Official Series Description


Lab Data Summary

Aggregate lab data for the COLAND soil series. This aggregation is based on all pedons with a current taxon name of COLAND, 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 COLAND 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
103UMN3288S1980MN063001(3288)Coland3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7241821,-95.0551682
104X53-135-2S1984IA105002Coland2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0121562,-91.1582544
104X53-135-1S1985IA105009Coland2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0081832,-91.1549697

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COLAND 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 COLAND 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 COLAND 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 COLAND 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 COLAND 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 COLAND 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 COLAND 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 mountains figure.

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Click the image to view it full size.

Soil series sharing subgroup-level classification with COLAND, 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-2010-09-02-10 | Emmet County - 1997

    Typical pattern of soils and parent material in the Millington-Spillville-Colo association (Soil Survey of Emmet County, Iowa; 1997).

  2. IA-2010-09-02-11 | Humboldt County - 2005

    Typical pattern of soils and parent material in the Spillville-Ridgeport-Coland association (Soil Survey of Humboldt County, Iowa; 2005).

  3. IA-2010-09-02-14 | Humboldt County - 2005

    Typical pattern of soils and parent material in the Lester-Spillville-Coland association (Soil Survey of Humboldt County, Iowa; 2005).

  4. IA-2010-09-09-07 | Bremer County - 2009

    Typical pattern of soils and parent material in the Spillville-Waukee-Coland association (Soil Survey of Bremer County, Iowa; 2009).

  5. IA-2010-09-09-22 | Webster County - 2008

    Typical pattern of soils and parent material in the Clarion-Coland association (Soil Survey of Webster County, Iowa; 2008).

  6. IA-2010-09-09-23 | Webster County - 2008

    Typical pattern of soils and parent material in the Lester-Coland-Wadena association (Soil Survey of Webster County, Iowa; 2008).

  7. IA-2011-05-31-15 | Delaware County - 1986

    Pattern of soils and parent material in the Spillville-Saude-Marshan association (Soil Survey of Delaware County, Iowa; 1986).

  8. IA-2011-05-31-28 | Floyd County - 1995

    Pattern of soils and parent material in the Saude-Coland-Lawler association (Soil Survey of Floyd County, Iowa; 1995).

  9. IA-2011-05-31-29 | Floyd County - 1995

    A cross section showing the parent material of some of the soils in Floyd County (Soil Survey of Floyd County, Iowa; 1995).

  10. IA-2011-05-31-31 | Greene County - 1985

    Pattern of soils and parent material in the Mayer-Biscay-Coland association (Soil Survey of Greene County, Iowa; 1985).

  11. IA-2011-05-31-32 | Greene County - 1985

    Pattern of soils and parent material in the Clarion-Coland-Storden association (Soil Survey of Greene County, Iowa; 1985).

  12. IA-2011-05-31-42 | Hardin County - 1985

    Pattern of soils and parent material in the Coland-Saude-Spillville association (Soil Survey of Hardin County, Iowa; 1985).

  13. IA-2011-05-31-46 | Hardin County - 1985

    Pattern of soils and parent material in the Hayden-Lester-Le Sueur association (Soil Survey of Hardin County, Iowa; 1985).

  14. IA-2011-06-01-29 | Osceola County - 1988

    Typical pattern of soils and parent material in the Wadena-Coland- Cylinder association (Soil Survey of Osceola County, Iowa; 1988).

  15. IA-2011-06-01-33 | Pocahontas County - 1985

    Typical pattern of soils and parent material in the Havelock-Coland-Estherville association (Soil Survey of Pocahontas County, Iowa; 1985).

  16. IA-2011-06-01-50 | Winnebago County - 1987

    Pattern of soils and parent material in the Clarion-Canisteo-Nicollet association (Soil Survey of Winnebago County, Iowa; 1987).

Map Units

Map units containing COLAND 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
Spillville-Coland-Shandep complex, 0 to 2 percent slopes, frequently flooded1585174934132862y8ppia01320011:12000
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58556974132672xl24ia01320011:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13514134132212xl4cia01320011:12000
Spillville, occasionally flooded-Coland, occasionally flooded-Urban land complex, 0 to 2 percent slopes4585386413321fw2yia01320011:12000
Coland, occasionally flooded-Urban land complex, 0 to 2 percent slopes413522450267h3jria01320011:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135656425502342wd8ria01519771:15840
Coland-Spillville complex, 2 to 5 percent slopes585B38882550284fjf3ia01519771:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded1135386525502332wd8via01519771:15840
Spillville-Coland-Shandep complex, 0 to 2 percent slopes, frequently flooded1585657016895852y8ppia01720081:12000
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded585259115860112xl24ia01720081:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135237515859752xl4cia01720081:12000
Spillville-Coland complex, 0 to 2 percent slopes, frequently flooded1585140914032062y8psia01919781:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58563574032502xl24ia01919781:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135183254033472xl4cia02319781:15840
Spillville-Coland complex, 0 to 2 percent slopes, frequently flooded158574564033522y8psia02319781:15840
Spillville-Coland complex, 0 to 2 percent slopes5853309403420fjskia02319781:15840
Coland, occasionally flooded-Terril complex, 1 to 4 percent slopes201B7404033752y8r6ia02319781:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded9361924747862xl24ia02319781:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13594964034572wd8ria02519791:15840
Coland clay loam, 2 to 4 percent slopes135B1060403458fjtsia02519791:15840
Coland-Spillville complex, 2 to 5 percent slopes585B310403489fjvsia02519791:15840
Coland-Spillville complex, channeled, 2 to 5 percent slopes1585B302403464fjtzia02519791:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13552264035072wd8ria02719791:15840
Coland-Spillville complex, 2 to 5 percent slopes201B4084403520fjwsia02719791:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13557364037722wd8ria03319781:15840
Coland-Hanlon complex, 0 to 2 percent slopes9361766403895fk8wia03319781:15840
Coland-Hanlon complex, channeled, 0 to 2 percent slopes1936824403800fk5tia03319781:15840
Coland-Terril complex, 1 to 4 percent slopes201B679403802fk5wia03319781:15840
Coland clay loam, 0 to 2 percent slopes1354853403904fk95ia03519871:15840
Terril-Coland, occasionally flooded complex, 2 to 9 percent slopes438C20984039072y6bcia03519871:15840
Spillville-Coland complex, 1 to 5 percent slopes585B9924039472zv9via03519871:15840
Spillville-Coland complex, 0 to 2 percent slopes, frequently flooded158561524039822y8psia03719891:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58559914040572xl24ia03719891:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13517894039782xl4cia03719891:15840
Spillville-Coland complex, 0 to 2 percent slopes, occasionally flooded585326031019462y6b5ia04120021:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded1353182399286fdh6ia04120021:12000
Coland-Terril complex, 2 to 5 percent slopes201B2885399302fdhqia04120021:12000
Spillville-Coland complex, channeled, 0 to 2 percent slopes, frequently flooded158522553992942y6b6ia04120021:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13581874045652wd8ria04919801:15840
Coland-Terril complex, 2 to 5 percent slopes201B5161404582fl01ia04919801:15840
Spillville-Coland complex, channeled, 0 to 2 percent slopes15851215404570fkznia04919801:15840
Spillville-Coland complex, channeled 0 to 2 percent slopes15854362404986flf2ia05519841:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58533064050662xl24ia05519841:15840
Coland clay loam, 0 to 2 percent slopes1353628405207fln6ia05719801:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135207918690422wd8ria05920111:12000
Coland-Spillville complex, 1 to 5 percent slopes, occasionally flooded586B556186904820qwwia05920111:12000
Coland-Spillville complex, 2 to 5 percent slopes585B2226405594fm1pia06319891:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded1355774055022wd8ria06319891:15840
Coland-Spillville complex, channeled, 0 to 2 percent slopes1585409405515flz4ia06319891:15840
Coland clay loam, channeled, 0 to 2 percent slopesC1353347405833fm9dia06519751:15840
Spillville-Coland-Shandep complex, 0 to 2 percent slopes, frequently flooded1585137124753512y8ppia06519751:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13510384056942xl4cia06519751:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13545064058372xl4cia06719891:15840
Spillville-Hanlon-Coland complex, channeled, 0 to 3 percent slopes19361788405864fmbdia06719891:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58511424060552xl24ia06719891:15840
Coland, occasionally flooded-Terril complex, 1 to 4 percent slopes201B2144058722y8r6ia06719891:15840
Coland-Turlin complex, 0 to 2 percent slopes235424792822p6wvia06719891:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135119554048642wd8ria06919771:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded113543014048572wd8via06919771:15840
Coland-Terril complex, 1 to 5 percent slopes201B2709404882fl9qia06919771:15840
Spillville-Coland complex, 0 to 2 percent slopes, frequently flooded15854124747092y8psia06919771:15840
Coland-Spillville complex, 1 to 5 percent slopes585B7171406245fmqpia07319831:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13564634061892wd8ria07319831:15840
Fluvaquents-Coland complex, 0 to 3 percent slopes23155423406200fmp7ia07319831:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded113527044061872wd8via07319831:15840
Coland-Spillville complex, channeled, 2 to 5 percent slopes1585B521406196fmp3ia07319831:15840
Coland-Spillville complex, channeled, 0 to 2 percent slopes1585492406195fmp2ia07319831:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13521094062782xl4cia07519731:15840
Spillville-Coland complex, 0 to 2 percent slopes585824746682p230ia07519731:15840
Spillville-Coland complex, 0 to 2 percent slopes, frequently flooded1585424746622y8psia07519731:15840
Spillville-Coland complex, channeled, 0 to 2 percent slopes15853110406461fmynia07919841:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13524244064532wd8ria07919841:15840
Coland-Terril complex, 1 to 5 percent slopes201B1198406468fmywia07919841:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13541564065232wd8ria08119871:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded113511174065182wd8via08119871:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13589504066142wd8ria08319821:15840
Coland-Terril complex, 2 to 5 percent slopes201B6993406637fn4bia08319821:15840
Coland-Spillville-Hanlon complex, channeled, 0 to 2 percent slopes19364003406636fn49ia08319821:15840
Coland-Spillville-Hanlon complex, 0 to 2 percent slopes9361277406708fn6mia08319821:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58538974069692xl24ia08919691:15840
Coland - Spillville complex, channeled, 0 to 2 percen slopes15853124745712p1zwia08919691:15840
Spillville-Coland complex, channeled, 0 to 2 percent slopes, frequently flooded15855137447466h0mdia09119981:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded1359954474872wd8ria09119981:12000
Coland-Terril complex, 2 to 5 percent slopes201B766447634h0stia09119981:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13536994075982wd8ria09919751:15840
Coland clay loam, 2 to 5 percent slopes135B1391407599fp4cia09919751:15840
Spillville-Coland Complex, channeled, 0 to 2 percent slopes, frequently flooded158540325065332q5t0ia09919751:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13515034079432xl4cia10319791:15840
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded58555284081822xl24ia10519881:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13543914083412wd8ria10919801:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded113512684083382wd8via10919801:15840
Coland-Urban land complex, 0 to 2 % slopes, rarely flooded413515126064492qcs0ia11319701:15840
Coland-Perks-Lawson complex, frequently flooded, 0 to 2 percent slopes15398650408723fq9mia11519841:15840
Coland clay loam, 0 to 2 percent slopes1352527408717fq9fia11519841:15840
Coland-Terril complex, 2 to 5 percent slopes201B1913409446fr1yia12719781:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13516524094162wd8ria12719781:15840
Coland-Turlin complex, 0 to 2 percent slopes2353219409652fr8lia13119711:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13515334096222xl4cia13119711:15840
Coland-Turlin complex, channeled, 0 to 2 percent slopesC2351268409733frc6ia13119711:15840
Spillville-Hanlon-Coland complex, channeled, 0 to 3 percent slopes193613624745792p204ia13119711:15840
Coland clay loam, rarely flooded, 0 to 2 percent slopes31354307409966frlqia13919861:15840
Coland clay loam, 2 to 5 percent slopes135B1856409919frk6ia13919861:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135561024992282wd8ria14319851:15840
Coland-Terril complex, 2 to 5 percent slopes201B332410116frrkia14319851:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13563284103702wd8ria15119821:15840
Coland clay loam, 2 to 5 percent slopes135B556410371fs0sia15119821:15840
Coland-Spillville complex, channeled, 2 to 5 percent slopes1585B81410378fs10ia15119821:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135111964128312wd8ria15319931:12000
Spillville-Coland complex, channeled, 0 to 2 percent slopes15858861412839fvldia15319931:12000
Coland, occasionally flooded-Terril complex, 2 to 5 percent slopes201B3514412867fvm9ia15319931:12000
Coland, occasionally flooded-Terril-Urban land complex, 2 to 5 percent slopes4201B441412929fvp9ia15319931:12000
Coland, occasionally flooded-Urban land complex, 0 to 2 percent slopes4135193412907fvnlia15319931:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13527054107632wd8ria16119751:15840
Coland clay loam, 2 to 4 percent slopes135B1202410764fsfgia16119751:15840
Coland-Spillville complex, channeled, 2 to 5 percent slopesC201B785410850fsj7ia16119751:15840
Coland-Spillville complex, 2 to 5 percent slopes201B457410775fsftia16119751:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135113974112792wd8ria16919811:15840
Coland-Terril complex, 1 to 5 percent slopes201B4345411293fszjia16919811:15840
Spillville-Coland complex, channeled, 0 to 2 percent slopes15853241411285fsz8ia16919811:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13548297979222wd8ria18720061:12000
Coland-Terril complex, 1 to 5 percent slopes201B875797929vs9nia18720061:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13527384122812wd8ria18919841:15840
Coland clay loam, 2 to 5 percent slopes135B931412282fv0fia18919841:15840
Coland-Spillville complex, 0 to 5 percent slopes585B375412317fv1kia18919841:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded135254413990862xl4cia19120051:12000
Turlin-Coland complex, 0 to 3 percent slopes, occasionally flooded2355061014251131dsia19120051:12000
Coland-Spillville complex, 0 to 2 percent slopes, occasionally flooded585346025814322xl24ia19520121:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded13539104126552wd8ria19719881:15840
Spillville-Coland complex, channeled, 0 to 2 percent slopes15853195412662fvdpia19719881:15840
Coland-Terril complex, 1 to 5 percent slopes201B1601412669fvdxia19719881:15840
Coland clay loam, 0 to 2 percent slopes, frequently flooded113512064126532wd8via19719881:15840
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183324633962622wd8rmn01519841:20000
Coland clay loam, 0 to 2 percent slopes, frequently floodedCU10613964082wd8vmn01919871:12000
Coland clay loam, 0 to 2 percent slopes, occasionally floodedCL3063964042wd8rmn01919871:12000
Coland clay loam, 0 to 2 percent slopes, occasionally floodedL219A983916782922wd8rmn03320081:12000
Coland clay loam, 0 to 2 percent slopes, frequently floodedL224A456016782932wd8vmn03320081:12000
Coland, frequently flooded-Spillville, occasionally flooded complex, 0 to 2 percent slopes1027A686113849642y8pjmn03920051:12000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183483653970882wd8vmn04319891:20000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183378993970872wd8rmn04319891:20000
Coland, frequently flooded-Spillville, occasionally flooded complex, 0 to 2 percent slopes1027A307816707272y8pjmn04920071:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183350433984932wd8rmn06319841:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183444893984942wd8vmn06319841:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183428033991542wd8vmn08519931:20000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded18339973991532wd8rmn08519931:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183478154000322wd8vmn09119851:20000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183349864000312wd8rmn09119851:20000
Coland, frequently flooded-Spillville, occasionally flooded complex, 0 to 2 percent slopes197449014004332y8pjmn09919861:15840
Coland clay loam, 0 to 2 percent slopes, frequently floodedL224A2323995792wd8vmn10120081:12000
Coland clay loam, 0 to 2 percent slopes, occasionally floodedL126A39247807862wd8rmn10520041:12000
Coland clay loam, 0 to 2 percent slopes, frequently floodedL127A25007807872wd8vmn10520041:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183384523740612wd8rmn12720081:12000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183460623740622wd8vmn12720081:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded18339664360532wd8rmn12919951:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded18349374360542wd8vmn12919951:20000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183315884315222wd8rmn14319911:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183410624315232wd8vmn14319911:20000
Coland clay loam, 0 to 2 percent slopes, occasionally floodedL126A32664554862wd8rmn16120011:12000
Coland clay loam, 0 to 2 percent slopes, frequently floodedL127A31904554872wd8vmn16120011:12000
Hanlon, rarely flooded-Coland, occasionally flooded, complex, 0 to 3 percent slopesL125A996455485h8z2mn16120011:12000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded183394974289252wd8rmn16519871:20000
Coland clay loam, 0 to 2 percent slopes, frequently flooded183427264289262wd8vmn16519871:20000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded66076188625337382qp9gmo13919751:24000
Coland clay loam, 0 to 2 percent slopes, occasionally flooded6607654025337372qp9gmo21919751:24000
Orion-Coland complex, 0 to 2 percent slopes, occasionally flooded1628A73117010101v319wi09320061:12000

Map of Series Extent

Approximate geographic distribution of the COLAND 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 .