Official Series Description


Lab Data Summary

Aggregate lab data for the SAWMILL soil series. This aggregation is based on all pedons with a current taxon name of SAWMILL, 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 SAWMILL 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
104X53-933-1S1983IA105005Sawmill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.1800938,-91.2671784
105X49-933-11983IA097008Sawmill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0372542,-90.3036429
105UMN2524S1977MN0552524Sawmill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.5407486,-91.2717285
108B84IL131015S1984IL131015Sawmill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1124007,-90.6921161
108B84IL131018S1984IL131018Sawmill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2707372,-90.757619
108B85P0667S1985IL021008Sawmill6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.8096267,-89.2454763
108B88P0108S1987IL187005Sawmill7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0673279,-90.6720121
108CX23-933-1S1971IA045005Sawmill1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8378911,-90.8851921
114B87IL027042S1987IL027042Sawmill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5197266,-89.5754333
115C83P061082IL131123Sawmill6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2682168,-91.0814726
115C65IL071001S1965IL071001Sawmill5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.880605,-90.998917
115C85IL149006S1985IL149006Sawmill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7499018,-91.2671767
115C85IL149014S1985IL149014Sawmill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6970533,-91.301541
115C85IL149036S1985IL149036Sawmill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7115267,-91.2788282

Water Balance

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

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with SAWMILL, 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. IA-2010-09-02-04 | Black Hawk County - 2006

    Typical pattern of soils and parent material in the Dinsdale-Klinger-Maxfield association (Soil Survey of Black Hawk County, Iowa; 2006).

  2. IA-2011-05-31-17 | Delaware County - 1986

    Pattern of soils and parent material in the Dinsdae-Sawmill-Tama association (Soil Survey of Delaware County, Iowa; 1986).

  3. IL-2010-09-01-26 | Hancock County - 2001

    Typical pattern of soils and parent material in the Fishhook-Elco-Atlas association (Soil Survey of Hancock County, Illinois; 2001).

  4. IL-2010-09-01-41 | Marshall County - 2002

    Typical pattern of soils and parent material in the Flanagan-Graymont-Elpaso association (Soil Survey of Marshall County, Illinois; 2002).

  5. IL-2010-09-01-51 | McDonough County - 1997

    Typical pattern of soils and parent material in the Sawmill-Wakeland-Tice association (Soil Survey of McDonough County, Illinois; 1997).

  6. IL-2010-09-01-74 | Stark County - 1996

    Typical pattern of soils and parent material in the Lawson-Sawmill association (Soil Survey of Stark County, Illinois; 1996).

  7. IL-2010-09-01-82 | Woodford County - 1999

    Typical pattern of soils and parent material in the Saybrook-Catlin-Tama association (Soil Survey of Woodford County, Illinois; 1999).

  8. IL-2010-09-24-05 | Christian County -

    Typical pattern of soils and underlying material in the Sawmill-Radford-Tice association (Soil Survey of Christian County, Illinois).

  9. IL-2011-08-03-13 | Christian County - 1994

    Typical pattern of soils and parent material in the Sawmill-Radford-Tice association (Soil Survey of Christian County, Illinois; 1994).

  10. IL-2011-08-04-26 | Henry County - 1984

    Pattern of soils in the Sawmill-Radford association (Soil Survey of Henry County, Illinois; 1984).

  11. IL-2011-08-04-44 | Knox County - 1986

    Typical pattern of soils and parent material in the Lawson-Sawmill-Huntsville association (Soil Survey of Knox County, Illinois; 1986).

  12. IL-2011-08-04-74 | Mercer County - 1991

    Typical pattern of soils and parent material in the Titus-Beaucoup association (Soil Survey of Mercer County, Illinois; 1991).

  13. IL-2011-08-04-92 | Putman County - 1992

    Typical pattern of soils and parent material in the Tama-Muscatine-Sable association (Soil Survey of Putnam County, Illinois; 1992).

  14. IL-2011-08-04-93 | Putman County - 1992

    Typical pattern of soils and parent material in the the Rozetta-Fayette-Miami association (Soil Survey of Putnam County, Illinois; 1992).

Map Units

Map units containing SAWMILL 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
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93388944132832wm7mia01320011:12000
Sawmill, occasionally flooded-Urban land complex, 0 to 2 percent slopes49331014133272wm7pia01320011:12000
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93391064044732wm7mia04519781:15840
Sawmill silty clay loam, shallow loess, 1 to 4 percent slopes, occasionally flooded933B47104050972wm7nia05519841:15840
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93331914049662wm7mia06919771:15840
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93336264063262wm7mia07519731:15840
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93310904067072wm7mia08319821:15840
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded93376724082232wm7mia10519881:15840
Sawmill silty clay loam, shallow loess, 1 to 4 percent slopes, occasionally flooded933B38644115702wm7nia17119891:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A51513946242w1z2il00720061:12000
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+1674519100462w1z7il01120071:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A4026508542w1z6il01120071:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A718629022w1z2il01120071:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A14417960922w1z2il01520051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A119615435152w1z8il01520051:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+9437960932w1z3il01520051:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A5377960952w1zbil01520051:12000
Sawmill silt loam, 0 to 2 percent slopes, rarely flooded, overwash7107A+18515428552w1z9il01520051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded, long duration3107L381814448602w1z5il01720031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A11732628382w1z6il01720031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A52214451912w1z8il01720031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A46314448582w1z2il01720031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A110732430012w1z2il01919991:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A110002617642w1z2il02119991:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A168514284162w1z2il02920051:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A703121087082ww9jil03120081:12000
Sawmill silty clay loam, undrained, cool, 0 to 2 percent slopes, frequently flooded1107A171521089202ytdlil03120081:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A472115925012w1z2il03920051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A102915925002w1z6il03920051:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A54052002332ytdkil04120041:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A11511664142w1z2il04120041:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A48751833952ww9jil04319981:12000
Sawmill silty clay loam, undrained, cool, 0 to 2 percent slopes, frequently flooded1107A10601833422ytdlil04319981:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107101733922w1z2il05119911:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A27781983472w1z2il05320011:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A37016156902w1z2il05719971:12000
Sawmill silty clay loam, warm mesic, 0 to 2 percent slopes, occasionally flooded8107wA4372115812yp4mil05919661:20000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A329215965352w1z6il06320051:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A307711439682ww9jil06320051:12000
Sawmill silty clay loam, undrained, cool, 0 to 2 percent slopes, frequently flooded1107A86711440362ytdlil06320051:12000
Sawmill mucky silt loam, ponded, 0 to 2 percent slopes, frequently flooded4107A68615903571qcwvil06320051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A38161751782w1z2il06719931:15840
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A15211752242w1z6il06719931:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A32756327132w1z2il07120051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A164510180522w1z8il07120051:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A94910030792w1zbil07120051:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+47814805132w1z3il07120051:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+141932448482w1z3il07320011:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A75092448492w1z2il07320011:12000
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+8232448612w1z7il07320011:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A84751755392ww9jil07519801:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A267284652w1z2il08320021:12000
Sawmill silty clay loam, undrained, cool, 0 to 2 percent slopes, frequently flooded1107A22715942ytdlil08920001:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A47329685912ww9jil09120031:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A247417156282ww9jil09320071:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+61406808732w1z3il09520021:12000
Sawmill silty clay loam, undrained, cool, 0 to 2 percent slopes, frequently flooded1107A43958042272ytdlil09720031:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A2758042072ww9jil09720031:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A297314278362ww9jil09920061:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A124413868532w1z6il09920061:12000
Sawmill silty clay loam, warm mesic, 0 to 2 percent slopes, occasionally flooded8107wA22171767622yp4mil10119521:42240
Sawmill silt loam, overwash, occasionally flooded8107+631767635xy1il10119521:42240
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A69061769622ww9jil10519911:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A146752087032w1z2il10720061:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A329715958002w1z6il10720061:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+327615958012w1z3il10720061:12000
Sawmill silty clay loam, sandy substratum, 0 to 2 percent slopes, frequently flooded3107AS258615961152w1z4il10720061:12000
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+83016909612w1z7il10720061:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A50326340972w1z2il10920021:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A166471991482w1z6il11320001:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A4911957662w1z2il11320001:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A991119139822w1z2il11520071:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A54619139782ytdkil11520071:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A19641992482w1z2il11719991:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A67461822422w1z6il12319971:15840
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A43371778192w1z6il12519891:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A19811777842w1z2il12519891:15840
Sawmill silty clay loam, sandy substratum, 0 to 2 percent slopes, frequently flooded3107AS130225179822w1z4il12519891:15840
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+7441778202w1z7il12519891:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded, long duration3107L34625179812w1z5il12519891:15840
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+1751777852w1z3il12519891:15840
Sawmill silty clay loam, sandy substratum, 0 to 2 percent slopes, frequently flooded3107AS221114123492w1z4il12920051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A95314063832w1z2il12920051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded, long duration3107L1914063842w1z5il12920051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A49972450222w1z2il13120001:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+46452450212w1z3il13120001:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A7652450272w1z8il13120001:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A30617215412w1z2il13520071:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A106016721102w1z2il13719841:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A24262465342w1z2il13919991:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A11902465152ytdkil13919991:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A314311443482w1z2il14120051:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A16162089502w1z2il14319861:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A736319124032w1z2il14720091:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A21431728932w1z6il15519871:15840
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, occasionally flooded1107A12451728632w1zcil15519871:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A70521986942w1z2il16120021:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A41071987022w1z8il16120021:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A13891986882w1zbil16120021:12000
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+7341987092w1z7il16120021:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A125371992942w1z2il16719991:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A632022292w1z2il16920001:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A40325420872w1z2il17119841:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded310741951790192w1z2il17319901:15840
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+173625423932w1z7il17519921:15840
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+9671790902w1z3il17519921:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A881790892w1z2il17519921:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A363617097882w1z2il17720061:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A210915920782w1zbil17720061:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A62701793982w1z2il17919911:15840
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A120225088372w1z6il17919911:15840
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A593116011162w1z2il18320061:12000
Sawmill silt loam, 0 to 2 percent slopes, frequently flooded, overwash3107A+26552449302w1z3il18720021:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A21222449312w1z2il18720021:12000
Sawmill silt loam, 0 to 2 percent slopes, occasionally flooded, overwash8107A+23947931412w1z7il19520031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, rarely flooded7107A9867931292w1z8il19520031:12000
Sawmill silty clay loam, undrained, 0 to 2 percent slopes, frequently flooded1107A8307931042w1zbil19520031:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A5027931132w1z2il19520031:12000
Sawmill silty clay loam, heavy till plain, 0 to 2 percent slopes, frequently flooded3107A18316187532ww9jil19720021:12000
Sawmill silty clay loam, 0 to 2 percent slopes, frequently flooded3107A27581742162w1z2il20119971:12000
Sawmill silty clay loam, 0 to 2 percent slopes, occasionally flooded8107A59068692512w1z6il20320081:12000
Sawmill silty clay loam, shallow loess, 0 to 2 percent slopes, occasionally flooded46715644004652wm7mmn09919861:15840
Sawmill silty clay loam4672294400779fg1cmn10919771:15840
Sawmill silt loam, calcareous variantSg2093268708g79pwi05920231:15840
Sawmill silt loam, calcareous variantSg2623403366g96fwi07920231:15840
Sawmill silt loam, calcareous variantSg3713268817g79pwi10120231:15840
Sawmill silt loam, calcareous variantSg7193403474g96fwi13320231:15840

Map of Series Extent

Approximate geographic distribution of the SAWMILL 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 .