Official Series Description


Lab Data Summary

Aggregate lab data for the MILTON soil series. This aggregation is based on all pedons with a current taxon name of MILTON, 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 MILTON 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
111AHM75031975IN057003Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0671528,-85.8766417
111ADC76311976IN031031Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3655278,-85.5877694
111ADC76341976IN031034Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3357,-85.6562639
111ARU78151978IN139015Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4738889,-85.5557639
111BHK-0271961-OH063-027Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9950562,-83.4488068
111BSA-0281972-OH147-028Milton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.225914,-82.8642807
111BWB76011976IN169001Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8235389,-85.7119972
111DWY77021977IN177002Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7720444,-84.8173444
111DCA86061986IN015006Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7104694,-86.5287639
99WD-0551954-OH173-055Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2044983,-83.4224472
99WD-0561954-OH173-056Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.2319984,-83.6202774
n/aPB-0181959-OH135-018Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aRO-0801959-OH141-080Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0361959-OH165-036Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-0011960-OH109-001Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-0041960-OH109-004Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPB-0411960-OH135-041Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0391960-OH165-039Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0401960-OH165-040Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-0101961-OH109-010Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-0131961-OH109-013Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0461961-OH165-046Milton2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0471961-OH165-047Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMT-0111963-OH113-011Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMT-0161964-OH113-016Milton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMT-0201965-OH113-020Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-0191968-OH109-019Milton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGN-0221970-OH057-022Milton4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aMM-011YYYY-OH109-011Milton3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MILTON 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 MILTON 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 MILTON 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 MILTON 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 MILTON 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 MILTON series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the MILTON 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 MILTON, 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. IN-2012-01-20-16 | Wabash County - February 1983

    Pattern of soils and underlying material in the Genesee-Milton-Shoals map unit (Soil Survey of Wabash County, Indiana; 1983).

  2. OH-2010-09-29-28 | Wood County - 2007

    Typical pattern of soils and parent material in the Millsdale-Castalia-Milton association (Soil Survey of Wood County, Ohio; 2007).

  3. OH-2012-02-16-44 | Wood County - December 1966

    Relationship of some local soils to underlying material and relief (Soil Survey of Wood County, Ohio; December 1966).

Map Units

Map units containing MILTON 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
Milton silt loam, 6 to 12 percent slopes739D35927146293gvil08920001:12000
Milton silt loam, 2 to 6 percent slopes739B23127146593gyil08920001:12000
Milton silt loam, 2 to 6 percent slopes, erodedMqbB23922073056yq8in00520021:12000
Milton silt loam, 0 to 2 percent slopesMqbA3482073066yq9in00520021:12000
Milton-Rock outcrop complex, 25 to 40 percent slopesMrbF3132072856ypmin00520021:12000
Milton silt loam, 6 to 12 percent slopes, erodedMqbC22262073046yq7in00520021:12000
Milton variant, channery silt loam, 1 to 4 percent slopes, flaggyMuB8431652045jx5in01519871:15840
Milton silt loam, 2 to 6 percent slopes, erodedMtB29461624025fzsin03119801:15840
Milton silt loam, 0 to 2 percent slopesMtA4041624015fzrin03119801:15840
Milton silt loam, 2 to 6 percent slopes, moderately erodedMtB23016128981r4bzin04119581:15840
Milton silt loam, 2 to 6 percent slopes, slightly erodedMtB1916128971r4byin04119581:15840
Milton Variant silt loam, 0 to 2 percent slopesMxA31731866355db7in05719761:15840
Milton silt loam, 0 to 2 percent slopesMtA7221614165dyzin06919801:15840
Milton silt loam, 2 to 6 percent slopesMtB5891614175dz0in06919801:15840
Milton silt loam, 6 to 15 percent slopesMtC2611614185dz1in06919801:15840
Milton-Urban land complex, 2 to 6 percent slopesYmtB20232168462yc3sin06919801:15840
Urban land-Milton complex, 2 to 6 percent slopesUmtB8032168302z69pin06919801:15840
Urban land-Milton complex, 6 to 15 percent slopesUmtC1432168312z69qin06919801:15840
Milton silt loam, 0 to 2 percent slopesMp2721619725fjxin10319771:20000
Milton silt loam, 0 to 3 percent slopesMzA5691609965djfin13919831:15840
Milton silt loam, 1 to 6 percent slopesMtB3211607375d82in14519681:15840
Milton silt loam, 2 to 6 percent slopes, slightly erodedMtB14316130461r4hrin16119581:15840
Milton silt loam, 2 to 6 percent slopes, moderately erodedMtB23016130471r4hsin16119581:15840
Milton silt loam, 0 to 2 percent slopesMsA18171612035dr3in16919801:15840
Milton silt loam, 2 to 6 percent slopes, erodedMsB212961612045dr4in16919801:15840
Milton variant silt loam, 30 to 70 percent slopesMtG9971612065dr6in16919801:15840
Milton silt loam, 6 to 12 percent slopes, erodedMsC25781612055dr5in16919801:15840
Milton variant silt loam, 0 to 2 percent slopesMsA2521612625dt0in17919881:15840
Milton clay loam, 2 to 6 percent slopes26B18518723668twmi11519801:15840
Milton loam, 0 to 2 percent slopesMnA561718375rt4oh00319981:12000
Milton silt loam, 2 to 6 percent slopesMtB8771717582w0vmoh02319971:15840
Milton silty clay loam, 6 to 12 percent slopes, erodedMvC25001717605rqnoh02319971:15840
Milton-Urban land complex, 2 to 6 percent slopesMxB4691717615rqpoh02319971:15840
Milton silt loam, 0 to 2 percent slopesMtA4631717575rqkoh02319971:15840
Milton silt loam, 2 to 6 percent slopesMoB9621720735s1roh04119971:12000
Milton-Lybrand complex, 12 to 18 percent slopes, erodedMpD24611720755s1toh04119971:12000
Milton silt loam, 6 to 12 percent slopes, erodedMoC24261720745s1soh04119971:12000
Milton silt loam, 0 to 2 percent slopesMnA18921721595s4joh04319981:12000
Milton silt loam, 2 to 6 percent slopesMnB4891721605s4koh04319981:12000
Milton silt loam, 2 to 6 percent slopes, moderately erodedMtB22721692615p41oh04719681:15840
Milton silt loam, 2 to 6 percent slopesMtB2161692602w0vmoh04719681:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMtC21111692625p42oh04719681:15840
Milton silt loam, 2 to 6 percent slopesMoB11681679192w0vmoh04919771:15840
Milton-Urban land complex, 2 to 6 percent slopesMpB4681679215mqtoh04919771:15840
Milton-Urban land complex, 6 to 12 percent slopesMpC3171679225mqvoh04919771:15840
Milton silt loam, 6 to 12 percent slopes, erodedMoC23011679205mqsoh04919771:15840
Milton silt loam, 2 to 6 percent slopesMtB19401693252w0vmoh05719741:15840
Milton soils, channery variant, 25 to 50 percent slopesMUF8391693055p5goh05719741:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMtC26241693265p64oh05719741:15840
Milton silt loam, 0 to 2 percent slopesMtA3551693245p62oh05719741:15840
Milton silt loam, 0 to 2 percent slopesMnA652644424pmkwoh06319971:12000
Morley, limestone substratum-Milton complex, 2 to 6 percent slopesMsB6076444272wvhyoh06319971:12000
Biglick-Milton complex, 2 to 6 percent slopesBgB191644370pmj4oh06319971:12000
Biglick-Milton complex, 0 to 2 percent slopesBgA125644369pmj3oh06319971:12000
Morley-Milton silt loams, 2 to 6 percent slopesMtB4351689532wvhtoh06519871:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMuC287914204771jp3voh07119731:15840
Milton silt loam, 2 to 6 percent slopesMuB74214204752w0vmoh07119731:15840
Milton silt loam, 2 to 6 percent slopes, moderately erodedMuB256214204761jp3toh07119731:15840
Milton silt loam, 12 to 18 percent slopes, moderately erodedMuD235514204781jp3woh07119731:15840
Milton clay loam, 6 to 12 percent slopes, severely erodedMwC316014204791jp3xoh07119731:15840
Milton silt loam, 2 to 6 percent slopesMnB3671679865msxoh07719881:15840
Milton silt loam, 0 to 2 percent slopesMnA1316059951qx59oh07719881:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMoC22961711425r2qoh09119771:15840
Milton silt loam, 12 to 18 percent slopes, moderately erodedMoD22371711435r2roh09119771:15840
Milton silt loam, 2 to 6 percent slopesMoB2021711415r2poh09119771:15840
Milton silt loam, 1 to 4 percent slopesMnB3911712065r4soh10119841:15840
Milton silt loam, 2 to 6 percent slopesMpB49171695212w0vmoh10919731:15840
Milton silt loam, 0 to 2 percent slopesMpA35571695205pddoh10919731:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMpC26891695235pdhoh10919731:15840
Milton silt loam, 2 to 6 percent slopes, moderately erodedMpB22141695225pdgoh10919731:15840
Milton silt loam, 12 to 18 percent slopes, moderately erodedMpD21221695245pdjoh10919731:15840
Milton silt loam, 2 to 6 percent slopesMsB22801702862w0vmoh11319691:15840
Milton silt loam, 2 to 6 percent slopes, moderately erodedMsB219271702875q64oh11319691:15840
Milton silt loam, 6 to 12 percent slopes, moderately erodedMsC212211702885q65oh11319691:15840
Milton silt loam, 0 to 2 percent slopesMsA10051702855q62oh11319691:15840
Milton-Urban land complex, undulatingMuB9961702915q68oh11319691:15840
Milton silty clay loam, 6 to 18 percent slopes, severely erodedMtD35211702905q67oh11319691:15840
Milton-Urban land complex, rollingMuC4251702925q69oh11319691:15840
Milton silt loam, 12 to 18 percent slopes, moderately erodedMsD21751702895q66oh11319691:15840
Milton-Urban land complex, hillyMuD721702935q6boh11319691:15840
Milton silt loam, 2 to 6 percent slopesMtB21401703975q9poh12319811:15840
Milton silt loam, 2 to 6 percent slopes, erodedMuB2673623349nxn1oh13520051:12000
Milton silt loam, 6 to 12 percent slopes, erodedMuC2444623351nxn3oh13520051:12000
Milton silt loam, 2 to 6 percent slopesMuB3312108632w0vmoh13520051:12000
Milton silt loam, 0 to 2 percent slopesMuA20321086472f2oh13520051:12000
Milton silt loam, 12 to 18 percent slopes, erodedMuD2200725929scd2oh13520051:12000
Milton silt loam, 18 to 25 percent slopes, erodedMuE2107725998scg9oh13520051:12000
Milton silt loam, 20 to 35 percent slopes, erodedMoE23731709235qvnoh14119971:15840
Milton silt loam, 2 to 6 percent slopesMoB841709212w0vmoh14119971:15840
Milton silt loam, 6 to 12 percent slopes, erodedMoC2801709225qvmoh14119971:15840
Milton silt loam, 0 to 2 percent slopesMnA29191699955pwqoh14719781:15840
Milton silt loam, 2 to 6 percent slopesMnB20021699965pwroh14719781:15840
Milton loam, 0 to 2 percent slopesMlA8115922021qftcoh14719781:15840
Morley, limestone substratum-Milton complex, 2 to 6 percent slopesMsB4515921742wvhyoh14719781:15840
Lykens-Milton silt loams, 2 to 6 percent slopesLzB2915922161qfttoh14719781:15840
Milton silt loam, 2 to 6 percent slopesMoB3971700522w0vmoh14919771:15840
Milton loam, 0 to 2 percent slopesMnA12011682525n2hoh17320001:12000
Milton loam, 2 to 6 percent slopesMnB1641682535n2joh17320001:12000
Lykens-Milton silt loams, 2 to 6 percent slopesLzB22531696315phzoh17519801:15840
Milton silt loam, 2 to 6 percent slopesMoB7441696405pj8oh17519801:15840
Milton silt loam, 0 to 2 percent slopesMoA5081696395pj7oh17519801:15840
Morley-Milton silt loams, 2 to 6 percent slopesMsB8915426612wvhtoh17519801:15840
Biglick-Milton complex, 2 to 6 percent slopesBkB5815426331ns7coh17519801:15840
Morley, limestone substratum-Milton complex, 2 to 6 percent slopesMtB1315426412wvhyoh17519801:15840
Milton silt loam, 0 to 2 percent slopesMzaA173425524g8slwi03919671:15840
Milton silt loam, 2 to 6 percent slopes, erodedMzaB2150425525g8smwi03919671:15840
Milton silt loam, 6 to 20 percent slopes, erodedMzaD279425526g8snwi03919671:15840

Map of Series Extent

Approximate geographic distribution of the MILTON 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 .