Official Series Description


Lab Data Summary

Aggregate lab data for the CABBA soil series. This aggregation is based on all pedons with a current taxon name of CABBA, 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 CABBA 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
5475ND0250081975ND025008Cabba5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.1561111,-102.4036111
5478P015277ND001007Cabba7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9855537,-102.2322235
5414N0308S2013SD105002Cabba7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.5764117,-102.4701417

Water Balance

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

Competing Series

Soil series competing with CABBA 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 CABBA 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 CABBA 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 terrace figure.

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

Soil series sharing subgroup-level classification with CABBA, 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. ND-2010-09-27-03 | Billings County - 2005

    Typical pattern of soils and underlying material in the Janesburg-Dogtooth association (Soil Survey of Billings County, North Dakota; 2005).

  2. ND-2010-09-27-07 | McKenzie County - 2006

    Typical pattern of soils and underlying material in the Williams-Temvik-Wilton-Zahl association (Soil Survey of McKenzie County, North Dakota; 2006).

  3. ND-2010-09-27-14 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Straw-Parshall-Manning-Stady association (Soil Survey of Morton County, North Dakota; 2002).

  4. ND-2010-09-27-15 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Amor-Rhoades-Cabba association (Soil Survey of Morton County, North Dakota; 2002).

  5. ND-2010-09-27-17 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Farland-Savage-Amor-Belfield association (Soil Survey of Morton County, North Dakota; 2002).

  6. ND-2010-09-27-19 | Morton County - 2002

    Typical pattern of soils and underlying materials in the Regent-Daglum-Morton association (Soil Survey of Morton County, North Dakota; 2002).

  7. ND-2012-02-07-02 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Belfield-Amor-Daglum association (Soil Survey of Adams County, North Dakota; September 1987).

  8. ND-2012-02-07-03 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Belfield-Daglum-Rhoades association (Soil Survey of Adams County, North Dakota; September 1987).

  9. ND-2012-02-07-04 | Adams County - September 1987

    Typical pattern of soils and underlying material in the Amor-Regent-Belfield association (Soil Survey of Adams County, North Dakota; September 1987).

  10. ND-2012-02-07-30 | Dunn County - April 1982

    Typical pattern of soils and underlying material in the Cabba-Cohagen-Rhoades association (Soil Survey of Dunn County, North Dakota; April 1982).

  11. ND-2012-02-07-31 | Dunn County - April 1982

    Typical pattern of soils and underlying material in the Morton-Rhoades-Savage association (Soil Survey of Dunn County, North Dakota; April 1982).

  12. ND-2012-02-07-33 | Dunn County - April 1982

    Typical pattern of soils and underlying material in the Williams-Amor-Arnegard association (Soil Survey of Dunn County, North Dakota; April 1982).

  13. ND-2012-02-07-35 | Dunn County - April 1982

    Typical pattern of soils and underlying material in the Straw-Velva association (Soil Survey of Dunn County, North Dakota; April 1982).

  14. ND-2012-02-07-40 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Chama-Golva-Cabba association (Soil Survey of Golden Valley County, North Dakota; July 1989).

  15. ND-2012-02-07-41 | Golden Valley County - July 1989

    Typical pattern of soils and parent material in the Absher-Belfield association (Soil Survey of Golden Valley County, North Dakota; July 1989).

  16. ND-2012-02-08-04 | Grant County - September 1988

    Typical pattern of soils and parent material in the Amor-Regent-Cabba association (Soil Survey of Grant County, North Dakota; September 1988).

  17. ND-2012-02-08-05 | Grant County - September 1988

    Typical pattern of soils and parent material in the Ekalaka-Desart-Lemert association (Soil Survey of Grant County, North Dakota; September 1988).

  18. ND-2012-02-08-08 | Grant County - September 1988

    Typical pattern of soils and parent material in the Ruso-Straw-Bowdle association (Soil Survey of Grant County, North Dakota; September 1988).

  19. ND-2012-02-08-10 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Moreau-Lawther-Amor association (Soil Survey of Hettinger County, North Dakota; May 1990).

  20. ND-2012-02-08-11 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Belfield-Amor-Regent association (Soil Survey of Hettinger County, North Dakota; May 1990).

  21. ND-2012-02-08-12 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Daglum-Belfield-Amor association (Soil Survey of Hettinger County, North Dakota; May 1990).

  22. ND-2012-02-08-13 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Harriet-Dagum-Belfield association (Soil Survey of Hettinger County, North Dakota; May 1990).

  23. ND-2012-02-08-14 | Hettinger County - May 1990

    Typical pattern of soils and underlying material in the Korchea-Bowdle-Parshall association (Soil Survey of Hettinger County, North Dakota; May 1990).

  24. ND-2012-02-08-25 | McIntosh County - 2001

    Typical pattern of soils and underlying material in the Williams-Arnegard-Amor association (Soil Survey of McIntosh County, North Dakota; 2001).

  25. ND-2012-02-08-30 | Mountrail County - June 1991

    Typical pattern of soils and parent material in the Cabba-Badland association (Soil Survey of Mountrail County, North Dakota; June 1991).

  26. SD-2012-03-15-07 | Corson County - July 1995

    Pattern of soils and parent material in the Reeder-Cabba association (Soil Survey of Corson County, SD; 1995).

  27. SD-2012-03-15-09 | Corson County - July 1995

    Pattern of soils and parent material in the Flasher-Vebar association (Soil Survey of Corson County, SD; 1995).

  28. SD-2012-03-16-05 | Ziebach County - March 1990

    Pattern of soils and parent material in the Trembles-Korchea-Banks and Lantry-Cabba-Rhoades associations (Soil Survey of Ziebach County, SD; 1990).

  29. SD-2012-03-16-06 | Ziebach County - March 1990

    Pattern of soils and parent material in the Reeder-Lantry association (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing CABBA 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
Pagoda-Coulterg-Cabba complex, 10 to 60 percent slopes7214705502113jvh6co67519861:24000
Dast-Cabba-Mowbray complex, 15 to 35 percent slopes325E10105343084cj07mt01119921:24000
Mowbray-Cabba-Vebar complex, 35 to 60 percent slopes152F9981342909chtlmt01119921:24000
Cabba-Rock outcrop complex, 15 to 45 percent slopes212E6323343026chycmt01119921:24000
Reeder-Cabba loams, 4 to 15 percent slopes142D1685342889chsymt01119921:24000
Cabba-Dast complex, 8 to 15 percent slopes312D1477343082cj05mt01119921:24000
Cabba silt loam, 8 to 15 percent slopes112D945342837chr8mt01119921:24000
Cambert-Cabba-Widen complex, 15 to 25 percent slopes733E42669343659cjlsmt01719951:24000
Lamedeer-Cabba-Ringling complex, 25 to 70 percent slopes702F30901343651cjljmt01719951:24000
Cambert-Cherry-Cabba silt loams, 12 to 25 percent slopes734E25134343660cjltmt01719951:24000
Doney-Broadus-Cabba complex, 15 to 25 percent slopes361E17644343409cjbqmt01719951:24000
Cherry-Cambert-Cabba silt loams, 8 to 15 percent slopes562D15729343541cjgzmt01719951:24000
Doney-Lamedeer-Cabba complex, 25 to 70 percent slopes862F14805343724cjnwmt01719951:24000
Doney-Macar-Cabba loams, 15 to 25 percent slopes832E14173343701cjn4mt01719951:24000
Bitton-Cabba-Ringling complex, 25 to 70 percent slopes631F11889343597cjjsmt01719951:24000
Macar-Doney-Cabba loams, 8 to 15 percent slopes982D10886343824cjs3mt01719951:24000
Doney-Lamedeer-Cabba complex, 8 to 25 percent slopes862E5942343723cjnvmt01719951:24000
Cambert-Cabba-Ringling complex, 8 to 45 percent slopes731E5694343656cjlpmt01719951:24000
Doney-Cabba-Wayden complex, 25 to 70 percent slopes831F3055343700cjn3mt01719951:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes212D415814871861lxjrmt02119711:24000
Reeder-Cabba loams, 4 to 15 percent slopes142D8704342089cgz4mt02519911:24000
Cabba-Cambert complex, 4 to 15 percent slopes112D3685342067cgyfmt02519911:24000
Cambert-Cabba complex, 2 to 8 percent slopes112C1716342066cgydmt02519911:24000
Cabba-Dast complex, 8 to 15 percent slopes312D846342198ch2nmt02519911:24000
Cabba-Wayden complex, 8 to 45 percent slopes412E677342224ch3hmt02519911:24000
Reeder-Cabba loams, 15 to 45 percent slopes142E584342090cgz5mt02519911:24000
Cabba-Dast complex, 15 to 25 percent slopes512E368342239ch3zmt02519911:24000
Cabba-Doney-Wayden complex, 4 to 8 percent slopes3713639342536chfkmt02719791:24000
Amor-Cabba loams, 4 to 8 percent slopes2010929342435chb9mt02719791:24000
Cabba-Wayden-Rock outcrop complex, 45 to 60 percent slopes388151342537chflmt02719791:24000
Doney-Cabba-Macar complex, 4 to 15 percent slopes639D69269465321nnkmt02719791:24000
Cabba-Wayden-Doney complex, 15 to 35 percent slopes684E68269466021m3mmt02719791:24000
Doney-Cabba complex, 2 to 8 percent slopes681C68269465721m35mt02719791:24000
Cabba-Whitecow-Doney complex, 15 to 35 percent slopes679E6526946561vk30mt02719791:24000
Cabba-Doney loams, 4 to 15 percent slopes682D14269465821m36mt02719791:24000
Cabba-Wayden-Doney complex, 4 to 15 percent slopes684D3269465921m2rmt02719791:24000
Cabba-Zahill complex, 25 to 60 percent slopes204F2723343871cjtmmt04119941:24000
Cabba-Rock outcrop complex, 25 to 60 percent slopes203F630343870cjtlmt04119941:24000
Cabba-Macar loams, 15 to 60 percent slopes205F450343872cjtnmt04119941:24000
Cabba-Wayden-Rock outcrop complex, 15 to 60 percent slopes201F5727344150ck3mmt05119921:24000
Zahill-Cabba complex, 15 to 45 percent slopes723F3976344257ck72mt05119921:24000
Cabba-Wayden complex, 4 to 15 percent slopes201D2737344148ck3kmt05119921:24000
Cambert-Dast-Cabba complex, 4 to 15 percent slopes4053718344403ckcsmt05519811:24000
Cambert-Cabba loams, 8 to 15 percent slopes3945999344401ckcqmt05519811:24000
Zahill-Cabba loams, 8 to 15 percent slopes17220800344374ckbvmt05519811:24000
Cabba-Badland complex, 15 to 45 percent slopes2617923344387ckc8mt05519811:24000
Cabba-Wabek-Dast complex, 15 to 45 percent slopes3015870344392ckcfmt05519811:24000
Zahill-Cabba loams, 15 to 45 percent slopes17313624344375ckbwmt05519811:24000
Cabba-Dast complex, 15 to 45 percent slopes2912750344390ckccmt05519811:24000
Cabba loam, 15 to 25 percent slopes2512701344386ckc7mt05519811:24000
Cambert-Barkof-Cabba complex, 4 to 15 percent slopes388979344400ckcpmt05519811:24000
Cabba-Barkof complex, 15 to 45 percent slopes273116344388ckc9mt05519811:24000
Cabba-Brandenburg complex, 8 to 45 percent slopes282643344389ckcbmt05519811:24000
Macar-Cabba loams, 8 to 15 percent slopes1111511344307ck8pmt05519811:24000
Shambo-Cabba loams, 8 to 15 percent slopes126820344323ck96mt05519811:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes1845114570317g65mt05519811:24000
Cabba-Barvon loams, 15 to 65 percent slopes289F74973344555ckjpmt06519961:24000
Cabba-Doney loams, 8 to 45 percent slopes282F380271910243223rrmt06519961:24000
Cabba-Rock outcrop complex, 8 to 45 percent slopes283F28383344544ckjbmt06519961:24000
Cabba-Barvon loams, 4 to 15 percent slopes284D17913344545ckjcmt06519961:24000
Doney-Cabba-Macar loams, 4 to 15 percent slopes281D17193344540ckj6mt06519961:24000
Cabba-Doney loams, 4 to 15 percent slopes285D14472344547ckjfmt06519961:24000
Barvon-Cabba loams, 2 to 8 percent slopes283D11046344543ckj9mt06519961:24000
Barvon-Cabba-Korchea loams, 3 to 25 percent slopes289D9627344554ckjnmt06519961:24000
Barvon-Cabba-Shambo loams, 4 to 15 percent slopes255D6939344529ckhvmt06519961:24000
Doney-Cabba loams, 2 to 8 percent slopes285C339191358521nvymt06519961:24000
Cambert, calcareous-Cabba-Cherry, calcareous complex, 8 to 25 percent slopes224078344837cktsmt07919861:24000
Cabba-Cambert, calcareous-Rock outcrop complex, 8 to 70 percent slopes192132344833cktnmt07919861:24000
Cherry, calcareous-Cambert, calcareous-Cabba silt loams, 4 to 15 percent slopes311984344869ckvtmt07919861:24000
Cambert, calcareous-Cabba-Dast complex, 4 to 15 percent slopes23542344839cktvmt07919861:24000
Cherry, calcareous-Lisk-Cabba complex, 8 to 25 percent slopes3241344872ckvxmt07919861:24000
Cherry-Cambert-Cabba silt loams, 4 to 15 percent slopes212D2212622160432dcz8mt08319731:24000
Cabba-Chama-Sen silt loams, 9 to 15 percent slopes53D25742493012ct44mt08319731:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C103332567191vztxmt08319731:24000
Cabba-Rock outcrop complex, 25 to 70 percent slopes201F2498345089cl2xmt10119921:24000
Cabba-Dast fine sandy loams, 25 to 45 percent slopes202F2349345090cl2ymt10119921:24000
Reeder-Cabba complex, 4 to 8 percent slopes411C2169345163cl59mt10119921:24000
Reeder-Cabba complex, 0 to 4 percent slopes411B1299345162cl58mt10119921:24000
Cabba-Doney clay loams, 8 to 25 percent slopes203E1177345091cl2zmt10119921:24000
Zahill-Dast-Cabba complex, 25 to 65 percent slopes722F815345258cl8cmt10119921:24000
Cabba loam, 4 to 8 percent slopes20C756345093cl31mt10119921:24000
Doney-Cabba complex, 4 to 15 percent slopes181D384345082cl2pmt10119921:24000
Cabba loam, 8 to 15 percent slopes20D213345094cl32mt10119921:24000
Chama-Cabba-Sen silt loams, 6 to 9 percent slopesE2737C83643456161vztxmt10919561:31680
Dogtooth-Janesburg-Cabba complex, 6 to 35 percent slopesE0701F44629921771vzrymt10919561:31680
Cabba-Rock outcrop complex, 8 to 45 percent slopes283F170861897372ckjbmt11119661:20000
Cabba-Ridge complex, 8 to 25 percent slopes282E11816190377521x13mt11119661:20000
Cabba-Doney loams, 4 to 15 percent slopes285D22041897360ckjfmt11119661:20000
Cabba-Barvon loams, 15 to 65 percent slopes289F21521913574ckjpmt11119661:20000
Doney-Cabba loams, 2 to 8 percent slopes285C1712189688821nvymt11119661:20000
Cabba-Doney loams, 8 to 45 percent slopes282F13311913571223rrmt11119661:20000
Doney-Cabba-Macar loams, 4 to 15 percent slopes281D9041913570ckj6mt11119661:20000
Cabba loam, hillyCb242421467904xr5mt60019691:24000
Boxwell complex, undulatingBo175651467794xqtmt60019691:24000
Cabba-Rock outcrop complex, very steepCK136941467864xr1mt60019691:24000
Cabba loam, undulatingCa124111467894xr4mt60019691:24000
Cabba-Reeder complex, undulatingCe66591467914xr6mt60019691:24000
Castner-Cabba complex, slopingCn46121467924xr7mt60019691:24000
Castner-Cabba complex, steepCo32691467934xr8mt60019691:24000
Fairfield-Cabba complex, slopingFh21911468154xrzmt60019691:24000
Cabba-Whitecow-Doney complex, 15 to 35 percent slopes679E6426946751vk30mt60219631:20000
Doney-Cabba complex, 2 to 8 percent slopes681C5269467721m35mt60219631:20000
Cabba-Zahill association, steep2411876346390cmfwmt60819761:24000
Cabba-Windham association, steep237537346383cmfnmt60819761:24000
Cabba loam, 8 to 35 percent slopes215014346376cmffmt60819761:24000
Cabba-Rock outcrop complex, 25 to 45 percent slopes221867346379cmfjmt60819761:24000
Macar-Cabba clay loams, 8 to 15 percent slopesMb44422347097cn5pmt61119711:24000
Wayden-Cabba association, steepWC16449347182cn8fmt61119711:24000
Wayden-Cabba association, hillyWA7304347181cn8dmt61119711:24000
Macar-Cabba clay loams, 4 to 8 percent slopesMa4916347096cn5nmt61119711:24000
Absarokee-Cabba clay loams, 8 to 15 percent slopesAg3363347025cn3cmt61119711:24000
Shane-Cabba clay loams, 8 to 15 percent slopesSh2995347141cn73mt61119711:24000
Absarokee-Cabba clay loams, 4 to 8 percent slopesAf2488347024cn3bmt61119711:24000
Shane-Cabba clay loams, 4 to 8 percent slopesSg2329347140cn72mt61119711:24000
Cabba-Rentsac complex, rollingCA1582347041cn3wmt61119711:24000
Shambo-Amor-Cabba loams, 15 to 45 percent slopes745F12609346905cmzhmt61519921:24000
Cabba-Macar loams, 15 to 60 percent slopes965F11013347001cn2lmt61519921:24000
Zahill-Cabba complex, 15 to 45 percent slopes723F5009346900cmzbmt61519921:24000
Cabba-Wayden-Rock outcrop complex, 25 to 70 percent slopes201F2594346624cmpfmt61519921:24000
Cabba-Reedwest-Anceney complex, 15 to 45 percent slopes747E3894155707570tmt62219971:24000
Cabba-Bacbuster complex, 15 to 60 percent slopes315F310915539256pnmt62219971:24000
Alder-Cabba complex, 8 to 25 percent slopes60D222215562256y2mt62219971:24000
Reedwest-Cabba complex, 35 to 60 percent slopes689F192215565956z8mt62219971:24000
Alder, stony-Cabba complex, 15 to 45 percent slopes360E127115542356qnmt62219971:24000
Martinsdale-Cabba complex, 8 to 15 percent slopes852D10941557485724mt62219971:24000
Reedwest-Cabba-Bowery complex, 15 to 45 percent slopes947E1056155770572vmt62219971:24000
Cabba-Castner complex, 15 to 60 percent slopes615F100915562556y5mt62219971:24000
Bacbuster-Cabba complex, 4 to 15 percent slopes315D71315539156pmmt62219971:24000
Cabba-Reedwest complex, 4 to 15 percent slopes415D66715546656s1mt62219971:24000
Reedwest-Cabba-Castner complex, 25 to 60 percent slopes347F60415540856q5mt62219971:24000
Cabba-Rock outcrop complex, cool, 15 to 60 percent slopes627F8674190149421tnjmt62420211:24000
Doney-Cabba complex, 8 to 15 percent slopes681D7174189518921m34mt62420211:24000
Cabba-Castner complex, 15 to 60 percent slopes628F5944190212021v9qmt62420211:24000
Doney-Cabba complex, 2 to 8 percent slopes681C5660189519021m35mt62420211:24000
Doney-Cabba-Macar complex, 4 to 15 percent slopes639D5442189669021nnkmt62420211:24000
Cabba-Rock outcrop complex, 15 to 60 percent slopes629F3934190212121v9rmt62420211:24000
Cabba-Whitecow-Rock outcrop complex, 25 to 60 percent slopes679F340617144761vk1pmt62420211:24000
Cabba-Whitecow-Doney complex, 15 to 35 percent slopes679E334217145171vk30mt62420211:24000
Amor-Cabba complex, 2 to 8 percent slopes680C2849190218821vcxmt62420211:24000
Cabba-Castner-Amherst complex, 4 to 15 percent slopes670D2288190236821vkqmt62420211:24000
Cabba-Whitecow-Doney complex, 4 to 15 percent slopes679D218017145041vk2lmt62420211:24000
Doney-Cabba complex, 15 to 35 percent slopes681E2018190150321tntmt62420211:24000
Cabba-Wayden-Doney complex, 4 to 15 percent slopes684D1894189517721m2rmt62420211:24000
Cabba-Rock outcrop complex, 4 to 35 percent slopes629E1703189881021qvymt62420211:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C156425232354z2wmt62420211:24000
Cabba-Castner complex, 2 to 15 percent slopes628D890189880921qvxmt62420211:24000
Cabba-Haverlon complex, 0 to 25 percent slopes613E778190263021vv5mt62420211:24000
Cabba loam, 2 to 15 percent slopes610D739194911023f6jmt62420211:24000
Cabba loam, 15 to 35 percent slopes610E420194911123f6kmt62420211:24000
Cabba-Wayden-Doney complex, 15 to 35 percent slopes684E331189520421m3mmt62420211:24000
Shambo-Cabba loams, 8 to 35 percent slopes25E21224851112pdywmt62420211:24000
Cabba-Vershal complex, 15 to 45 percent slopes357E17925232242l0vrmt62420211:24000
Cabba-Doney loams, 4 to 15 percent slopes682D90189519121m36mt62420211:24000
Doney-Cabba, moist loams, 35 to 60 percent slopes355F58251368550zwmt62420211:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E5631768364z2xmt62420211:24000
Reeder-Regent-Cabba loams, 2 to 8 percent slopes380C369261477984yspmt63019911:24000
Reeder-Regent-Cabba loams, 8 to 25 percent slopes380D354941477994ysqmt63019911:24000
Winspect-Cabba-Wayden complex, 8 to 35 percent slopes443E97281478204ytdmt63019911:24000
Wayden-Cabba-Regent complex, 15 to 45 percent slopes679E82351478844ywgmt63019911:24000
Regent-Wayden-Cabba complex, 15 to 45 percent slopes479E52301478254ytkmt63019911:24000
Wayden-Cabba-Rock outcrop complex, 15 to 60 percent slopes579E34161478604yvpmt63019911:24000
Bacbuster, very bouldery-Cabba, extremely stony-Castner complex, 15 to 45 percent slopes40E79823927572l9vqmt6321:24000
Bacbuster, very stony-Whitecow, very bouldery-Cabba, very bouldery families, complex, 8 to 45 percent slopes, landslides1025F61526044762r6y7mt6321:24000
Reedwest-Cabba-Watne complex, 4 to 15 percent slopes80D54924863082pg6hmt6321:24000
Alder, stony-Cabba complex, 15 to 45 percent slopes161441465384xh1mt63619831:24000
Reedwest-Cabba complex, 35 to 60 percent slopes19781465624xhtmt63619831:24000
Reedwest-Bacbuster-Cabba complex, 8 to 35 percent slopes658E123881480644z28mt63720141:24000
Bacbuster, very bouldery-Cabba, extremely stony-Castner complex, 15 to 45 percent slopes40E6736639050pfzjmt63720141:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes445C517824963772pqkbmt63720141:24000
Shambo-Cabba complex, 8 to 35 percent slopes125E367824963802pqkdmt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes445E282825173572q9zvmt63720141:24000
Reedwest-Roundor-Cabba complex, 2 to 8 percent slopes, foothills945C25291480834z2wmt63720141:24000
Cabba-Bacbuster-Fairfield complex, 8 to 35 percent slopes858E2402639902pgw0mt63720141:24000
Shambo-Cabba complex, 8 to 35 percent slopes, foothills25E13961480104z0jmt63720141:24000
Cabba-Vershal complex, 15 to 45 percent slopes357E122523841092l0vrmt63720141:24000
Reedwest-Cabba-Watne complex, 4 to 15 percent slopes80D113513833821hfj7mt63720141:24000
Cabba-Amor complex, 15 to 45 percent slopes858F819817727wfx9mt63720141:24000
Wilsall-Reedwest-Cabba complex, 15 to 45 percent slopes106F649603549n81bmt63720141:24000
Roundor-Cabba complex, 2 to 8 percent slopes845C5841480784z2qmt63720141:24000
Reedwest-Roundor-Cabba complex, 8 to 35 percent slopes, foothills945E3211480844z2xmt63720141:24000
Doney-Cabba complex, 2 to 8 percent slopes681C177251733221m35mt63720141:24000
Cabba loam, 2 to 15 percent slopes210D135185852820cyjmt63720141:24000
Doney-Cabba complex, 15 to 35 percent slopes681E27251733421tntmt63720141:24000
Doney-Cabba complex, 8 to 15 percent slopes681D20251733321m34mt63720141:24000
Cabba-Castner-Amherst complex, 2 to 15 percent slopes335D1424514989250z7mt63920001:24000
Cabba, moist-Rock outcrop complex, 15 to 60 percent slopes227F1101114978350vqmt63920001:24000
Wayden-Castner-Cabba complex, 2 to 15 percent slopes262D1015714982550x2mt63920001:24000
Cabba-Castner complex, 15 to 60 percent slopes208F824914975550ttmt63920001:24000
Doney-Cabba, moist loams, 35 to 60 percent slopes355F586414991250zwmt63920001:24000
Cabba-Rock outcrop complex, 15 to 60 percent slopes179F567514971350sgmt63920001:24000
Doney-Cabba loams, 2 to 8 percent slopes231C514414979050vymt63920001:24000
Cabba-Castner-Rock outcrop complex , moist, 25 to 60 percent slopes403F3269149964511kmt63920001:24000
Cabba loam, 2 to 15 percent slopes210D310114975850txmt63920001:24000
Cabba-Doney loams, 8 to 35 percent slopes307E294814987450ynmt63920001:24000
Doney-Cabba loams, 8 to 15 percent slopes231D274714979150vzmt63920001:24000
Amor-Cabba loams, 2 to 8 percent slopes225C273014978150vnmt63920001:24000
Cabba loam, 15 to 35 percent slopes210E178714975950tymt63920001:24000
Cabba-Vershal complex, 4 to 15 percent slopes357D166914991450zymt63920001:24000
Reedwest-Cabba loams, 2 to 8 percent slopes176C160214970950sbmt63920001:24000
Reedwest-Cabba-Castner complex, 15 to 60 percent slopes399F1538149960511fmt63920001:24000
Sagedale-Cabba complex, 2 to 8 percent slopes238C149414979750w5mt63920001:24000
Absarokee-Cabba loams, 2 to 8 percent slopes229C143814978550vsmt63920001:24000
Amor-Cabba loams, 8 to 15 percent slopes225D1080150019513bmt63920001:24000
Cabba very cobbly loam, 15 to 60 percent slopes398F626149959511dmt63920001:24000
Absarokee-Cabba loams, 8 to 15 percent slopes229D53814978650vtmt63920001:24000
Cabba-Vershal complex, 15 to 45 percent slopes357E47914991550zzmt63920001:24000
Cabba-Bowery complex, 2 to 60 percent slopes413E416149976511ymt63920001:24000
Cabba-Castner-Work complex, 4 to 35 percent slopes, bouldery437E284150002512smt63920001:24000
Cabba-Winifred clay loams, 2 to 8 percent slopes181C26714971550sjmt63920001:24000
Sagedale-Cabba complex, 8 to 35 percent slopes238F25114979850w6mt63920001:24000
Cabba-Winifred clay loams, 8 to 15 percent slopes181D4014971650skmt63920001:24000
Cabba-Windham complex, 8 to 25 percent slopes201D1837347629cnqvmt64119941:24000
Cabba association, 15 to 50 percent slopesCa238629347838cnylmt64319671:20000
Ringling-Cabba association, 15 to 50 percent slopesRt208321347907cp0tmt64319671:20000
Farland-Cabba association, 8 to 20 percent slopesFk18207347850cnyzmt64319671:20000
Farland-Cabba association, 4 to 8 percent slopesFh5888347849cnyymt64319671:20000
Relan-Cabba association, 4 to 8 percent slopesRh588347901cp0mmt64319671:20000
Shambo-Doney-Cabba loams, 8 to 35 percent slopes16624048347993cp3lmt64919851:24000
Barvon, dry-Doney-Cabba complex, 15 to 70 percent slopes1418499347964cp2nmt64919851:24000
Bitton, moist-Ringling, dry-Cabba complex, 25 to 70 percent slopes3213329348062cp5tmt64919851:24000
Doney-Bitton-Cabba complex, 15 to 35 percent slopes789787348112cp7fmt64919851:24000
Sagedale-Cabba-Wayden complex, 8 to 25 percent slopes1588791347984cp39mt64919851:24000
Bitton, moist-Doney-Cabba complex, 15 to 70 percent slopes295544348058cp5pmt64919851:24000
Cabba-Wayden-Sagedale complex, 25 to 70 percent slopes534215348085cp6kmt64919851:24000
Cabba-Wayden-Rock outcrop complex, 25 to 70 percent slopes523089348084cp6jmt64919851:24000
Shambo-Bitton-Cabba complex, 8 to 15 percent slopes1641682347991cp3jmt64919851:24000
Wayden-Castner-Cabba complex, 2 to 15 percent slopes262D1060361448d43mmt65519751:24000
Shane-Cabba clay loams, 4 to 10 percent slopes51715348184cp9rmt65519751:24000
Amor-Cabba loams, 2 to 15 percent slopes174D16597348394cpjjmt65719901:24000
Cabba-Amor loams, 15 to 35 percent slopes174E5620348395cpjkmt65719901:24000
Cabba-Wayden-Castner complex, 4 to 35 percent slopes574E4530348725cpw6mt65719901:24000
Cabba-Roundor-Windham complex, 25 to 60 percent slopes474F4357348673cptjmt65719901:24000
Beanlake-Cabba-Castner complex, 8 to 35 percent slopes527E3802348705cpvkmt65719901:24000
Cabba-Castner-Rock outcrop complex, 25 to 60 percent slopes271F3375348517cpnhmt65719901:24000
Winifred-Wayden-Cabba complex, 2 to 15 percent slopes285C2664348535cpp2mt65719901:24000
Wayden-Cabba-Winifred complex, 15 to 45 percent slopes187F1931348411cpk2mt65719901:24000
Zahill-Cabba-Cambert complex, 15 to 45 percent slopes7454440348282cpdxmt66119821:24000
Cabba-Cambert-Cherry silt loams, 8 to 15 percent slopes1051703348212cpbnmt66119821:24000
Cabba-Cambert silt loams, 15 to 45 percent slopes931882348289cpf4mt66119821:24000
Cabba-Cambert-Rock outcrop complex, 15 to 45 percent slopes1129719348213cpbpmt66119821:24000
Wabek-Cabba-Tinsley complex, 15 to 45 percent slopes6627081348273cpdmmt66119821:24000
Zahill-Cabba-Cambert complex, 8 to 15 percent slopes7319251348281cpdwmt66119821:24000
Bitton-Barvon-Cabba complex, 15 to 45 percent slopes424E26815316681ndtnmt66620081:24000
Cabba-Bacbuster-Gnojek complex, 2 to 15 percent slopes551D28954156939589kmt6691:24000
Cabba-Bacbuster-Doney complex, 2 to 15 percent slopes151D18373156846586kmt6691:24000
Cabba-Vershal-Rock outcrop complex, 15 to 60 percent slopes351F14268156909588lmt6691:24000
Bacbuster-Cabba complex, 15 to 45 percent slopes446F12618156919588xmt6691:24000
Cabba-Doney-Rock outcrop complex, 15 to 60 percent slopes5602F9663156724582mmt6691:24000
Cabba-Absarokee-Adel complex, 15 to 60 percent slopes5612F777615647757tnmt6691:24000
Cabba-Rock outcrop complex, 15 to 45 percent slopes451F77661569235891mt6691:24000

Map of Series Extent

Approximate geographic distribution of the CABBA 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 .