Official Series Description


Lab Data Summary

Aggregate lab data for the SAFFELL soil series. This aggregation is based on all pedons with a current taxon name of SAFFELL, 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 SAFFELL 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
11903N0740S98AR109002Saffell6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.1472206,-93.7877808
12286KY-139-01286KY-139-012Saffell4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0492439,-88.2544785
12207N0465S2007-TN-161-4Saffell7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6379738,-88.0026932
133AS89AL-131-11989AL131001Saffell3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.975,-87.4038889
135B03N0739S2001AR061002Saffell6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0063896,-93.9422226
135B03N0743S2001AR133002Saffell6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.875,-94.1666641
n/a86KY-139-00786KY-139-007Saffell4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SAFFELL 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 SAFFELL 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 SAFFELL 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 SAFFELL series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with SAFFELL 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 SAFFELL 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 SAFFELL 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 SAFFELL, 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. AL-2012-04-25-05 | Franklin County - March 1965

    Typical cross section of Franklin County showing some of the soils in relation to topographic position and main geological formations (Soil Survey of Franklin County, Alabama; March 1965).

  2. AR-2012-05-08-03 | Bradley County - April 1961

    General soil areas (Soil Survey of Bradley County, Arkansas; April 1961).

  3. KY-2012-01-27-14 | Carlisle and Hickman Counties - July 1997

    Relationship of soils to topography and underlying material in the Loring-Memphis general soil map unit in Carlisle and Hickman Counties (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

  4. KY-2012-02-01-05 | Livingston County - September 1993

    Relationship of soils to topography and underlying material in the Loring-Brandon-Saffell general soil map unit (Soil Survey of Livingston County, Kentucky; September 1993).

  5. MS-2012-02-06-06 | Carroll County - May 1990

    Pattern of soils and underlying material in the Natchez-Memphis-Saffell general soil map unit (Soil Survey of Carroll County, Mississippi; May 1990).

  6. TN-2010-11-02-10 | Hickman County - 2008

    Typical pattern of soils and parent material in the Biffle-Lax general soil map unit (Soil Survey of Hickman County, Tennessee; 2008).

  7. TN-2012-03-16-06 | Dickson County - 2002

    The relationship of soils, landscape, and parent material in the Saffell-Lax and the Armour-Humphreys-Sullivan general soil map units (Soil Survey of Dickson County, TN; 2002).

  8. TN-2012-03-19-35 | Wayne County - 2000

    Typical pattern of soils and parent material in the Brandon-Saffell-Lax and Humprheys-Ennis-Lobelville general soil map units (Soil Survey of Wayne County, TN; 2000).

  9. TN-2012-03-19-36 | Wayne County - 2000

    Typical pattern of soils and parent material in the Saffell-Luverne-Silerton general soil map unit (Soil Survey of Wayne County, TN; 2000).

Map Units

Map units containing SAFFELL 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
Shubuta-Saffell complex, 10 to 30 percent slopesSsE3964328093c0dnal00119721:20000
Saffell gravelly fine sandy loam, 2 to 8 percent slopesSaC3956328092c0dmal00119721:20000
Saffell gravelly sandy loam, 5 to 15 percent slopesSaD57022336282dz8jal00720071:24000
Saffell very gravelly sandy loam, 6 to 10 percent slopesSaC171843285462y6xkal02119671:20000
Saffell gravelly sandy loam, 2 to 6 percent slopesSaB11500328545c0w7al02119671:20000
Saffell gravelly sandy loam, 10 to 15 percent slopesSaD4049328547c0w9al02119671:20000
Smithdale-Saffell complex, 15 to 45 percent slopesSsF10140600098n4g0al02520041:24000
Saffell-Pikeville complex, 15 to 45 percent slopesSaF59605328707c11gal03319861:20000
Troup-Gritney-Saffell complex, 8 to 15 percent slopesTgD33239328743c12mal03519851:20000
Oktibbeha-Saffell complex, 5 to 25 percent slopesOsE27479328737c12fal03519851:20000
Saffell gravelly fine sandy loam, 4 to 12 percent slopes502990329089c1fsal04719771:20000
Smithdale-Saffell-Luverne complex, gravelly, 8 to 40 percent slopesSnF2100232720362zkvral05119481:20000
Saffell gravelly fine sandy loam, 2 to 5 percent slopesSaB3232329364c1qnal05319691:20000
Saffell gravelly fine sandy loam, 5 to 12 percent slopesSaC2338329365c1qpal05319691:20000
Saffell very gravelly fine sandy loam, 6 to 15 percent slopesGnD7253294612xz8mal05719631:15840
Terrace escarpmentsTc180329522c1wral05719631:15840
Saffell very gravelly fine sandy loam, 6 to 15 percent slopesGuD2270273295982xz8mal05919621:15840
Saffell gravelly fine sandy loam, 2 to 6 percent slopesSaB1821329596c1z4al05919621:15840
Smithdale-Saffell complex, 15 to 35 percent slopesSvE125024948382psg7al07520101:24000
Saffell very gravelly fine sandy loam, 6 to 15 percent slopesSaD94624945602xz8mal07520101:24000
Saffell gravelly fine sandy loam, 2 to 6 percent slopesSaB15224945592psfyal07520101:24000
Saffell and Bodine soils, steepSBF46045523056kk8sal07719731:20000
Saffell gravelly fine sandy loam, 6 to 10 percent slopesSaC10629523057kk8tal07719731:20000
Saffell-Luverne complex, 15 to 35 percent slopesSaE515325146212qcvnal08520111:24000
Saffell gravelly sandy loam, 2 to 8 percent slopesSaC19425203122qkgnal08520111:24000
Saffell very gravelly fine sandy loam, 6 to 15 percent slopes2896003306302xz8mal09319761:20000
Saffell-Lucy (flomaton) complex, 15 to 35 percent slopesSgF1038743308572v5lpal09919841:20000
Saffell very gravelly sandy loam, 8 to 15 percent slopesSfD422003308562v5lqal09919841:20000
Saffell very gravelly sandy loam, 5 to 8 percent slopesSfC4500330855c38ral09919841:20000
Saffell gravelly sandy loam, 5 to 15 percent slopesSaD6500331250c3phal10519961:24000
Saffell-Maubila complex, 2 to 5 percent slopesSbB1580331251c3pjal10519961:24000
Saffell-Smithdale-Luverne complex, 8 to 35 percent slopesSaF36250331672c443al13119971:24000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes, moderately erodedSaC2145285651842ykhbar01119591:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopesSaC51035651832tztcar01119591:20000
Saffell gravelly fine sandy loam, sloping phaseSaD1460565186lz3tar01119591:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes, moderately erodedSaD210135651872ykh9ar01119591:20000
Saffell gravelly fine sandy loam, 12 to 25 percent slopesSaE431565188lz3war01119591:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes, severely erodedSaC34015651852ykh8ar01119591:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes641016531794002tztcar01919831:20000
Saffell-Sacul association, rolling6681473179402lyp0ar01919831:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes6521563179401lynzar01919831:20000
Brandon-Saffell association, moderately steep1821767564050lxy5ar02119751:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopesSaC78965653142tztcar02519651:15840
Saffell gravelly fine sandy loam, 8 to 25 percent slopesSaE26195653152ykh4ar02519651:15840
Brandon-Saffell association, moderately steep67010564151ly1far03119761:20000
Brandon-Saffell association, moderately sloping51570564150ly1dar03119761:20000
Saffell gravelly fine sandy loam, 8 to 20 percent slopesSfE1026565475lzf4ar04319721:24000
Saffell gravelly fine sandy loam, 3 to 8 percent slopesSfC8765654742tztcar04319721:24000
Saffell gravelly fine sandy loam, 1 to 8 percent slopes12C388717158952ykhfar05320061:24000
Saffell gravelly fine sandy loam, 15 to 35 percent slopes12E325917158971vljjar05320061:24000
Saffell gravelly fine sandy loam, 8 to 15 percent slopes12D138517158962ykh5ar05320061:24000
Brandon-Saffell complex, 15 to 35 percent slopes4E31007577956mddrar05519951:24000
Brandon-Saffell complex, 8 to 15 percent slopes4D4484577953mddnar05519951:24000
Brandon-Saffell complex, 3 to 8 percent slopes4C2627577955mddqar05519951:24000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes3845975656642tztcar05719761:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes3940005656652ykh6ar05719761:20000
Oktibbeha-Saffell association, rolling293632565654lzlxar05719761:20000
Saffell-Sacul association, rolling66241763179292lyp0ar05919831:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes641571831792902tztcar05919831:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes6539073179291lynzar05919831:20000
Saffell gravelly sandy loam, 3 to 8 percent slopesSeC19265565714lznvar06119701:24000
Saffell gravelly sandy loam, 8 to 20 percent slopesSeE14463565715lznwar06119701:24000
Saffell gravelly sandy loam, 1 to 3 percent slopesSeB2741565713lzntar06119701:24000
Saffell gravelly fine sandy loam, 12 to 20 percent slopes534510565776lzqvar06319801:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes522852565775lzqtar06319801:20000
Saffell gravelly fine sandy loam, 8 to 15 percent slopesSfD27107215022ykh5ar09920001:24000
Saffell gravelly fine sandy loam, 3 to 8 percent slopesSfC14577215012tztcar09920001:24000
Saffell gravelly sandy loam, 3 to 10 percent slopesSlC7205566077m01kar10319691:20000
Saffell gravelly sandy loam, 1 to 3 percent slopesSlB1662566076m01jar10319691:20000
Brandon-Saffell complex, 12 to 20 percent slopesBsE7789564264ly52ar11119731:20000
Saffell-Urban land complex, 3 to 8 percent slopesSfC857566202m05lar11919721:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes1859045662252tztcar12519761:20000
Saffell-Urban land complex, 3 to 8 percent slopes192232566226m06car12519761:20000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes654544564942lyvyar67019811:20000
Saffell gravelly fine sandy loam, 1 to 3 percent slopes642750564941lyvxar67019811:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes669865649432ykh6ar67019811:20000
Brandon-Saffell complex, 18 to 25 percent slopes, eroded956E22895808061w3vhil12720041:12000
Brandon-Saffell complex, 10 to 18 percent slopes, eroded956D22334808059w3vfil12720041:12000
Brandon-Saffell complex, 10 to 18 percent slopes, severely eroded956D31702808060w3vgil12720041:12000
Brandon-Saffell complex, 10 to 18 percent slopes956D1034808058w3vdil12720041:12000
Brandon-Saffell complex, 25 to 35 percent slopes956F731808062w3vjil12720041:12000
Brandon-Saffell complex, 5 to 10 percent slopes, eroded956C2256808056w3vbil12720041:12000
Brandon-Saffell complex, 2 to 5 percent slopes956B212808055w3v9il12720041:12000
Brandon-Saffell complex, 5 to 10 percent slopes, severely eroded956C357808057w3vcil12720041:12000
Brandon-Saffell complex, 18 to 25 percent slopes, eroded956E21096608150ndtril15120031:12000
Brandon-Saffell complex, 10 to 18 percent slopes, eroded956D21037608148ndtpil15120031:12000
Brandon-Saffell complex, 10 to 18 percent slopes956D902608147ndtnil15120031:12000
Brandon-Saffell complex, 10 to 18 percent slopes, severely eroded956D3670608149ndtqil15120031:12000
Brandon-Saffell complex, 25 to 35 percent slopes956F395608151ndtsil15120031:12000
Brandon-Saffell complex, 5 to 10 percent slopes, severely eroded956C3237637249pd3fil15120031:12000
Brandon-Saffell complex, 5 to 10 percent slopes, eroded956C2212608166ndv8il15120031:12000
Brandon-Saffell complex, 2 to 5 percent slopes956B50608164ndv6il15120031:12000
Brandon-Saffell-Smithdale complex, 20 to 35 percent slopes, erodedBnE2148225706192wn5fky08319951:12000
Smithdale-Saffell complex, 35 to 55 percent slopes, erodedSsE2433570651m4t3ky08319951:12000
Saffell gravelly sandy loam, 2 to 10 percent slopesSaC127570649m4t1ky08319951:12000
Saffell gravelly silt loam, 20 to 40 percent slopesSaE2868549356lfn5ky13919891:20000
Brandon-Saffell-Smithdale complex, 20 to 35 percent slopes, erodedBnE2371415927322wn5fky60219721:12000
Saffell gravelly sandy loam, 2 to 10 percent slopesSaC30515926991qgbdky60219721:12000
Brandon-Saffell-Smithdale complex, 20 to 35 percent slopes, erodedBsE21205222325842wn5fky61019681:12000
Saffell-Smithdale-Brandon complex, 20 to 60 percent slopesSsF1021422325922dy63ky61019681:12000
Saffell-Smithdale-Brandon complex, 20 to 60 percent slopes, severely erodedSsF3706126234412qykgky61019681:12000
Saffell-Brandon complex, 12 to 25 percent slopes, erodedSbD2317622325982dy69ky61019681:12000
Saffell gravelly sandy loam, 2 to 12 percent slopesSaC104922325972dy68ky61019681:12000
Saffell-Brandon-Smithdale complex, 6 to 12 percent slopes, severely erodedSbC36922325912dy62ky61019681:12000
Loring-Memphis-Saffell complex, 12 to 30 percent slopes, severely erodedLsE321831570533m4p9ky61119911:20000
Brandon-Saffell complex, 20 to 50 percent slopesBxE41548549451lfr7ky62919791:20000
Saffell very gravelly silt loam, 20 to 60 percent slopesSgF6550549495lfsnky62919791:20000
Saffell very gravelly silt loam, 6 to 12 percent slopesSgC480549494lfsmky62919791:20000
Saffell gravelly loam, 15 to 45 percent slopes9002097499560212f06mo20119781:24000
Saffell gravelly sandy loam, 12 to 30 percent slopesSaE14015567457m1h2ms00519711:20000
Saffell gravelly sandy loam, 8 to 12 percent slopesSaD1555567456m1h1ms00519711:20000
Natchez-Saffell association, hilly60F13254567556m1l8ms01519851:20000
Saffell gravelly sandy loam, 17 to 40 percent slopesSaF10843567705m1r2ms02919811:20000
Saffell-Smithdale association, hillySF5300567702m1qzms02919811:20000
Saffell gravelly sandy loam, 12 to 17 percent slopesSaE4144567704m1r1ms02919811:20000
Guin gravelly sandy loam, 12 to 40 percent slopes (saffell)GgF298332141c4m7ms03119621:15840
Guin and Saffell gravelly sandy loams, 2 to 8 percent slopes (saffell)GsC225332142c4m8ms03119621:15840
Guin gravelly sandy loam, 8 to 12 percent slopes (saffell)GgD71332140c4m6ms03119621:15840
Saffell gravelly sandy loam, 15 to 40 percent slopes72F119355567821m1vtms03719921:20000
Saffell-Natchez complex, 12 to 50 percent slopesSf1955567990m218ms05119971:20000
Saffell gravelly sandy loam, 2 to 8 percent slopesSaC765567989m217ms05119971:20000
Saffell gravelly sandy loam, 8 to 45 percent slopesSaF383332483c4z8ms05719751:20000
Saffell gravelly sandy loam, 2 to 8 percent slopesSaC592332692c560ms06519721:20000
Saffell gravelly sandy loam, 12 to 17 percent slopesSaE2370332942c5g2ms07719721:20000
Saffell gravelly sandy loam, 2 to 5 percent slopesSaB597332941c5g1ms07719721:20000
Smithdale-Saffell complex, 15 to 35 percent slopesSnF5781333100c5m5ms08719771:20000
Smithdale-Saffell association, hillySR2538333093c5lyms08719771:20000
Smithdale-Saffell-Lucy association, hillySS12752333137c5ncms09119831:20000
Saffell gravelly sandy loam, 8 to 40 percent slopesSaF1601333138c5ndms09119831:20000
Saffell very gravelly fine sandy loam, 6 to 15 percent slopesGsD6683331692xz8mms09519631:15840
Memphis, Natchez, and Guin soils, 17 to 40 percent slopes, eroded (memphis, natchez, saffell)MnF27258568343m2dnms10719611:24000
Saffell gravelly fine sandy loam, 17 to 35 percent slopesSaF7442333667c66gms11319651:15840
Saffell gravelly fine sandy loam, 8 to 17 percent slopesSaE3281333666c66fms11319651:15840
Saffell gravelly fine sandy loam, 5 to 8 percent slopesSaC350333665c66dms11319651:15840
Saffell-Smithdale association, hillySA27431334243c6t1ms14119801:20000
Saffell loam, 15 to 25 percent slopes69717159511vll8ms14320061:24000
Saffell gravelly fine sandy loam, 2 to 8 percent slopes, erodedSaC2541334326c6wqms14719651:20000
Saffell gravelly fine sandy loam, 8 to 12 percent slopes, erodedSaD2284334327c6wrms14719651:20000
Saffell gravelly sandy loam, 15 to 40 percent slopes, severely eroded26F33022571055m574ms15720061:24000
Saffell gravelly fine sandy loam, 1 to 5 percent slopes63828571380m5kmok00519771:24000
Saffell gravelly fine sandy loam, 3 to 8 percent slopes45716571237m5f0ok02319771:24000
Saffell gravelly fine sandy loam, 5 to 12 percent slopesSeE21210571180m5c5ok08919701:24000
Saffell gravelly fine sandy loam, 1 to 5 percent slopesSeC3239571179m5c4ok08919701:24000
Saffell gravelly sandy loam, 5 to 20 percent slopes456510571298m5gzok12719771:24000
Saffell gravelly sandy loam, 3 to 5 percent slopes441737571297m5gyok12719771:24000
Saffell-Brandon complex, 12 to 25 percent slopes, erodedSaE2142825453812qshctn00520111:12000
Saffell-Brandon complex, 5 to 12 percent slopes, erodedSaC217125453822qshdtn00520111:12000
Saffell, Smithdale, and Brandon soils, 25 to 60 percent slopesSAF3725453802qshbtn00520111:12000
SAFFELL GRAVELLY SILT LOAM, HILLY PHASEEf1097327302bzl4tn03920081:24000
SAFFELL GRAVELLY SILT LOAM, STEEP PHASEEh641327304bzl6tn03920081:24000
SAFFELL GRAVELLY SILT LOAM, SEVERELY ERODED HILLY PHASEEg358327303bzl5tn03920081:24000
SAFFELL GRAVELLY SILT LOAM, ERODED HILLY PHASEEe212327301bzl3tn03920081:24000
ROUGH GULLIED LAND, SAFFELL, AND LEXINGTON SOILSRd170327346bzmktn03920081:24000
Saffell gravelly fine sandy loam, 20 to 60 percent slopesSaF8162527124kpj0tn04319931:24000
Saffell gravelly fine sandy loam, 12 to 20 percent slopesSaD5635527123kphztn04319931:24000
Waynesboro very gravelly sandy loam, 25 to 45 percent slopes (Saffell)WnF11188327681bzzctn07119611:15840
Waynesboro gravelly sandy loam, 12 to 25 percent slopes (Saffell)WmE6744327678bzz8tn07119611:15840
Bodine-Guin complex, 20 to 35 percent slopes (Bodine-Saffell)BeF6065327518bzt3tn07119611:15840
Waynesboro gravelly sandy loam, 5 to 8 percent slopes (Saffell)WmC5809327676bzz6tn07119611:15840
Waynesboro gravelly sandy loam, 8 to 12 percent slopes (Saffell)WmD2516327677bzz7tn07119611:15840
Waynesboro very gravelly sandy loam, 12 to 25 percent slopes (Saffell)WnE2202327680bzzbtn07119611:15840
Waynesboro very gravelly sandy loam, 5 to 12 percent slopes (Saffell)WnD1683327679bzz9tn07119611:15840
Saffell gravelly sandy loam, 5 to 12 percent slopesSaD604327625bzxktn07119611:15840
Saffell gravelly sandy loam, 12 to 20 percent slopesSaE371327626bzxltn07119611:15840
Saffell-Brandon complex, 12 to 25 percent slopes, erodedSaE2749125453012qs9gtn07920121:12000
Saffell, Smithdale, and Brandon soils, 25 to 60 percent slopesSAF588425453002qs9ftn07920121:12000
Saffell-Brandon complex, 5 to 12 percent slopes, erodedSaC2121625453022qs9htn07920121:12000
Saffell gravelly fine sandy loam, 20 to 60 percent slopesSaF108527486kpwptn08119971:24000
Saffell gravelly fine sandy loam, 12 to 20 percent slopesSaD19527485kpwntn08119971:24000
Saffell gravelly silt loam, 12 to 20 percent slopesSaD379530881ktf6tn10119991:24000
Saffell gravelly silt loam, 20 to 40 percent slopesSaE74530882ktf7tn10119991:24000
Saffell gravelly sandy loam, 12 to 30 percent slopesSaE2424327979c08ztn10919941:20000
Saffell gravelly sandy loam, 5 to 12 percent slopesSaC1229327978c08ytn10919941:20000
Saffell-Bodine complex, 20 to 40 percent slopesSbE2998831604451kyyttn16119531:20000
Saffell-Bodine complex, 40 to 70 percent slopesSbF586431604461kyyxtn16119531:20000
Saffell-Bodine complex, 12 to 20 percent slopesSbD528431604571ttwytn16119531:20000
Brandon-Saffell complex, 20 to 50 percent slopesBxE48231604692z6xstn16119531:20000
Saffell gravelly silt loam, 20 to 60 percent slopesGe40623969102lg5ptn16119531:20000
Saffell-Gullied land complex, 12 to 20 percent slopesRe17723969622lg7ctn16119531:20000
Saffell gravelly silt loam, 5 to 20 percent slopesGd17723969092lg5ntn16119531:20000
Saffell gravelly fine sandy loam, 20 to 60 percent slopesSaF29547328042c0c0tn18119961:24000
Saffell gravelly fine sandy loam, 12 to 20 percent slopesSaD7036328041c0bztn18119961:24000
Saffell gravelly sandy loam, 3 to 8 percent slopes332367575279m9mdtx03719781:20000
Saffell-Urban land complex, 3 to 8 percent slopes34186575280m9mftx03719781:20000

Map of Series Extent

Approximate geographic distribution of the SAFFELL 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 .