Official Series Description


Lab Data Summary

Aggregate lab data for the BIBB soil series. This aggregation is based on all pedons with a current taxon name of BIBB, 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 BIBB 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
133AS84AL-011-784AL011007-pgmBibb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0258806,-85.5979222
133AS88AL-131-588AL131005-pgmBibb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.8455556,-87.4697222
137S87SC025-17S1987SC025707Bibb3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.5755556,-79.9725

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BIBB 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 BIBB 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 BIBB 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 BIBB 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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Click the image to view it full size.

Competing Series

Soil series competing with BIBB 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 BIBB series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BIBB 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BIBB, 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-2010-08-27-01 | Clarke County - 2006

    Generalized patterns of soils and geomorphology and landscape relationships in general soil map units 2—Iuka-Bibb-Harleston, 6—Lucedale-Bama-Smithdale, 8—Smithdale-Wadley-Boykin, 9—Smithdale-Flomaton-Wadley, 10—Prim-Suggsville-Brantley, and 11—Okeelala-Brantley-Smithdale. The area illustrated is along Bassett Creek in the northeastern part of Clarke County, Alabama (Soil Survey of Clarke County, Alabama; 2006) .

  2. AL-2012-04-24-02 | Clarke County - August 2006

    Generalized patterns of soils and geomorphology and landscape relationships in general soil map units 2—Iuka-Bibb-Harleston, 6—Lucedale-Bama-Smithdale, 8—Smithdale-Wadley-Boykin, 9—Smithdale-Flomaton-Wadley, 10—Prim-Suggsville-Brantley, and 11—Okeelala-Brantley-Smithdale. The area illustrated is along Bassett Creek in the northeastern part of Clarke County, Alabama (Soil Survey of Clarke County, Alabama; August 2006).

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

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

  4. DC-2011-05-31-04 | District of Columbia - 1976

    Diagram of fall line between the Piedmont Plateau and the Coastal Plain. Diagram also shows the relationship of parent material and topography (Soil Survey of District of Columbia; 1976).

  5. LA-2012-02-01-01 | Bossier Parish - August 1962

    Physiographic relationships of general soil areas in the northwestern part of Bossier Parish. The area represented is about 12 miles square (Soil Survey of Bossier Parish, Louisiana; August 1962).

  6. MD-2012-02-03-01 | Anne Arundel County - February 1973

    Representative pattern of soils and parent material in soil association 2 (Soil Survey of Anne Arundel County, Maryland; February 1973).

  7. MD-2012-02-03-09 | Charles County - July 1974

    Cross section of association 1 showing topography, important soils, and underlying material (Soil Survey of Charles County, Maryland; July 1974).

  8. MD-2012-02-03-10 | Charles County - July 1974

    Cross section of association 2 showing topography, important soils, and underlying material (Soil Survey of Charles County, Maryland; July 1974).

  9. MS-2012-04-27-05 | Tippah County - February 1966

    Distribution and pattern of major soils in Mantachie-Bibb association (Soil Survey of Tippah County, Mississippi; February 1966).

  10. MS-2012-04-27-11 | Newton County - February 1960

    Soil associations of Newton County, Mississippi (Soil Survey of Newton County, Mississippi; February 1960).

  11. NC-2012-02-07-23 | Johnston County - October 1994

    The relationship of soils and landscapes in the Norfolk-Goldsboro-Rains map unit, the Rains-Goldsboro-Lynchburg map unit, and the Wehadkee-Bibb-Chewacla map unit (Soil Survey of Johnston County, North Carolina; October 1994).

  12. NC-2012-02-07-24 | Johnston County - October 1994

    The relationship of soils and landscapes in the Wagram-Blanton-Bonneau map unit and the Gilead-Uchee-Bibb map unit (Soil Survey of Johnston County, North Carolina; October 1994).

  13. NC-2012-02-07-40 | Sampson County - August 1985

    Pattern of soils in map units 1, 2, and 5 north of Clinton (Soil Survey of Sampson County, North Carolina; August 1985).

  14. TX-2012-03-21-12 | Jefferson County - February 1965

    Relative position of the major soils of the East Texas timberlands (Soil Survey of Jefferson County, TX; 1965).

Map Units

Map units containing BIBB 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
Myatt-Bibb associationMY15895328075c0d2al00119721:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBs58883280612svnyal00119721:20000
Osier-Bibb complexOk5630328082c0d9al00119721:20000
Bibb and Mantachie soils, local alluviumBb6072328102c0dyal00319611:20000
Iuka-Bibb complex, 0 to 1 percent slopes, frequently floodedIbA35200328266c0l7al00520011:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBdA2316022303112shs8al00720071:24000
Mantachie, Iuka, and Bibb soils, 0 to 1 percent slopes, frequently floodedMBA43870328423c0r9al01119861:20000
Mantachie, Bibb, and Iuka soils, 0 to 1 percent slopes, frequently floodedMIA56120328464c0smal01319961:20000
Myatt-Bibb association, levelMYA26468328523c0vjal02119671:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBb9573284872svnyal02119671:20000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA374003285932shs8al02319981:24000
Iuka, Bibb, and Mantachie soils, 0 to 1 percent slopes, frequently floodedIBA57350328641c0zbal02520041:24000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently flooded2205003286582svnyal03119761:20000
Bibb sandy loam, 0 to 1 percent slopes, frequently floodedBbA25775328717c11sal03519851:20000
Muckalee, Bibb, and Osier soils, 0 to 2 percent slopes, frequently floodedMBA51125328770c13hal03919851:20000
Iuka-Bibb sandy loams, 0 to 2 percent slopes, frequently floodedIbA6479328766c13cal03919851:20000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA246305816112shs8al04120051:24000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBa33713289562svnyal04519581:20000
Bibb soils, local alluviumBb183328957c19jal04519581:20000
Bibb soils, 0 to 2 percent slopesBh696113293162tsy5al05319691:20000
Bibb soilsBb7942329445c1t8al05719631:15840
Bibb soils, local alluviumBc3530329446c1t9al05719631:15840
Bibb loamBb9031329536c1x6al05919621:15840
Bibb and Osier soils, frequently floodedBb23773329618c1zval06119731:20000
Chastain and Bibb soilsCb4317329621c1zyal06119731:20000
Bibb silt loamBb3057329650c20wal06320131:
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBdA156563297432shs8al06520031:24000
Bibb, Osier, and Kinston soils, 0 to 1 percent slopes, frequently floodedBOA31335608102nds6al06920021:24000
Urban land-Bibb-Kinston complex, 0 to 2 percent slopes, frequently floodedUbA773656572q16ral06920021:24000
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBbA157903305582shs8al09119971:24000
Bibb soils4950330642c31wal09319761:20000
Johnston, Bibb and Pamlico soils, 0 to 1 percent slopes, frequently floodedJBA3622229950612x5qyal09720181:24000
Johnston, Bibb and Smithton soils, 0 to 3 percent slopes, frequently floodedJOA1159129950622x5qzal09720181:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK325029949662x5rkal09720181:24000
Bibb loam, 0 to 1 percent slopes, frequently floodedBrA38400330828c37wal09919841:20000
Bibb soils local, alluvium phasesBa1013330873c39bal10119581:20000
Bibb soils, frequently flooded96386331541c3zwal12519801:20000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK7488726420572x5rkal12920131:24000
Bibb-Iuka complex, 0 to 2 percent slopes, frequently floodedBiA933326420562rjqtal12920131:24000
Bibb silt loam, 0 to 1 percent slopes, frequently floodedBb7263656513730dkdar01119591:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently flooded5205475653702ynxcar02719831:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently flooded3A14690171590430dkcar05320061:24000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBbA175267215152ynxcar09920001:24000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBB256885660492ynxcar10319691:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBbA224255792022ynxcar13919921:24000
Bibb sandy loamBg17412856749sbdc00119751:12000
Pamlico, Bibb, and Rutlege soils, frequently flooded641156314810491lq4sfl01319971:20000
Pickney, Dorovan, and Bibb soils, frequently flooded664348713816051hcnxfl03920061:12000
Rutlege, Bibb, and Surrency soils, frequently flooded88936813816271hcpmfl03920061:12000
Bibb-Rains-Garcon complex, occasionally flooded89364813816281hcpnfl03920061:12000
Albany-Garcon-Bibb complex, 0 to 5 percent slopes, occasionally flooded94213014080951j87ffl03920061:12000
Bibb-Bigbee complex, undulating, occasionally flooded561870114885417kgtfl04719951:24000
Bibb association5316101017238134j4fl05919711:12000
Bibb soils, 0 to 2 percent slopes51095014249552tsy5fl06319771:20000
Bibb loamy sand, frequently flooded191330700482rhx6fl06519841:20000
Rutlege, Bibb and Surrency soils, 0 to 2 percent slopes, frequently flooded58470403227482xcy8fl07720041:24000
Elloree, Bibb, and Meggett soils, 0 to 3 percent slopes, frequently flooded3015070322718btt8fl07720041:24000
Pickney, Dorovan, and Bibb soils, frequently flooded6514625322756btvhfl07720041:24000
Bibb, Rains, and Garcon Soils, occasionally flooded9555013799221h9xmfl07720041:24000
Kinston, Johnston, and Bibb soils, frequently flooded434470014447251khc1fl09119891:20000
Bibb-Kinston association351450823750wn5lfl11319781:24000
Osier-Bibb-Albany complex, frequently flooded693423102338313bxcfl12120031:24000
Kinston-Johnston-Bibb complex, frequently flooded1538970323984bw43fl13119851:20000
Kinston-Bibb association, frequently flooded439510324014bw52fl13119851:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedOI366213245992wyxjga03319821:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedOSA130907542762wyxjga08720011:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKFA639103247682tl1sga10719931:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedOSA357503366042wyxjga13120001:12000
Bibb-Wehadkee complexBwc14495324792bwz5ga16519661:20000
Bibb sandy loamBh645512481545w9ga21519801:15840
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKBA234553347532tl1sga24320021:24000
Bibb and Osier soilsBO15265324864bx1hga24519791:15840
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKBA1501025803862qdyjga25120111:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKBA1983524253672tl1sga25920091:12000
Ochlockonee, Iuka, and Bibb soils, 0 to 5 percent slopes, frequently floodedOBB633024253972mdtmga25920091:12000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKBA1854024554192tl1sga30720091:12000
Ochlockonee, Iuka, and Bibb soils, 0 to 5 percent slopes, frequently floodedOBB103024554272nf2bga30720091:12000
Osier-Bibb association, frequently floodedOB21501251784680ga60219831:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedObs246493252112wyxjga60819651:20000
Johnston-Osier-Bibb associationJob3188612535046fkga60919671:20000
Osier-Johnston-Bibb associationOjb883512535546fqga60919671:20000
Kinston-Bibb association, 0 to 2 percent slopes, frequently floodedKB1130623253862wz35ga61019921:20000
Angelina and Bibb soils, frequently floodedAB1920512536746g3ga61319691:20000
Bibb sandy loam, frequently floodedBh25157126167478xga62019921:20000
Bibb-Meggett association, 0 to 2 percent slopes, frequently floodedBmA506626868012rz9qga62620131:24000
Bibb silt loamBh811012554546mvga62819771:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedBK459853257582tl1sga63419801:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedBB327113258172wyxjga63819871:20000
Bibb loamy sand, 0 to 2 percent slopes, frequently floodedBbA216026391262rj2dga63920121:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKb156353260022tl1sga64319741:20000
Johnston and Bibb soilsJB2173512580846xbga64419801:20000
Osier and Bibb soilsOs584512581846xnga64419801:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedObs645553260612wyxjga64719701:20000
Osier and Bibb soils, 0 to 2 percent slopes, frequently floodedBO353853261992wyxjga65019941:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKib350253262602tl1sga65219691:20000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedBk775153263382tl1sga65419791:20000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBhA2424747930t38sga65520121:24000
Kinston and Bibb soils, 0 to 2 percent slopes, frequently floodedKBA1722016050862tl1sga65820051:24000
Rosebloom and Bibb soils, 0 to 2 percent slopes, frequently floodedRB875022323302dxxnky61019681:12000
Enville-Bibb complex, 0 to 2 percent slopes, frequently floodedEb160222322172dxt0ky61019681:12000
Ouachita and Bibb soils, frequently floodedOB33253327011bz8rla10319851:24000
Ouachita, Bibb, and Jena soils, frequently floodedOB6819517241451vw3lla11719891:24000
Bibb silt loam, frequently floodedBm1256912829049hdmd03719751:20000
Bibb and Chastain fine sandy loams (bibb and una)Bc42149331969c4fpms02319631:15840
Bibb soilsBb7810331968c4fnms02319631:15840
Bibb silt loamBf5000332208c4pdms03519761:20000
Bibb and Jena soils, frequently floodedBG4987332209c4pfms03519761:20000
Bibb-Iuka complex, 0 to 2 percent slopes, frequently floodedBiA1811026421632rrxqms04120121:24000
Bibb, Johnston and Kinston soils, 0 to 1 percent slopes, frequently floodedBJK1395726421642x5rkms04120121:24000
Bigbee-Bibb complex, frequently floodedBg4904332386c4w4ms04519791:20000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBb124263326172tjl6ms06119741:20000
Bibb and Mantachie soils, frequently floodedBm9040332669c558ms06519721:20000
Bibb silt loam, frequently flooded618149332734c57cms06719841:20000
Trebloc silt loam and Bibb fine sandy loam, occasionally and frequently flooded1319060332703c56cms06719841:20000
Bibb sandy loam, 0 to 2 percent slopes, occasionally floodedBb4433327492tjl4ms06919911:20000
Kirkville-Bibb complex, 0 to 2 percent slopes, frequently floodedKb9431332886301k4ms07519801:20000
Kirkville-Bibb association, 0 to 2 percent slopes, frequently floodedKK8687332884301k5ms07519801:20000
Bigbee-Bibb association, 0 to 5 percent slopes, frequently floodedBB4653332875301k2ms07519801:20000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBb12303329482tjl6ms07920081:24000
Bibb silt loam, frequently floodedBb17506333113c5mlms09119831:20000
Bibb and Mantachie soilsBm40679333147c5npms09519631:15840
Bibb sandy loam, 0 to 2 percent slopes, occasionally floodedBb313523332622tjl4ms09919791:20000
Bibb-Mantachie association, frequently floodedBM9125333261c5scms09919791:20000
Mantachie soils (bibb) (0 to 2 percent slopes)Ma37916333327c5vhms10119571:20000
Mantachie very fine sandy loam, local alluvium phase (bibb) (0 to 2 percent slopes)Mb20721333328c5vjms10119571:20000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBa146273332982tjl6ms10119571:20000
Bibb sandy loamBd15005333532c623ms10919801:20000
Bibb and Trebloc soils, frequently floodedBM10434333593c642ms11119971:20000
Bibb silt loam, frequently floodedBk6805333598c647ms11119971:20000
Bibb loamBb1129333630c658ms11319651:15840
Bibb sandy loam, frequently floodedBb6724333798c6bpms11719951:24000
Bibb and Iuka sandy loams, frequently floodedBI2601333796c6bmms11719951:24000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBb86524313892tjl6ms12320091:24000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBb77253340402tjl6ms12919971:20000
Waverly and Bibb soils (rosebloom and bibb)Wb5544334225c6sgms13919631:15840
Bibb-Iuka complex, 0 to 1 percent slopes, frequently floodedBkA3909624034302shs8ms15320081:24000
Bibb and Johnston loams, frequently floodedBB196301113913qx8nc01519841:24000
Bibb sandy loam, 0 to 1 percent slopes, frequently floodedBbA25445186594720mnvnc06119551:24000
Bibb soilsBB156611015483132pjnc06519761:20000
Bibb loam, frequently floodedBB71961127963sclnc07919781:24000
Chastain and Bibb soils, 0 to 1 percent slopes, frequently floodedCbA366401130263sm0nc08319951:24000
Bibb soils, frequently floodedBb255461130843snwnc08519841:24000
Bibb soilsBB106681131503sr0nc09119811:24000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBb287491135193t3xnc10119861:24000
Bibb soils, frequently floodedBB85901159923wppnc10719731:20000
Bibb loam, frequently floodedBb227951111193qmhnc11719851:24000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBhA56522335572dz67nc12320071:24000
Bibb loam, 0 to 2 percent slopes, frequently floodedBb165111138913thxnc12519871:24000
Bibb loam, 0 to 2 percent slopes, frequently floodedBb95821108923qd5nc12719841:24000
Bibb complexBb247831143133tyjnc14719691:15840
Bibb soilsBB240801147583vdwnc15519721:20000
Bibb and Johnston soils, frequently floodedBH427941150413vq0nc16319821:24000
Bibb soils, 0 to 2 percent slopes, frequently floodedBaA243614086051j8rwnc16520061:12000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBbA584530502352xh99nc18319661:24000
Bibb sandy loamBb188091162293wybnc19119681:20000
Bibb loam, 0 to 2 percent slopes, frequently floodedBb210141164243x4mnc19519801:24000
Bibb sandy loam, frequently floodedBf90961319934fbvsc02519891:20000
Bibb sandy loam, 0 to 2 percent slopes, frequently floodedBfA1751618784nrwssc03119981:24000
Bibb sandy loamBb151971308734d5qsc07519851:20000
Bibb loamy sandBc143481317364f2ksc61519811:20000
Rosebloom and Bibb soils, 0 to 2 percent slopes, frequently floodedRO189025453792qsh9tn00520111:12000
Enville-Bibb complex, 0 to 2 percent slopes, frequently floodedEb66725453402qsfztn00520111:12000
Bibb silt loam, frequently floodedBB4350327196bzgqtn02319891:24000
BIBB SILT LOAMBb5392327260bzjstn03920081:24000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBa12863272592tjl6tn03920081:24000
Rosebloom and Bibb soils, frequently floodedRB16217327492bzs8tn06919961:24000
Rosebloom and Bibb soils, occasionally floodedRO2354327493bzs9tn06919961:24000
Waverly fine sandy loam (Bibb)Wa4473327664bzyttn07119611:15840
Beechy silt loam (Bibb)Bb27430327691bzzptn07719551:20000
Beechy fine sandy loam (Bibb)Ba4855327690bzzntn07719551:20000
Rosebloom and Bibb soils, 0 to 2 percent slopes, frequently floodedRO962925452972qs9btn07920121:12000
Enville-Bibb complex, 0 to 2 percent slopes, frequently floodedEb146125452542qs7ytn07920121:12000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently floodedBb256863279512tjl6tn10919941:20000
Bibb silt loam, frequently floodedBb4838576421mbt7tx20319891:24000
Bibb soils, frequently floodedBb9646575567m9xptx33919671:20000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBf405857603930d1htx49919931:24000
Bibb fine sandy loam, 0 to 1 percent slopes, frequently floodedBg1367557647530d1htx61620041:24000
Bibb-Chastain complex, 0 to 2 percent slopes, frequently flooded4A1246612102241xyva03319961:24000
Bibb fine sandy loam, 0 to 2 percent slopes, frequently flooded4A69751179293yq5va03619931:24000
Bibb sandy loam, 0 to 2 percent slopes, frequently flooded3A1175612150042fcva05719851:20000
Kinston and Bibb soils, 0 to 2 percent slopes, occasionally flooded7A88041186573zgnva09719951:24000
Bibb and Kinston soils, 0 to 2 percent slopes, frequently flooded3A8805694772r9z0va10119951:15840
Kinston-Bibb complex11435611963040h1va11919821:15840
Bibb and Levy soils27928120367417tva15919801:20000
Bibb sandy loam, 0 to 2 percent slopes, frequently flooded4A28800705260rnwbva17519961:24000
Bibb fine sandy loam, 0 to 4 percent slopesBb301712048441clva17919701:15840
Bibb fine sandy loam, 0 to 2 percent slopes, frequently flooded2A461812247143fpva18119971:24000
Bibb and Chastain soils, 0 to 2 percent slopes, frequently flooded4A741517230251vtygva18320061:24000
Bibb and Levy soils2725212060441hgva19319801:20000

Map of Series Extent

Approximate geographic distribution of the BIBB 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 .