Official Series Description


Lab Data Summary

Aggregate lab data for the CANEYVILLE soil series. This aggregation is based on all pedons with a current taxon name of CANEYVILLE, 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 CANEYVILLE 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
114AMO76011976IN105001Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3324,-86.6055528
114B03N0465S2002in079-004Caneyville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0738907,-85.7316666
115BM92099231992MO099107Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672644,-92.3451678
115BM92221151992MO221015Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM93099141993MO099187Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4178298,-90.628445
115BM94099241994MO099230Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3503309,-90.5742765
115BM95051241995MO051059Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.530637,-92.1812658
115BM95051591995MO051098Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4885966,-92.3975599
115BM01221072001MO221007Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM01221112001MO221011Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM01221192001MO221019Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM01221222001MO221022Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012
115BM06027522006MO027052CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7314444,-91.7840556
115BM06027532006MO027053CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7317222,-91.7841389
115BM06027542006MO027054CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7329444,-91.7842778
115BM06027722006MO027072CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7299444,-91.7781389
115BM07139752007MO13975CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9087222,-91.5816667
115BM07139762007MO13976CANEYVILLE4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9072222,-91.5783056
116AM94099131993MO099189Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2761653,-90.624278
116AM93099161993MO099190Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2753319,-90.6248336
116AM93099171993MO099191Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2794985,-90.6215001
116AM94099121993MO099216Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2803319,-90.6209446
116AM94099341994MO099242Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2831096,-90.6212224
116AM98613511998MO203051MCaneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.1182222,-91.180775
116AM98221361998MO221164Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1776368,-91.1169984
116AM98221451998MO221174Caneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1940111,-90.9445
116CM91123211991MO123021MCaneyville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5218048,-90.3702469
116CM93123221993MO123022MCaneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5067482,-90.3768921
116CM95123111995MO123011MCaneyville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3283348,-90.4997253
120A73KY-047-00177KY047003Caneyville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0220167,-87.32435
121JF77041977IN077004Caneyville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7019361,-85.4659583
122OR79021979IN117002Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5849833,-86.5088361
122LW78192015IN093002Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9469222,-86.5355694
122MO76052015IN105007Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0705917,-86.5882722
122OR79032015IN117002Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5844083,-86.5371389
122WS80062015IN175003Caneyville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.53325,-86.043895
12298P0119S1997IN043003CANEYVILLE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3886108,-86.0211105
12206N0327S2005IN061006Caneyville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1833344,-86.0999985
12494KY-135-05594KY-135-055Caneyville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6471417,-83.42445
127WVU0016S01WV025004Caneyville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8396111,-80.503
127WVU0029S01WV063007Caneyville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6928056,-80.4759722
n/a73KY-047-00373KY-047-003Caneyville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-05994KY-135-059Caneyville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-06094KY-135-060Caneyville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-135-06494KY-135-064Caneyville1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CANEYVILLE 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 CANEYVILLE 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 CANEYVILLE 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 CANEYVILLE 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 CANEYVILLE 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 CANEYVILLE 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 CANEYVILLE 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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Soil series sharing subgroup-level classification with CANEYVILLE, 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. =HYPERLINK(CONCATENATE(M51,E51)) | Mammoth Cave National Park - 2010

    Typical pattern of soils and underlying material in the Wallen-Caneyville-Bledsoe general soil map unit (Soil Survey of Mammoth Cave National Park, Kentucky; 2010).

  2. KY-2010-09-03-13 | Knott and Letcher Counties - 2004

    Typical pattern of soils and their relationship to geology and topography in the Kimper-Cloverlick-Renox-Highsplint general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).

  3. KY-2010-09-03-25 | Cumberland County - 1998

    Relationship of the soils in Garmon-Newbern-Carpenter general soil map unit and the underlying material (Soil Survey of Cumberland County, Kentucky; 1998).

  4. KY-2010-09-03-26 | Cumberland County - 1998

    Typical pattern of the soils and the underlying material in the Dewey-Lonewood-Caneyville general soil map unit (Soil Survey of Cumberland County, Kentucky; 1998).

  5. KY-2010-09-03-32 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Carpenter-Bledsoe-Berks general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  6. KY-2010-09-03-33 | Estill and Lee Counties - 2007

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Bledsoe-Gilpin general soil map unit in Estill County (Soil Survey of Estill and Lee Counties, Kentucky; 2007).

  7. KY-2010-09-10-05 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Caneyville-Lenberg-Zanesville association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  8. KY-2010-09-10-10 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Johnsburg-Clarkrange association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  9. KY-2010-09-10-11 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Wallen-Caneyville association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  10. KY-2010-09-10-12 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Baxter-Pembroke-Fredonia association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  11. KY-2012-01-26-01 | Adair County - April 1964

    Diagram of the Westmoreland-Caneyville-Baxter association in Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  12. KY-2012-01-26-02 | Adair County - April 1964

    Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  13. KY-2012-01-26-06 | Adair County - April 1964

    Geological cross section of Adair County showing the relationship of the soils to the underlying rocks (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  14. KY-2012-01-26-07 | Allen County - September 1989

    Relationship of soils to topography and underlying material in the Christian-Mountview-Bedford general soil map unit (Soil Survey of Allen County, Kentucky; September 1989).

  15. KY-2012-01-26-36 | Boyle and Mercer Counties - April 1983

    Typical pattern of soils and underlying material in the Garmon-Carpenter-Vertrees map unit (Soil Survey of Boyle and Mercer Counties, Kentucky; April 1983).

  16. KY-2012-01-26-40 | Breckinridge and Meade Counties - 2001

    Typical relationship of soils to topography and the underlying material in the Rosine-Gilpin-Zanesville general soil map unit (Soil Survey of Breckinridge and Meade Counties, Kentucky; 2001).

  17. KY-2012-01-26-41 | Breckinridge and Meade Counties - 2001

    Typical relationship of soils to topography and the underlying material in the Crider-Fredonia general soil map unit (Soil Survey of Breckinridge and Meade Counties, Kentucky; 2001).

  18. KY-2012-01-26-42 | Breckinridge and Meade Counties - 2001

    Typical relationship of soils to topography and the underlying material in the Baxter-Hammack-Crider general soil map unit (Soil Survey of Breckinridge and Meade Counties, Kentucky; 2001).

  19. KY-2012-01-27-01 | Bullitt and Spencer Counties - September 1986

    The relationship of soils to topography and underlying material in the Garmon-Crider general soil map unit (Soil Survey of Bullitt and Spencer Counties, Kentucky; September 1986).

  20. KY-2012-01-27-03 | Bullitt and Spencer Counties - September 1986

    The relationship of soils to topography and underlying material in the Caneyville-Crider general soil map unit (Soil Survey of Bullitt and Spencer Counties, Kentucky; September 1986).

  21. KY-2012-01-27-07 | Caldwell County - September 1966

    Typical pattern of soils and underlying materials in association 1 (Soil Survey of Caldwell County, Kentucky; September 1966).

  22. KY-2012-01-27-08 | Caldwell County - September 1966

    Typical pattern of soils and underlying materials in association 2 (Soil Survey of Caldwell County, Kentucky; September 1966).

  23. KY-2012-01-27-23 | Carter County - April 1983

    Pattern of soils, topography, and underlying material in the Caneyville-Bledsoe-Rock outcrop map unit (Soil Survey of Carter County, Kentucky; April 1983).

  24. KY-2012-01-27-30 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Pricetown-Teddy-Frankstown general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  25. KY-2012-01-27-33 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Frederick-Caneyville-Frankstown general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  26. KY-2012-01-27-47 | Clinton County - May 1994

    Pattern of soils and parent material in the Garmon-Caneyville-Dewey general soil map unit (Soil Survey of Clinton County, Kentucky; May 1994).

  27. KY-2012-01-27-48 | Clinton County - May 1994

    Pattern of soils and parent material in the Dewey-Mountview general soil map unit (Soil Survey of Clinton County, Kentucky; May 1994).

  28. KY-2012-01-27-49 | Clinton County - May 1994

    Pattern of soils and parent material in the Rock Outcrop-Caneyville-Sequoia-Shelocta general soil map unit (Soil Survey of Clinton County, Kentucky; May 1994).

  29. KY-2012-01-30-05 | Grayson County - December 1972

    Relationship of soils to topography and underlying material in the Caneyville-Weikert-Zanesville association (Soil Survey of Grayson County, Kentucky; December 1972).

  30. KY-2012-01-30-08 | Green and Taylor Counties - July 1982

    Pattern of soils and underlying material in the Frederick-Frankstown-Mountview general soil map unit (Soil Survey of Green and Taylor Counties, Kentucky; July 1982).

  31. KY-2012-01-30-16 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Caneyville-Fredonia-Hagerstown general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  32. KY-2012-01-30-17 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Baxter-Crider general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  33. KY-2012-01-30-18 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Frederick-Crider general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  34. KY-2012-01-30-20 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Nolichucky-Canmer general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  35. KY-2012-01-30-21 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Jefferson-Lily-Wellston general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  36. KY-2012-01-31-14 | Jackson and Owsley Counties - April 1989

    Typical pattern of soils and parent material in the Shelocta-Bledsoe-Gilpin map unit (Soil Survey of Jackson and Owsley Counties, Kentucky; April 1989).

  37. KY-2012-02-01-09 | Madison County - March 1973

    Relationship of soils to topography and underlying material in the Colyer-Weikert-Captina association (Soil Survey of Madison County, Kentucky; March 1973).

  38. KY-2012-02-01-39 | Pike County - June 1990

    Along Elkhorn Creek and Pine Mountain, the upper faulted mountains are in the Kimper-Sharondale-Berks-Shelocta general soil map unit, the lower mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit, and the valley is in the Yeager-Grigsby-Potomac-Hayter map unit (Soil Survey of Pike County, Kentucky; June 1990).

  39. KY-2012-02-01-56 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Caneyville-Frondorf-Wellston map unit (Soil Survey of Todd County, Kentucky; September 1987).

  40. KY-2012-02-01-57 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Frondorf-Welkert-Zanesville map unit (Soil Survey of Todd County, Kentucky; September 1987).

  41. KY-2012-02-01-58 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Sadler-Zanesville map unit (Soil Survey of Todd County, Kentucky; September 1987).

  42. KY-2012-02-01-59 | Todd County - September 1987

    Relationship of soils to topography and underlying material in the Fredonia-Pembroke-Caneyville map unit (Soil Survey of Todd County, Kentucky; September 1987).

  43. KY-2012-02-01-66 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Waynesboro-Garmon general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  44. KY-2012-02-01-67 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Frederick-Mountview general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  45. KY-2012-02-01-68 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Garmon-Caneyville general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  46. KY-2012-02-01-69 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Decatur-Bewleyville-Clarksville general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  47. KY-2012-02-01-70 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Caneyville-Rock outcrop-Rigley-Shelocta general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  48. KY-2012-05-09-02 | Mammoth Cave National Park - 2010

    Typical pattern of soils and underlying material in the Hagerstown-Fredonia general soil map unit (Soil Survey of Mammoth Cave National Park, Kentucky; 2010).

  49. MO-2010-09-08-09 | Madison County - 2005

    Typical pattern of soils and parent material in the Crider-Fourche-Caneyville association (Soil Survey of Madison County, Missouri; 2005).

Map Units

Map units containing CANEYVILLE 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
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG59702009356r2sin01920011:12000
Haggatt-Caneyville complex, karst, hilly, severely erodedHujD329052011356r97in01920011:12000
Haggatt-Caneyville silt loams, 12 to 25 percent slopes, erodedHtwD227012011236r8vin01920011:12000
Haggatt-Caneyville silt loams, karst, hilly, erodedHuhD222512011246r8win01920011:12000
Haggatt-Caneyville complex, 12 to 25 percent slopes, severely erodedHtzD316672011256r8xin01920011:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, erodedKxpD28942019516s4kin01920011:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, erodedKxmE24712105557233in01920011:12000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely erodedKxlC31392105277226in01920011:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely erodedKxlE324210533722din01920011:12000
Caneyville-Rock outcrop complex, 18 to 70 percent slopesCbzG2916526031sgnsin02519701:20000
Caneyville-Crider complex, 12 to 18 percent slopes, severely erodedCbtD31416526011sgnqin02519701:20000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely erodedKxlC3308818523966rgin04320001:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, erodedKxmE2301018524066rhin04320001:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely erodedKxlE3263818524166rjin04320001:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, erodedKxpD2206818524366rlin04320001:12000
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG25818523366r8in04320001:12000
Vertrees-Haggatt-Caneyville complex, karst, hilly, severely erodedVccD33775516781911tb96in06120071:12000
Vertrees-Crider-Caneyville complex, karst, rolling, severely erodedVcaC331891780677v6c4in06120071:12000
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG25391778581v45jin06120071:12000
Vertrees-Crider-Caneyville silt loams, karst, hilly, erodedVcbD21807416775731t9n8in06120071:12000
Caneyville-Haggatt-Knobcreek complex, karst, hilly, severely erodedCbsD311346798308vspwin06120071:12000
Knobcreek-Haggatt-Caneyville complex, karst, hilly, severely erodedKxsD3730017160581vlpqin06120071:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, hilly, erodedKxpD2609415858421q766in06120071:12000
Caneyville-Haggatt-Knobcreek silt loams, karst, hilly, erodedCbrD25307775595v126in06120071:12000
Knobcreek-Haggatt-Caneyville complex, karst, rolling, severely erodedKxtC35020780681v6c8in06120071:12000
Knobcreek-Haggatt-Caneyville complex, 6 to 12 percent slopes, severely erodedKxlC3229715858381q762in06120071:12000
Knobcreek-Haggatt-Caneyville silt loams, karst, rolling, erodedKxtC2181616985651v0hfin06120071:12000
Knobcreek-Haggatt-Caneyville complex, 12 to 25 percent slopes, severely erodedKxlE3178415858391q763in06120071:12000
Knobcreek-Haggatt-Caneyville silt loams, 12 to 25 percent slopes, erodedKxmE2132815858401q764in06120071:12000
Caneyville-Haggatt silty clay loams, karst, rolling, very severely eroded, very rockyCbxD4121016781931tb98in06120071:12000
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG2281914241227xqin07119851:15840
Eden-Caneyville complex, 25 to 60 percent slopesEgG386596464711csnin07719821:15840
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCaF326996463111cs4in07719821:15840
Haggatt-Caneyville silt loams, 12 to 25 percent slopes, erodedHcD2197566011r7xin07719821:15840
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG467116513701sfd0in07920101:12000
Caneyville and Grayford silt loams, 12 to 25 percent slopes, erodedCcgD2141816127351r45qin07920101:12000
Caneyville and Grayford silt loams, 12 to 25 percent slopes, severely erodedCcgD3594709113rswmin07920101:12000
Caneyville-Zenas silt loams, karst, rolling, erodedCcbC232617167611vmfdin07920101:12000
Caneyville silt loam, 12 to 20 percent slopes, erodedCbpD21350516515321sfk7in09319821:15840
Caneyville-Adyeville-Rock outcrop complex, 25 to 75 percent slopesCbxG1324116520781sg3vin09319821:15840
Crider-Caneyville silt loams, 12 to 18 percent slopes, eroded complexCtzD2931416515201sfjvin09319821:15840
Caneyville silt loam, 6 to 12 percent slopes, erodedCbpC2337216515311sfk6in09319821:15840
Caneyville-Rock outcrop complex, 25 to 60 percent slopesCcaG63324874992phfxin10119841:15840
Haggatt-Caneyville silt loams, 12 to 25 slopes, erodedHtwD223717081401vbg9in10119841:15840
Crider-Caneyville silt loams, 12 to 18 percent slopes, erodedCtwD2714430771kfmwin10119841:15840
Caneyville silt loam, 12 to 18 percent slopesCaD147435355212z8ysin10519791:15840
Caneyville-Hagerstown silt loams, 2 to 18 percent slopes, karstCb37795355222z8yrin10519791:15840
Corydon Variant-Caneyville Variant complex, 25 to 70 percent slopesCoF3597535524kz7zin10519791:15840
Hagerstown-Caneyville silt loams, karstHc1736535542kz8kin10519791:15840
Crider-Caneyville silt loams, 6 to 12 percent slopesCsC1499535528kz83in10519791:15840
Crider-Frederick-Caneyville silt loams, karst, 2 to 12 percent slopes, erodedCtyC21555714429801kfjrin11719801:15840
Crider-Caneyville silt loams, 12 to 18 percent slopes, erodedCtwD2766114429771kfjnin11719801:15840
Caneyville-Crider complex, 12 to 18 percent slopes, severely erodedCbtD3144914429701kfjfin11719801:15840
Caneyville-Rock outcrop complex, 18 to 70 percent slopesCbzG99214429721kfjhin11719801:15840
Caneyville-Crider silt loams, 18 to 25 percent slopesCbuE92814429711kfjgin11719801:15840
Haggatt-Caneyville silt loams, 18 to 25 percent slopes, erodedHasE23171660345kryin11919971:12000
Hagerstown-Caneyville silt loams, 12 to 18 percent slopes, erodedHeD213594535489kz6vin17519841:15840
Caneyville-Rock outcrop complex, 25 to 50 percent slopesCdF5365535465kz62in17519841:15840
Caneyville-Hagerstown silt loams, 18 to 25 percent slopes, erodedCaE23755535464kz61in17519841:15840
Frederick-Caneyville complex, 20 to 40 percent slopes, rockyFvE1587615924261qg1lky00120061:12000
Rock outcrop-Caneyville complex, 6 to 20 percent slopesRpD39115923991qg0qky00120061:12000
Caneyville-Rock outcrop complex, 20 to 50 percent slopes, erodedCaE25080548753lf0qky00319861:20000
Caneyville-Rock outcrop complex, 12 to 20 percent slopes, erodedCaD22650548752lf0pky00319861:20000
Caneyville-Bledsoe-Rock outcrop complex, 12 to 35 percent slopesCaE192117275191vzmfky01120061:12000
Bledsoe-Caneyville-Rock outcrop association, steepBRF10971550235lgkjky04319801:20000
Caneyville-Rock outcrop complex, 12 to 30 percent slopesCbD8529550239lgknky04319801:20000
Caneyville silt loam, 6 to 20 percent slopesCaC2346550238lgkmky04319801:20000
Caneyville silt loam, very rocky, 20 to 30 percent slopesCaE2970548880lf4tky04519891:20000
Caneyville silt loam, very rocky, 6 to 20 percent slopesCaD1680548879lf4sky04519891:20000
Caneyville silt loam, 6 to 12 percent slopesCaC640548878lf4rky04519891:20000
Rock outcrop-Caneyville complex, 6 to 35 percent slopesRoE270548909lf5rky04519891:20000
Caneyville-Rock outcrop complex, 6 to 30 percent slopesCoD17198549043lfb2ky04719771:20000
Caneyville silty clay, 6 to 20 percent slopes, severely erodedCnD38253549042lfb1ky04719771:20000
Caneyville silt loam, 6 to 12 percent slopesCaC6412549041lfb0ky04719771:20000
Caneyville silt loam, 2 to 6 percent slopesCaB1258549040lf9zky04719771:20000
Garmon-Caneyville association, very steepGcF23364551418lhspky05319901:20000
Caneyville-Rock outcrop-Standingstone complex, 12 to 35 percent slopesuCanF1106425838312r1vxky05319901:20000
Caneyville-Dewey complex, rocky, 6 to 20 percent slopesCdD9596551411lhsgky05319901:20000
Caneyville-Garmon association, steepCgD4716551412lhshky05319901:20000
Caneyville silty clay loam, rocky, 12 to 30 percent slopes, severely erodedCcD31523551410lhsfky05319901:20000
Caneyville silt loam, 6 to 12 percent slopesCaC1066551409lhsdky05319901:20000
Rock outcrop-Caneyville complex, 20 to 50 percent slopesRoF194551427lhszky05319901:20000
Caneyville-Crider-Rock outcrop complex, 15 to 40 percent slopesCcE2434549098lfcvky05519851:20000
Caneyville-Lonewood complex, rocky, 6 to 25 percent slopes, erodedCaD27830551434lht6ky05719911:20000
Caneyville very rocky silty clay, 8 to 25 percent slopes, severely erodedCnD35240549652lfyqky08519671:20000
Caneyville silty clay, 6 to 20 percent slopes, severely erodedClD35000549651lfypky08519671:20000
Caneyville very rocky silty clay loam, 10 to 20 percent slopesCeD3325549649lfymky08519671:20000
Caneyville silty clay loam, 6 to 12 percent slopesCcC2885549647lfykky08519671:20000
Caneyville very rocky silty clay loam, 20 to 40 percent slopesCeF2675549650lfynky08519671:20000
Caneyville silty clay loam, 12 to 20 percent slopesCcD1625549648lfylky08519671:20000
Caneyville-Rock outcrop complexCo1125549653lfyrky08519671:20000
Caneyville silty clay loam, 2 to 6 percent slopesCcB575549646lfyjky08519671:20000
Caneyville-Rock outcrop complex, 12 to 60 percent slopes, erodedCcF2244015330621ng8mky11120051:12000
Caneyville silt loam, 12 to 25 percent slopes, eroded, very rockyCaD2196915330611ng8lky11120051:12000
Urban land-Alfic Udarents-Caneyville complex, 12 to 25 percent slopesUlD163215364521nkszky11120051:12000
Caneyville silt loam, 6 to 12 percent slopes, eroded, very rockyCaC2104415330601ng8kky11120051:12000
Caneyville silt loam, 2 to 6 percent slopes, eroded, very rockyCaB248715330591ng8jky11120051:12000
Urban land-Alfic Udarents-Caneyville complex, 0 to 12 percent slopesUlC27815364511nksyky11120051:12000
Caneyville-Hagerstown-Rock outcrop complex, 12 to 45 percent slopes, erodedCaE26689550284lgm3ky13519981:20000
Caneyville-Rock outcrop complex, 12 to 30 percent slopes, erodedCeE21722550285lgm4ky13519981:20000
Talbott-Colbert rocky silt loams, 2 to 20 percent slopes (caneyville rocky)TcD18004548744lf0fky14119721:20000
Talbott-Colbert rocky silt loams, 20 to 50 percent slopes (caneyville rocky)TcF15002548745lf0gky14119721:20000
Rock outcrop-Fredonia-Colbert complex (caneyville rocky)Rx2656548736lf05ky14119721:20000
Caneyville rocky complex, 20 to 30 percent slopesCaE2149549725lg12ky16919651:15840
Baxter-Talbott rocky silt loams, 20 to 30 percent slopes, eroded (baxter, caneyville rocky)BeE21581549721lg0yky16919651:15840
Caneyville rocky complex, 30 to 50 percent slopesCaF1181549727lg14ky16919651:15840
Baxter-Talbott rocky silt loams, 12 to 20 percent slopes, eroded (baxter, caneyville rocky)BeD21081549720lg0xky16919651:15840
Baxter-Talbott rocky silty clay loams, 12 to 20 percent slopes, severely eroded (baxter, caneyville rocky)BfD3570549722lg0zky16919651:15840
Baxter-Talbott rocky silt loams, 6 to 12 percent slopes, eroded (baxter, caneyville rocky)BeC2515549719lg0wky16919651:15840
Caneyville rocky complex, 20 to 30 percent slopes, severely erodedCaE3505549726lg13ky16919651:15840
Christian rocky soils, 12 to 20 percent slopes (caneyville rocky)CeD478549735lg1dky16919651:15840
Talbott silty clay loam, 6 to 12 percent slopes, eroded (caneyville rocky)TcC2464549788lg33ky16919651:15840
Talbott silt loam, 6 to 12 percent slopes (caneyville rocky)TbC344549787lg32ky16919651:15840
Caneyville-Rock outcrop complex, 6 to 30 percent slopesCaD1090549893lg6hky17119771:20000
Bledsoe-Rock outcrop-Caneyville complex, 6 to 60 percent slopesBcF455550509lgvcky17319831:20000
Corydon silt loam, 2 to 6 percent slopes (caneyville)CnB325549940lg80ky17919671:15840
Lenberg-Caneyville silt loams, 12 to 20 percent slopes, severely erodeduLcD358330371932wv56ky18319831:20000
Lenberg-Caneyville silt loams, 6 to 12 percent slopes, severely erodeduLcC37830371922wv55ky18319831:20000
Caneyville silt loam, very rocky, 8 to 20 percent slopes, erodedCcD267551242lhm0ky18319831:20000
Beasley-Caneyville rocky silt loams, 30 to 60 percent slopesBnF5050551573lhypky18519751:20000
Caneyville-Beasley rocky silt loams, 12 to 30 percent slopesCbD5040551577lhytky18519751:20000
Caneyville silt loam, 6 to 12 percent slopesCaC820551576lhysky18519751:20000
Berks-Caneyville complex, 50 to 120 percent slopes, very rockyBcG1627550026lgbsky19519861:24000
Talbott rocky silt loam, 6 to 20 percent slopes (caneyville, rocky)TbD4665552460ljw9ky19919691:12000
Talbott rocky silty clay loam, 6 to 20 percent slopes, severely eroded (caneyville, rocky)TcD32963552462ljwcky19919691:12000
Needmore complex, 12 to 25 percent slopes (caneyville)NdD2362552441ljvpky19919691:12000
Fredonia-Frederick rocky silty clay loams, 6 to 20 percent slopes, severely eroded (caneyville rocky, frederick)FlD31882552410ljtpky19919691:12000
Talbott rocky silt loam, 20 to 30 percent slopes (caneyville, rocky)TbE158552461ljwbky19919691:12000
Talbott silty clay loam, 6 to 12 percent slopes, eroded (caneyville)TaC2143552459ljw8ky19919691:12000
Garmon-Caneyville association, very steepGCF43029552490ljx8ky20719791:20000
Caneyville-Garmon association, steepCGE14150552480ljwyky20719791:20000
Caneyville silt loam, very rocky, 6 to 12 percent slopesCaC540552481ljwzky20719791:20000
Caneyville-Rock outcrop complex, 6 to 30 percent slopesCoD18220551146lhhxky21919841:20000
Caneyville silty clay, 6 to 20 percent slopes, severely erodedCnD34410551145lhhwky21919841:20000
Caneyville silt loam, 6 to 12 percent slopesCaC4220551144lhhvky21919841:20000
Caneyville silt loam, 2 to 6 percent slopesCaB630551143lhhtky21919841:20000
Caneyville-Rock outcrop complex, 20 to 60 percent slopesCnF19601553852llb6ky22720041:12000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCnD10605553851llb5ky22720041:12000
Rock outcrop-Caneyville complex, 20 to 60 percent slopesRxF6382553879llc2ky22720041:12000
Caneyville silt loam, 6 to 12 percent slopesCaC1177553849llb3ky22720041:12000
Caneyville silty clay, 6 to 12 percent slopes, severely erodedCaC3396553850llb4ky22720041:12000
Caneyville silt loam, 2 to 6 percent slopesCaB280553848llb2ky22720041:12000
Caneyville-Urban land-Rock outcrop complex, 6 to 20 percent slopesCoD219553815ll90ky22720041:12000
Caneyville-Urban land-Rock outcrop complex, 20 to 30 percent slopesCoE118553816ll91ky22720041:12000
Caneyville-Rock outcrop-Standingstone complex, 12 to 35 percent slopesuCanF6477525838302r1vxky23119851:20000
Garmon-Caneyville association, very steepGcF27651550074lgdbky23119851:20000
Caneyville silt loam, 6 to 20 percent slopes, rockyCeD11758550062lgcyky23119851:20000
Caneyville-Garmon association, steepCgD6460550063lgczky23119851:20000
Caneyville silt loam, 6 to 12 percent slopesCaC3038550061lgcxky23119851:20000
Rock outcrop-Caneyville complex, 20 to 50 percent slopesRoF21550085lgdpky23119851:20000
Culleoka-Caneyville complex, 12 to 20 percent slopesCuD1553551531lhxbky60619791:20000
Caneyville-Vertrees silt loams, 12 to 20 percent slopesCeD1499551523lhx2ky60619791:20000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCcD816551522lhx1ky60619791:20000
Caneyville-Rock outcrop complex, 12 to 30 percent slopesCkD27834549565lfvxky60719921:20000
Caneyville silt loam, 12 to 20 percent slopes, erodedCaD23302549562lfvtky60719921:20000
Rock outcrop-Caneyville complex, 30 to 90 percent slopesRkF2657549616lfxkky60719921:20000
Westmoreland-Caneyville-Rock outcrop complex, 30 to 80 percent slopesWtF1603549631lfy1ky60719921:20000
Caneyville silty clay, 12 to 20 percent slopes, severely erodedCeD31397549564lfvwky60719921:20000
Caneyville silt loam, 6 to 12 percent slopes, erodedCaC21103549561lfvsky60719921:20000
Caneyville silty clay, 6 to 12 percent slopes, severely erodedCeC3503549563lfvvky60719921:20000
Caneyville silt loam, 6 to 12 percent slopes, erodedCaC9184550971lhb8ky60819831:20000
Caneyville-Rock outcrop complex, 20 to 40 percent slopesCnE6088550974lhbcky60819831:20000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCnD4381550973lhbbky60819831:20000
Caneyville-Beasley-Rock outcrop complex, 12 to 30 percent slopesCbD4229550972lhb9ky60819831:20000
Caneyville silt loam, 2 to 6 percent slopesCaB1984550970lhb7ky60819831:20000
Caneyville silt loam, 12 to 30 percent slopes, eroded, rockyCaE2189552919lkc3ky61819931:12000
Caneyville-Frederick silt loams, very rocky, 20 to 30 percent slopesCaE14670552546ljz2ky62019791:20000
Lowell-Caneyville silt loams, very rocky, 30 to 60 percent slopesLoF11883552562ljzlky62019791:20000
Caneyville silt loam, very rocky, 6 to 20 percent slopesCaC2096552545ljz1ky62019791:20000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCnD23405551025lhd0ky62119751:20000
Caneyville-Rock outcrop complex, 20 to 30 percent slopesCnE14615551026lhd1ky62119751:20000
Allegheny-Lenberg-Caneyville complex, 12 to 20 percent slopesAlD4835551023lhcyky62119751:20000
Shelocta and Caneyville soils and rock outcrop, steepSaE3172550715lh20ky62319851:20000
Caneyville-Renox-Bledsoe complex, 50 to 80 percent slopes, extremely stonyCbF1711550723lh28ky62619971:24000
Berks-Caneyville complex, 50 to 120 percent slopes, very rockyBcG273550722lh27ky62619971:24000
Caneyville-Shelocta rocky silt loams, 20 to 30 percent slopesCdE7692552257ljnrky62819731:20000
Caneyville-Hagerstown rocky silt loams, 6 to 20 percent slopesCcD6454552254ljnnky62819731:20000
Caneyville-Hagerstown rocky silt loams, 20 to 30 percent slopesCcE2517552255ljnpky62819731:20000
Caneyville-Shelocta rocky silt loams, 6 to 20 percent slopesCdD1011552256ljnqky62819731:20000
Caneyville-Rock outcrop complex, 20 to 50 percent slopes12F2355612217nk1yky63019661:15840
Caneyville-Rock outcrop complex, 12 to 30 percent slopesCdE2897551093lhg6ky63119761:20000
Caneyville silt loam, 12 to 20 percent slopesCcD1279551092lhg5ky63119761:20000
Caneyville silt loam, 6 to 12 percent slopesCcC839551091lhg4ky63119761:20000
Donahue rocky sandy loam, 6 to 20 percent slopes (caneyville)DoD336014787661lms4ky64519711:20000
Donahue rocky sandy loam, 20 to 40 percent slopes (caneyville)DoF236014787671lms5ky64519711:20000
Baxter very rocky silt loam, 20 to 30 percent slopes, eroded (caneyville rocky)BeE2226124529502nbhfky64619661:15840
Caneyville very rocky silty clay loam, 6 to 20 percent slopes, erodedCaD2115324529542nbhkky64619661:15840
Baxter very rocky silt loam, 6 to 20 percent slopes, eroded (caneyville rocky)BeD2108224529492nbhdky64619661:15840
Caneyville very rocky silty clay, 12 to 25 percent slopes, severely erodedCcD348024529552nbhlky64619661:15840
Caneyville silt loam, very rocky, 6 to 20 percent slopesCaD1841024530552nbltky64719891:20000
Caneyville silt loam, very rocky, 20 to 30 percent slopesCaE996724530562nblvky64719891:20000
Rock outcrop-Caneyville complex, 12 to 30 percent slopesRxE869524531032nbncky64719891:20000
Caneyville silty clay loam, very rocky, 6 to 20 percent slopes, severely erodedCeD3165724530572nblwky64719891:20000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCkD339423791592kvq2ky64820091:12000
Caneyville-Rock outcrop complex, 20 to 35 percent slopesCkE187123791602kvq3ky64820091:12000
Caneyville silt loam, 6 to 12 percent slopes, erodedCaC2136223791552kvpyky64820091:12000
Caneyville-Lenberg complex, 8 to 20 percent slopesCeD45623791572kvq0ky64820091:12000
Rock outcrop-Caneyville complex, 30 to 70 percent slopesRxF34124037652lp9tky64820091:12000
Caneyville silt loam, 20 to 30 percent slopes, very rockyCaE31523793722kvxyky64820091:12000
Caneyville silt loam, 6 to 20 percent slopes, very rockyCaD19023793712kvxxky64820091:12000
Caneyville-Lenberg-Rock outcrop complex, 20 to 30 percent slopesCgE12623791582kvq1ky64820091:12000
Caneyville silty clay loam, 6 to 20 percent slopes, eroded, very rockyCaD210023794432kw07ky64820091:12000
Rock outcrop-Caneyville complex, 12 to 30 percent slopesRxE7923794192kvzgky64820091:12000
Caneyville-Lenberg-Rock outcrop complex, 20 to 30 percent slopesCgE904424528412nbcxky70919951:20000
Caneyville-Lenberg complex, 8 to 20 percent slopesCeD753924528402nbcwky70919951:20000
Caneyville silt loam, 6 to 12 percent slopes, erodedCaC2618224528382nbctky70919951:20000
Caneyville-Rock outcrop complex, 6 to 20 percent slopesCkD565124528422nbcyky70919951:20000
Caneyville-Rock outcrop complex, 20 to 35 percent slopesCkE398424528432nbczky70919951:20000
Caneyville silt loam, 2 to 6 percent slopes, erodedCaB2107024528372nbcsky70919951:20000
Caneyville silty clay loam, 6 to 12 percent slopes, severely erodedCcC358724528392nbcvky70919951:20000
Caneyville flaggy silt loam, 25 to 45 percent slopesCeE120224011362lll0md00120091:12000
Caneyville silt loam, 15 to 25 percent slopesCcD99624011332llkxmd00120091:12000
Caneyville silt loam, 8 to 15 percent slopesCcC44024011322llkwmd00120091:12000
Caneyville flaggy silt loam, 15 to 25 percent slopesCeD39624011352llkzmd00120091:12000
Caneyville silt loam, 25 to 45 percent slopesCcE33424011342llkymd00120091:12000
Caneyville silt loam, 3 to 8 percent slopesCcB5024011312llkvmd00120091:12000
Caneyville-Bucklick complex, 8 to 15 percent slopes, rocky7315028825016752vxqmmo01720041:24000
Caneyville-Gasconade-Bucklick complex, 15 to 25 percent slopes, rocky7315118725016782vxqnmo01720041:24000
Caneyville-Gasconade-Bucklick complex, 15 to 25 percent slopes, rocky73151225016812vxqnmo03119781:24000
Caneyville silty clay loam, 3 to 8 percent slopes, eroded73257932605167n9qjmo05120021:24000
Caneyville-Rock outcrop complex, 8 to 15 percent slopes7328872325023092vxrsmo05520031:24000
Caneyville silt loam, 8 to 15 percent slopes732083225017742vxr2mo07119861:24000
Caneyville silt loam, 3 to 8 percent slopes73207425017702vxr1mo07119861:24000
Caneyville silt loam, 15 to 30 percent slopes73209125017782vxr3mo07119861:24000
Caneyville-Rock outcrop complex, 8 to 15 percent slopes7328812725023102vxrsmo09319881:24000
Caneyville silt loam, 3 to 8 percent slopes, rocky732937125023272vxrymo09319881:24000
Caneyville silt loam, 15 to 30 percent slopes732092352725017792vxr3mo09920001:24000
Caneyville silt loam, 8 to 15 percent slopes73208236525017752vxr2mo09920001:24000
Caneyville silt loam, 3 to 8 percent slopes73207190625017712vxr1mo09920001:24000
Caneyville-Bucklick complex, 3 to 8 percent slopes73149341825016732vxqlmo12319991:24000
Caneyville-Bucklick complex, 8 to 15 percent slopes, rocky73150238925016762vxqmmo12319991:24000
Caneyville-Gasconade-Bucklick complex, 15 to 25 percent slopes, rocky73151141725016792vxqnmo12319991:24000
Menfro-Caneyville silt loams, karst, 5 to 20 percent slopes, eroded601835233909601zjhzmo15719831:24000
Menfro-Caneyville-Rubble land complex, 20 to 60 percent slopes601844395909605zjj3mo15719831:24000
Gasconade-Caneyville complex, 14 to 35 percent slopes60098525909626zjjsmo15719831:24000
Caneyville silt loam, 15 to 20 percent slopes, stony73380325024722vxshmo15719831:24000
Caneyville silt loam, 15 to 20 percent slopes, stony73380681825024742vxshmo18619821:24000
Caneyville silt loam, 8 to 15 percent slopes73208647025017772vxr2mo18619821:24000
Caneyville silt loam, 3 to 8 percent slopes73207455325017732vxr1mo18619821:24000
Caneyville silt loam, 3 to 8 percent slopes732071834925017722vxr1mo18719791:24000
Caneyville silt loam, 8 to 15 percent slopes73208964925017762vxr2mo18719791:24000
Caneyville silt loam, 15 to 20 percent slopes, stony73380498825024732vxshmo18719791:24000
Caneyville silt loam, 1 to 5 percent slopes73530260013971771hww7mo18719791:24000
Caneyville-Rock outcrop complex, 8 to 15 percent slopes7328824625023112vxrsmo18719791:24000
Caneyville silt loam, 3 to 8 percent slopes, rocky7329311325023282vxrymo18719791:24000
Caneyville-Rock outcrop complex, 8 to 15 percent slopes73288935425023122vxrsmo22120031:24000
Caneyville silt loam, 3 to 8 percent slopes, rocky73293300225023292vxrymo22120031:24000
Caneyville-Bucklick complex, 8 to 15 percent slopes, rocky73150266625016772vxqmmo22320041:24000
Caneyville-Bucklick complex, 3 to 8 percent slopes7314956625016742vxqlmo22320041:24000
Caneyville-Gasconade-Bucklick complex, 15 to 25 percent slopes, rocky7315153925016802vxqnmo22320041:24000

Map of Series Extent

Approximate geographic distribution of the CANEYVILLE 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 .