Official Series Description


Lab Data Summary

Aggregate lab data for the TONGUE RIVER soil series. This aggregation is based on all pedons with a current taxon name of TONGUE RIVER, 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 TONGUE RIVER 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with TONGUE RIVER, 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 TONGUE RIVER 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
Tongue River loam, 5 to 60 percent slopesTrF1738509802k3h7co66119681:31680
Tongue River loam, 10 to 50 percent slopesTrF5448498231jqfzco66219681:24000
Stemple, stony-Tongue River-Yellowmule complex, 8 to 45 percent slopes, landslides816F707224853042pf53mt61220111:24000
Tongue River-Yellowmule-Helmville complex, 15 to 50 percent slopes, landslides728F165525153832ppjdmt61220111:24000
Leavitt-Tongue River-Knep complex, 4 to 35 percent slopes, landslides819E137224850892pdy5mt61220111:24000
Tongue River-Inabnit, very stony-Doolittle complex, 25 to 60 percent slopes822F114324864512pgc3mt61220111:24000
Tongue River-Hooligan-Leavitt complex, 8 to 45 percent slopes821F105324851792pf12mt61220111:24000
Stemple, very stony-Tongue River complex, 4 to 15 percent slopes, landslides820D24924864342pgbkmt61220111:24000
Tongue River-Hooligan-Leavitt complex, 8 to 45 percent slopes821F136524929502pf12mt61420121:24000
Leavitt-Tongue River-Knep complex, 4 to 35 percent slopes, landslides819E65124929492pdy5mt61420121:24000
Tongue River-Yellowmule-Helmville complex, 15 to 50 percent slopes, landslides728F61825416482ppjdmt61420121:24000
Tongue River-Inabnit, very stony-Doolittle complex, 25 to 60 percent slopes822F8425207502pgc3mt61420121:24000
Stemple, stony-Tongue River-Yellowmule complex, 8 to 45 percent slopes, landslides816F3225207482pf53mt61420121:24000
Tongue River-Arrowpeak, moist complex, 15 to 60 percent slopes379F1378149942510vmt63920001:24000
Tongue River-Cabba, moist-Adel loams, 15 to 60 percent slopes377F1330149940510smt63920001:24000
Tongue River-Timberlin complex, 35 to 60 percent slopes391F6371499515114mt63920001:24000
Tongue River-Danaher loams, 15 to 35 percent slopes358E5481499165100mt63920001:24000
Tongue River-Doby-Rock outcrop complex, 15 to 60 percent slopes405F202149966511mmt63920001:24000
Tongue River-Novary-Cowood complex, 4 to 45 percent slopes387E1281499495112mt63920001:24000
Jaegie-Gilispie-Tongue River loams, 20 to 70 percent slopes5656F2189741516swlwmt6691:24000
Yellowmule-Timberlin-Tongue River complex, 25 to 60 percent slopes5611F71115647657tmmt6691:24000
Tongue River-Arrowpeak, moist complex, 15 to 60 percent slopes379F370620226ntd9mt6691:24000
Tongue River-Cabba, moist-Adel loams, 15 to 60 percent slopes377F166620225ntd8mt6691:24000
Tongue River-Timberlin complex, 35 to 60 percent slopes391F3524813622p91ymt6691:24000
Tongue River-Gateway association, 2 to 35 percent slopes9053152139539qwy04319761:24000
Tongue River-Inchau complex, 10 to 30 percent slopes1681662733697smgnwy6471:24000
Tongue River-Gateway association, 2 to 35 percent slopes434022815805459gjwy65019821:24000
Tongue River-Inchau-Teton family, complex, 10 to 30 percent slopes215D245715793659bqwy65620081:24000
Roxal-Tongue River complex, 10 to 40 percent slopes201D2715793359bmwy65620081:24000
Buckskin-Tongue River-Helmville families, association, 0 to 60 percent slopes2643680151980534lwy66320121:24000
Buffork-Tongue River association *5219215330054j5wy66619781:24000
Buffork-Tongue River-Clayburn association *690015331154jjwy66619781:24000
Tongue River-Inchau-Farlow variant complex, 10 to 30 percent slopes2156906503092jwhswy71319861:24000
Roxal-Tongue River complex, hilly2012183503068jwh0wy71319861:24000

Map of Series Extent

Approximate geographic distribution of the TONGUE RIVER 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 .