Official Series Description


Lab Data Summary

Aggregate lab data for the CROOKED CREEK soil series. This aggregation is based on all pedons with a current taxon name of CROOKED CREEK, 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 CROOKED CREEK 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
4708N0281S07WY041008Crooked Creek7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0734711,-110.9619446

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CROOKED CREEK 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 CROOKED CREEK 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 CROOKED CREEK 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 CROOKED CREEK 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 CROOKED CREEK 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 CROOKED CREEK series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the CROOKED CREEK 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 .

There are insufficient data to create the 2D hillslope position figure.

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 CROOKED CREEK, 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-2011-06-01-10 | Duck Valley Indian Reservation - 1986

    Typical landscape and underlying material in an area of general soil map unit 2 (Soil Survey of Duck Valley Indian Reservation, Idaho; 1986).

Map Units

Map units containing CROOKED CREEK 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
Crooked Creek silty clay loam131212496447jnlfco62719801:24000
Welch-Crooked Creek complex, 0 to 2 percent slopes695273270920hxw9id67519921:24000
Crooked Creek-Bear Lake complex, 0 to 2 percent slopes105137484826j8hkid67719841:24000
Crooked Creek silt loam, 0 to 2 percent slopes181536789822n5tid76319981:24000
Crooked Creek silt loamCx1094476071hzd4nv61219681:24000
Crooked Creek clay loam, drainedCY402476072hzd5nv61219681:24000
Marsh-Crooked Creek complexMc230476111hzffnv61219681:24000
Crooked Creek, moderately wet-Crooked Creek association18513595477131j0hbnv76319861:24000
Crooked Creek-Welch-Crooked Creek, drained association1884700477144j0hrnv76319861:24000
Cotant-Chen-Crooked Creek association1293930477057j0dynv76319861:24000
Lynnbow-Lerrow-Crooked Creek association2013211477166j0jgnv76319861:24000
Crooked Creek silty clay loam, frequently flooded, 0 to 2 percent slopes1843165477130j0h9nv76319861:24000
Crooked Creek-Crooked Creek, occasionally flooded-Crooked Creek, drained association1862195477136j0hhnv76319861:24000
Welch-Crooked Creek complex, 0 to 2 percent slopes6952846474619hxw9nv76420211:24000
Welch-Crooked Creek association, dry0345525474849hy3qnv76519861:24000
Welch-Crooked Creek association, wet0314900474847hy3nnv76519861:24000
Crooked Creek, drained-Crooked Creek-Welch association2112215474945hy6tnv76519861:24000
Geysen-Crooked Creek-Batan association7311215475099hycsnv76519861:24000
Welch-Crooked Creek complex, 0 to 2 percent slopes695113270893hxw9nv76519861:24000
Crooked Creek, gravelly substratum-Crooked Creek association1898979478809j27gnv76719861:24000
Welch-Crooked Creek-Welch, occasioanlly flooded association6955258478981j2f0nv76719861:24000
Crooked Creek-Hussa-Alburz association1824453478781j26knv76719861:24000
Devilsgait-Crooked Creek association4423785478910j2bqnv76719861:24000
Crooked Creek silty clay loam, frequently flooded, 0 to 2 percent slopes1843650478793j26ynv76719861:24000
Crooked Creek-Welsum association1833301478790j26vnv76719861:24000
Crooked Creek-Devilsgait-Ocala association1872976478794j26znv76719861:24000
Crooked Creek-Crooked Creek, gravelly substratum-Ocala association1812764478780j26jnv76719861:24000
Halleck, occasionally flooded-Halleck-Crooked Creek association6981979478982j2f1nv76719861:24000
Welch-Crooked Creek association, dry034138126338582rgn0nv76719861:24000
Crooked Creek silty clay loam, 0 to 2 percent slopes213178481228j4rhut60119851:24000
Crooked Creek-Hupp complex, 1 to 6 percent slopes22891481229j4rjut60119851:24000
Crooked Creek silty clay loamCt1395506527k02lut60919741:24000
Crooked Creek clay loam, 1 to 3 percent slopesCrA1275504223jxp8ut62219671:24000
Crooked Creek clay loam, 3 to 10 percent slopesCrC189504224jxp9ut62219671:24000

Map of Series Extent

Approximate geographic distribution of the CROOKED CREEK 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 .