Official Series Description


Lab Data Summary

Aggregate lab data for the TETON soil series. This aggregation is based on all pedons with a current taxon name of TETON, 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 TETON 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
4640A0213S1958MT045001Teton5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.158802,-110.5830612

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TETON 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 TETON 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 TETON 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 TETON 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 flats position figure.

Competing Series

Soil series competing with TETON 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 TETON 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 TETON 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 TETON, 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 TETON 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
Adel-Teton family association, 25 to 50 percent slopes83755509401k329co6471:24000
Teton loam, 2 to 8 percent slopes2284767342466chc9mt02719791:24000
Teton-Cheadle loams, 8 to 15 percent slopes2313180342470chcfmt02719791:24000
Teton-Adel loams, 8 to 15 percent slopes2292747342467chcbmt02719791:24000
Teton-Cheadle loams, 2 to 8 percent slopes2302120342469chcdmt02719791:24000
Teton-Cheadle channery loams, 2 to 8 percent slopes2321183342471chcgmt02719791:24000
Teton-Adel stony loamsTh147871474414yf5mt60219631:20000
Teton-Cheadle stony loams, 4 to 15 percent slopesTm63451474434yf7mt60219631:20000
Teton-Cheadle stony loams, 15 to 35 percent slopesTn46381474444yf8mt60219631:20000
Teton loam, 2 to 8 percent slopesTd32941474394yf3mt60219631:20000
Teton loam, 8 to 15 percent slopesTf10771474404yf4mt60219631:20000
Woodhurst-Teton-Cheadle soilsWt10571474684yg1mt60219631:20000
Teton-Cheadle channery loams, 4 to 15 percent slopesTk5161474424yf6mt60219631:20000
Splitro-Sawcreek sandy loams, hillySVb5496346148cm62mt60719701:24000
Teton complex, 25 to 45 percent slopesTFb4378346172cm6vmt60719701:24000
Teton loam, 8 to 25 percent slopesTFa2533346171cm6tmt60719701:24000
Teton stony loam, moderately steepTD4438347156cn7lmt61119711:24000
Whitore-Teton-Tibson complex, 8 to 35 percent slopes696E7192348780cpxzmt65719901:24000
Teton-Tibson-Cheadle complex, 4 to 35 percent slopes196E2905348426cpkkmt65719901:24000
Teton-Cheadle loams, 8 to 15 percent slopes431D26315316701ndtqmt66620081:24000
Tongue River-Inchau-Teton family, complex, 10 to 30 percent slopes215D245715793659bqwy65620081:24000
Shurtleff-Arbucap-Teton complex, 2 to 15 percent slopes71371971624860512pfy6wy7231:24000

Map of Series Extent

Approximate geographic distribution of the TETON 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 .