Official Series Description


Lab Data Summary

Aggregate lab data for the FEATHERLEGS soil series. This aggregation is based on all pedons with a current taxon name of FEATHERLEGS, 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 FEATHERLEGS were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FEATHERLEGS 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 FEATHERLEGS 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 FEATHERLEGS 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 FEATHERLEGS 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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Competing Series

Soil series competing with FEATHERLEGS 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 FEATHERLEGS 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 FEATHERLEGS 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 FEATHERLEGS, 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

No block diagrams are available.

Map Units

Map units containing FEATHERLEGS 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
Featherlegs, very stony-Motoqua families-Rock outcrop complex, 15 to 60 percent slopes112365512361k64sut6461:24000
Featherlegs, very stony-Motoqua families-Rock outcrop complex, 1 to 15 percent slopes24432512360k64rut6461:24000
Brownrigg-Featherlegs-Wolf complex, 10 to 40 percent slopes1101208349533cqq8wy02719931:24000
Featherlegs-Wolf-Brownrigg complex, 3 to 10 percent slopes125533349563cqr7wy02719931:24000
Featherlegs-Wolf loams, 6 to 10 percent slopes124141349561cqr5wy02719931:24000
Featherlegs-Wolf loams, 0 to 6 percent slopes123100349559cqr3wy02719931:24000
Brown-Featherlegs-Recluse complex, 5 to 40 percent slopes119544831044723hq2wy03119981:24000
Featherlegs-Recluse loams, 3 to 15 percent slopes155297191045103hr9wy03119981:24000
Featherlegs-Greenhope-Curabith fine sandy loams, 3 to 15 percent slopes152258911045073hr6wy03119981:24000
Greenhope-Featherlegs complex, 0 to 6 percent slopes167153651045223hrpwy03119981:24000
Featherlegs-Curabith fine sandy loams, 0 to 3 percent slopes15189031045063hr5wy03119981:24000
Featherlegs-Recluse loams, 3 to 6 percent slopes15441031045093hr8wy03119981:24000
Featherlegs-Recluse loams, 0 to 3 percent slopes15321441045083hr7wy03119981:24000
Featherlegs-Bayard fine sandy loams, 0 to 6 percent slopes15014101045053hr4wy03119981:24000
Featherlegs fine sandy loam, wet, 0 to 3 percent slopes1496171045033hr2wy03119981:24000
Brown-Featherlegs-Recluse complex, 5 to 40 percent slopes2461215879971q9fqwy60119911:24000
Brown-Featherlegs-Recluse complex, 5 to 40 percent slopes115352316696631t1f3wy60920061:24000
Featherlegs-Recluse loams, 3 to 15 percent slopes146179816696841t1fswy60920061:24000
Treoff-Featherlegs complex, 10 to 55 percent slopes, extremely stony7107238366920b31wy63319871:24000
Brownrigg-Featherlegs-Wolf complex, 10 to 40 percent slopes4E170961048923j4mwy71519741:20000
Featherlegs-Wolf loams, 0 to 6 percent slopes11B162681048493j37wy71519741:20000
Featherlegs-Wolf-Brownrigg complex, 3 to 10 percent slopes12C81781048513j39wy71519741:20000
Featherlegs-Wolf loams, 6 to 10 percent slopes11C19641048503j38wy71519741:20000
Brown-Featherlegs-Recluse complex, 5 to 40 percent slopes40135714148101jh71wy71519741:20000
Featherlegs-Recluse loams, 3 to 15 percent slopes5414014148231jh7gwy71519741:20000
Featherlegs-Bayard fine sandy loams, 0 to 6 percent slopes434914148131jh74wy71519741:20000
Treoff-Featherlegs complex, 10 to 55 percent slopes, extremely stony7103769185674620b31wy71920131:24000
Featherlegs-Naturita-Willowman complex, 0 to 6 percent slopes7022334185674420b2zwy71920131:24000
Featherlegs, extremely stony-Moskee sandy loams, 6 to 15 percent slopes7032098185674520b30wy71920131:24000
Featherlegs, extremely stony-Moskee sandy loams, 0 to 6 percent slopes7121163186814920pywwy71920131:24000
Featherlegs fine sandy loam, 3 to 6 percent slopes628624186813720pyhwy71920131:24000

Map of Series Extent

Approximate geographic distribution of the FEATHERLEGS 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 .