Official Series Description


Lab Data Summary

Aggregate lab data for the SHELOCTA soil series. This aggregation is based on all pedons with a current taxon name of SHELOCTA, 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 SHELOCTA 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
12467KY-175-00667KY-175-006Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0550778,-83.3429667
12467KY-175-00867KY-175-008Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0237889,-83.3705944
12484KY-069-UK484KY-069-UK4Shelocta3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4205856,-83.6129761
12486KY-069-00786KY-069-007Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4061623,-83.5079422
12490KY-135-00390KY-135-003Shelocta1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4611626,-83.331543
12508N018607KY650101Shelocta7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7169444,-84.545
12508N018707KY650102Shelocta7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6695556,-84.54275
12510KY-125-00210KY125FSC002Shelocta1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9799156,-84.2734756
12507N01872006TN137002SShelocta6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6026573,-84.8003464
12571KY-025-00871KY-025-008Shelocta3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4686611,-83.1405694
12576KY-025-00176KY-025-001Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4736786,-83.163765
12576KY-025-00276KY-025-002Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4764557,-83.1651535
12586P005985KY013005Shelocta6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7313881,-83.8286133
12586P005885KY095008Shelocta6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9319458,-83.1986084
12586P006085KY095009Shelocta6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9702797,-83.2316666
12586P068986WV005005Shelocta7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0144463,-81.8758316
12540A4303S1963KY147001Shelocta5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6177788,-84.4030533
147VPI0187V1992-VA091-187Shelocta2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5534722,-79.6667778
147VPI0188V1992-VA091-188Shelocta2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.54575,-79.6678333
147VPI0170V1992-WV075-170Shelocta2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2803056,-79.7913333
n/aWS-0091967-OH167-009Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPK-0111982-OH131-011Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a67KY-165-00767KY-165-007Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a69KY-051-00169KY-051-001Sheloctan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a69KY-095-00169KY-095-001Sheloctan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a69KY-127-00469KY-127-004Sheloctan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a69KY-131-00269KY-131-002Sheloctan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a69KY-175-00169KY-175-001Sheloctan/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a73KY-089-04673KY-089-046Shelocta3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a76KY-217-01076KY-217-010Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83P067183KY195008Shelocta6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a84KY-069-01084KY-069-010Shelocta2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a84KY-197-00584KY-197-005Shelocta1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-159-00294KY-159-002Shelocta1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-205-00294KY-205-002Shelocta1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A4346S1963TN129001Shelocta5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aSC-013YYYY-OH145-013Shelocta4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHELOCTA 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 SHELOCTA 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 SHELOCTA 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 SHELOCTA 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 SHELOCTA 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 SHELOCTA 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 SHELOCTA 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 SHELOCTA, 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-2010-09-03-01 | Clay County - 2003

    Typical pattern of soils and parent material in the Shelocta-Cloverlick-Highsplint general soil map unit. This unit covers about 80 percent of the county. Most areas are hilly and forested (Soil Survey of Clay County, Kentucky; 2003).

  2. KY-2010-09-03-02 | Clay County - 2003

    Typical pattern of soils and parent material in the Shelocta-Fairpoint-Bethesda-Gilpin general soil map unit. This map unit is primarily in the west-central part of the county. It has been extensively mined for coal (Soil Survey of Clay County, Kentucky; 2003)

  3. KY-2010-09-03-11 | Knott and Letcher Counties - 2004

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

  4. KY-2010-09-03-12 | Knott and Letcher Counties - 2004

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

  5. 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).

  6. KY-2010-09-03-14 | Knott and Letcher Counties - 2004

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

  7. KY-2010-09-03-15 | Knott and Letcher Counties - 2004

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

  8. KY-2010-09-03-16 | Knott and Letcher Counties - 2004

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

  9. KY-2010-09-03-17 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topography in the Udorthents-Nelse-Allegheny and Shelocta-Hazleton-Blairton general soil map units. The Udorthents-Nelse-Allegheny general soil map unit is along the Tug and Lavista Forks of the Big Sandy River and their major tributaries, and the Shelocta-Hazleton-Blairton general soil map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  10. KY-2010-09-03-18 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topography in the Hazleton-Shelocta-Fiveblock and Grigsby-Shelocta-Orrville general soil map units. The Hazleton-Shelocta-Fiveblock general soil map unit is on the mountains and in the surface mined areas, and the Grigsby-Shelocta-Orrville general soil map unit is in the valleys (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  11. KY-2010-09-03-20 | Lewis County - 2004

    Typical pattern of soils and parent material in the Skidmore-Shelocta-Haymond general soil map unit.

  12. KY-2010-09-03-21 | Lewis County - 2004

    Typical pattern of soils and parent material in the Covedale-Trappist general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  13. KY-2010-09-03-22 | Lewis County - 2004

    Typical pattern of soils and parent material in the Blairton-Berks-Brownsville general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  14. KY-2010-09-03-23 | Lewis County - 2004

    Typical pattern of soils and parent material in the Berks-Brownsville-Blairton general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  15. KY-2010-09-03-24 | Lewis County - 2004

    Typical pattern of soils and parent material in the Berks-Brownsville-Shelocta general soil map unit (Soil Survey of Lewis County, Kentucky; 2004).

  16. 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).

  17. KY-2010-09-03-34 | Estill and Lee Counties - 2007

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

  18. KY-2010-09-03-35 | Estill and Lee Counties - 2007

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

  19. KY-2010-09-03-36 | Estill and Lee Counties - 2007

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

  20. KY-2010-09-03-39 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Helechawa-Gilpin-Hazleton general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  21. KY-2010-09-03-40 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Pope-Helechawa-Gilpin general soil map unit in Magoffin County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  22. KY-2010-09-03-41 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Kimper-Shelocta-Fedscreek-Gilpin general soil map unit in Magoffin County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  23. KY-2010-09-03-42 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Latham-Marrowbone general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  24. KY-2010-09-03-43 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Gilpin-Shelocta-Latham general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  25. KY-2010-09-03-44 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Rigley-Shelocta-Gilpin-Rock outcrop general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  26. KY-2010-09-03-46 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Shelocta-Gilpin-Allegheny-Grigsby general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  27. KY-2010-09-10-02 | Butler and Edmonson Counties -

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

  28. KY-2010-09-10-03 | Butler and Edmonson Counties -

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

  29. KY-2010-09-10-04 | Butler and Edmonson Counties -

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

  30. KY-2010-09-10-06 | Butler and Edmonson Counties -

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

  31. KY-2010-09-27-01 | Floyd and Johnson Counties - 2000

    Relationship of soils to topography and geology in the Fedscreek-Hazleton-Shelocta-Gilpin general soil map unit (Soil Survey of Floyd and Johnson Counties, Kentucky; 2000).

  32. KY-2012-01-26-26 | Bell and Harlan Counties - December 1992

    Typical pattern of soils in the Kimper-Shelocta-Varilla general soil map unit, showing the relationship of the soils to parent material and topography (Soil Survey of Bell and Harlan Counties, Kentucky; December 1992).

  33. KY-2012-01-27-21 | Carter County - April 1983

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

  34. KY-2012-01-27-22 | Carter County - April 1983

    Pattern of soils, topography, and underlying material in the Pope-Shelocta-Whitley map unit (Soil Survey of Carter County, Kentucky; April 1983).

  35. 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).

  36. KY-2012-01-27-61 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Huntington-Newark-Morehead association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  37. KY-2012-01-27-62 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Shelocta-Brookside-Latham association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  38. KY-2012-01-27-63 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Shelocta-Jefferson-Dekalb association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  39. KY-2012-01-27-64 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Shelocta-Latham-Jefferson association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  40. KY-2012-01-30-01 | Floyd and Johnson Counties - 2000

    Relationship of soils to topography and geology in the Hazleton-Fedscreek-Dekalb-Marrowbone general soil map unit (Soil Survey of Floyd and Johnson Counties, Kentucky; 2000).

  41. KY-2012-01-30-03 | Floyd and Johnson Counties - 2000

    Relationship of soils to topography and geology in the Fedscreek-Hazleton-Shelocta-Gilpin general soil map unit (Soil Survey of Floyd and Johnson Counties, Kentucky; 2000).

  42. KY-2012-01-30-04 | Grayson County - December 1972

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

  43. 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).

  44. KY-2012-01-30-10 | Green and Taylor Counties - July 1982

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

  45. KY-2012-01-31-12 | Jackson and Owsley Counties - April 1989

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

  46. KY-2012-01-31-13 | Jackson and Owsley Counties - April 1989

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

  47. 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).

  48. KY-2012-01-31-25 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Shelocta-Latham-DeKalb map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  49. KY-2012-01-31-26 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Rigley-Lily-Shelocta map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  50. KY-2012-01-31-27 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Sehlocta-Latham map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  51. KY-2012-01-31-28 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Shelocta-Bledsoe-Steinsburg map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  52. KY-2012-01-31-29 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Stendal-Shelocta map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  53. KY-2012-01-31-32 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Wernock-Shelocta-Latham map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  54. KY-2012-02-01-17 | McCreary-Whitley Area - 1970

    General location of the Muse and Shelocta soils in a typical area of the Jellico Mountains. Small areas of sandstone cliffs are common (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  55. KY-2012-02-01-23 | McCreary-Whitley Area - 1970

    General location of Tate and Shelocta soils on a typical benched landscape in association 8 (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  56. KY-2012-02-01-24 | McCreary-Whitley Area - 1970

    The relationship of rock formations and relief to some of the soil associations on the general soil map of the McCreary-Whitley Area (Soil Survey of McCreary-Whitley Area, Kentucky; 1970).

  57. KY-2012-02-01-35 | Montgomery County - January 1986

    The pattern of soils and relationship to topography and underlying material in the Lenberg-Trappist-Colyer general soil map unit (Soil Survey of Montgomery County, Kentucky; January 1986).

  58. KY-2012-02-01-36 | Montgomery County - January 1986

    The pattern of soils and relationship to topography and underlying material in the Shelocta-Berks-Bledsoe general soil map unit (Soil Survey of Montgomery County, Kentucky; January 1986).

  59. 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).

  60. KY-2012-02-01-45 | Powell and Wolfe Counties - September 1993

    Typical pattern of soils and parent material in the Sheloctal-Gilpin-Latham general soil map unit (Soil Survey of Powell and Wolfe Counties, Kentucky; September 1993).

  61. 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).

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

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

  63. OH-2010-09-29-20 | Fairfield County - 2005

    Typical pattern of soils and parent material in the Shelocta-Berks-Gilpin association (Soil Survey of Fairfield County, Ohio; 2005).

  64. OH-2010-09-29-23 | Ross County - 2003

    Typical pattern of soils and parent material in the Cruze-Rossmoyne-Shelocta general soil map unit (Soil Survey of Ross County, Ohio; 2003).

  65. OH-2010-09-29-24 | Vinton County - 2004

    Typical pattern of soils and parent material in the Shelocta-Brownsville-Germano general soil map unit (Soil Survey of Vinton County, Ohio; 2004).

  66. OH-2012-02-16-39 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Shelocta-Brownsville association (Soil Survey of Scioto County, Ohio; January 1989).

  67. OH-2012-02-16-40 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Latham-Wharton-Shelocta association (Soil Survey of Scioto County, Ohio; January 1989).

  68. OH-2012-02-16-41 | Scioto County - January 1989

    Typical pattern of soils and parent material in the Shelocta-Steinsburg-Latham association (Soil Survey of Scioto County, Ohio; January 1989).

  69. TN-2010-11-02-06 | Cumberland County - 2006

    The pattern of soils and parent material in the Jefferson-Varilla-Shelocta general soil map unit (Soil Survey of Cumberland County, Tennessee; 2006).

  70. TN-2010-11-02-29 | Overton County - 2005

    The relationship of soils and landscapes in the Lily-Gilpin and Gilpin-Shelocta-Bouldin general soil map units (Soil Survey of Overton County, Tennessee; 2005).

  71. VA-2010-11-05-06 | Buchanan County -

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia).

  72. VA-2010-11-05-14 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from "Geology of the Virginia Portion of the Clintwood and Jenkings East Quadrangles" (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  73. VA-2010-11-05-15 | Dickenson County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Dickenson County, Virginia; 2009).

  74. VA-2010-11-05-16 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  75. VA-2010-11-05-17 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  76. VA-2010-11-05-31 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).

  77. VA-2010-11-05-35 | Scott County - 2006

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Scott County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Scott County, Virginia; 2006).

  78. VA-2012-05-10-03 | Buchanan County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Buchanan County, Virginia; 2009).

  79. VA-2012-05-10-04 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  80. VA-2012-05-10-05 | Buchanan County - 2009

    An illustration of an area that has been surface-mined for coal that shows a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Buchanan County, Virginia; 2009).

  81. VA-2012-05-11-01 | Dickenson County - 2009

    Diagram of a sequence of residual, colluvial, and alluvial soils. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Dickenson County, Virginia; 2009).

  82. VA-2012-05-11-02 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and multiple exposed highwalls. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  83. VA-2012-05-11-03 | Dickenson County - 2009

    Illustration of an area that has been surface mined for coal, showing a sequence of native residual and colluvial soils, mine soils, rock outcrop, and a single exposed highwall. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position and geologic strata (Soil Survey of Dickenson County, Virginia; 2009).

  84. VA-2012-05-11-04 | Dickenson County - 2009

    An idealized cross-section of the north-central section of the survey area showing the relationship among landforms, geology, and soils. Geology adapted from “Geology of the Virginia Portion of the Clintwood and Jenkins East Quadrangles” (Diffenbach, 1988) (Soil Survey of Dickenson County, Virginia; 2009).

  85. VA-2012-05-11-11 | Russell County - 2007

    Diagram of a sequence of landform positions in the Appalachian Plateau area of Russell County. The soils named on the land surface are shown in their natural relationship to each other and in their relationship to landform position (Soil Survey of Russell County, Virginia; 2007).

  86. WV-2012-03-23-02 | Boone County - June 1994

    Typical pattern of soils and parent material in the Berks-Shelocta general soil map unit (Soil Survey of Boone County, WV; 1994).

Map Units

Map units containing SHELOCTA 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
Shelocta channery loam, 5 to 15 percent slopesSkD205202386125xzvga12920071:12000
Shelocta channery loam, 2 to 15 percent slopesShC90562967lwt7ga64820011:12000
Shelocta-Gilpin silt loams, 20 to 60 percent slopes, erodedSpF21381317275291vzmrky01120061:12000
Shelocta silt loam, 6 to 20 percent slopesSlD18917274861vzlcky01120061:12000
Shelocta-Skidmore complex, 0 to 6 percent slopes, frequently floodedShB1917274851vzlbky01120061:12000
Shelocta-Highsplint-Gilpin complex, 20 to 70 percent slopes, very stonyuShgF7550630987132x5k0ky02519911:24000
Shelocta-Gilpin-Kimper complex, 20 to 70 percent slopesSkE65785550346lgp3ky02519911:24000
Handshoe-Fedscreek-Shelocta complex, 30 to 80 percent slopes, very stonyuHfsF2277730987172x5j1ky02519911:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF197775503392x5jgky02519911:24000
Latham-Shelocta association, steepLTF98258550244lgktky04319801:20000
Latham-Shelocta silt loams, 20 to 30 percent slopesLsE29387550247lgkxky04319801:20000
Shelocta silt loam, 6 to 12 percent slopesSaC2677550260lglbky04319801:20000
Shelocta silt loam, 12 to 20 percent slopesSaD2318550261lglcky04319801:20000
Shelocta silt loam, 2 to 6 percent slopesSaB1997550259lgl9ky04319801:20000
Shelocta-Highsplint-Gilpin complex, 20 to 70 percent slopes, very stonySlF908305525362x5k0ky05119941:24000
Shelocta-Kimper-Cloverlick complex, 20 to 80 percent slopes, very stonySkF842365525352qytpky05119941:24000
Gilpin-Shelocta complex, 20 to 35 percent slopesGlE278395525242qytjky05119941:24000
Gilpin-Shelocta complex, 12 to 20 percent slopes, erodedGlD22456552523ljybky05119941:24000
Gilpin-Shelocta complex, 3 to 12 percent slopes, erodedGlC21223552522ljy9ky05119941:24000
Shelocta channery silt loam, 6 to 12 percent slopesShC7775525342w8j0ky05119941:24000
Shelocta gravelly silt loam, 2 to 6 percent slopesShB578552533ljynky05119941:24000
Shelocta-Handshoe-Fedscreek complex, 30 to 60 percent slopes, stonyuShfF5105830987062xnk5ky06320071:12000
Gilpin-Shelocta complex, 25 to 45 percent slopesGsE3341118846712184vky06320071:12000
Shelocta-Grigsby-Orrville complex, 2 to 15 percent slopesSoC414518846632184lky06320071:12000
Shelocta loam, 12 to 30 percent slopesShD84215284831n9hxky06320071:12000
Shelocta loam, 6 to 12 percent slopesShC5218846642184mky06320071:12000
Shelocta-Wharton complex, 20 to 55 percent slopesSrF1573552739lk59ky06919891:20000
Shelocta gravelly silt loam, 20 to 40 percent slopesShF466552738lk58ky06919891:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesShD329552737lk57ky06919891:20000
Shelocta gravelly silt loam, 4 to 12 percent slopesShC230552736lk56ky06919891:20000
Shelocta gravelly silt loam, 6 to 12 percent slopesShC5365549685lfzsky08519671:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesShD1115549686lfztky08519671:20000
Shelocta gravelly silt loam, 2 to 6 percent slopesShB685549684lfzrky08519671:20000
Shelocta gravelly silt loam, 12 to 20 percent slopes, severely erodedShD3295549687lfzvky08519671:20000
Berks-Brownsville-Shelocta complex, 30 to 65 percent slopes, erodedBoF251455550278lglxky13519981:20000
Shelocta silt loam, 20 to 45 percent slopes, erodedSkF22934550321lgn9ky13519981:20000
Shelocta-Skidmore complex, 2 to 6 percent slopesSmB2765550322lgnbky13519981:20000
Shelocta gravelly silt loam, 6 to 12 percent slopesShC2219550319lgn7ky13519981:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesShD994550320lgn8ky13519981:20000
Shelocta gravelly silt loam, 12 to 25 percent slopesSlD152013979151hxn1ky15119681:20000
Shelocta-Berks complex, 20 to 60 percent slopesSlF5140550543lgwgky17319831:20000
Lenberg-Shelocta complex, 20 to 50 percent slopes, erodedLnF5033550528lgvzky17319831:20000
Trappist-Colyer-Shelocta complex, 12 to 30 percent slopes, erodedTsE2200550548lgwmky17319831:20000
Bledsoe-Shelocta complex, 12 to 35 percent slopesBlE859550510lgvdky17319831:20000
Latham-Shelocta-Rock outcrop complex, 20 to 60 percent slopesLaF833550525lgvwky17319831:20000
Shelocta silt loam, 6 to 15 percent slopesShC317550542lgwfky17319831:20000
Handshoe-Fedscreek-Shelocta complex, 30 to 80 percent slopes, very stonyuHfsF6539430256972x5j1ky19519861:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF5107031584492x5jgky19519861:24000
Shelocta-Muse complex, 15 to 50 percent slopes, very stonySmE1856550050lgckky19519861:24000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1841929970762qyt0ky19919691:12000
Muse-Shelocta complex, 30 to 50 percent slopesMuF16317552439ljvmky19919691:12000
Shelocta-Jefferson complex, 20 to 30 percent slopesShE14206552455ljw4ky19919691:12000
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF1118829970792qytdky19919691:12000
Muse-Shelocta complex, 20 to 30 percent slopesMuE4690552437ljvkky19919691:12000
Shelocta-Jefferson complex, 12 to 20 percent slopesShD2709552454ljw3ky19919691:12000
Muse-Shelocta complex, 20 to 30 percent slopes, severely erodedMuE31046552438ljvlky19919691:12000
Muse-Shelocta complex, 12 to 20 percent slopesMuD706552436ljvjky19919691:12000
Shelocta gravelly silt loam, 12 to 20 percent slopesSgD244552453ljw2ky19919691:12000
Shelocta channery silt loam, 6 to 12 percent slopesSgC1155524522w8j0ky19919691:12000
Rigley-Shelocta-Muse complex, steepRMF47145550083lgdmky23119851:20000
Latham-Shelocta silt loams, 30 to 50 percent slopesLsF117038550403lgqyky60519751:20000
Latham-Shelocta silt loams, 20 to 30 percent slopesLsE15674550402lgqxky60519751:20000
Shelocta gravelly silt loam, 2 to 6 percent slopesScB3883550419lgrgky60519751:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesScD2437550421lgrjky60519751:20000
Shelocta gravelly silt loam, 6 to 12 percent slopesScC2014550420lgrhky60519751:20000
Shelocta silt loam, 6 to 12 percent slopesShC430549422lfq9ky61519711:20000
Shelocta silt loam, 12 to 25 percent slopesShD294549423lfqbky61519711:20000
Shelocta-Gilpin complex, 20 to 65 percent slopes, stonySgF891545577992qyt7ky61620041:24000
Gilpin-Shelocta complex, 20 to 35 percent slopesGsE94645577662qytjky61620041:24000
Shelocta silt loam, 4 to 12 percent slopesSeC1887557797lqfgky61620041:24000
Shelocta silt loam, 12 to 20 percent slopesSeD1293557798lqfhky61620041:24000
Garmon-Shelocta complex, 25 to 60 percent slopesGaF27499552561ljzkky62019791:20000
Shelocta-Lenberg complex, 12 to 30 percent slopesSlD7441552580lk05ky62019791:20000
Shelocta silt loam, 6 to 12 percent slopesShC2250552579lk04ky62019791:20000
Shelocta silt loam, 2 to 6 percent slopesShB341552578lk03ky62019791:20000
Shelocta-Gilpin complex, 20 to 65 percent slopes, stonySgF1817375507172qyt7ky62319851:20000
Shelocta-Cutshin-Gilpin complex, 20 to 75 percent slopes, very stonyScF225665507162tqhbky62319851:20000
Shelocta and Caneyville soils and rock outcrop, steepSaE3172550715lh20ky62319851:20000
Shelocta-Highsplint-Gilpin complex, 20 to 70 percent slopes, very stonyuShgF7237430987162x5k0ky62619971:24000
Handshoe-Fedscreek-Shelocta complex, 30 to 80 percent slopes, very stonyuHfsF5864730987142x5j1ky62619971:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF463195507262x5jgky62619971:24000
Highsplint-Shelocta-Muse complex, 30 to 80 percent slopes, extremely stonyHtF1989550739lh2sky62619971:24000
Highsplint-Shelocta-Dekalb complex, 35 to 80 percent slopes, very stonyHsF1935550738lh2rky62619971:24000
Gilpin-Shelocta complex, 12 to 25 percent slopesGlD979550732lh2kky62619971:24000
Shelocta-Muse complex, 15 to 50 percent slopes, very stonySmF231550747lh31ky62619971:24000
Shelocta-Latham complex, 30 to 60 percent slopes, stonySLF1867805522302w8hzky62719841:20000
Shelocta-Latham silt loams, 20 to 30 percent slopesSLE15861552229ljmvky62719841:20000
Shelocta channery silt loam, 6 to 12 percent slopesShC85455522332w8j0ky62719841:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesShD4381552234ljn0ky62719841:20000
Shelocta gravelly silt loam, 2 to 6 percent slopesShB1325552232ljmyky62719841:20000
Bledsoe-Shelocta-Rock outcrop complex, 15 to 90 percent slopesBEF791552211ljm8ky62719841:20000
Steinsburg-Shelocta-Rock outcrop complex, 35 to 80 percent slopesSSF745552231ljmxky62719841:20000
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF5290529970802qytdky62819731:20000
Shelocta-Latham complex, 30 to 60 percent slopes, stonySdF514205522942w8hzky62819731:20000
Shelocta-Latham silt loams, 20 to 30 percent slopes complexSdE44053552293ljpxky62819731:20000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1976129970772qyt0ky62819731:20000
Shelocta-Rigley complex, 20 to 30 percent slopesSgE8677552295ljpzky62819731:20000
Caneyville-Shelocta rocky silt loams, 20 to 30 percent slopesCdE7692552257ljnrky62819731:20000
Shelocta gravelly silt loam, 20 to 30 percent slopesSbE5409552290ljptky62819731:20000
Shelocta-Latham silt loams, 12 to 20 percent slopesSdD3647552292ljpwky62819731:20000
Shelocta gravelly silt loam, 12 to 20 percent slopesSbD2688552289ljpsky62819731:20000
Shelocta channery silt loam, 6 to 12 percent slopesSbC10355522882w8j0ky62819731:20000
Caneyville-Shelocta rocky silt loams, 6 to 20 percent slopesCdD1011552256ljnqky62819731:20000
Shelocta-Highsplint-Sequoia complex, 30 to 80 percent slopes, rocky11F101156612216nk1xky63019661:15840
Shelocta-Sequoia complex, 20 to 35 percent slopes, rocky22E65656609622ngc7ky63019661:15840
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF3214429970812qytdky63019661:15840
Shelocta-Bouldin complex, 30 to 75 percent slopes, extremely stony, very rocky14F28888735551spdgky63019661:15840
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF2404029970782qyt0ky63019661:15840
Shelocta-Lily complex, 20 to 35 percent slopes, rocky2E9185609706ngfyky63019661:15840
Shelocta channery silt loam, 8 to 20 percent slopes22D213609557ng94ky63019661:15840
Shelocta-Cutshin-Gilpin complex, 20 to 75 percent slopes, very stonySCF1341335521462tqhbky63319791:24000
Shelocta-Highsplint-Gilpin complex, 20 to 70 percent slopes, very stonyuShgF11491830987152x5k0ky63319791:24000
Shelocta-Gilpin complex, 20 to 65 percent slopes, stonySaF695305508502qyt7ky63419891:20000
Gilpin-Shelocta complex, 20 to 35 percent slopesGpE55695508292qytjky63419891:20000
Shelocta-Kimper-Cloverlick complex, 20 to 80 percent slopes, very stonySkF750515521332qytpky63819891:24000
Shelocta-Highsplint-Gilpin complex, 20 to 70 percent slopes, very stonyShF736615521322x5k0ky63819891:24000
Shelocta-Kimper-Cutshin complex, 20 to 55 percent slopes, very stonySmF36762552134ljjsky63819891:24000
Shelocta-Gilpin silt loams, 20 to 35 percent slopesSgE7935552131ljjpky63819891:24000
Gilpin-Shelocta silt loams, 12 to 20 percent slopesGsD5128552118ljj8ky63819891:24000
Shelocta gravelly silt loam, 2 to 6 percent slopesSeB510552129ljjmky63819891:24000
Gilpin-Shelocta silt loams, 3 to 12 percent slopesGsC460552117ljj7ky63819891:24000
Shelocta channery silt loam, 6 to 12 percent slopesSeC4275521302w8j0ky63819891:24000
Handshoe-Fedscreek-Shelocta complex, 30 to 80 percent slopes, very stonyuHfsF9260630257012x5j1ky63919911:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF577865508792x5jgky63919911:24000
Shelocta-Handshoe-Fedscreek complex, 30 to 60 percent slopes, stonyuShfF4108430987072xnk5ky63919911:24000
Shelocta-Grigsby-Stokly complex, 2 to 15 percent slopesShC11774550881lh7cky63919911:24000
Potomac-Shelocta-Grigsby complex, 2 to 15 percent slopesPsC4387550876lh76ky63919911:24000
Fedscreek-Shelocta complex, 20 to 50 percent slopesFsF2258550865lh6vky63919911:24000
Shelocta loam, 6 to 15 percent slopesSeC1066550880lh7bky63919911:24000
Shelocta-Handshoe-Fedscreek complex, 30 to 60 percent slopes, stonyuShfF7641730987082xnk5ky64019961:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF513755508932x5jgky64019961:24000
Handshoe-Fedscreek-Shelocta complex, 30 to 80 percent slopes, very stonyuHfsF4116330257022x5j1ky64019961:24000
Shelocta-Grigsby-Orrville complex, 2 to 15 percent slopesSgC11633550914lh8fky64019961:24000
Shelocta silt loam, 12 to 30 percent slopesSeE2577550913lh8dky64019961:24000
Shelocta-Handshoe-Fedscreek complex, 30 to 60 percent slopes, stonyuShfF14258230987092xnk5ky64119941:24000
Shelocta-Gilpin complex, 20 to 65 percent slopes, stonySlF628745509592qyt7ky64119941:24000
Latham-Shelocta-Gilpin complex, 12 to 30 percent slopesLsE22735550944lh9dky64119941:24000
Cloverlick-Shelocta-Kimper complex, 20 to 80 percent slopes, very stonyuCskF561231584532x5jgky64119941:24000
Shelocta silt loam, 12 to 20 percent slopesShD1166550958lh9vky64119941:24000
Shelocta silt loam, 6 to 12 percent slopesShC825550957lh9tky64119941:24000
Latham-Shelocta silt loams, 20 to 30 percent slopesLsE2714214787981lmt5ky64519711:20000
Latham-Shelocta silt loams, 30 to 50 percent slopesLsF2126114787991lmt6ky64519711:20000
Latham-Shelocta silt loams, 12 to 20 percent slopesLsD350014787971lmt4ky64519711:20000
Shelocta-Latham-Gilpin complex, 20 to 30 percent slopesSgE35523792262kvs7ky64820091:12000
Shelocta-Latham-Gilpin complex, 12 to 20 percent slopes, erodedSgD211323792242kvs5ky64820091:12000
Shelocta-Latham-Gilpin complex, 20 to 30 percent slopesSgE10636324529092nbg3ky70919951:20000
Shelocta-Latham-Gilpin complex, 12 to 20 percent slopes, erodedSgD23022224529072nbg1ky70919951:20000
Shelocta-Latham-Gilpin complex, 12 to 20 percent slopes, severely erodedSgD329824529082nbg2ky70919951:20000
Shelocta-Muse-Colyer association, steepSoE335901701225q0toh00119871:15840
Shelocta-Berks association, very steepShF329771701205q0roh00119871:15840
Shelocta-Muse association, hillySmD108671701215q0soh00119871:15840
Shelocta-Berks association, steepShE56291701195q0qoh00119871:15840
Shelocta-Brownsville association, very steepSkF479618958862t330oh00119871:15840
Trappist-Shelocta association, steepTsF56189588021mtfoh00119871:15840
Shelocta-Brownsville association, steepSkE3718958852t327oh00119871:15840
Shelocta-Berks complex, 25 to 40 percent slopesSeE79621723062wdq7oh04519981:12000
Shelocta silt loam, 15 to 25 percent slopesSdD25361723052wdp8oh04519981:12000
Shelocta-Cruze complex, 15 to 25 percent slopesSfD7991723075s99oh04519981:12000
Shelocta-Cruze complex, 25 to 40 percent slopesSfE1381723085s9boh04519981:12000
Trappist-Shelocta association, steepTwE65214206961jpbxoh07119731:15840
Shelocta-Berks association, very steepSeF30814206791jpbcoh07119731:15840
Shelocta-Cruze-Weikert association, steepSgE7714205621jp6loh07119731:15840
Shelocta-Muse-Colyer association, steepSfE2314206801jpbdoh07119731:15840
Shelocta-Berks association, steepSeE1514206781jpbboh07119731:15840
Dekalb-Shelocta-Rock outcrop complex, 40 to 70 percent slopesDkF3123513980702xb26oh07319861:15840
Shelocta-Berks complex, 25 to 40 percent slopesSbE3063513980962wdq7oh07319861:15840
Shelocta-Cruze silt loams, 25 to 40 percent slopesScE1861513980981hxtyoh07319861:15840
Shelocta-Cruze silt loams, 15 to 25 percent slopesScD1690613980971hxtxoh07319861:15840
Shelocta silt loam, 15 to 25 percent slopesSaD930913980952wdp8oh07319861:15840
Shelocta silt loam, 8 to 15 percent slopesSaC921613980942wdp7oh07319861:15840
Shelocta-Cruze silt loams, 40 to 70 percent slopesScF307013980991hxtzoh07319861:15840
Shelocta-Brownsville association, very steepSdF85513981911hxxyoh07319861:15840
Shelocta-Latham association, steepShLZE11929324510672n8jpoh07919811:15840
Brownsville-Shelocta association, steepBsF101825360112z525oh07919811:15840
Shelocta-Rarden association, steepShRZE1287524510552n8j9oh07919811:15840
Shelocta-Wharton-Latham association, steepSWLZE1167124510532n8j7oh07919811:15840
Shelocta-Brownsville association, very steepSbF149514605011l0ryoh07919811:15840
Shelocta-Brownsville association, steepSbE144514605391l0t5oh07919811:15840
Shelocta-Steinsburg association, very steepSeF36814605401l0t6oh07919811:15840
Steinsburg-Shelocta association, very steepSsF63100536184kzy8oh08719891:15840
Shelocta-Latham association, steepShLZE11340024511152n8l7oh08719891:15840
Shelocta-Wharton-Latham association, steepSWLZE1185024511162n8l8oh08719891:15840
Shelocta silt loam, 2 to 6 percent slopesSbB613536177kzy1oh08719891:15840
Shelocta silt loam, 15 to 25 percent slopesSbD4645361792wdp8oh08719891:15840
Shelocta silt loam, 6 to 15 percent slopesSbC194536178kzy2oh08719891:15840
Shelocta silt loam, 3 to 8 percent slopesSgB6114550942wdp6oh08719891:15840
Shelocta silt loam, 8 to 15 percent slopesSgC514550952wdp7oh08719891:15840
Shelocta-Cruze complex, 25 to 40 percent slopesSfE26699500rgwjoh12719841:15840
Shelocta-Cruze complex, 15 to 25 percent slopesSfD1699499rgwhoh12719841:15840
Shelocta-Brownsville association, steepSnF811255377232t327oh13119841:15840
Trappist-Shelocta association, steepTsF18045537739l1kfoh13119841:15840
Shelocta-Latham association, steepSpF17294537725l1jzoh13119841:15840
Shelocta-Rigley association, steepSoF9719537724l1jyoh13119841:15840
Shelocta-Cruze-Weikert association, steepSgE82816890171tpkfoh13119841:15840
Shelocta silt loam, 15 to 25 percent slopesShD5755377222wdp8oh13119841:15840
Shelocta-Wharton-Latham association, steepSWLZE147624626992nnmxoh13119841:15840
Shelocta-Brownsville association, very steepSlF18916890162t330oh13119841:15840
Shelocta-Cruze-Weikert association, steepShE339701709605qwvoh14119971:15840
Shelocta-Brownsville association, very steepSgF219151709592t330oh14119971:15840
Shelocta-Rigley association, steepSkE10721709615qwwoh14119971:15840
Shelocta silt loam, 12 to 20 percent slopesSfD7961709585qwsoh14119971:15840
Shelocta-Brownsville association, very steepScF115340537312l13noh14519841:15840
Shelocta-Wharton-Latham association, steepSWLZE17063524800482p7pkoh14519841:15840
Shelocta-Brownsville association, steepScE19830537311l13moh14519841:15840
Shelocta-Steinsburg association, very steepSeF12526537313l13poh14519841:15840
Shelocta silt loam, 3 to 8 percent slopesSbB108805373082wdp6oh14519841:15840
Steinsburg-Shelocta association, very steepSsF368114608141l131oh14519841:15840
Latham-Brownsville-Shelocta association, steepLBSZE1360524526642nb66oh14519841:15840
Shelocta silt loam, 15 to 25 percent slopesSbD35845373102wdp8oh14519841:15840
Shelocta silt loam, 8 to 15 percent slopesSbC21195373092wdp7oh14519841:15840
Shelocta-Muse-Colyer association, steepSmE93914608241l13coh14519841:15840
Shelocta-Brownsville association, very steepSdF33338536427l063oh16319981:15840
Dekalb-Shelocta-Rock outcrop complex, 40 to 70 percent slopesDkF184814818462xb26oh16319981:15840
Shelocta-Cruze silt loams, 15 to 25 percent slopesScD89114818501lqzmoh16319981:15840
Shelocta-Rarden association, steepShRZE182624535912nc53oh16319981:15840
Shelocta-Berks complex, 25 to 40 percent slopesSfE50214818492wdq7oh16319981:15840
Shelocta silt loam, 8 to 15 percent slopesSaC23414818472wdp7oh16319981:15840
Shelocta-Cruze silt loams, 25 to 40 percent slopesScE20614818511lqznoh16319981:15840
Shelocta-Latham association, steepShLZE13724533762nby5oh16319981:15840
Shelocta silt loam, 15 to 25 percent slopesSaD1214818482wdp8oh16319981:15840
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF438824238392mc6cpa00520121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF114724224942m9szpa00520121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF204224287562mj9zpa03120121:24000
Shelocta silt loam, 8 to 15 percent slopesShC10724094482lw74pa03120121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF9824252982mdqfpa03120121:24000
Shelocta silt loam, 3 to 8 percent slopesShB6624094472lw73pa03120121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF934815910361qdlrpa05120051:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF249915911551qdqlpa05120051:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF721117209421vrs8pa06320121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF334223938212lbz1pa06320121:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF249723990122ljchpa06520121:12000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF95223990112ljcgpa06520121:12000
Shelocta silt loam, 3 to 8 percent slopesShB17024099852lwsgpa06520121:12000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopesShF32366544633l8qtpa12920031:24000
Shelocta-Gilpin channery silt loams, 25 to 75 percent slopes, very stonySxF1523581198mhsbpa12920031:24000
Shelocta silt loam, 20 to 35 percent slopesSoE87526483knvbtn01920001:24000
Jefferson-Shelocta complex, 20 to 45 percent slopesJsF232245238782wmkktn03519981:24000
Jefferson-Varilla-Shelocta complex, 20 to 60 percent slopes, very stonyJvF196145238802wmk8tn03519981:24000
Varilla-Shelocta complex, 15 to 30 percent slopes, very rockyVsE4292523903kl53tn03519981:24000
Jefferson-Shelocta complex, 10 to 20 percent slopesJsD38485238772wmkhtn03519981:24000
Jefferson-Varilla-Shelocta complex, 10 to 20 percent slopes, very stonyJvD569523879kl4btn03519981:24000
Shelocta silt loam, 12 to 20 percent slopesScD3155526556knxptn09120001:24000
Shelocta silt loam, 20 to 35 percent slopesScE2592526557knxqtn09120001:24000
Shelocta silt loam, 5 to 12 percent slopesScC2432526555knxntn09120001:24000
Shelocta silt loam, 35 to 50 percent slopesScF733526558knxrtn09120001:24000
Shelocta silt loam, 3 to 12 percent slopesShC1659527932kqc2tn12319741:20000
Shelocta silt loam, 12 to 25 percent slopesShD1281527933kqc3tn12319741:20000
Gilpin-Shelocta complex, 40 to 70 percent slopesGsF19387843394x9m8tn13320031:24000
Shelocta-Pineville complex, 20 to 70 percent slopes, very stonySpF322843399x9mftn13320031:24000
Jefferson-Varilla-Shelocta complex, 20 to 60 percent slopes, very stonyJvF37287288632wmk8tn14320031:24000

Map of Series Extent

Approximate geographic distribution of the SHELOCTA 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 .