bridger, very stony-Adel complex, 2 to 8 percent slopes424C365149989512cmt63920001:24000
Adel-Timberlin complex, 8 to 35 percent slopes410E353149972511tmt63920001:24000
Babb-Tibson-Adel complex, 4 to 35 percent slopes296E6250348549cppjmt65719901:24000
Bynum-Adel-Doby complex, 4 to 35 percent slopes194E4719348423cpkgmt65719901:24000
Adel-Burnette-Bynum complex, 4 to 35 percent slopes294E3943348547cppgmt65719901:24000
Adel-Doby-Hanson complex, 8 to 35 percent slopes197E3507348428cpkmmt65719901:24000
Cheadle-Adel-Doby complex, 15 to 60 percent slopes904F3168348823cpzcmt65719901:24000
Adel-Gallatin-Shedhorn complex, 0 to 8 percent slopes198C1803348429cpknmt65719901:24000
Adel-Burnette-Sebud complex, 4 to 35 percent slopes394E855348618cprrmt65719901:24000
Adel loam, 2 to 15 percent slopes410D1915316661ndtlmt66620081:24000
Cabba-Absarokee-Adel complex, 15 to 60 percent slopes5612F777615647757tnmt6691:24000
Billman-Adel-Tolbert complex, 25 to 60 percent slopes860F54141017233134hzmt6691:24000
Maciver, very stony-Adel-Tiban, very bouldery complex, 2 to 35 percent slopes3528E3487655069pzn8mt6691:24000
Tophat-Adel-Bangtail complex, 4 to 25 percent slopes5547E2645741487swkymt6691:24000
Adel-Dailybasin, very stony complex, 8 to 25 percent slopes5405E200415647057tfmt6691:24000
Libeg, stony-Adel-Coppenhaver, stony complex, 15 to 60 percnet slopes, stony8601F1957156764583xmt6691:24000
Tiban stony - Adel- Arrowpeak complex, 15 to 60 percent slopes6605F164615655257x2mt6691:24000
Foolhen, very bouldery-Adel-Maurice, bouldery complex, 4 to 35 percent slopes3535E1391697299rdljmt6691:24000
Libeg,stony - Coppenhaver,stony -Adel Complex , 4 to 15 percent slopes8406E1193699356rgqwmt6691:24000
Adel-Mooseflat, mucky peat, complex, 4 to 15 percent slopes3410E1082696028rc8jmt6691:24000
Spanpeak, very stony - Woodhall, stony - Adel complex, 15 to 60 percent slopes8602F1075156766583zmt6691:24000
Booneville very stony -Adel -Copenhaver stony complex ,moist, 15 to 60 percent slopes3616F1058697430rdqrmt6691:24000
Boonville, extremely bouldery-Adel-Spanpeak, bouldery complex, 8 to 45 percent slopes3502F85415663757ztmt6691:24000
Marcetta - Maciver,stony -Adel complex, 4 to 35 percent3531E843697303rdlnmt6691:24000
Libeg stony - Adel - Surdal complex,moist, 15 to 35 percent slopes8503F715156765583ymt6691:24000
Lymanson-Cheadle-Adel, complex, 8 to 35 percent slopes348E172620218ntd1mt6691:24000
Tongue River-Cabba, moist-Adel loams, 15 to 60 percent slopes377F166620225ntd8mt6691:24000
Adel loam, 8 to 25 percent slopes314E11924827032pbg6mt6691:24000
Millerlake-Arrowpeak-Adel complex, 8 to 35 percent slopes385E111620229ntddmt6691:24000
Beeftrail, occasionally flooded-Adel-Monaberg complex, 4 to 15 percent slopes139D1350320493brhhmt67020071:24000
Work, stony-Adel-Kilgore, rarely flooded complex, 2 to 15 percent slopes25D872320259br7ymt67020071:24000
Ratiopeak, very stony-Bridger-Adel complex, 8 to 30 percent slopes170E82714246751jth8mt67020071:24000
Danielvil, very bouldery-Monaberg, bouldery-Adel complex, 8 to 35 percent slopes126E793320368brcgmt67020071:24000
Sebud, stony-Adel complex, 12 to 30 percent slopes911E77914248561jtp3mt67020071:24000
Monaberg-Adel complex, 4 to 20 percent slopes140D560320309br9kmt67020071:24000
Bridger-Adel complex, 4 to 15 percent slopes943D15214248301jtn8mt67020071:24000
Adel-Maciver, moist-Faim complex, 25 to 70 percent slopesANF245433729586472wrg6ut0131:24000
Adel silt loam, 40 to 80 percent slopesADG1220482189j5rhut62719711:24000
Lucky Star-Horsethief-Adel families complex, 30 to 60 percent slopes820331487130hm1ut6451:24000
Lucky Star-Adel families complex, 30 to 60 percent slopes713331290130gxhut6451:24000
Skylick-Adel-Clayburn families complex, 15 to 60 percent slopesmt4815918331484030hl3ut6451:24000
Dateman, extremely stony-Adel families complex, 15 to 60 percent slopesmt546768331484130hl4ut6451:24000
Adel family, 15 to 65 percent slopes67621512411k66dut6461:24000
Behanin-Adel-Bickmore families association, 15 to 60 percent slopes107581631mj79ut6491:24000
Northwater-Adel-Doct, very stony families, complex, 3 to 25 percent slopes545108800723vw6sut6511:24000
Adel-Pagosa association, rolling1023441502180jvkcwy62519851:24000
Hobacker-Adel-Bearmouth families, complex2222231830565212xts8wy66519961:62500
Thayne-Adel complex, 30 to 60 percent slopes *59321715331054jhwy66619781:24000
Buffork-Adel association *4123715328954htwy66619781:24000
Adel variant loam *157915325654grwy66619781:24000
Midfork, stony-Indart-Adel families, complex, 8 to 35 percent slopes30195629804422wqqswy6671:24000
Foolhen, stony-Finn, occasionally flooded-Adel families, complex, 0 to 6 percent slopes13128829804352wqqkwy6671:24000
Midfork, stony-Hobacker-Adel families, complex, 15 to 60 percent slopes4152729804452wqqwwy6671:24000
Adel-Blazon-Rentsac association, steep -- draft61027742572293jx2twy7371:24000

Map of Series Extent

Approximate geographic distribution of the ADEL 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 .