Official Series Description


Lab Data Summary

Aggregate lab data for the CLARINDA soil series. This aggregation is based on all pedons with a current taxon name of CLARINDA, 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 CLARINDA 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
107B40A1391S1953IA165004Clarinda6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.601944,-95.0594406
107B13N0535S2012IA009001Clarinda6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.5208357,-94.9748058
108C84P042883IA107005Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4302788,-92.2183304
108D08N06361992IA159102Clarinda7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8138694,-94.447775
108D08N0633S2008IA003001Clarinda7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0231705,-94.7316666
108D08N0634S2008IA003002Clarinda7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0868683,-94.7394562
109M88129041988MO129004mClarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5055083,-93.395075
109M88129061988MO129006Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5308342,-93.3911133
109M89197051989MO197005Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9162472,-93.9829222
109M89197061989MO197006Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9162472,-93.9829222
109M89197951989MO197095Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9162472,-93.9829222
109M07227012007MO227001Clarinda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4147224,-94.2494431
109M07227022007MO227002Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.414444,-94.2497253
109M08129012008MO129001Clarinda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4416656,-93.4680557
109M08129022008MO129002Clarinda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.478611,-93.4594421
109M08129032008MO129003Clarinda4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4783325,-93.4588852
109M08171082008MO171001Clarinda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5740667,-93.0839583
10984P042983IA185001Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.730835,-93.3775024
10984P043283IA185004Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7836113,-93.4758301
10985P030684IA1770014Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7166672,-91.9416656
10985P052584IA1850031Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7694435,-93.4833298
10985P052684IA1850032Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7694435,-93.4833298
10985P052984IA1850043Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7694435,-93.4833298
10986P039285IA1770015Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7166672,-91.9333344
10986P041485IA1850053Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8919449,-93.1755524
10988P059287IA159005Clarinda6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8739052,-94.2424545
10988P059387IA159006Clarinda6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8416672,-94.0749969
10987P039087IA1770017Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7116661,-91.9477768
10987P039187IA1770018Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7116661,-91.9472198
10987P039287IA1770019Clarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7116661,-91.9463882
10987P039387IA177007AClarinda5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7119446,-91.9463882
10908N0635S2008IA053001Clarinda7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.839695,-93.7671967
10908N0638S2008MO227001Clarinda7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.4145851,-94.2497482
115BM87171121987MO171012Clarinda3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9672203,-92.3450012

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CLARINDA 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 CLARINDA 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 CLARINDA 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 CLARINDA 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 CLARINDA 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 CLARINDA 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 CLARINDA 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with CLARINDA, 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-2010-09-02-17 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Haig-Grundy-Clarinda association (Soil Survey of Jefferson County, Iowa; 1999).

  2. IA-2010-09-02-19 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Taintor-Mahaska-Otley association (Soil Survey of Jefferson County, Iowa; 1999).

  3. IA-2010-09-02-20 | Keokuk County - 2003

    Typical pattern of soils and parent material in the Taintor-Mahaska association (Soil Survey of Keokuk County, Iowa; 2003).

  4. IA-2010-09-02-21 | Keokuk County - 2003

    Typical pattern of soils and parent material in the Otley-Mahaska-Nira association (Soil Survey of Keokuk County, Iowa; 2003).

  5. IA-2010-09-03-01 | Van Buren County - 2004

    Typical pattern of soils and parent material in the Haig-Grundy-Clarinda association (Soil Survey of Van Buren County, Iowa; 2004).

  6. IA-2010-09-03-03 | Van Buren County - 2004

    Typical pattern of soils and parent material in the Edina-Seymour-Clarinda association (Soil Survey of Van Buren County, Iowa; 2004).

  7. IA-2010-09-09-02 | Adams County - 2008

    Typical pattern of soils and parent material in the Sharpsburg-Macksburg association (Soil Survey of Adams County, Iowa; 2008).

  8. IA-2010-09-09-03 | Adams County - 2008

    Typical pattern of soils and parent material in the Sharpsburg-Shelby association (Soil Survey of Adams County, Iowa; 2008).

  9. IA-2011-05-31-04 | Audubon County - 1984

    Pattern of soils and parent material in the Marshall-Exira association (Soil Survey of Audubon County, Iowa; 1984).

  10. IA-2011-05-31-09 | Davis County - 1991

    Typical pattern of soils and parent material in the Edina-Seymour-Clarinda association (Soil Survey of Davis County, Iowa; 1991).

  11. IA-2011-05-31-55 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Taintor-Mahaska-Otley association (Soil Survey of Jefferson County, Iowa; 1999).

  12. IA-2011-05-31-58 | Jefferson County - 1999

    Typical pattern of soils and parent material in the Haig-Grundy-Clarinda association (Soil Survey of Jefferson County, Iowa; 1999).

  13. IA-2011-06-01-12 | Lucas County - 1999

    Typical pattern of soils and parent material in the Grundy-Haig-Arispe association (Soil Survey of Lucas County, Iowa; 1999).

  14. IA-2011-06-01-13 | Lucas County - 1999

    Typical pattern of soils and parent material in the Arispe-Lamoni-Shelby association (Soil Survey of Lucas County, Iowa; 1999).

  15. IA-2011-06-01-38 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Nira-Sharpsburg-Shelby association (Soil Survey of Ringgold County, Iowa; 1992).

  16. IA-2011-06-01-41 | Ringgold County - 1992

    Typical pattern of soils and parent material in the Arispe-Shelby-Lamoni association (Soil Survey of Ringgold County, Iowa; 1992).

Map Units

Map units containing CLARINDA 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
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D243574021592y6bsia00119761:15840
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C242204021582y6bpia00119761:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C16444021572y6bria00119761:15840
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, eroded469C2595317118512y6bwia00320081:12000
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C2501514048432y6bpia00320081:12000
Clarinda silty clay loam, 9 to 14 percent slopes222D159319078562218ria00320081:12000
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D2120614048452y6bsia00320081:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, severely eroded469C321819078652y6bxia00320081:12000
Clarinda silty clay, 9 to 14 percent slopes, severely eroded222D313614048472y6btia00320081:12000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C2265064026612tfyzia00719701:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C25964026602tfyyia00719701:15840
Clarinda soils, 5 to 9 percent slopes, severely eroded222C31424402662fj03ia00719701:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D24054026632tfzcia00719701:15840
Clarinda silty clay loam, deep loess, 9 to 14 percent slopes, eroded222D28544027592y6bqia00919821:15840
Clarinda silty clay loam eroded-severely eroded complex, 9 to 14 percent slopes229D2119424849222y6bnia02920101:12000
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, erodedY222D2117418680352y6bsia02920101:12000
Clarinda silty clay loam, 5 to 9 percent slopes, erodedY222C291018680322y6bpia02920101:12000
Clarinda silty clay loam eroded-severely eroded complex, 5 to 9 percent slopes229C214724992132y6c2ia02920101:12000
Clarinda silty clay, 9 to 14 percent slopes, severely erodedY222D3925070192y6btia02920101:12000
Clarinda silty clay loam, deep loess, 9 to 14 percent slopes, erodedZ222D2225070202y6bqia02920101:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, eroded469C2125070142y6bwia02920101:12000
Lamoni-Clarinda-Shelby complex, 5 to 9 percent slopes, severely eroded469C3125070132y6bxia02920101:12000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C2135234041202tfyzia03919871:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C10024041192tfyyia03919871:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D29424041222tfzcia03919871:15840
Clarinda silty clay, 5 to 9 percent slopes, severely eroded222C37334041212tfzdia03919871:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C2146194046652tfyzia05119881:15840
Clarinda silty clay loam, 5 to 9 percent slopes, severely eroded222C31924046662tfz9ia05119881:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C292384047772tfyzia05319861:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D225934047782tfzcia05319861:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C24754047762tfyyia05319861:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C1134405229flnxia05719801:15840
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D212984063592y6bsia07719681:15840
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C22024063582y6bpia07719681:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C21286406830fnbkia08719821:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C810406829fnbjia08719821:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C2611407635fp5jia09919751:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D2496407636fp5kia09919751:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C275974077572tfyzia10119921:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C8044077562tfyyia10119921:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C2906447055h064ia10719981:12000
Clarinda silty clay loam, 5 to 9 percent slopes222C155447054h063ia10719981:12000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C215724084482tfyzia11119761:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C13454084472tfyyia11119761:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C279694088872tfyzia11719911:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D27164088892tfzcia11719911:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C6854088862tfyyia11719911:15840
Clarinda silty clay loam, 5 to 9 percent slopes, severely eroded222C32184088882tfz9ia11719911:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C7864091762y6bria12119681:15840
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C25524091772y6bpia12119681:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C21716409293fqx0ia12319711:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D21318409294fqx1ia12319711:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C727409292fqwzia12319711:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C29144127502tfyzia12519761:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C1314127492tfyyia12519761:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D21334409453fr25ia12719781:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C226694097572tfyzia13519821:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D28824097582tfzcia13519821:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C3224097562tfyyia13519821:15840
Clarinda silty clay loam, deep loess, 9 to 14 percent slopes, erodedZ222D257354098482y6bqia13719871:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately erodedZ222C22633216638frgwia13719871:15840
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D213132166422y6bsia13719871:15840
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C2174098472y6bpia13719871:15840
Clarinda silty clay loam, deep loess, 9 to 14 percent slopes, eroded222D27344104642y6bqia15519861:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D22859410565fs71ia15719781:15840
Clarinda silty clay loam, 5 to 9 percent slopes moderately eroded222C2556410564fs70ia15719781:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C275410563fs6zia15719781:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C272954106722tfyzia15919871:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C33804106712tfyyia15919871:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D27684106742tfzcia15919871:15840
Clarinda silty clay loam, 9 to 14 percent slopes222D6744106732tfzbia15919871:15840
Clarinda silty clay loam, deep loess, 9 to 14 percent slopes, eroded222D24984374382y6bqia16520051:12000
Clarinda silty clay loam, 9 to 14 percent slopes moderately eroded222D2181411430ft3yia17119891:15840
Clarinda silty clay loam, 5 to 9 percent slopes, eroded222C257144116002y6bpia17319891:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C31394115992y6bria17319891:15840
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D22724116012y6bsia17319891:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C294664116892tfyzia17519751:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C56714116882tfyyia17519751:15840
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D218744116912y6bsia17519751:15840
Clarinda silty clay loam, 9 to 14 percent slopes222D1219411690ftdbia17519751:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C232764130352tfyzia17719941:12000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C217364117812tfyzia17919781:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C7754117802tfyyia17919781:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C213354119092tfyzia18119751:15840
Clarinda silty clay loam, dissected till plain, 9 to 14 percent slopes, eroded222D212994119102y6bsia18119751:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C6374119082tfyyia18119751:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C21601412021ftr0ia18319831:15840
Clarinda silty clay loam, 5 to 9 percent slopes, severely eroded222C31178412022ftr1ia18319831:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D2932412023ftr2ia18319831:15840
Clarinda silty clay loam, 9 to 14 percent slopes, severely eroded222D3376412024ftr3ia18319831:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded222C23171918604682tfyzia18519661:15840
Clarinda silty clay loam, 5 to 9 percent slopes222C237124225452tfyyia18519661:15840
Clarinda silty clay, 5 to 9 percent slopes, severely eroded222C3192518604692tfzdia18519661:15840
Clarinda silty clay loam, 9 to 14 percent slopes, moderately eroded222D2142618604702tfzcia18519661:15840
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded30047105225310422tfyzmo04919811:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded30047405125310432tfyzmo06319741:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded3004773125310442tfyzmo07519821:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, eroded301135725313002y6bvmo07519821:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, severely eroded301142025313022qnrrmo07519821:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, eroded301131625312972y6bvmo08119751:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, severely eroded30114725313032qnrrmo08119751:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded30047332725310452tfyzmo12919931:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded3004788525310462tfyzmo14719831:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, eroded3011317225312982y6bvmo14719831:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded30047916425310472tfyzmo17119891:24000
Clarinda silty clay loam, 5 to 9 percent slopes, moderately eroded30047145725310412tfyzmo19719931:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, eroded30113733325312992y6bvmo22719651:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes, severely eroded30114358325313012qnrrmo22719651:24000
Lagonda and Clarinda soils, 5 to 11 percent slopes301122198887697ysqdmo22719651:24000

Map of Series Extent

Approximate geographic distribution of the CLARINDA 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 .