Official Series Description


Lab Data Summary

Aggregate lab data for the ELKCREEK soil series. This aggregation is based on all pedons with a current taxon name of ELKCREEK, 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 ELKCREEK 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
1092P013991ID047010ELKCREEK5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.1916656,-114.0986099

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELKCREEK 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 ELKCREEK 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 ELKCREEK 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 ELKCREEK 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 hills figure.

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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.

Competing Series

Soil series competing with ELKCREEK 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 ELKCREEK 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 ELKCREEK 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 hills figure.

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

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 ELKCREEK, 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-2010-08-31-17 | 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 17 (Soil Survey of Wood River Area, Idaho; 2005).

Map Units

Map units containing ELKCREEK 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
Elkcreek-Rock outcrop complex, 0 to 30 percent slopes1714150817692r2qid67319771:24000
Elkcreek-Gaib complex, 0 to 30 percent slopes145301817662r2mid67319771:24000
Elkcreek-Rock outcrop complex, 30 to 60 percent slopes184201817702r2rid67319771:24000
Gaib-Elkcreek complex, 0 to 30 percent slopes193047817712r2sid67319771:24000
Gaib-Elkcreek complex, 30 to 60 percent slopes202771817732r2vid67319771:24000
Elkcreek-Polecreek complex, 0 to 30 percent slopes161963817682r2pid67319771:24000
Elkcreek loam, 0 to 30 percent slopes131170817652r2lid67319771:24000
Elkcreek-Manard complex, 0 to 30 percent slopes15834817672r2nid67319771:24000
Elkcreek-Gaib complex, 30 to 60 percent slopes353151793202njqid68019851:24000
Elkcreek-Polecreek complex, 4 to 30 percent slopes362362793212njrid68019851:24000
Mulshoe-Rock outcrop-Elkcreek complex, 12 to 35 percent slopes1335800818632r5rid68119931:24000
Elkcreek-Mulshoe-Simonton complex, 1 to 12 percent slopes512895820452rcmid68119931:24000
Elkcreek-Mulshoe complex, 1 to 8 percent slopes501315820352rc9id68119931:24000
Elkcreek-Mulshoe-Simonton complex, 12 to 35 percent slopes521240820562rczid68119931:24000
Elkcreek-Demast complex, 10 to 50 percent slopes572279025195812r0yid68520121:24000
Gaib-Elkcreek-Simonton association, 20 to 60 percent slopes632050425195882r15id68520121:24000
Gaib-Elkcreek-Rock outcrop association, 2 to 20 percent slopes621917925195872r14id68520121:24000
Simonton-Elkcreek complex, 10 to 50 percent slopes1511273425195112qypid68520121:24000
Elkcreek-Gaib-Simonton complex, 12 to 30 percent slopes581089325195822r0zid68520121:24000

Map of Series Extent

Approximate geographic distribution of the ELKCREEK 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 .