Official Series Description


Lab Data Summary

Aggregate lab data for the CULLEOKA soil series. This aggregation is based on all pedons with a current taxon name of CULLEOKA, 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 CULLEOKA 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
12290KY-057-00290KY-057-002Culleoka2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9209099,-85.2874451
12665PA0030081965PA003008Culleoka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3080556,-80.0619444
12665PA0030091965PA003009Culleoka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3102778,-80.0419444
12681PA0590041981PA059004Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7791667,-80.1205556
126WVU0040S02WV051003Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9108333,-80.6522222
12666PA125011S1966PA125011Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2094444,-80.3316667
12666PA125012S1966PA125012Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1472222,-80.1613889
12681PA059005S1981PA059005Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7672222,-80.1058333
n/a00KY-001-00200KY-001-002Culleoka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a00KY-001-00400KY-001-004Culleoka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aBT-s011955-OH013-S01Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aBT-s021955-OH013-S02Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aBT-w041961-OH013-W04Culleoka3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJF-0061978-OH081-006Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPR-0031979-OH127-003Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPR-0061979-OH127-006Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPR-0071979-OH127-007Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJF-0161984-OH081-016Culleoka5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aBT-0321985-OH013-032Culleoka4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CULLEOKA 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 CULLEOKA 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 CULLEOKA 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 CULLEOKA 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 CULLEOKA 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 CULLEOKA 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 CULLEOKA 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 CULLEOKA, 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. KY-2010-09-03-04 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Culleoka-Eden general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  2. 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).

  3. KY-2012-01-27-38 | Clark County - 1964

    Major soil series in soil association 5, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  4. KY-2012-01-27-40 | Clark County - 1964

    Major soil series in soil association 7, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  5. KY-2012-01-27-45 | Clark County - 1964

    Geolgic cross section of Clark County, showing some of the principal soils and their relation to the rock formations (Soil Survey of Clark County, Kentucky; 1964).

  6. KY-2012-01-27-70 | Fayette County - February 1968

    Relationship of soils to topography and underlying material in association 5 (Soil Survey of Fayette County, Kentucky; February 1968).

  7. KY-2012-01-31-24 | Jessamine and Woodford Counties - December 1983

    Pattern of soils and underlying material in Eden-Culleoka unit (Soil Survey of Jessamine and Woodford Counties, Kentucky; December 1983).

  8. OH-2012-02-16-13 | Belmont County - July 1981

    Typical pattern of soils in the Westmoreland-Dekalb-Lowell association (Soil Survey of Belmont County, Ohio; July 1981).

  9. OH-2012-02-16-14 | Belmont County - July 1981

    Typical pattern of soils in the Westmoreland-Lowell association (Soil Survey of Belmont County, Ohio; July 1981).

  10. PA-2012-03-12-08 | Beaver and Lawrence Counties - April 1982

    Pattern of soils and parent material in Gilpin-Guernsey-Culleoka association (Soil Survey of Beaver and Lawrence Counties, PA; 1982).

  11. PA-2012-03-13-34 | Greene and Washington Counties - September 1983

    Typical pattern of soils and underlying material in the Dormont-Culleoka association (Soil Survey of Greene and Washington Counties, PA; 1983).

  12. TN-2012-03-19-05 | Hardin County - June 1963

    Major soil series in soil associations 8 and 10 and their relationship to the landscape (Soil Survey of Hardin County, TN; 1963).

  13. TN-2012-03-19-21 | Maury County - October 1959

    Sketch showing relative positions of soils in the Inman-Culleoka-Hicks-Maury (coarse phases) assciation (Soil Survey of Maury County, TN; 1959).

  14. TN-2012-03-19-40 | Williamson County - August 1964

    Major and minor soils and underlying parent materials in the Stiversville-Culleoka-Inman association (Soil Survey of Williamson County, TN; 1964).

Map Units

Map units containing CULLEOKA 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
Weikert-Culleoka complex, 6 to 12 percent slopesWcC745415924871qg3kky00120061:12000
Weikert-Culleoka complex, 12 to 20 percent slopesWcD678015924881qg3lky00120061:12000
Culleoka-Weikert complex, 2 to 6 percent slopesCwB150215924861qg3jky00120061:12000
Urban land-Weikert-Culleoka complex, 2 to 20 percent slopesUw146614133791jfqwky00120061:12000
Culleoka silt loam, 20 to 30 percent slopes, erodedCvE24388550132lgg6ky04919621:15840
Culleoka flaggy silt loam, 30 to 50 percent slopes, erodedCuF21528550128lgg2ky04919621:15840
Culleoka silt loam, 6 to 12 percent slopes, erodedCvC21436550130lgg4ky04919621:15840
Culleoka silt loam, 12 to 20 percent slopes, erodedCvD2750550131lgg5ky04919621:15840
Culleoka flaggy silt loam, 20 to 30 percent slopes, erodedCuE2475550127lgg1ky04919621:15840
Culleoka silt loam, 2 to 6 percent slopesCvB271550129lgg3ky04919621:15840
Culleoka flaggy silt loam, 30 to 50 percent slopesCwF871513978611hxl9ky15119681:20000
Culleoka flaggy silt loam, 20 to 30 percent slopesCwE822113978601hxl8ky15119681:20000
Culleoka silt loam, 6 to 12 percent slopesCuC311313978581hxl6ky15119681:20000
Culleoka silt loam, 12 to 20 percent slopesCuD133513978591hxl7ky15119681:20000
Culleoka silt loam, 2 to 6 percent slopesCuB107613978571hxl5ky15119681:20000
Culleoka-Caneyville complex, 12 to 20 percent slopesCuD1553551531lhxbky60619791:20000
Eden-Culleoka association, 25 to 50 percent slopes, eroded, stonyEfF223274552940lkcsky61819931:12000
Culleoka silt loam, 12 to 25 percent slopes, erodedCuD24592552935lkcmky61819931:12000
Culleoka silt loam, 6 to 12 percent slopes, erodedCuC22950552934lkclky61819931:12000
Culleoka silt loam, 2 to 6 percent slopesCuB336552933lkckky61819931:12000
Culleoka flaggy silt loam, 20 to 30 percent slopesCfE2319551868lj86ky62419761:20000
Culleoka silt loam, 6 to 12 percent slopesCcC822551866lj84ky62419761:20000
Culleoka silt loam, 12 to 20 percent slopesCcD460551867lj85ky62419761:20000
Culleoka flaggy silt loam, 30 to 50 percent slopes, erodedCfF234513988471hym3ky64319651:15840
Culleoka silt loam, 6 to 12 percent slopes, erodedCsC216013988481hym4ky64319651:15840
Culleoka silt loam, 8 to 15 percent slopesCuC3736537071l0vwoh01319781:15840
Culleoka silt loam, 3 to 8 percent slopesCuB2754537070l0vvoh01319781:15840
Culleoka silt loam, 3 to 8 percent slopesCuB7909537976l1t2oh01919811:15840
Culleoka silt loam, 8 to 15 percent slopesCuC314692691l9wsoh11119681:15840
Culleoka silt loam, 3 to 8 percent slopesCbB215954871qk7boh15119671:15840
Gilpin, Weikert, Culleoka channery silt loams and 25 to 80 percent slopesGSF470745416872wds4pa00319731:15840
Urban land-Culleoka complex, moderately steepUCD23551541724l5pzpa00319731:15840
Urban land-Culleoka complex, gently slopingUCB12747541723l5pypa00319731:15840
Culleoka channery silt loam, 15 to 25 percent slopesCuD81725416692s5gppa00319731:15840
Urban land-Culleoka complex, steepUCE7947541725l5q0pa00319731:15840
Culleoka channery silt loam, 8 to 15 percent slopesCuC47575416682s5gnpa00319731:15840
Culleoka-Weikert shaly silt loams, 15 to 25 percent slopesCwD2581541672l5n9pa00319731:15840
Culleoka channery silt loam, 3 to 8 percent slopesCuB15805416672s5gmpa00319731:15840
Culleoka-Weikert shaly silt loams, 8 to 15 percent slopesCwC1307541671l5n8pa00319731:15840
Culleoka-Weikert shaly silt loams, 3 to 8 percent slopesCwB757541670l5n7pa00319731:15840
Culleoka channery silt loam, 8 to 15 percent slopesCuC16424216502s5gnpa00520121:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE13924217312s5gzpa00520121:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB12624216492s5gmpa00520121:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD11624217302s5gypa00520121:24000
Culleoka channery silt loam, 15 to 25 percent slopesCuD5124216512s5gppa00520121:24000
Culleoka channery silt loam, 8 to 15 percent slopesCuC162229002572s5gnpa00719781:15840
Culleoka channery silt loam, 3 to 8 percent slopesCuB151629002562s5gmpa00719781:15840
Culleoka channery silt loam, 15 to 25 percent slopesCuD60529002582s5gppa00719781:15840
Culleoka-Weikert channery silt loams, 8 to 15 percent slopesCyC1663543622l7p6pa01719971:24000
Culleoka-Weikert channery silt loams, 3 to 8 percent slopesCyB1208543621l7p5pa01719971:24000
Weikert-Culleoka complex, 15 to 25 percent slopesWfD706543761l7tppa01719971:24000
Culleoka channery silt loam, 8 to 15 percent slopesCuC6624086192s5gnpa03120121:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB5624086182s5gmpa03120121:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD1467115910422s5gypa05120051:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE1261815910432s5gzpa05120051:24000
Culleoka channery silt loam, 8 to 15 percent slopesCuC916715910402s5gnpa05120051:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB695815910392s5gmpa05120051:24000
Lowell-Culleoka complex, 25 to 80 percent slopes, very rockyLxF610515910481qdm4pa05120051:24000
Culleoka channery silt loam, 15 to 25 percent slopesCuD273915910412s5gppa05120051:24000
Urban land-Culleoka complex, 0 to 8 percent slopesUeB67115911261qdpnpa05120051:24000
Urban land-Culleoka complex, 8 to 25 percent slopesUeD20015911271qdpppa05120051:24000
Culleoka channery silt loam, 8 to 15 percent slopesCuC202523938322s5gnpa06320121:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB140923938312s5gmpa06320121:24000
Dormont-Culleoka complex, 15 to 25 percent slopesDrD93623938352s5gypa06320121:24000
Culleoka channery silt loam, 15 to 25 percent slopesCuD41523938332s5gppa06320121:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE30723938362s5gzpa06320121:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB28324872422s5gmpa06520121:12000
Culleoka channery silt loam, 8 to 15 percent slopesCuC11824872432s5gnpa06520121:12000
Culleoka channery silt loam, 15 to 25 percent slopesCuD6129004102s5gppa07319781:15840
Culleoka channery silt loam, 8 to 15 percent slopesCuC1729004092s5gnpa07319781:15840
Culleoka channery silt loam, 3 to 8 percent slopesCuB229004082s5gmpa07319781:15840
Dormont-Culleoka complex, 15 to 25 percent slopesDrD100415445662s5gypa12920031:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDrE74345445672s5gzpa12920031:24000
Culleoka channery silt loam, 3 to 8 percent slopesCuB43015445612s5gmpa12920031:24000
Lowell-Culleoka complex, 25 to 80 percent slopes, very rockyLxF4275530797ktbhpa12920031:24000
Urban land-Culleoka complex, 8 to 25 percent slopesUeD3549544654l8rhpa12920031:24000
Urban land-Culleoka complex, 0 to 8 percent slopesUeB3299544652l8rfpa12920031:24000
Culleoka channery silt loam, 8 to 15 percent slopesCuC26735445622s5gnpa12920031:24000
Culleoka channery silt loam, 15 to 25 percent slopesCuD12785445632s5gppa12920031:24000
Dormont-Culleoka complex, 25 to 50 percent slopesDtF2876765421532s5gzpa61119791:15840
Dormont-Culleoka complex, 15 to 25 percent slopesDtD1456765421522s5gypa61119791:15840
Culleoka channery silt loam, 15 to 25 percent slopesCaD412275421402s5gppa61119791:15840
Culleoka channery silt loam, 8 to 15 percent slopesCaC257145421392s5gnpa61119791:15840
Weikert-Culleoka complex, 15 to 25 percent slopesWeD23337542178l65mpa61119791:15840
Culleoka channery silt loam, 3 to 8 percent slopesCaB170915421382s5gmpa61119791:15840
Weikert-Culleoka complex, 3 to 8 percent slopesWeB15176542176l65kpa61119791:15840
Weikert-Culleoka complex, 8 to 15 percent slopesWeC11553542177l65lpa61119791:15840
Culleoka-Upshur complex, 15 to 25 percent slopesCkD2395542143l64hpa61119791:15840
Culleoka-Upshur complex, 8 to 15 percent slopesCkC1685542142l64gpa61119791:15840
Culleoka-Upshur complex, 3 to 8 percent slopesCkB670542141l64fpa61119791:15840
Culleoka loam, 12 to 20 percent slopes, severely erodedCuD3871527289kppbtn05519651:15840
Culleoka loam, 12 to 20 percent slopes, eroded (uneroded)CuD2722527288kpp9tn05519651:15840
Culleoka flaggy loam, 15 to 35 percent slopesCyE668527292kppftn05519651:15840
Culleoka loam, 20 to 35 percent slopesCuE657527290kppctn05519651:15840
Culleoka loam, 20 to 35 percent slopes, severely erodedCuE3448527291kppdtn05519651:15840
Culleoka loam, 5 to 12 percent slopes, eroded (uneroded)CuC2289527286kpp7tn05519651:15840
Culleoka loam, 5 to 12 percent slopes, severely erodedCuC3244527287kpp8tn05519651:15840
Culleoka silt loam, 12 to 35 percent slopesCkF1134327538bztrtn07119611:15840
Culleoka silt loam, 5 to 12 percent slopesCkD355327537bztqtn07119611:15840
Westmoreland-Culleoka complex, 25 to 35 percent slopes41E328714026921j2m4va02120051:24000
Culleoka-Berks complex, 35 to 70 percent slopes13F226314026931j2m5va02120051:24000
Westmoreland-Culleoka complex, 15 to 25 percent slopes41D131814026911j2m3va02120051:24000
Berks-Culleoka complex, 25 to 35 percent slopes6E403724810682p8rgva04520101:24000
Culleoka-Berks complex, 15 to 25 percent slopes14D264324810672p8rfva04520101:24000
Berks-Culleoka complex, 35 to 70 percent slopes6G151024810692p8rhva04520101:24000
Culleoka-Berks complex, 8 to 15 percent slopes14C57424810662p8rdva04520101:24000
Berks-Culleoka complex, 55 to 70 percent slopes8G36625074732q7p2va19520101:24000
Culleoka loam, 35 to 55 percent slopes, very stonyCyF34539553049lkh9wv02520021:24000
Culleoka loam, 25 to 35 percent slopes, very stonyCyE8963553048lkh8wv02520021:24000
Culleoka loam, 8 to 15 percent slopesCuC7167553046lkh6wv02520021:24000
Culleoka loam, 15 to 25 percent slopesCuD5426553047lkh7wv02520021:24000
Culleoka loam, 3 to 8 percent slopesCuB1706553045lkh5wv02520021:24000
Dormont-Culleoka complex, 35 to 70 percent slopes, very stonyDsF55677749372t4s9wv05120071:12000
Dormont-Culleoka complex, 25 to 35 percent slopesDrE31094749371t4s8wv05120071:12000
Culleoka-Dormont complex, 15 to 25 percent slopesCmD288207493692s5hdwv05120071:12000
Culleoka-Dormont-Peabody complex, 35 to 65 percent slopes, very stonyCrF1726617206371vrgfwv05120071:12000
Culleoka-Dormont-Peabody complex, 15 to 25 percent slopesCpD44531884886218cswv05120071:12000
Culleoka-Dormont-Peabody complex, 25 to 35 percent slopesCpE430916035931qtntwv05120071:12000
Culleoka channery silt loam, 8 to 15 percent slopesClC240816057872s5gnwv05120071:12000
Culleoka-Dormont complex, 8 to 15 percent slopesCmC214716023172s5hfwv05120071:12000
Culleoka-Peabody complex, 15 to 25 percent slopesCyD11861884889218cwwv05120071:12000
Culleoka-Dormont-Urban land complex, 15 to 25 percent slopesCuD921749374t4scwv05120071:12000
Culleoka-Dormont-Peabody complex, 8 to 15 percent slopesCpC8801884892218czwv05120071:12000
Culleoka-Dormont-Urban land complex, 8 to 15 percent slopesCuC57616026761qsq7wv05120071:12000
Culleoka loam, 35 to 55 percent slopes, very stonyCyF45517142131vjs6wv06319621:24000
Culleoka loam, 25 to 35 percent slopes, very stonyCyE23217142121vjs5wv06319621:24000
Culleoka loam, 15 to 25 percent slopesCuD17617142111vjs4wv06319621:24000
Culleoka loam, 8 to 15 percent slopesCuC16517142101vjs3wv06319621:24000
Culleoka silt loam, 35 to 55 percent slopesCuF2057515397k99qwv07519921:24000
Culleoka silt loam, 8 to 15 percent slopesCuC1052515394k99mwv07519921:24000
Culleoka silt loam, 15 to 25 percent slopesCuD718515395k99nwv07519921:24000
Culleoka silt loam, 25 to 35 percent slopesCuE573515396k99pwv07519921:24000
Culleoka silt loam, 3 to 8 percent slopesCuB561515393k99lwv07519921:24000
Culleoka-Lowell complex, 15 to 25 percent slopesCuD102313841931hgcdwv60020051:24000
Culleoka-Lowell complex, 25 to 35 percent slopesCuE55513841941hgcfwv60020051:24000
Lowell-Culleoka complex, 8 to 15 percent slopesLzC27713841951hgcgwv60020051:24000
Culleoka silt loam, 25 to 35 percent slopesCuE6249515783k9q5wv61019731:20000
Culleoka silt loam, 15 to 25 percent slopesCuD3370515782k9q4wv61019731:20000
Culleoka silt loam, 35 to 60 percent slopes, severely erodedCuF32841515785k9q7wv61019731:20000
Culleoka silt loam, 8 to 15 percent slopesCuC2589515781k9q3wv61019731:20000
Culleoka silt loam, 25 to 35 percent slopes, severely erodedCuE31293515784k9q6wv61019731:20000
Gilpin-Culleoka-Upshur silt loams, 35 to 65 percent slopesGuF698215143872t1ljwv61119771:20000
Culleoka-Westmoreland silt loams, 25 to 35 percent slopesCwE35180514360k878wv61119771:20000
Gilpin-Culleoka-Upshur silt loams, 25 to 35 percent slopesGuE265255143862t1lhwv61119771:20000
Culleoka-Westmoreland silt loams, 35 to 65 percent slopesCwF22900514361k879wv61119771:20000
Culleoka-Westmoreland silt loams, 15 to 25 percent slopesCwD21835514359k877wv61119771:20000
Gilpin-Culleoka-Upshur silt loams, 15 to 25 percent slopesGuD163755143852t1lgwv61119771:20000
Culleoka-Westmoreland silt loams, 8 to 15 percent slopesCwC7013514358k876wv61119771:20000
Gilpin-Culleoka silt loams, 35 to 65 percent slopesGcF3380514383k880wv61119771:20000
Gilpin-Culleoka silt loams, 25 to 35 percent slopesGcE3025514382k87zwv61119771:20000
Urban land-Culleoka complex, 15 to 25 percent slopesUeD1955514414k890wv61119771:20000
Gilpin-Culleoka-Upshur silt loams, 8 to 15 percent slopesGuC16955143842t1lfwv61119771:20000
Gilpin-Culleoka silt loams, 15 to 25 percent slopesGcD1325514381k87ywv61119771:20000
Culleoka-Westmoreland silt loams, 3 to 8 percent slopesCwB1111514357k875wv61119771:20000
Gilpin-Culleoka-Upshur complex, 25 to 35 percent slopes, severely erodedGwE3965514389k886wv61119771:20000
Gilpin-Culleoka-Upshur complex, 15 to 25 percent slopes, severely erodedGwD3510514388k885wv61119771:20000
Gilpin-Culleoka silt loams, 8 to 15 percent slopesGcC305514380k87xwv61119771:20000
Culleoka silt loam, 30 to 65 percent slopesCuF13842516579k9xzwv7131:24000

Map of Series Extent

Approximate geographic distribution of the CULLEOKA 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 .