Official Series Description


Lab Data Summary

Aggregate lab data for the RAYNE soil series. This aggregation is based on all pedons with a current taxon name of RAYNE, 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 RAYNE 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
12407N0397S2005PA031009Rayne6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2270317,-79.5863953
12408N0304S2007PA063234Rayne6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8182373,-79.1518402
12665PA0030031965PA003003Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5591667,-79.9930556
12672PA1250461972PA125046Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.2538889,-80.4908333
12771PA1110011971PA111001Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0486111,-79.0619444
12771PA1110021971PA111002Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0241667,-79.11
12771PA1110031971PA111003Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.995,-79.1805556
12772PA1290211972PA129021Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1666667,-79.2738889
12773PA0330121973PA033012Rayne5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1863889,-78.5491667
12773PA0330131973PA033013Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1813889,-78.5313889
n/aCS-0221965-OH031-022Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aBT-0041974-OH013-004Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0091978-OH079-009Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMS-0221982-OH119-022Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a94KY-237-UK194KY-237-UK1Rayne4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RAYNE 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 RAYNE 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 RAYNE 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 RAYNE 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 RAYNE 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 RAYNE 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 RAYNE 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 RAYNE, 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-2010-09-03-11 | 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).

  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-2010-09-03-14 | 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).

  4. 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).

  5. 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).

  6. 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).

  7. 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).

  8. 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).

  9. 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).

  10. 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).

  11. 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).

  12. KY-2012-01-31-15 | Jackson and Owsley Counties - April 1989

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

  13. NY-2012-02-15-44 | Seneca Nation of Indians - August 1984

    Typical relationship of soils to parent material in the Allegheny River Valley (Soil Survey of Seneca Nation of Indians, New York; August 1984).

  14. PA-2012-03-12-03 | Allegheny County - August 1981

    The pattern of soils and underlying material in the Gilpin--Wharton-Upshur soil association (Soil Survey of Allegheny County, PA; 1981).

  15. PA-2012-03-13-02 | Cambria County - September 1985

    Typical pattern of soils and parent material in the Gilpin-Ernest-Wharton association (Soil Survey of Cambria County, PA; 1985).

  16. PA-2012-03-13-08 | Centre County - August 1981

    Typical pattern of soils and underlying material in association 2 (Soil Survey of Centre County, PA; 1981).

  17. PA-2012-03-13-12 | Clearfield County - August 1988

    Typical pattern of soils and underlying material in the Rayne-Gilpin-Ernest association (Soil Survey of Clearfield County, PA; 1988).

  18. PA-2012-03-13-15 | Clearfield County - August 1988

    Typical pattern of soils and underlying material in the Udorthents-Gilpin-Rayne association (Soil Survey of Clearfield County, PA; 1988).

  19. PA-2012-03-14-12 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Rayne-Gilpin-Wharton-Cavode soils (Soil Survey of Somerset County, PA; 1983).

  20. PA-2012-03-14-13 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Hazleton-Cookport soils (Soil Survey of Somerset County, PA; 1983).

  21. PA-2012-03-14-14 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Berks-Weikert soils (Soil Survey of Somerset County, PA; 1983).

  22. PA-2012-03-14-16 | Somerset County - December 1983

    Typical pattern of soils and underlying material in area of Ernest-Rayne-Gilpin soils (Soil Survey of Somerset County, PA; 1983).

  23. WV-2010-11-08-08 | Lincoln County - 2007

    Typical pattern of soils and parent material in an area of the Rayne-Gilpin-Matewan general soil map unit (Soil Survey of Lincoln County, West Virginia; 2007).

Map Units

Map units containing RAYNE 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
Gilpin-Rayne-Sequoia complex, 25 to 55 percent slopes, very stonyGsF691855525252tqhjky05119941:24000
Rayne-Gilpin complex, 4 to 12 percent slopesRgC5361557793lqfbky61620041:24000
Gilpin-Rayne-Sequoia complex, 12 to 25 percent slopesGrD3220557765lqdfky61620041:24000
Gilpin-Rayne-Sequoia silt loams, 12 to 25 percent slopesGrD18782550706lh1qky62319851:20000
Gilpin-Rayne silt loams, 2 to 6 percent slopesGpB7100550705lh1pky62319851:20000
Dekalb-Gilpin-Rayne complex, 25 to 65 percent slopes, very rockyDrF39070550729lh2gky62619971:24000
Gilpin-Rayne-Sequoia complex, 25 to 55 percent slopes, very stonyGtF498255521192tqhjky63819891:24000
Rayne-Gilpin complex, 6 to 15 percent slopesRaC576550877lh77ky63919911:24000
Rayne-Marrowbone-Dekalb complex, 20 to 80 percent slopes, very rockyRaF48755550911lh8bky64019961:24000
Rayne-Gilpin complex, 4 to 12 percent slopesRgC860550952lh9nky64119941:24000
Rayne silt loam, 15 to 25 percent slopes, extremely stonyReD416624012362llp7md00120091:12000
Rayne silt loam, 8 to 15 percent slopes, extremely stonyReC97324012352llp6md00120091:12000
Rayne silt loam, 15 to 25 percent slopesRaD56524012342llp5md00120091:12000
Rayne silt loam, 25 to 45 percent slopes, extremely stonyReE53424012372llp8md00120091:12000
Rayne silt loam, 8 to 15 percent slopesRaC29724012332llp4md00120091:12000
Rayne-Urban land complex, 8 to 15 percent slopesRnC15024010472llh4md00120091:12000
Rayne silt loam, 3 to 8 percent slopesRaB8724012322llp3md00120091:12000
Rayne channery silt loam, 25 to 35 percent slopes497E302299899b225ny00320131:24000
Rayne channery silt loam, 15 to 25 percent slopes497D82299898b224ny00320131:24000
Rayne channery silt loam, 25 to 35 percent slopes497E143712896209qclny00920021:24000
Rayne channery silt loam, 15 to 25 percent slopes497D27622896199qckny00920021:24000
Rayne channery silt loam, 35 to 50 percent slopes497F11132896219qcmny00920021:24000
Rayne channery silt loam, 25 to 35 percent slopes, extremely bouldery498E7502896229qcnny00920021:24000
Rayne channery silt loam, 25 to 35 percent slopesRaE23372893159q1rny60519811:24000
Rayne channery silt loam, 35 to 65 percent slopesRaF14402893169q1sny60519811:24000
Rayne channery silt loam, 15 to 25 percent slopesRaD10252893149q1qny60519811:24000
Rayne channery silt loam, 8 to 15 percent slopesRaC1712893139q1pny60519811:24000
Rayne extremely bouldery silt loam, 25 to 35 percent slopesRbE1372893199q1wny60519811:24000
Rayne extremely bouldery silt loam, 35 to 65 percent slopesRbF1262893209q1xny60519811:24000
Rayne extremely bouldery silt loam, 15 to 25 percent slopesRbD1122893189q1vny60519811:24000
Rayne channery silt loam, 3 to 8 percent slopesRaB542893129q1nny60519811:24000
Rayne extremely bouldery silt loam, 8 to 15 percent slopesRbC182893179q1tny60519811:24000
Rayne silt loam, Conemaugh geology, 8 to 15 percent slopesRycC1059331752962z38xpa00319731:15840
Rayne silt loam, Conemaugh geology, 3 to 8 percent slopesRycB646131752952z38wpa00319731:15840
Rayne silt loam, 2 to 8 percent slopesRyB100541717l5prpa00319731:15840
Rayne silt loam, 8 to 15 percent slopesRyC48541718l5pspa00319731:15840
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRnC1642224238382mc6bpa00520121:24000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRnB782324238372mc69pa00520121:24000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRnD234224238362mc68pa00520121:24000
Rayne-Gilpin channery silt loams, 8 to 25 percent slopes, very stonyRsD106624224952m9t0pa00520121:24000
Rayne silt loam, Conemaugh geology, 8 to 15 percent slopesRycC1312031752982z38xpa00719781:15840
Rayne silt loam, Conemaugh geology, 3 to 8 percent slopesRycB796931752972z38wpa00719781:15840
Rayne-Gilpin channery silt loams, 25 to 65 percent slopesRgF1197541880l5w0pa00919891:24000
Rayne-Gilpin very stony silt loams, 8 to 25 percent slopesRpD59541882l5w2pa00919891:24000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRgD42541879l5vzpa00919891:24000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRgC36541878l5vypa00919891:24000
Rayne channery silt loam, 15 to 25 percent slopesReD2628716072ps13pa00919891:24000
Rayne channery silt loam, 3 to 8 percent slopesReB2428716062ps11pa00919891:24000
Rayne-Gilpin very stony silt loams, 3 to 8 percent slopesRpB8541881l5w1pa00919891:24000
Rayne silt loam, Conemaugh geology, 3 to 8 percent slopesRycB175831752992z38wpa01919841:15840
Rayne silt loam, Conemaugh geology, 8 to 15 percent slopesRycC81731753002z38xpa01919841:15840
Gilpin-Rayne silt loams, 8 to 15 percent slopesGtC11372541914l5x3pa02119781:20000
Gilpin-Rayne silt loams, 15 to 25 percent slopesGtD5358541915l5x4pa02119781:20000
Rayne silt loam, 15 to 25 percent slopesRaD804541937l5xvpa02119781:20000
Rayne silt loam, 3 to 8 percent slopesRaB437541935l5xspa02119781:20000
Rayne silt loam, 8 to 15 percent slopesRaC313541936l5xtpa02119781:20000
Rayne silt loam, 2 to 10 percent slopesRaB503538345l25zpa02719751:20000
Rayne-Gilpin channery silt loams, 8 to 25 percent slopes, very stonyRsD2211524754km1kpa03120121:24000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRnB1346529763ks84pa03120121:24000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRnC589529764ks85pa03120121:24000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRnD209529765ks86pa03120121:24000
Rayne-Gilpin channery silt loams, 0 to 8 percent slopes, very stonyRsB108557475lq32pa03120121:24000
Rayne channery silt loam, 25 to 65 percent slopesRbF64809538550l2dlpa03319811:20000
Rayne-Gilpin complex, 15 to 25 percent slopesRcD45647538551l2dmpa03319811:20000
Rayne silt loam, 3 to 8 percent slopesRaB4382538548l2djpa03319811:20000
Rayne silt loam, 8 to 15 percent slopesRaC2390538549l2dkpa03319811:20000
Rayne channery silt loam, 8 to 25 percent slopes, very stonyRgD544015911541qdqkpa05120051:24000
Rayne channery silt loam, 0 to 8 percent slopes, very stonyRgB166515911531qdqjpa05120051:24000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRnB25515910881qdnfpa05120051:24000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRnD15215910901qdnhpa05120051:24000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRnC10615910891qdngpa05120051:24000
Rayne channery silt loam, 3 to 8 percent slopesReB25328716162ps11pa06119741:20000
Rayne-Gilpin channery silt loams, 25 to 65 percent slopesRgF1672871620l5w0pa06119741:20000
Rayne channery silt loam, 8 to 15 percent slopesReC10828716172ps12pa06119741:20000
Rayne channery silt loam, 15 to 25 percent slopesReD7428716182ps13pa06119741:20000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRnC1260417209101vrr7pa06320121:24000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRnD747723938902lc18pa06320121:24000
Rayne-Gilpin channery silt loams, 8 to 25 percent slopes, very stonyRsD507217209561vrsqpa06320121:24000
Rayne-Gilpin channery silt loams, 0 to 8 percent slopes, very stonyRsB118917209551vrsppa06320121:24000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRnB35317209091vrr6pa06320121:24000
Rayne-Gilpin channery silt loams, 8 to 25 percent slopes, very stonyRsD784423990092ljcdpa06520121:12000
Rayne-Gilpin channery silt loams, 0 to 8 percent slopes, very stonyRsB290323990082ljccpa06520121:12000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRnB151623990052ljc8pa06520121:12000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRnD67623990072ljcbpa06520121:12000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRnC33423990062ljc9pa06520121:12000
Rayne silt loam, Conemaugh geology, 8 to 15 percent slopesRycC14831753022z38xpa07319781:15840
Rayne silt loam, Conemaugh geology, 3 to 8 percent slopesRycB7631753012z38wpa07319781:15840
Rayne-Gilpin channery silt loams, 25 to 65 percent slopesRgF45005542114l63kpa11119771:20000
Rayne-Gilpin channery silt loams, 8 to 15 percent slopesRgC40727542112l63hpa11119771:20000
Rayne-Gilpin very stony silt loams, 8 to 25 percent slopesRpD34298542116l63mpa11119771:20000
Rayne-Gilpin channery silt loams, 3 to 8 percent slopesRgB33744542111l63gpa11119771:20000
Rayne-Gilpin channery silt loams, 15 to 25 percent slopesRgD24509542113l63jpa11119771:20000
Rayne-Gilpin very stony silt loams, 3 to 8 percent slopesRpB11852542115l63lpa11119771:20000
Rayne channery silt loam, 8 to 25 percent slopes, very stonyRgD10421544601l8pspa12920031:24000
Rayne channery silt loam, 0 to 8 percent slopes, very stonyRgB4217544581l8p4pa12920031:24000
Berks-Lowell-Rayne complex, 25 to 65 percent slopes3E31501517116kc35va12119801:15840
Berks-Lowell-Rayne complex, 15 to 25 percent slopes3D7973517115kc34va12119801:15840
Rayne-Berks-Groseclose complex, 30 to 60 percent slopes28F14588521277khfdva15519811:15840
Leck Kill-Rayne silt loams, 15 to 30 percent slopes15D2302521248khdgva15519811:15840
Rayne silt loam, 15 to 30 percent slopes27D2257521275khfbva15519811:15840
Leck Kill-Rayne silt loams, 7 to 15 percent slopes15C1852521247khdfva15519811:15840
Rayne silt loam, 7 to 15 percent slopes27C1832521274khf9va15519811:15840
Rayne silt loam, 30 to 45 percent slopes27E1420521276khfcva15519811:15840
Rayne-Berks complex, 35 to 60 percent slopes23E2792518933kdzsva19719881:15840
Rayne-Berks complex, 15 to 35 percent slopes23D1903518932kdzrva19719881:15840
Rayne-Berks complex, 7 to 15 percent slopes23C1714518931kdzqva19719881:15840
Rayne-Matewan complex, 35 to 65 percent slopes, very stonyRmF66376557377lpzxwv04320051:24000
Rayne silt loam, 3 to 8 percent slopesRaB5418186811720pxvwv07719551:24000
Rayne silt loam, 8 to 15 percent slopesRaC953186811920pxxwv07719551:24000
Rayne silt loam, 8 to 15 percent slopes, severely erodedRaC3176186812020pxywv07719551:24000
Rayne silt loam, 3 to 8 percent slopes, severely erodedRaB3126186811820pxwwv07719551:24000
Rayne silt loam, 3 to 8 percent slopesRaB374515825k9rjwv61019731:20000
Rayne silt loam, 8 to 15 percent slopesRaC139515826k9rkwv61019731:20000

Map of Series Extent

Approximate geographic distribution of the RAYNE 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 .