Official Series Description


Lab Data Summary

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the SNOWMORE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the SNOWMORE series and siblings. 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 SNOWMORE 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Competing Series

Soil series competing with SNOWMORE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the SNOWMORE 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 SNOWMORE 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.

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

Soil series sharing subgroup-level classification with SNOWMORE, 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. ID-2010-08-31-13 | Wood River Area, Gooding County and Parts of Blaine, Lincoln, and Minidoka Counties - 2005

    Typical pattern of soils and underlying material in general soil map unit 10 (Soil Survey of Wood River Area, Idaho; 2005).

Map Units

Map units containing SNOWMORE 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
Snowmore-Willhill association, 2 to 25 percent slopes16039375486019j9r1id67519921:24000
Hardtrigger-Snowmore-Vickery complex, 1 to 5 percent slopes7538109486262j9zwid67519921:24000
Bruncan-Snowmore silt loams, 1 to 8 percent slopes3129323486170j9wxid67519921:24000
Snowmore-Troughs complex, 1 to 10 percent slopes15926846486013j9qvid67519921:24000
Snowmore-Igert-Bruncan complex, 1 to 12 percent slopes15822317486011j9qsid67519921:24000
Snowmore ashy silt loam, 2 to 15 percent slopes1826882486066260nbid67519921:24000
Vickery-Snowmore complex, 1 to 5 percent slopes1884445486078j9syid67519921:24000
Snowmore gravelly ashy fine sandy loam, 2 to 15 percent slopes367169532709452qy3tid67519921:24000
Snowmore-Minveno-Hoosegow complex, 2 to 10 percent slopes17418055819082r76id68119931:24000
Snowmore-Idow-Bruncan complex, 2 to 8 percent slopes1725745819062r74id68119931:24000
Snowmore-Wako-Harsan complex, 1 to 4 percent slopes1775740819112r79id68119931:24000
Snowmore-Besslen-Hoosegow complex, 1 to 4 percent slopes1714070819052r73id68119931:24000
Snowmore-Purdam-Power complex, 1 to 4 percent slopes1753025819092r77id68119931:24000
Snowmore-Idow-Harsan complex, 0 to 4 percent slopes1732990819072r75id68119931:24000
Harsan-Snowmore-Idow complex, 1 to 4 percent slopes772645821302rgcid68119931:24000
Kecko-Snowmore complex, 2 to 20 percent slopes1001520818262r4kid68119931:24000
Snowmore-Purdam-Power complex, 4 to 12 percent slopes176790819102r78id68119931:24000
Coltroop-Snowmore association22056555477171j0jmnv76319861:24000
Linkup-Snowmore-Ratsow association16755120477097j0g7nv76319861:24000
Snowmore, cobbly-Snowmore, very cobbly-Snowmore association27814040477223j0l9nv76319861:24000
Olac-Snowmore association26413925477202j0kmnv76319861:24000
Snowmore association980255725199822qjpqnv76319861:24000
Snowmore, cobbly-Snowmore association27802500477222j0l8nv76319861:24000
Snowmore-Zevadez association981243325199792qjpmnv76319861:24000
Snowmore-Willhill association27832190477225j0lcnv76319861:24000
Snowmore-Zevadez-Snowmore, cobbly association27821447477224j0lbnv76319861:24000
Alley-Snowmore-Rock outcrop association14507058475218hyhmnv76919861:24000
Snowmore-Devada association98327382476008hzb3nv77719931:24000
Devada-Snowmore-Midraw association6768237475878hz5xnv77719931:24000
Burrita-Snowmore-Rock outcrop association6577997475863hz5fnv77719931:24000
Snowmore-Vanwyper-Devada association9844069476009hzb4nv77719931:24000
Dacker-Devada-Snowmore association7822146475925hz7fnv77719931:24000
Snowmore gravelly ashy fine sandy loam, 2 to 15 percent slopes36779332708622qy3tnv77719931:24000
Snowmore association980652476006hzb1nv77719931:24000
Snowmore-Zevadez association981392476007hzb2nv77719931:24000
Snowmore ashy silt loam, 2 to 15 percent slopes1821653682026418260nbor64420211:24000
Snowmore gravelly ashy fine sandy loam, 2 to 15 percent slopes36714782825652312qy3tor64420211:24000
Snowmore-Bogusrim-Muni complex, 2 to 15 percent slopes50353930729868732wbl0or64420211:24000
Snowmore-Bogusrim, very stony surface-Muni complex, 2 to 15 percent slopes50353177029468352wmbkor6451:24000

Map of Series Extent

Approximate geographic distribution of the SNOWMORE 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 .